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Nuclear and Particle Physics
Nuclear and Particle Physics B. R. Martin
# 2006 John Wiley & Sons, Ltd. ISBN: 0-470-01999-9
Nuclear and Particle Physics
B. R. Martin
Department of Physics and Astronomy, University College London
Copyright # 2006 John Wiley & Sons Ltd, The Atrium, Southern Gate, Chichester,
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Library of Congress Cataloging-in-Publication Data
Martin, B. R. (Brian Robert)
Nuclear and particle physics/B. R. Martin.
p. cm.
ISBN-13: 978-0-470-01999-3 (HB)
ISBN-10: 0-470-01999-9 (HB)
ISBN-13: 978-0-470-02532-1 (pbk.)
ISBN-10: 0-470-02532-8 (pbk.)
1. Nuclear physics–Textbooks. 2. Particle physics–Textbooks. I. Title.
QC776.M34 2006
539.70
2–dc22
2005036437
British Library Cataloguing in Publication Data
A catalogue record for this book is available from the British Library
ISBN-13 978-0 470 01999 9 (HB) ISBN-10 0 470 01999 9 (HB)
978-0 470 02532 8 (PB) 0 470 02532 8 (PB)
Typeset in 10.5/12.5pt Times by Thomson Press (India) Limited, New Delhi
Printed and bound in Great Britain by Antony Rowe Ltd., Chippenham, Wiltshire
This book is printed on acid-free paper responsibly manufactured from sustainable forestry
in which at least two trees are planted for each one used for paper production.
To Claire
Contents
Preface xi
Notes xiii
Physical Constants and Conversion Factors xv
1 Basic Concepts 1
1.1 History 1
1.1.1 The origins of nuclear physics 1
1.1.2 The emergence of particle physics: the standard model and hadrons 4
1.2 Relativity and antiparticles 7
1.3 Symmetries and conservation laws 9
1.3.1 Parity 10
1.3.2 Charge conjugation 12
1.4 Interactions and Feynman diagrams 13
1.4.1 Interactions 13
1.4.2 Feynman diagrams 15
1.5 Particle exchange: forces and potentials 17
1.5.1 Range of forces 17
1.5.2 The Yukawa potential 19
1.6 Observable quantities: cross sections and decay rates 20
1.6.1 Amplitudes 21
1.6.2 Cross-sections 23
1.6.3 Unstable states 27
1.7 Units: length, mass and energy 29
Problems 30
2 Nuclear Phenomenology 33
2.1 Mass spectroscopy and binding energies 33
2.2 Nuclear shapes and sizes 37
2.2.1 Charge distribution 37
2.2.2 Matter distribution 42
2.3 Nuclear instability 45
2.4 Radioactive decay 47
2.5 Semi-empirical mass formula: the liquid drop model 50
2.6 -decay phenomenology 55
2.6.1 Odd-mass nuclei 55
2.6.2 Even-mass nuclei 58
2.7 Fission 59
2.8 -decays 62
2.9 Nuclear reactions 62
Problems 67
3 Particle Phenomenology 71
3.1 Leptons 71
3.1.1 Lepton multiplets and lepton numbers 71
3.1.2 Neutrinos 74
3.1.3 Neutrino mixing and oscillations 76
3.1.4 Neutrino masses 79
3.1.5 Universal lepton interactions – the number of neutrinos 84
3.2 Quarks 86
3.2.1 Evidence for quarks 86
3.2.2 Quark generations and quark numbers 89
3.3 Hadrons 92
3.3.1 Flavour independence and charge multiplets 92
3.3.2 Quark model spectroscopy 96
3.3.3 Hadron masses and magnetic moments 102
Problems 108
4 Experimental Methods 111
4.1 Overview 111
4.2 Accelerators and beams 113
4.2.1 DC accelerators 113
4.2.2 AC accelerators 115
4.2.3 Neutral and unstable particle beams 122
4.3 Particle interactions with matter 123
4.3.1 Short-range interactions with nuclei 123
4.3.2 Ionization energy losses 125
4.3.3 Radiation energy losses 128
4.3.4 Interactions of photons in matter 129
4.4 Particle detectors 131
4.4.1 Gas detectors 131
4.4.2 Scintillation counters 137
4.4.3 Semiconductor detectors 138
4.4.4 Particle identification 139
4.4.5 Calorimeters 142
4.5 Layered detectors 145
Problems 148
5 Quark Dynamics: the Strong Interaction 151
5.1 Colour 151
5.2 Quantum chromodynamics (QCD) 153
5.3 Heavy quark bound states 156
5.4 The strong coupling constant and asymptotic freedom 160
5.5 Jets and gluons 164
5.6 Colour counting 166
viii CONTENTS
5.7 Deep inelastic scattering and nucleon structure 168
Problems 177
6 Electroweak Interactions 181
6.1 Charged and neutral currents 181
6.2 Symmetries of the weak interaction 182
6.3 Spin structure of the weak interactions 186
6.3.1 Neutrinos 187
6.3.2 Particles with mass: chirality 189
6.4 W
and Z0
bosons 192
6.5 Weak interactions of hadrons 194
6.5.1 Semileptonic decays 194
6.5.2 Neutrino scattering 198
6.6 Neutral meson decays 201
6.6.1 CP violation 202
6.6.2 Flavour oscillations 206
6.7 Neutral currents and the unified theory 208
Problems 213
7 Models and Theories of Nuclear Physics 217
7.1 The nucleon – nucleon potential 217
7.2 Fermi gas model 220
7.3 Shell model 223
7.3.1 Shell structure of atoms 223
7.3.2 Nuclear magic numbers 225
7.3.3 Spins, parities and magnetic dipole moments 228
7.3.4 Excited states 230
7.4 Non-spherical nuclei 232
7.4.1 Electric quadrupole moments 232
7.4.2 Collective model 236
7.5 Summary of nuclear structure models 236
7.6 -decay 238
7.7 -decay 242
7.7.1 Fermi theory 242
7.7.2 Electron momentum distribution 244
7.7.3 Kurie plots and the neutrino mass 246
7.8 -emission and internal conversion 248
7.8.1 Selection rules 248
7.8.2 Transition rates 250
Problems 252
8 Applications of Nuclear Physics 255
8.1 Fission 255
8.1.1 Induced fission – fissile materials 255
8.1.2 Fission chain reactions 258
8.1.3 Nuclear power reactors 260
8.2 Fusion 266
8.2.1 Coulomb barrier 266
CONTENTS ix
8.2.2 Stellar fusion 267
8.2.3 Fusion reaction rates 270
8.2.4 Fusion reactors 273
8.3 Biomedical applications 278
8.3.1 Biological effects of radiation: radiation therapy 278
8.3.2 Medical imaging using radiation 282
8.3.3 Magnetic resonance imaging 290
Problems 294
9 Outstanding Questions and Future Prospects 297
9.1 Particle physics 297
9.1.1 The Higgs boson 297
9.1.2 Grand unification 300
9.1.3 Supersymmetry 304
9.1.4 Particle astrophysics 307
9.2 Nuclear physics 315
9.2.1 The structure of hadrons and nuclei 316
9.2.2 Quark–gluon plasma, astrophysics and cosmology 320
9.2.3 Symmetries and the standard model 323
9.2.4 Nuclear medicine 324
9.2.5 Power production and nuclear waste 326
Appendix A: Some Results in Quantum Mechanics 331
A.1 Barrier penetration 331
A.2 Density of states 333
A.3 Perturbation theory and the Second Golden Rule 335
Appendix B: Relativistic Kinematics 339
B.1 Lorentz transformations and four-vectors 339
B.2 Frames of reference 341
B.3 Invariants 344
Problems 345
Appendix C: Rutherford Scattering 349
C.1 Classical physics 349
C.2 Quantum mechanics 352
Problems 354
Appendix D: Solutions to Problems 355
References 393
Bibliography 397
Index 401
x CONTENTS
Preface
It is common practice to teach nuclear physics and particle physics together in an
introductory course and it is for such a course that this book has been written. The
material is presented so that different selections can be made for a short course of
about 25–30 lectures depending on the lecturer’s preferences and the students’
backgrounds. On the latter, students should have taken a first course in quantum
physics, covering the traditional topics in non-relativistic quantum mechanics and
atomic physics. A few lectures on relativistic kinematics would also be useful, but
this is not essential as the necessary background is given in appendix B and is only
used in a few places in the book. I have not tried to be rigorous, or present proofs
of all the statements in the text. Rather, I have taken the view that it is more
important that students see an overview of the subject which for many – possibly
the majority – will be the only time they study nuclear and particle physics. For
future specialists, the details will form part of more advanced courses. Never-
theless, space restrictions have still meant that it has been necessary to make a
choice of topics covered and doubtless other, equally valid, choices could have
been made. This is particularly true in Chapter 8, which deals with applications of
nuclear physics, where I have chosen just three major areas to discuss. Nuclear and
particle physics have been, and still are, very important parts of the entire subject
of physics and its practitioners have won an impressive number of Nobel Prizes.
For historical interest, I have noted in the footnotes many of the awards for work
related to the field.
Some parts of the book dealing with particle physics owe much to a previous book,
Particle Physics, written with Graham Shaw of Manchester University, and I am
grateful to him and the publisher, John Wiley and Sons, for permission to adapt some
ofthatmaterialforusehere.IalsothankColinWilkinforcommentsonallthechapters
of the book, David Miller and Peter Hobson for comments on Chapter 4 and Bob
Speller for comments on the medical physics section of Chapter 8. If errors or
misunderstandingsstillremain(andanysuchareofcourseduetomealone)Iwouldbe
grateful to hear about them. I have set up a website (www.hep.ucl.ac.uk/brm/
npbook.html) where I will post any corrections and comments.
Brian R. Martin
January 2006
Notes
References
References are referred to in the text in the form Ab95, where Ab is the start of the
first author’s surname and 1995 is the year of publication. A list of references with
full publication details is given at the end of the book.
Data
Data for particle physics may be obtained from the biannual publications of the
Particle Data Group (PDG) and the 2004 edition of the PDG definitive Review
of Particle Properties is given in Ei04. The PDG Review is also available at
http://pdg.lbl.gov and this site contains links to other sites where compilations of
particle data may be found. Nuclear physics data are available from a number of
sources. Examples are: the combined Isotopes Project of the Lawrence Berkeley
Laboratory, USA, and the Lund University Nuclear Data WWW Service, Sweden
(http://ie.lbl.gov/toi.html), the National Nuclear Data Center (NNDC) based
at Brookhaven National Laboratory, USA (http://www.nndc.bnl.gov), and
the Nuclear Data Centre of the Japan Atomic Energy Research Institute
(http://www.nndc.tokai.jaeri.go.jp). All three sites have extensive links to other
data compilations. It is important that students have some familiarity with these
data compilations.
Problems
Problems are provided for all chapters and appendices except Chapter 9 and
Appendices A and D. They are an integral part of the text. The problems are
mainly numerical and require values of physical constants that are given in a table
following these notes. A few also require input data that may be found in the
references given above. Solutions to all the problems are given in Appendix D.
Illustrations
Some illustrations in the text have been adapted from, or are loosely based on,
diagrams that have been published elsewhere. In a few cases they have been
reproduced exactly as previously published. In all cases this is stated in the
captions. I acknowledge, with thanks, permission to use such illustrations from the
relevant copyright holders.
xiv NOTES
Physical Constants
and Conversion Factors
Quantity Symbol Value
Speed of light in vacuum c 2:998  108
ms1
Planck’s constant h 4:136  1024
GeV s

h  h=2 6:582  1025
GeV s

hc 1:973  1016
GeV m
ð
hcÞ2
3:894  1031
GeV2
m2
electron charge (magnitude) e 1:602  1019
C
Avogadro’s number NA 6:022  1026
kg-mole1
Boltzmann’s constant kB 8:617  1011
MeV K1
electron mass me 0:511 MeV=c2
proton mass mp 0:9383 GeV=c2
neutron mass mn 0:9396 GeV=c2
W boson mass MW 80:43 GeV=c2
Z boson mass MZ 91:19 GeV=c2
atomic mass unit u  ð 1
12 mass12
C atomÞ 931:494 MeV=c2
Bohr magneton B  e
h=2me 5:788  1011
MeV T1
Nuclear magneton N  e
h=2mp 3:152  1014
MeV T1
gravitational constant GN 6:709  1039

hcðGeV=c2
Þ2
fine structure constant   e2
=40
hc 7:297  103
¼ 1=137:04
Fermi coupling constant GF=ð
hcÞ3
1:166  105
GeV2
strong coupling constant sðMZc2
Þ 0.119
1 eV ¼ 1:602  1019
J 1 eV=c2
¼ 1:783  1036
kg
1 fermi ¼ 1 fm  1015
m 1 barn ¼ 1 b  1028
m2
1 Tesla ¼ 1T ¼ 0:561  1030
MeV=c2
C1
s1
1 year ¼ 3:1536  107
s
1
Basic Concepts
1.1 History
Although this book will not follow a strictly historical development, to ‘set the
scene’ this first chapter will start with a brief review of the most important
discoveries that led to the separation of nuclear physics from atomic physics as a
subject in its own right and later work that in its turn led to the emergence of
particle physics from nuclear physics.1
1.1.1 The origins of nuclear physics
Nuclear physics as a subject distinct from atomic physics could be said to date
from 1896, the year that Henri Becquerel observed that photographic plates were
being fogged by an unknown radiation emanating from uranium ores. He had
accidentally discovered radioactivity: the fact that some nuclei are unstable and
spontaneously decay. In the years that followed, the phenomenon was extensively
investigated, notably by the husband and wife team of Pierre and Marie Curie and
by Ernest Rutherford and his collaborators,2
and it was established that there were
three distinct types of radiation involved: these were named (by Rutherford) -, -
and -rays. We know now that -rays are bound states of two protons and two
neutrons (we will see later that they are the nuclei of helium atoms), -rays are
electrons and -rays are photons, the quanta of electromagnetic radiation, but the
historical names are still commonly used.
1
An interesting account of the early period, with descriptions of the personalities involved, is given in Se80.
An overview of the later period is given in Chapter 1 of Gr87.
2
The 1903 Nobel Prize in Physics was awarded jointly to Becquerel for his discovery and to Pierre and Marie
Curie for their subsequent research into radioactivity. Rutherford had to wait until 1908, when he was
awarded the Nobel Prize in Chemistry for his ‘investigations into the disintegration of the elements and the
chemistry of radioactive substances’.
Nuclear and Particle Physics B. R. Martin
# 2006 John Wiley  Sons, Ltd. ISBN: 0-470-01999-9
At about the same time as Becquerel’s discovery, J. J. Thomson was extending
the work of Perrin and others on the radiation that had been observed to occur
when an electric field was established between electrodes in an evacuated glass
tube, and in 1897 he was the first to definitively establish the nature of these
‘cathode rays’. We now know the emanation consists of free electrons, (the name
‘electron’ had been coined in 1894 by Stoney) denoted e
(the superscript denotes
the electric charge) and Thomson measured their mass and charge.3
The view of the
atom at that time was that it consisted of two components, with positive and negative
electric charges, the latter now being the electrons. Thomson suggested a model
where the electrons were embedded and free to move in a region of positive charge
filling the entire volume of the atom – the so-called ‘plum pudding model’.
This model could account for the stability of atoms, but could not account for
the discrete wavelengths observed in the spectra of light emitted from excited
atoms. Neither could it explain the results of a classic series of experiments
performed in 1911 at the suggestion of Rutherford by his collaborators, Geiger and
Marsden. These consisted of scattering -particles by very thin gold foils. In the
Thomson model, most of the -particles would pass through the foil, with only a
few suffering deflections through small angles. Rutherford suggested they should
look for large-angle scattering and to their surprise they found that some particles
were indeed scattered through very large angles, even greater than 90
. Rutherford
showed that this behaviour was not due to multiple small-angle deflections, but
could only be the result of the -particles encountering a very small positively
charged central nucleus. (The reason for these two different behaviours is
discussed in Appendix C.)
To explain the results of these experiments Rutherford formulated a ‘planetary’
model, where the atom was likened to a planetary system, with the electrons (the
‘planets’) occupying discrete orbits about a central positively charged nucleus (the
‘Sun’). Because photons of a definite energy would be emitted when electrons
moved from one orbit to another, this model could explain the discrete nature of
the observed electromagnetic spectra when excited atoms decayed. In the simplest
case of hydrogen, the nucleus is a single proton (p) with electric charge þe, where e
is the magnitude of the charge on the electron4
, orbited by a single electron.
Heavier atoms were considered to have nuclei consisting of several protons. This
view persisted for a long time and was supported by the fact that the masses of
many naturally occurring elements are integer multiples of a unit that is about
1 per cent smaller than the mass of the hydrogen atom. Examples are carbon and
nitrogen, with masses of 12.0 and 14.0 in these units. However, it could not explain
why not all atoms obeyed this rule. For example, chlorine has a mass of 35.5 in these
3
J. J. Thomson received the 1906 Nobel Prize in Physics for his discovery. A year earlier, Philipp von Lenard
had received the Physics Prize for his work on cathode rays.
4
Why the charge on the proton should have exactly the same magnitude as that on the electron is a very long-
standing puzzle, the solution to which is suggested by some as yet unproven, but widely believed, theories of
particle physics that will be discussed briefly in Chapter 9.
2 CH1 BASIC CONCEPTS
units. At about the same time, the concept of isotopism (a name coined by Soddy)
was conceived. Isotopes are atoms whose nuclei have different masses, but the same
charge. Naturally occurring elements were postulated to consist of a mixture of
different isotopes, giving rise to the observed masses.5
The explanation of isotopes had to wait 20 years until a classic discovery by
Chadwick in 1932. His work followed earlier experiments by Irène Curie (the
daughter of Pierre and Marie Curie) and her husband Frédéric Joliot.6
They had
observed that neutral radiation was emitted when -particles bombarded beryllium
and later work had studied the energy of protons emitted when paraffin was
exposed to this neutral radiation. Chadwick refined and extended these experi-
ments and demonstrated that they implied the existence of an electrically neutral
particle of approximately the same mass as the proton. He had discovered the
neutron (n) and in so doing had produced almost the final ingredient for under-
standing nuclei.7
There remained the problem of reconciling the planetary model with the
observation of stable atoms. In classical physics, the electrons in the planetary
model would be constantly accelerating and would therefore lose energy by
radiation, leading to the collapse of the atom. This problem was solved by Bohr
in 1913. He applied the newly emerging quantum theory and the result was the
now well-known Bohr model of the atom. Refined modern versions of this model,
including relativistic effects described by the Dirac equation (the relativistic
analogue of the Schrödinger equation that applies to electrons), are capable of
explaining the phenomena of atomic physics. Later workers, including Heisenberg,
another of the founders of quantum theory,8
applied quantum mechanics to the
nucleus, now viewed as a collection of neutrons and protons, collectively called
nucleons. In this case, however, the force binding the nucleus is not the
electromagnetic force that holds electrons in their orbits, but is a short-range9
force whose magnitude is independent of the type of nucleon, proton or neutron
(i.e. charge-independent). This binding interaction is called the strong nuclear
force.
These ideas still form the essential framework of our understanding of the
nucleus today, where nuclei are bound states of nucleons held together by a strong
charge-independent short-range force. Nevertheless, there is still no single theory
that is capable of explaining all the data of nuclear physics and we shall see that
different models are used to interpret different classes of phenomena.
5
Frederick Soddy was awarded the 1921 Nobel Prize in Chemistry for his work on isotopes.
6
Irène Curie and Frédéric Joliot received the 1935 Nobel Prize in Chemistry for ‘synthesizing new
radioactive elements’.
7
James Chadwick received the 1935 Nobel Prize in Physics for his discovery of the neutron.
8
Werner Heisenberg received the 1932 Nobel Prize in Physics for his contributions to the creation of
quantum mechanics and the idea of isospin symmetry, which we will discuss in Chapter 3.
9
The concept of range will be discussed in more detail in Section 1.5.1, but for the present it may be taken as
the effective distance beyond which the force is insignificant.
HISTORY 3
1.1.2 The emergence of particle physics: the standard model
and hadrons
By the early 1930s, the 19th century view of atoms as indivisible elementary
particles had been replaced and a larger group of physically smaller entities now
enjoyed this status: electrons, protons and neutrons. To these we must add two
electrically neutral particles: the photon () and the neutrino (). The photon was
postulated by Planck in 1900 to explain black-body radiation, where the classical
description of electromagnetic radiation led to results incompatible with experi-
ments.10
The neutrino was postulated by Fermi in 1930 to explain the apparent
non-conservation of energy observed in the decay products of some unstable nuclei
where -rays are emitted, the so-called -decays. Prior to Fermi’s suggestion,
-decay had been viewed as a parent nucleus decaying to a daughter nucleus and
an electron. As this would be a two-body decay, it would imply that the electron
would have a unique momentum, whereas experiments showed that the electron
actually had a momentum spectrum. Fermi’s hypothesis of a third particle (the
neutrino) in the final state solved this problem, as well as a problem with angular
momentum conservation, which was apparently also violated if the decay was two-
body. The -decay data implied that the neutrino mass was very small and was
compatible with the neutrino being massless.11
It took more than 25 years before
Fermi’s hypothesis was confirmed by Reines and Cowan in a classic experiment in
1956 that detected free neutrinos from -decay.12
The 1950s also saw technological developments that enabled high-energy
beams of particles to be produced in laboratories. As a consequence, a wide
range of controlled scattering experiments could be performed and the greater
use of computers meant that sophisticated analysis techniques could be devel-
oped to handle the huge quantities of data that were being produced. By the
1960s this had resulted in the discovery of a very large number of unstable
particles with very short lifetimes and there was an urgent need for a theory that
could make sense of all these states. This emerged in the mid 1960s in the form
of the so-called quark model, first suggested by Murray Gell-Mann and
independently and simultaneously by George Zweig, who postulated that the
new particles were bound states of three families of more fundamental physical
particles.
10
X-rays had already been observed by Röntgen in 1895 (for which he received the first Nobel Prize in
Physics in 1901) and -rays were seen by Villard in 1900, but it was Planck who first made the startling
suggestion that electromagnetic energy was quantized. For this he was awarded the 1918 Nobel Prize in
Physics. Many years later, he said that his hypothesis was an ‘act of desperation’ as he had exhausted all
other possibilities.
11
However, in Section 3.1.4 we will discuss recent evidence that neutrinos have very small, but non-zero,
masses.
12
A description of this experiment is given in Chapter 12 of Tr75. Frederick Reines shared the 1995 Nobel
Prize in Physics for his work in neutrino physics and particularly for the detection of the electron neutrino.
4 CH1 BASIC CONCEPTS
Gell-Mann called these quarks (q).13
Because no free quarks were detected
experimentally, there was initially considerable scepticism for this view. We now
know that there is a fundamental reason why quarks cannot be observed as free
particles (it will be discussed in Chapter 5), but at the time many physicists looked
upon quarks as a convenient mathematical description, rather than physical
particles.14
However, evidence for the existence of quarks as real particles came
in the 1960s from a series of experiments analogous to those of Rutherford and his
co-workers, where high-energy beams of electrons and neutrinos were scattered
from nucleons. (These experiments will also be discussed in Chapter 5.) Analysis
of the angular distributions of the scattered particles showed that the nucleons were
themselves bound states of three point-like charged entities, with properties
consistent with those hypothesized in the quark model. One of these properties
was unexpected and unusual: quarks have fractional electric charges, in practice
 1
3 e and þ 2
3 e. This is essentially the picture today, where elementary particles
are now considered to be a small number of physical entities, including quarks, the
electron, neutrinos, the photon and a few others we shall meet, but no longer
nucleons.
The best theory of elementary particles we have at present is called, rather
prosaically, the standard model. This aims to explain all the phenomena of particle
physics, except those due to gravity, in terms of the properties and interactions of a
small number of elementary (or fundamental) particles, which are now defined as
being point-like, without internal structure or excited states. Particle physics thus
differs from nuclear physics in having a single theory to interpret its data.
An elementary particle is characterized by, amongst other things, its mass, its
electric charge and its spin. The latter is a permanent angular momentum
possessed by all particles in quantum theory, even when they are at rest. Spin
has no classical analogue and is not to be confused with the use of the same word
in classical physics, where it usually refers to the (orbital) angular momentum of
extended objects. The maximum value of the spin angular momentum about any
axis is s
hð
h  h=2Þ, where h is Planck’s constant and s is the spin quantum
number, or spin for short. It has a fixed value for particles of any given type (for
example s ¼ 1
2 for electrons) and general quantum mechanical principles restrict
the possible values of s to be 0, 1
2, 1, 3
2, . . .. Particles with half-integer spin are
called fermions and those with integer spin are called bosons. There are three
families of elementary particles in the standard model: two spin-1
2 families of
fermions called leptons and quarks; and one family of spin-1 bosons. In addition,
13
Gell-Mann received the 1969 Nobel Prize in Physics for ‘contributions and discoveries concerning the
classification of elementary particles and their interactions’. For the origin of the word ‘quark’, he cited the
now famous quotation ‘Three quarks for Muster Mark’ from James Joyce’s book Finnegans Wake. Zweig
had suggested the name ‘aces’, which with hindsight might have been more appropriate, as later experiments
revealed that there were four and not three families of quarks.
14
This was history repeating itself. In the early days of the atomic model many very distinguished scientists
were reluctant to accept that atoms existed, because they could not be ‘seen’ in a conventional sense.
HISTORY 5
at least one other spin-0 particle, called the Higgs boson, is postulated to explain
the origin of mass within the theory.15
The most familiar elementary particle is the electron, which we know is bound
in atoms by the electromagnetic interaction, one of the four forces of nature.16
One
test of the elementarity of the electron is the size of its magnetic moment. A
charged particle with spin necessarily has an intrinsic magnetic moment l. It can
be shown from the Dirac equation that a point-like spin-1
2 particle of charge q and
mass m has a magnetic moment l ¼ ðq=mÞS, where S is its spin vector, and hence l
has magnitude  ¼ q
h=2m. The magnetic moment of the electron very accurately
obeys this relation, confirming that electrons are elementary.
The electron is a member of the family of leptons. Another is the neutrino,
which was mentioned earlier as a decay product in -decays. Strictly speaking, this
particle should be called the electron neutrino, written e, because it is always
produced in association with an electron (the reason for this is discussed in
Section 3.1.1). The force responsible for -decay is an example of a second
fundamental force, the weak interaction. Finally, there is the third force, the
(fundamental) strong interaction, which, for example, binds quarks in nucleons.
The strong nuclear force mentioned in Section 1.1.1 is not the same as this
fundamental strong interaction, but is a consequence of it. The relation between
the two will be discussed in more detail later.
The standard model also specifies the origin of these three forces. In classical
physics the electromagnetic interaction is propagated by electromagnetic waves,
which are continuously emitted and absorbed. While this is an adequate descrip-
tion at long distances, at short distances the quantum nature of the interaction must
be taken into account. In quantum theory, the interaction is transmitted discon-
tinuously by the exchange of photons, which are members of the family of
fundamental spin-1 bosons of the standard model. Photons are referred to as the
gauge bosons, or ‘force carriers’, of the electromagnetic interaction. The use of the
word ‘gauge’ refers to the fact that the electromagnetic interaction possesses a
fundamental symmetry called gauge invariance. For example, Maxwell’s equa-
tions of classical electromagnetism are invariant under a specific phase transfor-
mation of the electromagnetic fields – the gauge transformation.17
This property is
common to all the three interactions of nature we will be discussing and has
profound consequences, but we will not need its details in this book. The weak and
strong interactions are also mediated by the exchange of spin-1 gauge bosons. For
the weak interaction these are the Wþ
, W
and Z0
bosons (again the superscripts
denote the electric charges) with masses about 80–90 times the mass of the proton.
15
In the theory without the Higgs boson, all elementary particles are predicted to have zero mass, in obvious
contradiction with experiment. A solution to this problem involving the Higgs boson will be discussed briefly
in Chapter 9.
16
Gravity is so weak that it can be neglected in nuclear and particle physics at presently accessible energies.
Because of this, we will often refer in practice to the three forces of nature.
17
See, for example, Appendix C.2 of Ma97.
6 CH1 BASIC CONCEPTS
For the strong interaction, the force carriers are called gluons. There are eight
gluons, all of which have zero mass and are electrically neutral.18
In addition to the elementary particles of the standard model, there are other
important particles we will be studying. These are the hadrons, the bound states of
quarks. Nucleons are examples of hadrons,19
but there are several hundred more,
not including nuclei, most of which are unstable and decay by one of the three
interactions. It was the abundance of these states that drove the search for a
simplifying theory that would give an explanation for their existence and led to the
quark model in the 1960s. The most common unstable example of a hadron is the
pion, which exists in three electrical charge states, written ðþ
; 0
; 
Þ. Hadrons
are important because free quarks are unobservable in nature and so to deduce
their properties we are forced to study hadrons. An analogy would be if we had to
deduce the properties of nucleons by exclusively studying the properties of nuclei.
Since nucleons are bound states of quarks and nuclei are bound states of
nucleons, the properties of nuclei should, in principle, be deducible from the
properties of quarks and their interactions, i.e. from the standard model. In
practice, however, this is far beyond present calculational techniques and some-
times nuclear and particle physics are treated as two almost separate subjects.
However, there are many connections between them and in introductory treatments
it is still useful to present both subjects together.
The remaining sections of this chapter are devoted to introducing some of the
basic theoretical tools needed to describe the phenomena of both nuclear and
particle physics, starting with a key concept: antiparticles.
1.2 Relativity and Antiparticles
Elementary particle physics is also called high-energy physics. One reason for this
is that if we wish to produce new particles in a collision between two other
particles, then because of the relativistic mass–energy relation E ¼ mc2
, energies
are needed at least as great as the rest masses of the particles produced. The second
reason is that to explore the structure of a particle requires a probe whose
wavelength is smaller than the structure to be explored. By the de Broglie
relation ¼ h=p, this implies that the momentum p of the probing particle, and
hence its energy, must be large. For example, to explore the internal structure of
the proton using electrons requires wavelengths that are much smaller than the
18
Note that the word ‘electric’ has been used when talking about charge. This is because the weak and strong
interactions also have associated ‘charges’ which determine the strengths of the interactions, just as the
electric charge determines the strength of the electromagnetic interaction. This will be discussed in more
detail in later chapters.
19
The magnetic moments of the proton and neutron do not obey the prediction of the Dirac equation and this
is evidence that nucleons have structure and are not elementary. The proton magnetic moment was first
measured by Otto Stern using a molecular beam method that he developed and for this he received the 1943
Nobel Prize in Physics.
RELATIVITY AND ANTIPARTICLES 7
classical radius of the proton, which is roughly 1015
m. This in turn requires
electron energies that are greater than 103
times the rest energy of the electron,
implying electron velocities very close to the speed of light. Hence any explanation
of the phenomena of elementary particle physics must take account of the
requirements of the theory of special relativity, in addition to those of quantum
theory. There are very few places in particle physics where a non-relativistic
treatment is adequate, whereas the need for a relativistic treatment is far less in
nuclear physics.
Constructing a quantum theory that is consistent with special relativity leads to
the conclusion that for every particle of nature, there must exist an associated
particle, called an antiparticle, with the same mass as the corresponding particle.
This important theoretical prediction was first made by Dirac and follows from the
solutions of the equation he first wrote down to describe relativistic electrons.20
The Dirac equation is of the form
i
h
@Cðx; tÞ
@t
¼ Hðx; ^
p
pÞCðx; tÞ; ð1:1Þ
where ^
p
p ¼ i
hr is the usual quantum mechanical momentum operator and the
Hamiltonian was postulated by Dirac to be
H ¼ ca ^
p
p þ mc2
: ð1:2Þ
The coefficients a and  are determined by the requirement that the solutions of
Equation (1.1) are also solutions of the Klein–Gordon equation 21

h2 @2
Cðx; tÞ
@t2
¼ 
h2
c2
r2
Cðx; tÞ þ m2
c4
Cðx; tÞ: ð1:3Þ
This leads to the conclusion that a and  cannot be simple numbers; their simplest
forms are 4 4 matrices. Thus the solutions of the Dirac equation are four-
component wavefunctions (called spinors) with the form22
Cðx; tÞ ¼
C1ðx; tÞ
C2ðx; tÞ
C3ðx; tÞ
C4ðx; tÞ
0
B
B
@
1
C
C
A: ð1:4Þ
20
Paul Dirac shared the 1933 Nobel Prize in Physics with Erwin Schrödinger. The somewhat cryptic citation
stated ‘for the discovery of new productive forms of atomic theory’.
21
This is a relativistic equation, which is ‘derived’ by starting from the relativistic mass–energy relation
E2
¼ p2
c2
þ m2
c4
and using the usual quantum mechanical operator substitutions, ^
p
p ¼ i
hr and
E ¼ i
h@=@t.
22
The details may be found in most quantum mechanics books, for example, pp. 475–477 of Sc68.
8 CH1 BASIC CONCEPTS
The interpretation of Equation (1.4) is that the four components describe the two
spin states of a negatively charged electron with positive energy and the two spin
states of a corresponding particle having the same mass but with negative energy.
Two spin states arise because in quantum mechanics the projection in any direction
of the spin vector of a spin-1
2 particle can only result in one of the two values 1
2,
called ‘spin up’ and ‘spin down’, respectively. The two energy solutions arise from
the two solutions of the relativistic mass–energy relation E ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
p2c2 þ m2c4
p
.
The latter states can be shown to behave in all respects as positively charged
electrons (called positrons), but with positive energy. The positron is referred to as
the antiparticle of the electron. The discovery of the positron by Anderson in 1933,
with all the predicted properties, was a spectacular verification of the Dirac
prediction.
Although Dirac originally made his prediction for electrons, the result is general
and is true whether the particle is an elementary particle or a hadron. If we denote
a particle by P, then the antiparticle is in general written with a bar over it, i.e. 
P
P.
For example, the antiparticle of the proton is the antiproton 
p
p,23
with negative
electric charge; and associated with every quark, q, is an antiquark, 
q
q. However,
for some very common particles the bar is usually omitted. Thus, for example,
in the case of the positron eþ
, the superscript denoting the charge makes
explicit the fact that the antiparticle has the opposite electric charge to that of
its associated particle. Electric charge is just one example of a quantum number
(spin is another) that characterizes a particle, whether it is elementary or composite
(i.e. a hadron).
Many quantum numbers differ in sign for particle and antiparticle, and electric
charge is an example of this. We will meet others later. When brought together,
particle–antiparticle pairs, each of mass m, can annihilate, releasing their com-
bined rest energy 2mc2
as photons or other particles. Finally, we note that there is
symmetry between particles and antiparticles, and it is a convention to call the
electron the particle and the positron its antiparticle. This reflects the fact that the
normal matter contains electrons rather than positrons.
1.3 Symmetries and Conservation Laws
Symmetries and the invariance properties of the underlying interactions play an
important role in physics. Some lead to conservation laws that are universal.
Familiar examples are translational invariance, leading to the conservation of
linear momentum; and rotational invariance, leading to conservation of angular
momentum. The latter plays an important role in nuclear and particle physics as it
leads to a scheme for the classification of states based, among other quantum
23
Carl Anderson shared the 1936 Nobel Prize in Physics for the discovery of the positron. The 1958 Prize
was awarded to Emilio Segrè and Owen Chamberlain for their discovery of the antiproton.
SYMMETRIES AND CONSERVATION LAWS 9
numbers, on their spins.24
Another very important invariance that we have briefly
mentioned is gauge invariance. This fundamental property of all three interactions
restricts the forms of the interactions in a profound way that initially is contra-
dicted by experiment. This is the prediction of zero masses for all elementary
particles, mentioned earlier. There are theoretical solutions to this problem whose
experimental verification (or otherwise) is probably the most eagerly awaited
result in particle physics today.
In nuclear and particle physics we need to consider additional symmetries of the
Hamiltonian and the conservation laws that follow and in the remainder of this
section we discuss two of the most important of these that we will need later –
parity and charge conjugation.
1.3.1 Parity
Parity was first introduced in the context of atomic physics by Eugene Wigner in
1927.25
It refers to the behaviour of a state under a spatial reflection, i.e. x ! x.
If we consider a single-particle state, represented for simplicity by a non-
relativistic wavefunction ðx; tÞ, then under the parity operator, ^
P
P,
^
P
P ðx; tÞ  P ðx; tÞ: ð1:5Þ
Applying the operator again, gives
^
P
P
2
ðx; tÞ ¼ P^
P
P ðx; tÞ ¼ P2
ðx; tÞ; ð1:6Þ
implying P ¼ 1. If the particle is an eigenfunction of linear momentum p, i.e.
ðx; tÞ  pðx; tÞ ¼ exp½iðp x  EtÞ; ð1:7Þ
then
^
P
P pðx; tÞ ¼ P pðx; tÞ ¼ P pðx; tÞ ð1:8Þ
and so a particle at rest, with p ¼ 0, is an eigenstate of parity. The eigenvalue
P ¼ 1 is called the intrinsic parity, or just the parity, of the state. By considering
a multiparticle state with a wavefunction that is the product of single-particle
wavefunctions, it is clear that parity is a multiplicative quantum number.
The strong and electromagnetic interactions, but not the weak interactions, are
invariant under parity, i.e. the Hamiltonian of the system remains unchanged under
24
These points are explored in more detail in, for example, Chapter 4 of Ma97.
25
Eugene Wigner shared the 1963 Nobel Prize in Physics, principally for his work on symmetries.
10 CH1 BASIC CONCEPTS
a parity transformation on the position vectors of all particles in the system. Parity
is therefore conserved, by which we mean that the total parity quantum number
remains unchanged in the interaction. Compelling evidence for parity conservation
in the strong and electromagnetic interactions comes from the absence of
transitions between nuclear states and atomic states, respectively, that would
violate parity conservation. The evidence for non-conservation of parity in the
weak interaction will be discussed in detail in Chapter 6.
There is also a contribution to the total parity if the particle has an orbital
angular momentum l. In this case its wave function is a product of a radial part Rnl
and an angular part Ym
l ð ; Þ:
lmnðxÞ ¼ RnlYm
l ð ; Þ; ð1:9Þ
where n and m are the principal and magnetic quantum numbers and Ym
l ð ; Þ is a
spherical harmonic. It is straightforward to show from the relations between
Cartesian ðx; y; zÞ and spherical polar co-ordinates ðr; ; Þ, i.e.
x ¼ r sin cos ; y ¼ r sin sin ; z ¼ r cos ; ð1:10Þ
that the parity transformation x ! x implies
r ! r; !   ;  !  þ ; ð1:11Þ
and from this it can be shown that
Ym
l ð ; Þ ! Ym
l ð  ;  þ Þ ¼ ðÞl
Ym
l ð ; Þ: ð1:12Þ
Equation (1.12) may easily be verified directly for specific cases; for example,
for the first three spherical harmonics,
Y0
0 ¼
1
4
1
2
; Y0
1 ¼
3
4
1
2
cos ; Y 1
1 ¼
3
8
1
2
sin e i
: ð1:13Þ
Hence
^
P
P lmnðxÞ ¼ P lmnðxÞ ¼ PðÞl
lmnðxÞ; ð1:14Þ
i.e. lmnðxÞ is an eigenstate of parity with eigenvalue Pð1Þl
.
An analysis of the Dirac Equation (1.1) for relativistic electrons, shows that it is
invariant under a parity transformation only if Pðeþ
e
Þ ¼ 1. This is a general
result for all fermion–antifermion pairs, so it is a convention to assign P ¼ þ1 to
all leptons and P ¼ 1 to their antiparticles. We will see in Chapter 3 that in
strong interactions quarks can only be created as part of a quark–antiquark pair, so
the intrinsic parity of a single quark cannot be measured. For this reason, it is also
SYMMETRIES AND CONSERVATION LAWS 11
a convention to assign P ¼ þ1 to quarks. Since quarks are fermions, it follows
from the Dirac result that P ¼ 1 for antiquarks. The intrinsic parities of hadrons
then follow from their structure in terms of quarks and the orbital angular
momentum between the constituent quarks, using Equation (1.14). This will be
explored in Chapter 3 as part of the discussion of the quark model.
1.3.2 Charge conjugation
Charge conjugation is the operation of changing a particle into its antiparticle.
Like parity, it gives rise to a multiplicative quantum number that is conserved in
strong and electromagnetic interactions, but violated in the weak interaction. In
discussing charge conjugation, we will need to distinguish between states such as
the photon  and the neutral pion 0
that do not have distinct antiparticles and
those such as the þ
and the neutron, which do. Particles in the former class we
will collectively denote by a and those of the latter type will be denoted by b. It is
also convenient at this point to extend our notation for states. Thus we will
represent a state of type a having a wavefunction a by ja; ai and similarly for a
state of type b. Then under the charge conjugation operator, ^
C
C,
^
C
Cja; ai ¼ Caja; ai; ð1:15aÞ
and
^
C
Cjb; bi ¼ j
b
b; 
b
bi; ð1:15bÞ
where Ca is a phase factor analogous to the phase factor in Equation (1.5).26
Applying the operator twice, in the same way as for parity, leads to Ca ¼ 1. From
Equation (1.15a), we see that states of type a are eigenstates of ^
C
C with eigenvalues
1, called their C-parities. States with distinct antiparticles can only form
eigenstates of ^
C
C as linear combinations.
As an example of the latter, consider a þ

pair with orbital angular
momentum L between them. In this case
^
C
Cjþ

; Li ¼ ð1ÞL
jþ

; Li; ð1:16Þ
because interchanging the pions reverses their relative positions in the spatial
wavefunction. The same factor occurs for spin-1
2 fermion pairs f
f
f, but in addition
there are two other factors. The first is ð1ÞSþ1
, where S is the total spin of the pair.
26
A phase factor could have been inserted in Equation (1.15b), but it is straightforward to show that the
relative phase of the two states b and 
b
b cannot be measured and so a phase introduced in this way would have
no physical consequences.
12 CH1 BASIC CONCEPTS
This follows directly from the structure of the spin wavefunctions:
12 Sz ¼ 1
1ffiffi
2
p ð1#2 þ #12Þ Sz ¼ 0
#1#2 Sz ¼ 1
9
=
;
S ¼ 1 ð1:17aÞ
and
1ffiffi
2
p ð1#2  #12Þ Sz ¼ 0 S ¼ 0; ð1:17bÞ
where i ð#iÞ represents particle i having spin ‘up’ (‘down’) in the z-direction. A
second factor ð1Þ arises whenever fermions and antifermions are interchanged.
This has its origins in quantum field theory.27
Combining these factors, finally
we have
^
C
Cj f
f
f; J; L; Si ¼ ð1ÞLþS
j f
f
f; J; L; Si; ð1:18Þ
for fermion–antifermion pairs having total, orbital and spin angular momentum
quantum numbers J, L and S, respectively.
1.4 Interactions and Feynman Diagrams
We now turn to a discussion of particle interactions and how they can be described
by the very useful pictorial methods of Feynman diagrams.
1.4.1 Interactions
Interactions involving elementary particles and/or hadrons are conveniently
summarized by ‘equations’ by analogy with chemical reactions, in which the
different particles are represented by symbols which usually – but not always –
have a superscript to denote their electric charge. In the interaction
e þ n ! e
þ p; ð1:19Þ
for example, an electron neutrino e collides with a neutron n to produce an
electron e
and a proton p, whereas the equation
e
þ p ! e
þ p ð1:20Þ
27
See, for example, pp. 249–250 of Go86.
INTERACTIONS AND FEYNMAN DIAGRAMS 13
represents an electron and proton interacting to give the same particles in the final
state, but in general travelling in different directions. In such equations, conserved
quantum numbers must have the same total values in initial and final states.
Particles may be transferred from initial to final states and vice versa, when they
become antiparticles. Thus the process

þ p ! 
þ p; ð1:21aÞ
also implies the reaction
p þ 
p
p ! þ
þ 
; ð1:22Þ
which is obtained by taking the proton from the final state to an antiproton in the
initial state and the negatively charged pion in the initial state to a positively
charged pion in the final state.
The interactions in Equations (1.20) and (1.21a), in which the particles remain
unchanged, are examples of elastic scattering, in contrast to the reactions in
Equations (1.19) and (1.22), where the final-state particles differ from those in the
initial state. Collisions between a given pair of initial particles do not always lead
to the same final state, but can lead to different final states with different
probabilities. For example, the collision of a negatively charged pion and a proton
can give rise to elastic scattering (Equation (1.21a)) and a variety of other
reactions, such as

þ p ! n þ 0
and 
þ p ! p þ 
þ 
þ þ
; ð1:21bÞ
depending on the initial energy. In particle physics it is common to refer (rather
imprecisely) to such interactions as ‘inelastic’ scattering.
Similar considerations apply to nuclear physics, but the term inelastic scattering
is reserved for the case where the final state is an excited state of the parent nucleus
A, that subsequently decays, for example via photon emission, i.e.
a þ A ! a þ A
; A
! A þ ; ð1:23Þ
where a is a projectile and A
is an excited state of A. A useful shorthand notation
used in nuclear physics for the general reaction a þ A ! b þ B is Aða; bÞB. It is
usual in nuclear physics to further subdivide types of interactions according to the
underlying mechanism that produced them. We will return to this in Section 2.9, as
part of a more general discussion of nuclear reactions.
Finally, many particles are unstable and spontaneously decay to other, lighter
(i.e. having less mass) particles. An example of this is the free neutron (i.e. one not
bound in a nucleus), which decays by the -decay reaction
n ! p þ e
þ 

e; ð1:24Þ
14 CH1 BASIC CONCEPTS
with a mean lifetime of about 900 s.28
The same notation can also be used in
nuclear physics. For example, many nuclei decay via the -decay reaction. Thus,
denoting a nucleus with Z protons and N nucleons as (Z, N ), we have
ðZ; NÞ ! ðZ  1; NÞ þ eþ
þ e: ð1:25Þ
This is also a weak interaction. This reaction is effectively the decay of a proton
bound in a nucleus. Although a free proton cannot decay by the -decay
p ! n þ eþ
þ e because it violates energy conservation (the final-state particles
have greater total mass than the proton), a proton bound in a nucleus can decay
because of its binding energy. This will be explained in Chapter 2.
1.4.2 Feynman diagrams
The forces producing all the above interactions are due to the exchange of particles
and a convenient way of illustrating this is to use Feynman diagrams. There are
mathematical rules and techniques associated with these that enable them to be
used to calculate the quantum mechanical probabilities for given reactions to
occur, but in this book Feynman diagrams will only be used as a convenient very
useful pictorial description of reaction mechanisms.
We first illustrate them at the level of elementary particles for the case of
electromagnetic interactions, which arise from the emission and/or absorption of
photons. For example, the dominant interaction between two electrons is due to the
exchange of a single photon, which is emitted by one electron and absorbed by the
other. This mechanism, which gives rise to the familiar Coulomb interaction at
large distances, is illustrated in the Feynman diagram Figure 1.1(a).
In such diagrams, we will use the convention that particles in the initial state are
shown on the left and particles in the final state are shown on the right. (Some
authors take time to run along the y-axis.) Spin-1
2 fermions (such as the electron)
28
The reason that this decay involves an antineutrino rather than a neutrino will become clear in Chapter 3.
Figure 1.1 One-photon exchange in (a) e
þ e
! e
þ e
and (b) eþ
þ eþ
! eþ
þ eþ
INTERACTIONS AND FEYNMAN DIAGRAMS 15
are drawn as solid lines and photons are drawn as wiggly lines. Arrowheads
pointing to the right indicate that the solid lines represent electrons. In the case of
photon exchange between two positrons, which is shown in Figure 1.1(b), the
arrowheads on the antiparticle (positron) lines are conventionally shown as
pointing to the left. In interpreting these diagrams, it is important to remember:
(1) that the direction of the arrows on fermion lines does not indicate the particle’s
direction of motion, but merely whether the fermions are particles or antiparticles,
and (2) that particles in the initial state are always to the left and particles in the
final state are always to the right.
A feature of the above diagrams is that they are constructed from combinations
of simple three-line vertices. This is characteristic of electromagnetic processes.
Each vertex has a line corresponding to a single photon being emitted or absorbed,
while one fermion line has the arrow pointing toward the vertex and the other away
from the vertex, guaranteeing charge conservation at the vertex, which is one of
the rules of Feynman diagrams.29
For example, a vertex like Figure 1.2 would
correspond to a process in which an electron emitted a photon and turned into a
positron. This would violate charge conservation and is therefore forbidden.
Feynman diagrams can also be used to describe the fundamental weak and
strong interactions. This is illustrated by Figure 1.3(a), which shows contributions
to the elastic weak scattering reaction e
þ e ! e
þ e due to the exchange of a
Z0
, and by Figure 1.3(b), which shows the exchange of a gluon g (represented by a
coiled line) between two quarks, which is a strong interaction.
Feynman diagrams can also be drawn at the level of hadrons. As an illustration,
Figure 1.4 shows the exchange of a charged pion (shown as a dashed line) between
a proton and a neutron. We shall see later that this mechanism is a major
contribution to the strong nuclear force between a proton and a neutron.
We turn now to consider in more detail the relation between exchanged particles
and forces.
29
Compare Kirchhoff’s laws in electromagnetism.
e–
e+
γ
Figure 1.2 The forbidden vertex e
! eþ
þ 
16 CH1 BASIC CONCEPTS
1.5 Particle Exchange: Forces and Potentials
This section starts with a discussion of the important relationship between forces
and particle exchanges and then relates this to potentials. Although the idea of a
potential has its greatest use in non-relativistic physics, nevertheless it is useful to
illustrate concepts and is used in later sections as an intermediate step in relating
theoretical Feynman diagrams to measurable quantities. The results can easily be
extended to more general situations.
1.5.1 Range of forces
At each vertex of a Feynman diagram, charge is conserved by construction. We
will see later that, depending on the nature of the interaction (strong, weak or
electromagnetic), other quantum numbers are also conserved. However, it is easy
to show that energy and momentum cannot be conserved simultaneously.
Consider the general case of a reaction A þ B ! A þ B mediated by the
exchange of a particle X, as shown in Figure 1.5. In the rest frame of the incident
Figure 1.3 (a) Contributions of (a) Z0
exchange to the elastic weak scattering reaction
e
þ e ! e
þ e, and (b) gluon exchange contribution to the strong interaction q þ q ! q þ q
Figure 1.4 Single-pion exchange in the reaction p þ n ! n þ p
PARTICLE EXCHANGE: FORCES AND POTENTIALS 17
particle A, the lower vertex represents the virtual process (‘virtual’ because X does
not appear as a real particle in the final state),
AðMAc2
; 0Þ ! AðEA; pAcÞ þ XðEX; pAcÞ; ð1:26Þ
where EA is the total energy of particle A and pA is its three-momentum.30
Thus, if
we denote by PA the four-vector for particle A,
PA ¼ ðEA=c; pAÞ ð1:27Þ
and
P2
A ¼ E2
A=c2
 p2
A ¼ M2
Ac2
: ð1:28Þ
Applying this to the diagram and imposing momentum conservation, gives
EA ¼ ðp2
c2
þ M2
Ac4
Þ1=2
; EX ¼ ðp2
c2
þ M2
Xc4
Þ1=2
; ð1:29Þ
where p ¼ jpj. The energy difference between the final and initial states is given by
E ¼ EX þ EA  MAc2
! 2pc; p ! 1
! MXc2
; p ! 0 ð1:30Þ
and thus E  MXc2
for all p, i.e. energy is not conserved. However, by the
Heisenberg uncertainty principle, such an energy violation is allowed, but only for
a time   
h=E, so we immediately obtain
r  R  
h=MXc ð1:31Þ
30
A resumé of relativistic kinematics is given in Appendix B.
Figure 1.5 Exchange of a particle X in the reaction A þ B ! A þ B
18 CH1 BASIC CONCEPTS
as the maximum distance over which X can propagate before being absorbed by
particle B. This maximum distance is called the range of the interaction and this
was the sense of the word used in Section 1.1.1.
The electromagnetic interaction has an infinite range, because the exchanged
particle is a massless photon. In contrast, the weak interaction is associated with
the exchange of very heavy particles – the W and Z bosons. These lead to ranges
that from Equation (1.31) are of the order of RW;Z  2 1018
m. The funda-
mental strong interaction has infinite range because, like the photon, gluons have
zero mass. On the other hand, the strong nuclear force, as exemplified by Figure 1.4
for example, has a much shorter range of approximately (1–2) 1015
m. We will
comment briefly on the relation between these two different manifestations of the
strong interaction in Section 7.1.
1.5.2 The Yukawa potential
In the limit that MA becomes large, we can regard B as being scattered by a static
potential of which A is the source. This potential will in general be spin dependent,
but its main features can be obtained by neglecting spin and considering X to be a
spin-0 boson, in which case it will obey the Klein–Gordon equation

h2 @2
ðx; tÞ
@t2
¼ 
h2
c2
r2
ðx; tÞ þ M2
Xc4
ðx; tÞ: ð1:32Þ
The static solution of this equation satisfies
r2
ðxÞ ¼
M2
Xc4

h2
ðxÞ; ð1:33Þ
where ðxÞ is interpreted as a static potential. For MX ¼ 0 this equation is the same
as that obeyed by the electrostatic potential, and for a point charge e interacting
with a point charge þe at the origin, the appropriate solution is the Coulomb potential
VðrÞ ¼ eðrÞ ¼ 
e2
40
1
r
; ð1:34Þ
where r ¼ jxj and 0 is the dielectric constant. The corresponding solution in the
case where M2
X 6¼ 0 is easily verified by substitution to be
VðrÞ ¼ 
g2
4
er=R
r
; ð1:35Þ
where R is the range defined earlier and g, the so-called coupling constant, is a
parameter associated with each vertex of a Feynman diagram and represents the
PARTICLE EXCHANGE: FORCES AND POTENTIALS 19
basic strength of the interaction.31
For simplicity, we have assumed equal strengths
for the couplings of particle X to the particles A and B.
The form of VðrÞ in Equation (1.35) is called a Yukawa potential, after the physicist
who first introduced the idea of forces due to massive particle exchange in 1935.32
As MX ! 0, R ! 1 and the Coulomb potential is recovered from the Yukawa
potential, while for very large masses the interaction is approximately point-like
(zero range). It is conventional to introduce a dimensionless parameter X by
X ¼
g2
4
hc
; ð1:36Þ
that characterizes the strength of the interaction at short distances r  R. For the
electromagnetic interaction this is the fine structure constant
  e2
=40
hc  1=137 ð1:37Þ
that governs the splittings of atom energy levels.33
The forces between hadrons are also generated by the exchange of particles. Thus,
in addition to the electromagnetic interaction between charged hadrons, all hadrons,
whether charged or neutral, experience a strong short-range interaction, which in the
case of two nucleons, for example, has a range of about 1015
m, corresponding to
the exchange of a particle with an effective mass of about 1
7th the mass of the proton.
The dominant contribution to this force is the exchange of a single pion, as shown in
Figure 1.4. This nuclear strong interaction is a complicated effect that has its origins
in the fundamental strong interactions between the quark distributions within the two
hadrons. Two neutral atoms also experience an electromagnetic interaction (the van
der Waals force), which has its origins in the fundamental Coulomb forces, but is of
much shorter range. Although an analogous mechanism is not in fact responsible for
the nuclear strong interaction, it is a useful reminder that the force between two
distributions of particles can be much more complicated than the forces between
their components. We will return to this point when we discuss the nature of the
nuclear potential in more detail in Section 7.1.
1.6 Observable Quantities: Cross Sections and Decay Rates
We have mentioned earlier that Feynman diagrams can be turned into probabilities
for a process by a set of mathematical rules (the Feynman Rules) that can be
31
Although we call g a (point) coupling constant, in general it will have a dependence on the momentum
carried by the exchanged particle. We ignore this in what follows.
32
For this insight, Hideki Yukawa received the 1949 Nobel Prize in Physics.
33
Like g, the coupling X will in general have a dependence on the momentum carried by particle X. In the
case of the electromagnetic interaction, this dependence is relatively weak.
20 CH1 BASIC CONCEPTS
derived from the quantum theory of the underlying interaction.34
We will not
pursue this in detail in this book, but rather will show in principle their relation to
observables, i.e. things that can be measured, concentrating on the cases of two-
body scattering reactions and decays of unstable states.
1.6.1 Amplitudes
The intermediate step is the amplitude f, the modulus squared of which is directly
related to the probability of the process occurring. It is also called the invariant
amplitude because, as we shall show, it is directly related to observable quantities
and these have to be the same in all inertial frames of reference. To get some
qualitative idea of the structure of f, we will use non-relativistic quantum
mechanics and assume that the coupling constant g2
is small compared with
4
hc, so that the interaction is a small perturbation on the free particle solution,
which will be taken as plane waves.
If we expand the amplitude in a power series in g2
and keep just the first term
(i.e. lowest-order perturbation theory), then the amplitude for a particle in an initial
state with momentum qi to be scattered to a final state with momentum qf by a
potential VðxÞ is proportional to
fðq2
Þ ¼
ð
d3
xVðxÞ exp½iq x=
h; ð1:38Þ
i.e. the Fourier transform of the potential, where q  qi  qf is the momentum
transfer.35
The integration may be done using polar co-ordinates. Taking q in the x-
direction, gives
q x ¼ jqjr cos ð1:39Þ
and
d3
x ¼ r2
sin d dr d; ð1:40Þ
where r ¼ jxj. For the Yukawa potential, the integral in Equation (1.38) gives
fðq2
Þ ¼
g2

h2
q2 þ M2
Xc2
: ð1:41Þ
34
In the case of the electromagnetic interaction, the theory is called Quantum Electrodynamics (QED) and is
spectacularly successful in explaining experimental results. Richard Feynman shared the 1965 Nobel Prize in
Physics with Sin-Itiro Tomonoga and Julian Schwinger for their work on formulating quantum electro-
dynamics. The Feynman Rules are discussed in an accessible way in Gr87.
35
See, for example, Chapter 11 of Ma92.
OBSERVABLE QUANTITIES: CROSS SECTIONS AND DECAY RATES 21
This amplitude corresponds to the exchange of a single particle, as shown for
example in Figures 1.3 and 1.4. The structure of the amplitude, which is quite
general, is a numerator proportional to the product of the couplings at the two
vertices (or equivalently X in this case), and a denominator that depends on the
mass of the exchanged particle and its momentum transfer squared. The denomi-
nator is called the propagator for particle X. In a relativistic calculation, the term
q2
becomes q2
, where q is the four-momentum transfer.
Returning to the zero-range approximation, one area where it is used extensively
is in weak interactions, particularly applied to nuclear decay processes. In these
situations, MX ¼ MW;Z and f ! GF, where GF, the so-called Fermi coupling
constant, is given from Equation (1.36) by
GF
ð
hcÞ3
¼
4W
ðMW c2Þ2
¼ 1:166 105
GeV2
: ð1:42Þ
The numerical value is obtained from analyses of decay processes, including that
of the neutron and a heavier version of the electron called the muon, whose
properties will be discussed in Chapter 3.
All the above is for the exchange of a single particle. It is also possible to draw
more complicated Feynman diagrams that correspond to the exchange of more
than one particle. An example of such a diagram for elastic e
e
scattering, where
two photons are exchanged, is shown in Figure 1.6.
The number of vertices in any diagram is called the order n, and when the
amplitude associated with any given Feynman diagram is calculated, it always
contains a factor of ð
ffiffiffiffi

p
Þn
. Since the probability is proportional to the square of
the modulus of the amplitude, the former will contain a factor n
. The probability
associated with the single-photon exchange diagrams of Figure 1.1 thus contain a
factor of 2
and the contribution from two-photon exchange is of the order of 4
.
Figure 1.6 Two-photon exchange in the reaction e
þ e
! e
þ e
22 CH1 BASIC CONCEPTS
As   1=137, the latter is usually very small compared with the contribution
from single-photon exchange.
This is a general feature of electromagnetic interactions: because the fine structure
constant is very small, in most cases only the lowest-order diagrams that contribute to
a given process need be taken into account, and more complicated higher-order
diagrams with more vertices can (to a good approximation) be ignored in many
applications.
1.6.2 Cross-sections
The next step is to relate the amplitude to measurables. For scattering reactions,
the appropriate observable is the cross-section. In a typical scattering experiment, a
beam of particles is allowed to hit a target and the rates of production of various
particles in the final state are counted.36
It is clear that the rates will be
proportional to: (a) the number N of particles in the target illuminated by the
beam, and (b) the rate per unit area at which beam particles cross a small surface
placed in the beam at rest with respect to the target and perpendicular to the beam
direction. The latter is called the flux and is given by
J ¼ nbvi; ð1:43Þ
where nb is the number density of particles in the beam and vi their velocity in the
rest frame of the target. Hence the rate Wr at which a specific reaction r occurs in a
particular experiment can be written in the form
Wr ¼ JNr; ð1:44aÞ
where r, the constant of proportionality, is called the cross-section for reaction r.
If the beam has a cross-sectional area S, its intensity is I ¼ JS and so an alternative
expression for the rate is
Wr ¼ NrI=S ¼ Irntt; ð1:44bÞ
where nt is the number of target particles per unit volume and t is the thickness of
the target. If the target consists of an isotopic species of atomic mass MA (in atomic
mass units-defined in Section 1.7 below), then nt ¼ NA=MA, where  is the density
of the target and NA is Avogadro’s constant. Thus, Equation (1.44b) may be written
Wr ¼ IrðtÞNA=MA; ð1:44cÞ
36
The practical aspects of experiments are discussed in Chapter 4.
OBSERVABLE QUANTITIES: CROSS SECTIONS AND DECAY RATES 23
where ðtÞ is a measure of the amount of material in the target, expressed in units
of mass per unit area. The form of Equation (1.44c) is particularly useful for the
case of thin targets, commonly used in experiments. In the above, the product JN is
called the luminosity L, i.e.
L  JN ð1:45Þ
and contains all the dependencies on the densities and geometries of the beam and
target. The cross-section is independent of these factors.
It can be seen from the above equations that the cross-section has the dimensions
of an area; the rate per target particle Jr at which the reaction occurs is equal to
the rate at which beam particles would hit a surface of area r, placed in the beam
at rest with respect to the target and perpendicular to the beam direction. Since the
area of such a surface is unchanged by a Lorentz transformation in the beam
direction, the cross-section is the same in all inertial frames of reference, i.e. it is a
Lorentz invariant.
The quantity r is better named the partial cross-section, because it is the cross-
section for a particular reaction r. The total cross-section  is defined by
 
X
r
r: ð1:46Þ
Another useful quantity is the differential cross-section, drð ; Þ=d, which is
defined by
dWr  JN
drð ; Þ
d
d; ð1:47Þ
where dWr is the measured rate for the particles to be emitted into an element of
solid angle d ¼ d cos d in the direction ð ; Þ, as shown in Figure 1.7.
The total cross-section is obtained by integrating the partial cross-section over
all angles, i.e.
r ¼
ð2
0
d
ð1
1
d cos
drð ; Þ
d
: ð1:48Þ
The final step is to write these formulae in terms of the scattering amplitude fðq2
Þ
appropriate for describing the scattering of a non-relativistic spinless particle from
a potential.
To do this it is convenient to consider a single beam particle interacting with a
single target particle and to confine the whole system in an arbitrary volume V
(which cancels in the final result). The incident flux is then given by
J ¼ nbvi ¼ vi=V ð1:49Þ
24 CH1 BASIC CONCEPTS
and since the number of target particles is N ¼ 1, the differential rate is
dWr ¼
vi
V
drð ; Þ
d
d: ð1:50Þ
In quantum mechanics, provided the interaction is not too strong, the transition
rate for any process is given in perturbation theory by the Born approximation37
dWr ¼
2

h




ð
d3
x 
f VðxÞ i




2
ðEfÞ: ð1:51Þ
The term ðEfÞ is the density-of-states factor (see below) and we take the initial
and final state wavefunctions to be plane waves:
i ¼
1
ffiffiffiffi
V
p exp½iqi x=
h; f ¼
1
ffiffiffiffi
V
p exp½iqf x=
h; ð1:52Þ
37
This equation is a form of the Second Golden Rule. It is discussed in Appendix A.
Figure 1.7 Geometry of the differential cross-section: a beam of particles is incident along the
z-axis and collides with a stationary target at the origin; the differential cross-section is
proportional to the rate for particles to be scattered into a small solid angle d in the direction
ð ; Þ
OBSERVABLE QUANTITIES: CROSS SECTIONS AND DECAY RATES 25
where the final momentum qf lies within a small solid angle d located in the
direction ð ; Þ (see Figure 1.7.). Then, by direct integration,
dWr ¼
2

hV2
j fðq2
Þj2
ðEfÞ; ð1:53Þ
where fðq2
Þ is the scattering amplitude defined in Equation (1.38).
The density of states ðEfÞ that appears in Equation (1.51) is the number of
possible final states with energy lying between Ef and Ef þ dEf and is given by38
ðEfÞ ¼
V
ð2
hÞ3
q2
f
vf
d: ð1:54Þ
If we use this and Equation (1.53) in Equation (1.50), we have
d
d
¼
1
42
h4
q2
f
vivf
j fðq2
Þj2
: ð1:55Þ
Although this result has been derived in the laboratory system, because we have
taken a massive target it is also valid in the centre-of-mass system. For a finite
mass target it would be necessary to make a Lorentz transformation on Equation
(1.55). The expression is also true for the general two-body relativistic scattering
process a þ b ! c þ d.
All the above is for spinless particles, so finally we have to generalize Equation
(1.55) to include the effects of spin. Suppose the initial-state particles a and b, have
spins sa and sb and the final-state particles c and d have spins sc and sd. The total
numbers of spin substates available to the initial and final states are gi and gf,
respectively, given by
gi ¼ ð2sa þ 1Þð2sb þ 1Þ and gf ¼ ð2sc þ 1Þ ð2sd þ 1Þ: ð1:56Þ
If the initial particles are unpolarized (which is the most common case in practice),
then we must average over all possible initial spin configurations (because each is
equally likely) and sum over the final configurations. Thus, Equation (1.55) becomes
d
d
¼
gf
42
h4
q2
f
vivf
jMfij2
; ð1:57Þ
where
jMfij2
 j fðq2Þj2
ð1:58Þ
and the bar over the amplitude denotes a spin-average of the squared matrix
element.
38
The derivation is given in detail in Appendix A.
26 CH1 BASIC CONCEPTS
1.6.3 Unstable states
In the case of an unstable state, the observable of interest is its lifetime at rest , or
equivalently its natural decay width, given by  ¼ 
h=, which is a measure of the
rate of the decay reaction. In general, an initial unstable state will decay to several
final states and in this case we define f as the partial width for channel f and
 ¼
X
f
f ð1:59Þ
as the total decay width, while
Bf  f = ð1:60Þ
is defined as the branching ratio for decay to channel f.
The energy distribution of an unstable state to a final state f has the Breit–Wigner
form
Nf ðWÞ /
f
ðW  MÞ2
c4 þ 2=4
; ð1:61Þ
where M is the mass of the decaying state and W is the invariant mass of the decay
products.39
The Breit–Wigner formula is shown in Figure 1.8 and is the same
formula that describes the widths of atomic and nuclear spectral lines. (The overall
factor depends on the spins of the particles involved.) It is a symmetrical bell-
shaped curve with a maximum at W ¼ M and a full width  at half the maximum
height of the curve. It is proportional to the number of events with invariant mass W.
If an unstable state is produced in a scattering reaction, then the cross section for
that reaction will show an enhancement described by the same Breit–Wigner formula.
In this case we say we have produced a resonance state. In the vicinity of a resonance
of mass M, and width , the cross-section for the reaction i ! f has the form
fi /
if
ðE  Mc2Þ2
þ 2=4
; ð1:62Þ
where E is the total energy of the system. Again, the form of the overall constant
will depend on the spins of the particles involved. Thus, for example, if the
resonance particle has spin j and the spins of the initial particles are s1 and s2, then
fi ¼

h2
q2
i
2j þ 1
ð2s1 þ 1Þð2s2 þ 1Þ
if
ðE  Mc2Þ2
þ 2=4
: ð1:63Þ
39
This form arises from a state that decays exponentially with time, although a proper proof of this is quite
lengthy. See, for example, Appendix B of Ma97.
OBSERVABLE QUANTITIES: CROSS SECTIONS AND DECAY RATES 27
In practice there will also be kinematical and angular momentum effects that will
distort this formula from its perfectly symmetric shape.
An example of resonance formation in 
p interactions is given in Figure 1.9,
which shows the 
p total cross-section in the centre-of-mass energy range
Figure 1.8 The Breit--Wigner formula (Equation (1.61))
Figure 1.9 Total cross-sections for 
p interactions (data from Ca68)
28 CH1 BASIC CONCEPTS
1.2–2.4 GeV. (The units used in the plots will become clear after the next section.)
Two enhancements can be seen that are of the approximate Breit–Wigner resonance
form and there are two other maxima at higher energies. In principle, the mass and
width of a resonance may be obtained by using a Breit–Wigner formula and varying
M and  to fit the cross-section in the region of the enhancement. In practice, more
sophisticated methods are used that fit a wide range of data, including differential
cross-sections, simultaneously and also take account of non-resonant contributions
to the scattering. The widths obtained from such analyses are of the order of
100 MeV, with corresponding interaction times of order 1023
s, which is consistent
with the time taken for a relativistic pion to transit the dimension of a proton.
Resonances are also a feature of interactions in nuclear physics and we will return to
this in Section 2.9 when we discuss nuclear reaction mechanisms.
1.7 Units: Length, Mass and Energy
Most branches of science introduce special units that are convenient for their own
purposes. Nuclear and particle physics are no exceptions. Distances tend to be measured
in femtometres (fm) or, equivalently fermis, with 1 fm  1015
m. In these units, the
radius of the proton is about 0.8 fm. The range of the strong nuclear force between
protons and neutrons is of the order of 1–2 fm, while the range of theweak force is of the
order of 103
fm. For comparison, the radii of atoms are of the order of 105
fm. A
common unit for area is the barn (b) defined by 1 b ¼ 1028
m2
. For example, the total
cross-section for pp scattering (a strong interaction) is a few tens of millibarns (mb)
(compare also the 
p total cross-section in Figure 1.9), whereas the same quantity for
p scattering (a weak interaction) is a few tens of femtobarns (fb), depending on the
energies involved. Nuclear cross-sections are very much larger and increase approxi-
mately like A2=3
, where A is the total number of nucleons in the nucleus.
Energies are invariably specified in terms of the electron volt (eV) defined as the
energy required to raise the electric potential of an electron or proton by 1 V.
In SI units, 1 eV ¼ 1:6 1019
J. The units 1 keV ¼ 103
eV, 1 MeV ¼ 106
eV,
1 GeV ¼ 109
eV and 1 TeV ¼ 1012
eV are also in general use. In terms of these
units, atomic ionization energies are typically a few eV, the energies needed to
bind nucleons in heavy nuclei are typically 7–8 MeV per particle, and the highest
particle energies produced in the laboratory are of the order of 1 TeV for protons.
Momenta are specified in eV=c, MeV=c, etc..
In order to create a new particle of mass M, an energy at least as great as its rest
energy Mc2
must be supplied. The rest energies of the electron and proton are
0.51 MeV and 0.94 GeV respectively, whereas the W and Z0
bosons have rest
energies of 80 GeV and 91 GeV, respectively. Correspondingly, their masses are
conveniently measured in MeV=c2
or GeV=c2
, so that, for example,
Me ¼ 0:51 MeV=c2
; Mp ¼ 0:94 GeV=c2
;
MW ¼ 80:3 GeV=c2
; MZ ¼ 91:2 GeV=c2
ð1:64Þ
UNITS: LENGTH, MASS AND ENERGY 29
In SI units, 1 MeV=c2
¼ 1:78 1030
kg. In nuclear physics it is also common to
express masses in atomic mass units (u), where 1 u ¼ 1:661 1027
kg ¼
931:5 MeV=c2
.
Although practical calculations are expressed in the above units, it is usual in
particle physics to make theoretical calculations in units chosen such that

h  h=2 ¼ 1 and c ¼ 1 (called natural units) and many books do this. However,
as this book is about both nuclear and particle physics, only practical units will be
used.
A table giving numerical values of fundamental and derived constants, together
with some useful conversion factors is given on page XV.
Problems
1.1 ‘Derive’ the Klein–Gordon equation using the information in Footnote 21 and verify
that Equation (1.35) is a static solution of the equation.
1.2 Verify that the spherical harmonic Y1
1 ¼
ffiffi
3
8
q
sin ei
is an eigenfunction of parity
with eigenvalue P ¼ 1.
1.3 A proton and antiproton at rest in an S-state annihilate to produce 0
0
pairs. Show
that this reaction cannot be a strong interaction.
1.4 Suppose that an intrinsic C-parity factor is introduced into Equation (1.15b), which
then becomes ^
C
Cjb; bi ¼ Cbj
b
b; 
b
bi. Show that the eigenvalue corresponding to any
eigenstate of ^
C
C is independent of Cb, so that Cb cannot be measured.
1.5 Consider the reaction 
d ! nn, where d is a spin-1 S-wave bound state of a proton
and a neutron called the deuteron and the initial pion is at rest. Deduce the intrinsic
parity of the negative pion.
1.6 Write down equations in symbol form that describe the following interactions:
(a) elastic scattering of an electron antineutrino and a positron;
(b) inelastic production of a pair of neutral pions in proton–proton interactions;
(c) the annihilation of an antiproton with a neutron to produce three pions.
1.7 Draw a lowest-order Feynman diagram for the following processes:
(a) e elastic scattering;
(b) n ! p þ e
þ 

e;
30 CH1 BASIC CONCEPTS
(c) eþ
e
! eþ
e
;
(d) a fourth-order diagram for the reaction  þ  ! eþ
þ e
.
1.8 Calculate the energy–momentum transfer between two particles equivalent to a
distance of approach of (a) 1fm and (b) 103
fm. Assuming that the intrinsic
strengths of the fundamental weak and electromagnetic interactions are approxi-
mately equal, compare the relative sizes of the invariant (scattering) amplitudes for
weak and electromagnetic processes at these two energy–momentum transfers.
1.9 Verify by explicit integration that fðqÞ ¼ g2

h2
½q2
þ m2
c2
1
is the amplitude
corresponding to the Yukawa potential
VðrÞ ¼ 
g2
4
er=R
r
;
where R ¼ 
h=mc is the range and r ¼ jxj.
1.10 Two beams of particles consisting of n bunches with Niði ¼ 1; 2Þ particles in each,
traverse circular paths and collide ‘head-on’. Show that in this case the general
expression Equation (1.45) for the luminosity reduces to L ¼ nN1N2f =A, where A is
the cross-sectional area of the beam and f is the frequency, i.e. f ¼ 1=T, where T is
the time taken for the particles to make one traversal of the ring.
1.11 A thin (density 1 mg cm2
) target of 24
Mg (MA ¼ 24:3 atomic mass units) is
bombarded with a 10 nA beam of alpha particles. A detector subtending a solid
angle of 2 103
sr, records 20 protons/s. If the scattering is isotropic, determine
the cross-section for the 24
Mgð; pÞ reaction.
PROBLEMS 31
2
Nuclear Phenomenology
In this chapter we start to examine some of the things that can be learned from
experiments, beginning with basic facts about nuclei, including what can be deduced
about their shapes and sizes. Then we discuss the important topic of nuclear stability
and the phenomenology of the various ways that unstable nuclei decay to stable
states. Finally, we briefly review the classification of reactions in nuclear physics.
Before that we need to introduce some notation.
2.1 Mass Spectroscopy and Binding Energies
Nuclei are specified by:
Z – atomic number ¼ the number of protons,
N – neutron number ¼ the number of neutrons,
A – mass number ¼ the number of nucleons, so that A ¼ Z þ N.
We will also refer to A as the nucleon number. The charge on the nucleus is
þZe, where e is the absolute value of the electric charge on the electron. Nuclei
with combinations of these three numbers are also called nuclides and are written
A
Y or A
ZY, where Y is the chemical symbol for the element. Some other common
nomenclature is:
nuclides with the same mass number are called isobars,
nuclides with the same atomic number are called isotopes,
nuclides with the same neutron number are called isotones.
Nuclear and Particle Physics B. R. Martin
# 2006 John Wiley  Sons, Ltd. ISBN: 0-470-01999-9
The concept of isotopes was introduced in Chapter 1. For example, stable isotopes
of carbon are 12
C and 13
C, and the unstable isotope used in dating ancient objects
(see later in this chapter) is 14
C; all three have Z ¼ 6.
Just as in the case of electrons in atoms, the forces that bind the nucleons in
nuclei contribute to the total mass of an atom M(Z, A) and in terms of the masses of
the proton Mp and neutron Mn
MðZ; AÞ  Z ðMp þ meÞ þ N Mn: ð2:1Þ
The mass deficit is defined as
MðZ; AÞ  MðZ; AÞ  Z ðMp þ meÞ  N Mn ð2:2Þ
and Mc2
is called the binding energy B. Binding energies may be calculated if
masses are measured accurately. One way of doing this is by using the techniques
of mass spectroscopy. The principle of the method is shown in Figure 2.1.
A source of ions of charge q, containing various isotopes passes through a region
where there are uniform electric (E) and magnetic (B1) fields at right angles. The
electric field will exert a force qE in one direction and the magnetic field will exert
a force qvB1 in the opposite direction, where v is the speed of the ions. By
balancing these forces, ions of a specific speed v ¼ E=B1 can be selected and
allowed to pass through a collimating slit. Ions with other velocities (shown as
dashed lines) are deflected. The beam is then allowed to continue through a second
Figure 2.1 Schematic diagram of a mass spectrometer (adapted from Kr88 Copyright John
Wiley  Sons, Inc.)
34 CH2 NUCLEAR PHENOMENOLOGY
uniform magnetic field B2 where it will be bent into a circular path of radius ,
given by
mv ¼ qB2 ð2:3Þ
and since q, B2 and v are fixed, particles with a fixed ratio q=m will bend in a path
with a unique radius. Hence isotopes may be separated and focused onto a detector
(e.g. a photographic plate). In the common case where B1 ¼ B2 ¼ B,
q
m
¼
E
B2
: ð2:4Þ
In practice, to achieve high accuracy, the device is used to measure mass
differences rather than absolute values of mass.1
Conventional mass spectroscopy cannot be used to find the masses of very short-
lived nuclei and in these cases the masses are determined from kinematic analysis
of nuclear reactions as follows. Consider the inelastic reaction Aða; aÞA
, where A
is the short-lived nucleus whose mass is to be determined. The kinematics of this
are:
aðEi; piÞ þ AðmAc2
; 0Þ ! aðEf ; pf Þ þ A
ð~
E
E; p
~Þ; ð2:5Þ
where we use tilded quantities to denote the energy, mass, etc. of A
. Equating the
total energy before the collision
EtotðinitialÞ ¼ Ei þ mac2
þ mAc2
ð2:6aÞ
to the total energy after the collision
EtotðfinalÞ ¼ Ef þ ~
E
E þ mac2
þ ~
m
m c2
ð2:6bÞ
gives the following expression for the change in energy of the nucleus:
E  ð~
m
m  mAÞc2
¼ Ei  Ef  ~
E
E ¼
p2
i
2ma

p2
f
2ma

~
p
p2
2~
m
m
; ð2:7Þ
where we have assumed non-relativistic kinematics. If the initial momentum of the
projectile is along the x-direction and the scattering angle is , then from
momentum conservation,
ð~
p
pÞx ¼ pi  pf cos  ; ð~
p
pÞy ¼ pf sin  ð2:8Þ
1
Practical details of mass spectroscopy may be found in, for example, Chapter 3 of Kr88.
MASS SPECTROSCOPY AND BINDING ENERGIES 35
and using these in Equation (2.7) gives
E ¼ Ei 1 
ma
~
m
m
 
 Ef 1 þ
ma
~
m
m
 
þ
2ma
~
m
m
EiEf
 1=2
cos : ð2:9Þ
This formula can be used iteratively to deduce E and hence the mass of the excited
nucleus A
, from measurements of the initial and final energy of the projectile by
initially setting ~
m
m ¼ mA on the right-hand side because E is small in comparison
with mA. One final point is that the energies in Equation (2.9) are measured in the
laboratory system, whereas the final energies (masses) will be needed in the centre-of-
mass system.2
The necessary transformation is easily found to be
ECM ¼ Elab 1 þ ma=mA
ð Þ1
: ð2:10Þ
A similar formula to Equation (2.9) may be derived for the general reaction
A(a,b)B:
E ¼ Ei 1 
ma
mB
 
 Ef 1 þ
mb
mB
 
þ
2
mB
mambEiEf
 1=2
cos  þ Q; ð2:11Þ
where Q is the kinetic energy released in the reaction.
A commonly used quantity of interest is the binding energy per nucleon B=A.
This is shown schematically in Figure 2.2 for nuclei that are stable or long-lived.
2
A discussion of these two systems is given in Appendix C.
Figure 2.2 Binding energy per nucleon as a function of mass number A for stable and long-
lived nuclei
36 CH2 NUCLEAR PHENOMENOLOGY
This shows that B=A peaks at a value of 8.7 MeV for a mass number of about 56
(close to iron) and thereafter falls very slowly. Excluding very light nuclei, the
binding energy per nucleon is between 7 and 9 MeV over a wide range of the
periodic table. In Section 2.5 we will discuss a model that provides an explanation
for the shape of this curve.
2.2 Nuclear Shapes and Sizes
The shape and size of a nucleus may be found from scattering experiments; i.e. a
projectile is scattered from the nucleus and the angular distribution of the scattered
particles examined, as was done by Rutherford and his collaborators when they
deduced the existence of the nucleus. The interpretation is simplest in those cases
where the projectile itself has no internal structure, i.e. it is an elementary particle,
and electrons are often used. In this case the relevant force is electromagnetic and we
learn about the charge distribution in the nucleus. The first experiments of this type
were performed by Hofstader and his collaborators in the late 1950s.3
If instead of an
electron a hadron is used as the projectile, the force is dominantly the nuclear strong
interaction and we find information about the matter density. Neutrons are com-
monly used so that Coulomb effects are absent. We discuss these two cases in turn.
2.2.1 Charge distribution
To find the amplitude for electron–nucleus scattering, we should in principle solve
the Schrödinger (or Dirac) equation using a Hamiltonian that includes the full
electromagnetic interaction and use nuclear wavefunctions. This can only be done
numerically. However, in Appendix C we derive a simple formula that describes the
electromagnetic scattering of a charged particle in the so-called Born approxima-
tion, which assumes Z 1 and uses plane waves for the initial and final states.
This leads to the Rutherford cross-section, which in its relativistic form may be
written
d
dO
 
Rutherford
¼
Z2
2
ð
hcÞ2
4E2 sin4
ð=2Þ
; ð2:12Þ
where E is the total initial energy of the projectile and  is the angle through which
it is scattered. Note that Equation (2.12) is of order 2
because it corresponds to
the exchange of a single photon. Although Equation (2.12) has a limited range of
applicability, it is useful to discuss the general features of electron scattering.
Equation (2.12) actually describes the scattering of a spin-0 point-like projectile of
unit charge from a fixed point-like target with electric charge Ze, i.e. the charge
3
Robert Hofstader shared the 1961 Nobel Prize in Physics for his pioneering electron scattering experiments.
NUCLEAR SHAPES AND SIZES 37
distribution of the target is neglected. It therefore needs to be modified in a number of
ways before it can be used in practice. We will state the modifications without proof.
Firstly, taking account of the electron spin leads to the so-called Mott cross-
section
d
dO
 
Mott
¼
d
dO
 
Rutherford
1  2
sin2
ð=2Þ
 
; ð2:13Þ
where ¼ v=c and v is the velocity of the initial electron. At higher energies, the
recoil of the target needs to be taken into account and this introduces a factor E0
=E
on the right-hand side of Equation (2.13), where E0
is the final energy of the
electron. At higher energies we also need to take account of the interaction with
the magnetic moment of the target in addition to its charge. The final form for the
differential cross-section is
d
dO
 
spin 1
2
¼
d
dO
 
Mott
E0
E
1 þ 2 tan2 
2
; ð2:14Þ
where
¼
q2
4M2c2
ð2:15Þ
and M is the target mass. Because the energy loss of the electron to the recoiling
nucleus is no longer negligible, q, the previous momentum transfer, has been
replaced by the four-momentum transfer q, whose square is
q2
¼ ðp  p0
Þ2
¼ 2m2
ec2
 2ðEE0
c2
 p
j j p0
j j cos Þ 
4EE0
c2
sin2
ð=2Þ; ð2:16Þ
where pð p0
Þ is the four-momentum of the initial (final) electron. (Because q2
0, it
is common practice to replace it with Q2
¼ q2
, so as to work with positive
quantities.4
) For the rest of this discussion it will be sufficient to ignore the magnetic
interaction, although we will use a variant of the full form (2.16) in Chapter 6.
The final modification is due to the spatial extension of the nucleus. If the spatial
charge distribution within the nucleus is written f (x) then we define the form factor
F(q2
) by
Fðq2
Þ 
1
Ze
ð
eiqx=
h
fðxÞ d3
x with Ze ¼
ð
fðxÞ d3
x; ð2:17Þ
4
To remove any confusion, in the non-relativistic case, which we use in the rest of this chapter, q is
interpreted to be q ¼ jqj  0 where q  p  p0
, as was used in Section 1.6.1. We will need the four-
momentum definition of q in Chapter 6.
38 CH2 NUCLEAR PHENOMENOLOGY
i.e. the Fourier transform of the charge distribution.5
In the case of a spherically
symmetric charge distribution, the angular integrations in Equations (2.17) may be
done using spherical polar coordinates to give
Fðq2
Þ ¼
4 
h
Zeq
ð
1
0
rðrÞsin
qr

h
 
dr; ð2:18Þ
where q ¼ jqj and ðrÞ is the radial charge distribution. The final form of the
experimental cross-section in this approximation is given by6
d
dO
 
expt
¼
d
dO
 
Mott
Fðq2
Þ
2
: ð2:19Þ
Two examples of measured cross-sections are shown in Figure 2.3. Striking
features are the presence of a number of well-defined minima superimposed on a
Figure 2.3 Elastic differential cross-sections as a function of the scattering angle for 450 MeV
electrons from 58
Ni and 758 MeV electrons from 48
Ca; the solid lines are fits as described in the
text (adapted from Si75 (58
Ni data) and Be67 (48
Ca data), Copyright American Physical Society)
5
Strictly this formula assumes that the recoil of the target nucleus is negligible and the interaction is
relatively weak, so that perturbation theory may be used.
6
If the magnetic interaction were included, another form factor would be necessary, as is the case in high-
energy electron scattering discussed in Chapter 6.
NUCLEAR SHAPES AND SIZES 39
Publisher's Note:
Permission to reproduce this image
online was not granted by the
copyright holder. Readers are kindly
requested to refer to the printed version
of this chapter.
rapid decrease in the cross-section with angle. These features are common to all
elastic data, although not all nuclei show so many minima as those shown.
The minima are due to the form factor and we can make this plausible by taking
the simple case where the nuclear charge distribution is represented by a hard
sphere such that
ðrÞ ¼ constant; r a
¼ 0 r  a
ð2:20Þ
where a is a constant. In this case, evaluation of Equation (2.18) gives
Fðq2
Þ ¼ 3 sinðbÞ  bcosðbÞ
½ b3
; ð2:21Þ
where b  qa=
h. Thus Fðq2
Þ will be zero at values of b for which b ¼ tanðbÞ. In
practice, as we will see below, ðrÞ is not a hard sphere, and although it is
approximately constant for much of the nuclear volume, it falls smoothly to zero at
the surface. Smoothing the edges of the radial charge distribution (2.20) modifies
the positions of the zeros, but does not alter the argument that the minima in the
cross-sections are due to the spatial distribution of the nucleus. Their actual
positions and depths result from a combination of the form factor and the form of
the point-like amplitude. We shall see below that the minima can tell us about the
size of the nucleus.
If one measures the cross-section for a fixed energy at various angles (and hence
various q2
), the form factor can in principle be extracted using Equation (2.19) and
one might attempt to find the charge distribution from the inverse Fourier
transform
fðxÞ ¼
Ze
ð2 Þ3
ð
Fðq2
Þ eiqx=
h
d3
q: ð2:22Þ
However, q2
only has a finite range for a fixed initial electron energy and even within
this range the rapid fall in the cross-section means that in practice measurements
cannot be made over a sufficiently wide range of angles for the integral in Equation
(2.22) to be evaluated accurately. Thus, even within the approximations used,
reliable charge distributions cannot be found from Equation (2.22). Therefore
different strategies must be used to deduce the charge distribution. In one approach,
plausible – but very general – parameterized forms (for example a sum of Gaussians)
are chosen for the charge distribution and are used to modify the point-like
electromagnetic interaction. The resulting Schrödinger (or Dirac) equation is solved
numerically to produce an amplitude, and hence a cross-section, for electron–
nucleus scattering. The parameters of the charge distribution are then varied to give
a good fit of the experimental data. The solid curves in Figure 2.3 are obtained in
this way.
40 CH2 NUCLEAR PHENOMENOLOGY
Some radial charge distributions for various nuclei obtained by these methods
are shown in Figure 2.4. They are well represented by the form
chðrÞ ¼
0
ch
1 þ eðraÞ=b
; ð2:23Þ
where a and b for medium and heavy nuclei are found to be
a 1:07A1=3
fm and b 0:54 fm: ð2:24Þ
From this we can deduce that the charge density is approximately constant in the
nuclear interior and falls fairly rapidly to zero at the nuclear surface, as anticipated
above. The value of 0
ch is in the range 0.06–0.08 for medium to heavy nuclei and
decreases slowly with increasing mass number.
Figure 2.4 Radial charge distributions ch of various nuclei, in units of e fm3
; the thickness
of the curves near r ¼ 0 is a measure of the uncertaintity in ch (adapted from Fr83)
NUCLEAR SHAPES AND SIZES 41
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Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf
Martin - Nuclear and Particle Physics - An Introduction.pdf

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Martin - Nuclear and Particle Physics - An Introduction.pdf

  • 1.
  • 2. Nuclear and Particle Physics Nuclear and Particle Physics B. R. Martin # 2006 John Wiley & Sons, Ltd. ISBN: 0-470-01999-9
  • 3. Nuclear and Particle Physics B. R. Martin Department of Physics and Astronomy, University College London
  • 4. Copyright # 2006 John Wiley & Sons Ltd, The Atrium, Southern Gate, Chichester, West Sussex PO19 8SQ, England Telephone (+44) 1243 779777 Email (for orders and customer service enquiries): cs-books@wiley.co.uk Visit our Home Page on www.wileyeurope.com or www.wiley.com All Rights Reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, scanning or otherwise, except under the terms of the Copyright, Designs and Patents Act 1988 or under the terms of a licence issued by the Copyright Licensing Agency Ltd, 90 Tottenham Court Road, London W1T 4LP, UK, without the permission in writing of the Publisher. Requests to the Publisher should be addressed to the Permissions Department, John Wiley & Sons Ltd, The Atrium, Southern Gate, Chichester, West Sussex PO19 8SQ, England, or emailed to permreq@wiley.co.uk, or faxed to (+44) 1243 770620. Designations used by companies to distinguish their products are often claimed as trademarks. All brand names and product names used in this book are trade names, service marks, trademarks or registered trademarks of their respective owners. The Publisher is not associated with any product or vendor mentioned in this book. This publication is designed to provide accurate and authoritative information in regard to the subject matter covered. It is sold on the understanding that the Publisher is not engaged in rendering professional services. If professional advice or other expert assistance is required, the services of a competent professional should be sought. Other Wiley Editorial Offices John Wiley & Sons Inc., 111 River Street, Hoboken, NJ 07030, USA Jossey-Bass, 989 Market Street, San Francisco, CA 94103-1741, USA Wiley-VCH Verlag GmbH, Boschstr. 12, D-69469 Weinheim, Germany John Wiley & Sons Australia Ltd, 42 McDougall Street, Milton, Queensland 4064, Australia John Wiley & Sons (Asia) Pte Ltd, 2 Clementi Loop # 02-01, Jin Xing Distripark, Singapore 129809 John Wiley & Sons Canada Ltd, 22 Worcester Road, Etobicoke, Ontario, Canada M9W 1L1 Wiley also publishes its books in a variety of electronic formats. Some content that appears in print may not be available in electronic books. Library of Congress Cataloging-in-Publication Data Martin, B. R. (Brian Robert) Nuclear and particle physics/B. R. Martin. p. cm. ISBN-13: 978-0-470-01999-3 (HB) ISBN-10: 0-470-01999-9 (HB) ISBN-13: 978-0-470-02532-1 (pbk.) ISBN-10: 0-470-02532-8 (pbk.) 1. Nuclear physics–Textbooks. 2. Particle physics–Textbooks. I. Title. QC776.M34 2006 539.70 2–dc22 2005036437 British Library Cataloguing in Publication Data A catalogue record for this book is available from the British Library ISBN-13 978-0 470 01999 9 (HB) ISBN-10 0 470 01999 9 (HB) 978-0 470 02532 8 (PB) 0 470 02532 8 (PB) Typeset in 10.5/12.5pt Times by Thomson Press (India) Limited, New Delhi Printed and bound in Great Britain by Antony Rowe Ltd., Chippenham, Wiltshire This book is printed on acid-free paper responsibly manufactured from sustainable forestry in which at least two trees are planted for each one used for paper production.
  • 6. Contents Preface xi Notes xiii Physical Constants and Conversion Factors xv 1 Basic Concepts 1 1.1 History 1 1.1.1 The origins of nuclear physics 1 1.1.2 The emergence of particle physics: the standard model and hadrons 4 1.2 Relativity and antiparticles 7 1.3 Symmetries and conservation laws 9 1.3.1 Parity 10 1.3.2 Charge conjugation 12 1.4 Interactions and Feynman diagrams 13 1.4.1 Interactions 13 1.4.2 Feynman diagrams 15 1.5 Particle exchange: forces and potentials 17 1.5.1 Range of forces 17 1.5.2 The Yukawa potential 19 1.6 Observable quantities: cross sections and decay rates 20 1.6.1 Amplitudes 21 1.6.2 Cross-sections 23 1.6.3 Unstable states 27 1.7 Units: length, mass and energy 29 Problems 30 2 Nuclear Phenomenology 33 2.1 Mass spectroscopy and binding energies 33 2.2 Nuclear shapes and sizes 37 2.2.1 Charge distribution 37 2.2.2 Matter distribution 42 2.3 Nuclear instability 45 2.4 Radioactive decay 47 2.5 Semi-empirical mass formula: the liquid drop model 50 2.6 -decay phenomenology 55 2.6.1 Odd-mass nuclei 55 2.6.2 Even-mass nuclei 58
  • 7. 2.7 Fission 59 2.8 -decays 62 2.9 Nuclear reactions 62 Problems 67 3 Particle Phenomenology 71 3.1 Leptons 71 3.1.1 Lepton multiplets and lepton numbers 71 3.1.2 Neutrinos 74 3.1.3 Neutrino mixing and oscillations 76 3.1.4 Neutrino masses 79 3.1.5 Universal lepton interactions – the number of neutrinos 84 3.2 Quarks 86 3.2.1 Evidence for quarks 86 3.2.2 Quark generations and quark numbers 89 3.3 Hadrons 92 3.3.1 Flavour independence and charge multiplets 92 3.3.2 Quark model spectroscopy 96 3.3.3 Hadron masses and magnetic moments 102 Problems 108 4 Experimental Methods 111 4.1 Overview 111 4.2 Accelerators and beams 113 4.2.1 DC accelerators 113 4.2.2 AC accelerators 115 4.2.3 Neutral and unstable particle beams 122 4.3 Particle interactions with matter 123 4.3.1 Short-range interactions with nuclei 123 4.3.2 Ionization energy losses 125 4.3.3 Radiation energy losses 128 4.3.4 Interactions of photons in matter 129 4.4 Particle detectors 131 4.4.1 Gas detectors 131 4.4.2 Scintillation counters 137 4.4.3 Semiconductor detectors 138 4.4.4 Particle identification 139 4.4.5 Calorimeters 142 4.5 Layered detectors 145 Problems 148 5 Quark Dynamics: the Strong Interaction 151 5.1 Colour 151 5.2 Quantum chromodynamics (QCD) 153 5.3 Heavy quark bound states 156 5.4 The strong coupling constant and asymptotic freedom 160 5.5 Jets and gluons 164 5.6 Colour counting 166 viii CONTENTS
  • 8. 5.7 Deep inelastic scattering and nucleon structure 168 Problems 177 6 Electroweak Interactions 181 6.1 Charged and neutral currents 181 6.2 Symmetries of the weak interaction 182 6.3 Spin structure of the weak interactions 186 6.3.1 Neutrinos 187 6.3.2 Particles with mass: chirality 189 6.4 W and Z0 bosons 192 6.5 Weak interactions of hadrons 194 6.5.1 Semileptonic decays 194 6.5.2 Neutrino scattering 198 6.6 Neutral meson decays 201 6.6.1 CP violation 202 6.6.2 Flavour oscillations 206 6.7 Neutral currents and the unified theory 208 Problems 213 7 Models and Theories of Nuclear Physics 217 7.1 The nucleon – nucleon potential 217 7.2 Fermi gas model 220 7.3 Shell model 223 7.3.1 Shell structure of atoms 223 7.3.2 Nuclear magic numbers 225 7.3.3 Spins, parities and magnetic dipole moments 228 7.3.4 Excited states 230 7.4 Non-spherical nuclei 232 7.4.1 Electric quadrupole moments 232 7.4.2 Collective model 236 7.5 Summary of nuclear structure models 236 7.6 -decay 238 7.7 -decay 242 7.7.1 Fermi theory 242 7.7.2 Electron momentum distribution 244 7.7.3 Kurie plots and the neutrino mass 246 7.8 -emission and internal conversion 248 7.8.1 Selection rules 248 7.8.2 Transition rates 250 Problems 252 8 Applications of Nuclear Physics 255 8.1 Fission 255 8.1.1 Induced fission – fissile materials 255 8.1.2 Fission chain reactions 258 8.1.3 Nuclear power reactors 260 8.2 Fusion 266 8.2.1 Coulomb barrier 266 CONTENTS ix
  • 9. 8.2.2 Stellar fusion 267 8.2.3 Fusion reaction rates 270 8.2.4 Fusion reactors 273 8.3 Biomedical applications 278 8.3.1 Biological effects of radiation: radiation therapy 278 8.3.2 Medical imaging using radiation 282 8.3.3 Magnetic resonance imaging 290 Problems 294 9 Outstanding Questions and Future Prospects 297 9.1 Particle physics 297 9.1.1 The Higgs boson 297 9.1.2 Grand unification 300 9.1.3 Supersymmetry 304 9.1.4 Particle astrophysics 307 9.2 Nuclear physics 315 9.2.1 The structure of hadrons and nuclei 316 9.2.2 Quark–gluon plasma, astrophysics and cosmology 320 9.2.3 Symmetries and the standard model 323 9.2.4 Nuclear medicine 324 9.2.5 Power production and nuclear waste 326 Appendix A: Some Results in Quantum Mechanics 331 A.1 Barrier penetration 331 A.2 Density of states 333 A.3 Perturbation theory and the Second Golden Rule 335 Appendix B: Relativistic Kinematics 339 B.1 Lorentz transformations and four-vectors 339 B.2 Frames of reference 341 B.3 Invariants 344 Problems 345 Appendix C: Rutherford Scattering 349 C.1 Classical physics 349 C.2 Quantum mechanics 352 Problems 354 Appendix D: Solutions to Problems 355 References 393 Bibliography 397 Index 401 x CONTENTS
  • 10. Preface It is common practice to teach nuclear physics and particle physics together in an introductory course and it is for such a course that this book has been written. The material is presented so that different selections can be made for a short course of about 25–30 lectures depending on the lecturer’s preferences and the students’ backgrounds. On the latter, students should have taken a first course in quantum physics, covering the traditional topics in non-relativistic quantum mechanics and atomic physics. A few lectures on relativistic kinematics would also be useful, but this is not essential as the necessary background is given in appendix B and is only used in a few places in the book. I have not tried to be rigorous, or present proofs of all the statements in the text. Rather, I have taken the view that it is more important that students see an overview of the subject which for many – possibly the majority – will be the only time they study nuclear and particle physics. For future specialists, the details will form part of more advanced courses. Never- theless, space restrictions have still meant that it has been necessary to make a choice of topics covered and doubtless other, equally valid, choices could have been made. This is particularly true in Chapter 8, which deals with applications of nuclear physics, where I have chosen just three major areas to discuss. Nuclear and particle physics have been, and still are, very important parts of the entire subject of physics and its practitioners have won an impressive number of Nobel Prizes. For historical interest, I have noted in the footnotes many of the awards for work related to the field. Some parts of the book dealing with particle physics owe much to a previous book, Particle Physics, written with Graham Shaw of Manchester University, and I am grateful to him and the publisher, John Wiley and Sons, for permission to adapt some ofthatmaterialforusehere.IalsothankColinWilkinforcommentsonallthechapters of the book, David Miller and Peter Hobson for comments on Chapter 4 and Bob Speller for comments on the medical physics section of Chapter 8. If errors or misunderstandingsstillremain(andanysuchareofcourseduetomealone)Iwouldbe grateful to hear about them. I have set up a website (www.hep.ucl.ac.uk/brm/ npbook.html) where I will post any corrections and comments. Brian R. Martin January 2006
  • 11. Notes References References are referred to in the text in the form Ab95, where Ab is the start of the first author’s surname and 1995 is the year of publication. A list of references with full publication details is given at the end of the book. Data Data for particle physics may be obtained from the biannual publications of the Particle Data Group (PDG) and the 2004 edition of the PDG definitive Review of Particle Properties is given in Ei04. The PDG Review is also available at http://pdg.lbl.gov and this site contains links to other sites where compilations of particle data may be found. Nuclear physics data are available from a number of sources. Examples are: the combined Isotopes Project of the Lawrence Berkeley Laboratory, USA, and the Lund University Nuclear Data WWW Service, Sweden (http://ie.lbl.gov/toi.html), the National Nuclear Data Center (NNDC) based at Brookhaven National Laboratory, USA (http://www.nndc.bnl.gov), and the Nuclear Data Centre of the Japan Atomic Energy Research Institute (http://www.nndc.tokai.jaeri.go.jp). All three sites have extensive links to other data compilations. It is important that students have some familiarity with these data compilations. Problems Problems are provided for all chapters and appendices except Chapter 9 and Appendices A and D. They are an integral part of the text. The problems are mainly numerical and require values of physical constants that are given in a table following these notes. A few also require input data that may be found in the references given above. Solutions to all the problems are given in Appendix D.
  • 12. Illustrations Some illustrations in the text have been adapted from, or are loosely based on, diagrams that have been published elsewhere. In a few cases they have been reproduced exactly as previously published. In all cases this is stated in the captions. I acknowledge, with thanks, permission to use such illustrations from the relevant copyright holders. xiv NOTES
  • 13. Physical Constants and Conversion Factors Quantity Symbol Value Speed of light in vacuum c 2:998 108 ms1 Planck’s constant h 4:136 1024 GeV s h h=2 6:582 1025 GeV s hc 1:973 1016 GeV m ð hcÞ2 3:894 1031 GeV2 m2 electron charge (magnitude) e 1:602 1019 C Avogadro’s number NA 6:022 1026 kg-mole1 Boltzmann’s constant kB 8:617 1011 MeV K1 electron mass me 0:511 MeV=c2 proton mass mp 0:9383 GeV=c2 neutron mass mn 0:9396 GeV=c2 W boson mass MW 80:43 GeV=c2 Z boson mass MZ 91:19 GeV=c2 atomic mass unit u ð 1 12 mass12 C atomÞ 931:494 MeV=c2 Bohr magneton B e h=2me 5:788 1011 MeV T1 Nuclear magneton N e h=2mp 3:152 1014 MeV T1 gravitational constant GN 6:709 1039 hcðGeV=c2 Þ2 fine structure constant e2 =40 hc 7:297 103 ¼ 1=137:04 Fermi coupling constant GF=ð hcÞ3 1:166 105 GeV2 strong coupling constant sðMZc2 Þ 0.119 1 eV ¼ 1:602 1019 J 1 eV=c2 ¼ 1:783 1036 kg 1 fermi ¼ 1 fm 1015 m 1 barn ¼ 1 b 1028 m2 1 Tesla ¼ 1T ¼ 0:561 1030 MeV=c2 C1 s1 1 year ¼ 3:1536 107 s
  • 14. 1 Basic Concepts 1.1 History Although this book will not follow a strictly historical development, to ‘set the scene’ this first chapter will start with a brief review of the most important discoveries that led to the separation of nuclear physics from atomic physics as a subject in its own right and later work that in its turn led to the emergence of particle physics from nuclear physics.1 1.1.1 The origins of nuclear physics Nuclear physics as a subject distinct from atomic physics could be said to date from 1896, the year that Henri Becquerel observed that photographic plates were being fogged by an unknown radiation emanating from uranium ores. He had accidentally discovered radioactivity: the fact that some nuclei are unstable and spontaneously decay. In the years that followed, the phenomenon was extensively investigated, notably by the husband and wife team of Pierre and Marie Curie and by Ernest Rutherford and his collaborators,2 and it was established that there were three distinct types of radiation involved: these were named (by Rutherford) -, - and -rays. We know now that -rays are bound states of two protons and two neutrons (we will see later that they are the nuclei of helium atoms), -rays are electrons and -rays are photons, the quanta of electromagnetic radiation, but the historical names are still commonly used. 1 An interesting account of the early period, with descriptions of the personalities involved, is given in Se80. An overview of the later period is given in Chapter 1 of Gr87. 2 The 1903 Nobel Prize in Physics was awarded jointly to Becquerel for his discovery and to Pierre and Marie Curie for their subsequent research into radioactivity. Rutherford had to wait until 1908, when he was awarded the Nobel Prize in Chemistry for his ‘investigations into the disintegration of the elements and the chemistry of radioactive substances’. Nuclear and Particle Physics B. R. Martin # 2006 John Wiley Sons, Ltd. ISBN: 0-470-01999-9
  • 15. At about the same time as Becquerel’s discovery, J. J. Thomson was extending the work of Perrin and others on the radiation that had been observed to occur when an electric field was established between electrodes in an evacuated glass tube, and in 1897 he was the first to definitively establish the nature of these ‘cathode rays’. We now know the emanation consists of free electrons, (the name ‘electron’ had been coined in 1894 by Stoney) denoted e (the superscript denotes the electric charge) and Thomson measured their mass and charge.3 The view of the atom at that time was that it consisted of two components, with positive and negative electric charges, the latter now being the electrons. Thomson suggested a model where the electrons were embedded and free to move in a region of positive charge filling the entire volume of the atom – the so-called ‘plum pudding model’. This model could account for the stability of atoms, but could not account for the discrete wavelengths observed in the spectra of light emitted from excited atoms. Neither could it explain the results of a classic series of experiments performed in 1911 at the suggestion of Rutherford by his collaborators, Geiger and Marsden. These consisted of scattering -particles by very thin gold foils. In the Thomson model, most of the -particles would pass through the foil, with only a few suffering deflections through small angles. Rutherford suggested they should look for large-angle scattering and to their surprise they found that some particles were indeed scattered through very large angles, even greater than 90 . Rutherford showed that this behaviour was not due to multiple small-angle deflections, but could only be the result of the -particles encountering a very small positively charged central nucleus. (The reason for these two different behaviours is discussed in Appendix C.) To explain the results of these experiments Rutherford formulated a ‘planetary’ model, where the atom was likened to a planetary system, with the electrons (the ‘planets’) occupying discrete orbits about a central positively charged nucleus (the ‘Sun’). Because photons of a definite energy would be emitted when electrons moved from one orbit to another, this model could explain the discrete nature of the observed electromagnetic spectra when excited atoms decayed. In the simplest case of hydrogen, the nucleus is a single proton (p) with electric charge þe, where e is the magnitude of the charge on the electron4 , orbited by a single electron. Heavier atoms were considered to have nuclei consisting of several protons. This view persisted for a long time and was supported by the fact that the masses of many naturally occurring elements are integer multiples of a unit that is about 1 per cent smaller than the mass of the hydrogen atom. Examples are carbon and nitrogen, with masses of 12.0 and 14.0 in these units. However, it could not explain why not all atoms obeyed this rule. For example, chlorine has a mass of 35.5 in these 3 J. J. Thomson received the 1906 Nobel Prize in Physics for his discovery. A year earlier, Philipp von Lenard had received the Physics Prize for his work on cathode rays. 4 Why the charge on the proton should have exactly the same magnitude as that on the electron is a very long- standing puzzle, the solution to which is suggested by some as yet unproven, but widely believed, theories of particle physics that will be discussed briefly in Chapter 9. 2 CH1 BASIC CONCEPTS
  • 16. units. At about the same time, the concept of isotopism (a name coined by Soddy) was conceived. Isotopes are atoms whose nuclei have different masses, but the same charge. Naturally occurring elements were postulated to consist of a mixture of different isotopes, giving rise to the observed masses.5 The explanation of isotopes had to wait 20 years until a classic discovery by Chadwick in 1932. His work followed earlier experiments by Irène Curie (the daughter of Pierre and Marie Curie) and her husband Frédéric Joliot.6 They had observed that neutral radiation was emitted when -particles bombarded beryllium and later work had studied the energy of protons emitted when paraffin was exposed to this neutral radiation. Chadwick refined and extended these experi- ments and demonstrated that they implied the existence of an electrically neutral particle of approximately the same mass as the proton. He had discovered the neutron (n) and in so doing had produced almost the final ingredient for under- standing nuclei.7 There remained the problem of reconciling the planetary model with the observation of stable atoms. In classical physics, the electrons in the planetary model would be constantly accelerating and would therefore lose energy by radiation, leading to the collapse of the atom. This problem was solved by Bohr in 1913. He applied the newly emerging quantum theory and the result was the now well-known Bohr model of the atom. Refined modern versions of this model, including relativistic effects described by the Dirac equation (the relativistic analogue of the Schrödinger equation that applies to electrons), are capable of explaining the phenomena of atomic physics. Later workers, including Heisenberg, another of the founders of quantum theory,8 applied quantum mechanics to the nucleus, now viewed as a collection of neutrons and protons, collectively called nucleons. In this case, however, the force binding the nucleus is not the electromagnetic force that holds electrons in their orbits, but is a short-range9 force whose magnitude is independent of the type of nucleon, proton or neutron (i.e. charge-independent). This binding interaction is called the strong nuclear force. These ideas still form the essential framework of our understanding of the nucleus today, where nuclei are bound states of nucleons held together by a strong charge-independent short-range force. Nevertheless, there is still no single theory that is capable of explaining all the data of nuclear physics and we shall see that different models are used to interpret different classes of phenomena. 5 Frederick Soddy was awarded the 1921 Nobel Prize in Chemistry for his work on isotopes. 6 Irène Curie and Frédéric Joliot received the 1935 Nobel Prize in Chemistry for ‘synthesizing new radioactive elements’. 7 James Chadwick received the 1935 Nobel Prize in Physics for his discovery of the neutron. 8 Werner Heisenberg received the 1932 Nobel Prize in Physics for his contributions to the creation of quantum mechanics and the idea of isospin symmetry, which we will discuss in Chapter 3. 9 The concept of range will be discussed in more detail in Section 1.5.1, but for the present it may be taken as the effective distance beyond which the force is insignificant. HISTORY 3
  • 17. 1.1.2 The emergence of particle physics: the standard model and hadrons By the early 1930s, the 19th century view of atoms as indivisible elementary particles had been replaced and a larger group of physically smaller entities now enjoyed this status: electrons, protons and neutrons. To these we must add two electrically neutral particles: the photon () and the neutrino (). The photon was postulated by Planck in 1900 to explain black-body radiation, where the classical description of electromagnetic radiation led to results incompatible with experi- ments.10 The neutrino was postulated by Fermi in 1930 to explain the apparent non-conservation of energy observed in the decay products of some unstable nuclei where -rays are emitted, the so-called -decays. Prior to Fermi’s suggestion, -decay had been viewed as a parent nucleus decaying to a daughter nucleus and an electron. As this would be a two-body decay, it would imply that the electron would have a unique momentum, whereas experiments showed that the electron actually had a momentum spectrum. Fermi’s hypothesis of a third particle (the neutrino) in the final state solved this problem, as well as a problem with angular momentum conservation, which was apparently also violated if the decay was two- body. The -decay data implied that the neutrino mass was very small and was compatible with the neutrino being massless.11 It took more than 25 years before Fermi’s hypothesis was confirmed by Reines and Cowan in a classic experiment in 1956 that detected free neutrinos from -decay.12 The 1950s also saw technological developments that enabled high-energy beams of particles to be produced in laboratories. As a consequence, a wide range of controlled scattering experiments could be performed and the greater use of computers meant that sophisticated analysis techniques could be devel- oped to handle the huge quantities of data that were being produced. By the 1960s this had resulted in the discovery of a very large number of unstable particles with very short lifetimes and there was an urgent need for a theory that could make sense of all these states. This emerged in the mid 1960s in the form of the so-called quark model, first suggested by Murray Gell-Mann and independently and simultaneously by George Zweig, who postulated that the new particles were bound states of three families of more fundamental physical particles. 10 X-rays had already been observed by Röntgen in 1895 (for which he received the first Nobel Prize in Physics in 1901) and -rays were seen by Villard in 1900, but it was Planck who first made the startling suggestion that electromagnetic energy was quantized. For this he was awarded the 1918 Nobel Prize in Physics. Many years later, he said that his hypothesis was an ‘act of desperation’ as he had exhausted all other possibilities. 11 However, in Section 3.1.4 we will discuss recent evidence that neutrinos have very small, but non-zero, masses. 12 A description of this experiment is given in Chapter 12 of Tr75. Frederick Reines shared the 1995 Nobel Prize in Physics for his work in neutrino physics and particularly for the detection of the electron neutrino. 4 CH1 BASIC CONCEPTS
  • 18. Gell-Mann called these quarks (q).13 Because no free quarks were detected experimentally, there was initially considerable scepticism for this view. We now know that there is a fundamental reason why quarks cannot be observed as free particles (it will be discussed in Chapter 5), but at the time many physicists looked upon quarks as a convenient mathematical description, rather than physical particles.14 However, evidence for the existence of quarks as real particles came in the 1960s from a series of experiments analogous to those of Rutherford and his co-workers, where high-energy beams of electrons and neutrinos were scattered from nucleons. (These experiments will also be discussed in Chapter 5.) Analysis of the angular distributions of the scattered particles showed that the nucleons were themselves bound states of three point-like charged entities, with properties consistent with those hypothesized in the quark model. One of these properties was unexpected and unusual: quarks have fractional electric charges, in practice 1 3 e and þ 2 3 e. This is essentially the picture today, where elementary particles are now considered to be a small number of physical entities, including quarks, the electron, neutrinos, the photon and a few others we shall meet, but no longer nucleons. The best theory of elementary particles we have at present is called, rather prosaically, the standard model. This aims to explain all the phenomena of particle physics, except those due to gravity, in terms of the properties and interactions of a small number of elementary (or fundamental) particles, which are now defined as being point-like, without internal structure or excited states. Particle physics thus differs from nuclear physics in having a single theory to interpret its data. An elementary particle is characterized by, amongst other things, its mass, its electric charge and its spin. The latter is a permanent angular momentum possessed by all particles in quantum theory, even when they are at rest. Spin has no classical analogue and is not to be confused with the use of the same word in classical physics, where it usually refers to the (orbital) angular momentum of extended objects. The maximum value of the spin angular momentum about any axis is s hð h h=2Þ, where h is Planck’s constant and s is the spin quantum number, or spin for short. It has a fixed value for particles of any given type (for example s ¼ 1 2 for electrons) and general quantum mechanical principles restrict the possible values of s to be 0, 1 2, 1, 3 2, . . .. Particles with half-integer spin are called fermions and those with integer spin are called bosons. There are three families of elementary particles in the standard model: two spin-1 2 families of fermions called leptons and quarks; and one family of spin-1 bosons. In addition, 13 Gell-Mann received the 1969 Nobel Prize in Physics for ‘contributions and discoveries concerning the classification of elementary particles and their interactions’. For the origin of the word ‘quark’, he cited the now famous quotation ‘Three quarks for Muster Mark’ from James Joyce’s book Finnegans Wake. Zweig had suggested the name ‘aces’, which with hindsight might have been more appropriate, as later experiments revealed that there were four and not three families of quarks. 14 This was history repeating itself. In the early days of the atomic model many very distinguished scientists were reluctant to accept that atoms existed, because they could not be ‘seen’ in a conventional sense. HISTORY 5
  • 19. at least one other spin-0 particle, called the Higgs boson, is postulated to explain the origin of mass within the theory.15 The most familiar elementary particle is the electron, which we know is bound in atoms by the electromagnetic interaction, one of the four forces of nature.16 One test of the elementarity of the electron is the size of its magnetic moment. A charged particle with spin necessarily has an intrinsic magnetic moment l. It can be shown from the Dirac equation that a point-like spin-1 2 particle of charge q and mass m has a magnetic moment l ¼ ðq=mÞS, where S is its spin vector, and hence l has magnitude ¼ q h=2m. The magnetic moment of the electron very accurately obeys this relation, confirming that electrons are elementary. The electron is a member of the family of leptons. Another is the neutrino, which was mentioned earlier as a decay product in -decays. Strictly speaking, this particle should be called the electron neutrino, written e, because it is always produced in association with an electron (the reason for this is discussed in Section 3.1.1). The force responsible for -decay is an example of a second fundamental force, the weak interaction. Finally, there is the third force, the (fundamental) strong interaction, which, for example, binds quarks in nucleons. The strong nuclear force mentioned in Section 1.1.1 is not the same as this fundamental strong interaction, but is a consequence of it. The relation between the two will be discussed in more detail later. The standard model also specifies the origin of these three forces. In classical physics the electromagnetic interaction is propagated by electromagnetic waves, which are continuously emitted and absorbed. While this is an adequate descrip- tion at long distances, at short distances the quantum nature of the interaction must be taken into account. In quantum theory, the interaction is transmitted discon- tinuously by the exchange of photons, which are members of the family of fundamental spin-1 bosons of the standard model. Photons are referred to as the gauge bosons, or ‘force carriers’, of the electromagnetic interaction. The use of the word ‘gauge’ refers to the fact that the electromagnetic interaction possesses a fundamental symmetry called gauge invariance. For example, Maxwell’s equa- tions of classical electromagnetism are invariant under a specific phase transfor- mation of the electromagnetic fields – the gauge transformation.17 This property is common to all the three interactions of nature we will be discussing and has profound consequences, but we will not need its details in this book. The weak and strong interactions are also mediated by the exchange of spin-1 gauge bosons. For the weak interaction these are the Wþ , W and Z0 bosons (again the superscripts denote the electric charges) with masses about 80–90 times the mass of the proton. 15 In the theory without the Higgs boson, all elementary particles are predicted to have zero mass, in obvious contradiction with experiment. A solution to this problem involving the Higgs boson will be discussed briefly in Chapter 9. 16 Gravity is so weak that it can be neglected in nuclear and particle physics at presently accessible energies. Because of this, we will often refer in practice to the three forces of nature. 17 See, for example, Appendix C.2 of Ma97. 6 CH1 BASIC CONCEPTS
  • 20. For the strong interaction, the force carriers are called gluons. There are eight gluons, all of which have zero mass and are electrically neutral.18 In addition to the elementary particles of the standard model, there are other important particles we will be studying. These are the hadrons, the bound states of quarks. Nucleons are examples of hadrons,19 but there are several hundred more, not including nuclei, most of which are unstable and decay by one of the three interactions. It was the abundance of these states that drove the search for a simplifying theory that would give an explanation for their existence and led to the quark model in the 1960s. The most common unstable example of a hadron is the pion, which exists in three electrical charge states, written ðþ ; 0 ; Þ. Hadrons are important because free quarks are unobservable in nature and so to deduce their properties we are forced to study hadrons. An analogy would be if we had to deduce the properties of nucleons by exclusively studying the properties of nuclei. Since nucleons are bound states of quarks and nuclei are bound states of nucleons, the properties of nuclei should, in principle, be deducible from the properties of quarks and their interactions, i.e. from the standard model. In practice, however, this is far beyond present calculational techniques and some- times nuclear and particle physics are treated as two almost separate subjects. However, there are many connections between them and in introductory treatments it is still useful to present both subjects together. The remaining sections of this chapter are devoted to introducing some of the basic theoretical tools needed to describe the phenomena of both nuclear and particle physics, starting with a key concept: antiparticles. 1.2 Relativity and Antiparticles Elementary particle physics is also called high-energy physics. One reason for this is that if we wish to produce new particles in a collision between two other particles, then because of the relativistic mass–energy relation E ¼ mc2 , energies are needed at least as great as the rest masses of the particles produced. The second reason is that to explore the structure of a particle requires a probe whose wavelength is smaller than the structure to be explored. By the de Broglie relation ¼ h=p, this implies that the momentum p of the probing particle, and hence its energy, must be large. For example, to explore the internal structure of the proton using electrons requires wavelengths that are much smaller than the 18 Note that the word ‘electric’ has been used when talking about charge. This is because the weak and strong interactions also have associated ‘charges’ which determine the strengths of the interactions, just as the electric charge determines the strength of the electromagnetic interaction. This will be discussed in more detail in later chapters. 19 The magnetic moments of the proton and neutron do not obey the prediction of the Dirac equation and this is evidence that nucleons have structure and are not elementary. The proton magnetic moment was first measured by Otto Stern using a molecular beam method that he developed and for this he received the 1943 Nobel Prize in Physics. RELATIVITY AND ANTIPARTICLES 7
  • 21. classical radius of the proton, which is roughly 1015 m. This in turn requires electron energies that are greater than 103 times the rest energy of the electron, implying electron velocities very close to the speed of light. Hence any explanation of the phenomena of elementary particle physics must take account of the requirements of the theory of special relativity, in addition to those of quantum theory. There are very few places in particle physics where a non-relativistic treatment is adequate, whereas the need for a relativistic treatment is far less in nuclear physics. Constructing a quantum theory that is consistent with special relativity leads to the conclusion that for every particle of nature, there must exist an associated particle, called an antiparticle, with the same mass as the corresponding particle. This important theoretical prediction was first made by Dirac and follows from the solutions of the equation he first wrote down to describe relativistic electrons.20 The Dirac equation is of the form i h @Cðx; tÞ @t ¼ Hðx; ^ p pÞCðx; tÞ; ð1:1Þ where ^ p p ¼ i hr is the usual quantum mechanical momentum operator and the Hamiltonian was postulated by Dirac to be H ¼ ca ^ p p þ mc2 : ð1:2Þ The coefficients a and are determined by the requirement that the solutions of Equation (1.1) are also solutions of the Klein–Gordon equation 21 h2 @2 Cðx; tÞ @t2 ¼ h2 c2 r2 Cðx; tÞ þ m2 c4 Cðx; tÞ: ð1:3Þ This leads to the conclusion that a and cannot be simple numbers; their simplest forms are 4 4 matrices. Thus the solutions of the Dirac equation are four- component wavefunctions (called spinors) with the form22 Cðx; tÞ ¼ C1ðx; tÞ C2ðx; tÞ C3ðx; tÞ C4ðx; tÞ 0 B B @ 1 C C A: ð1:4Þ 20 Paul Dirac shared the 1933 Nobel Prize in Physics with Erwin Schrödinger. The somewhat cryptic citation stated ‘for the discovery of new productive forms of atomic theory’. 21 This is a relativistic equation, which is ‘derived’ by starting from the relativistic mass–energy relation E2 ¼ p2 c2 þ m2 c4 and using the usual quantum mechanical operator substitutions, ^ p p ¼ i hr and E ¼ i h@=@t. 22 The details may be found in most quantum mechanics books, for example, pp. 475–477 of Sc68. 8 CH1 BASIC CONCEPTS
  • 22. The interpretation of Equation (1.4) is that the four components describe the two spin states of a negatively charged electron with positive energy and the two spin states of a corresponding particle having the same mass but with negative energy. Two spin states arise because in quantum mechanics the projection in any direction of the spin vector of a spin-1 2 particle can only result in one of the two values 1 2, called ‘spin up’ and ‘spin down’, respectively. The two energy solutions arise from the two solutions of the relativistic mass–energy relation E ¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi p2c2 þ m2c4 p . The latter states can be shown to behave in all respects as positively charged electrons (called positrons), but with positive energy. The positron is referred to as the antiparticle of the electron. The discovery of the positron by Anderson in 1933, with all the predicted properties, was a spectacular verification of the Dirac prediction. Although Dirac originally made his prediction for electrons, the result is general and is true whether the particle is an elementary particle or a hadron. If we denote a particle by P, then the antiparticle is in general written with a bar over it, i.e. P P. For example, the antiparticle of the proton is the antiproton p p,23 with negative electric charge; and associated with every quark, q, is an antiquark, q q. However, for some very common particles the bar is usually omitted. Thus, for example, in the case of the positron eþ , the superscript denoting the charge makes explicit the fact that the antiparticle has the opposite electric charge to that of its associated particle. Electric charge is just one example of a quantum number (spin is another) that characterizes a particle, whether it is elementary or composite (i.e. a hadron). Many quantum numbers differ in sign for particle and antiparticle, and electric charge is an example of this. We will meet others later. When brought together, particle–antiparticle pairs, each of mass m, can annihilate, releasing their com- bined rest energy 2mc2 as photons or other particles. Finally, we note that there is symmetry between particles and antiparticles, and it is a convention to call the electron the particle and the positron its antiparticle. This reflects the fact that the normal matter contains electrons rather than positrons. 1.3 Symmetries and Conservation Laws Symmetries and the invariance properties of the underlying interactions play an important role in physics. Some lead to conservation laws that are universal. Familiar examples are translational invariance, leading to the conservation of linear momentum; and rotational invariance, leading to conservation of angular momentum. The latter plays an important role in nuclear and particle physics as it leads to a scheme for the classification of states based, among other quantum 23 Carl Anderson shared the 1936 Nobel Prize in Physics for the discovery of the positron. The 1958 Prize was awarded to Emilio Segrè and Owen Chamberlain for their discovery of the antiproton. SYMMETRIES AND CONSERVATION LAWS 9
  • 23. numbers, on their spins.24 Another very important invariance that we have briefly mentioned is gauge invariance. This fundamental property of all three interactions restricts the forms of the interactions in a profound way that initially is contra- dicted by experiment. This is the prediction of zero masses for all elementary particles, mentioned earlier. There are theoretical solutions to this problem whose experimental verification (or otherwise) is probably the most eagerly awaited result in particle physics today. In nuclear and particle physics we need to consider additional symmetries of the Hamiltonian and the conservation laws that follow and in the remainder of this section we discuss two of the most important of these that we will need later – parity and charge conjugation. 1.3.1 Parity Parity was first introduced in the context of atomic physics by Eugene Wigner in 1927.25 It refers to the behaviour of a state under a spatial reflection, i.e. x ! x. If we consider a single-particle state, represented for simplicity by a non- relativistic wavefunction ðx; tÞ, then under the parity operator, ^ P P, ^ P P ðx; tÞ P ðx; tÞ: ð1:5Þ Applying the operator again, gives ^ P P 2 ðx; tÞ ¼ P^ P P ðx; tÞ ¼ P2 ðx; tÞ; ð1:6Þ implying P ¼ 1. If the particle is an eigenfunction of linear momentum p, i.e. ðx; tÞ pðx; tÞ ¼ exp½iðp x EtÞ; ð1:7Þ then ^ P P pðx; tÞ ¼ P pðx; tÞ ¼ P pðx; tÞ ð1:8Þ and so a particle at rest, with p ¼ 0, is an eigenstate of parity. The eigenvalue P ¼ 1 is called the intrinsic parity, or just the parity, of the state. By considering a multiparticle state with a wavefunction that is the product of single-particle wavefunctions, it is clear that parity is a multiplicative quantum number. The strong and electromagnetic interactions, but not the weak interactions, are invariant under parity, i.e. the Hamiltonian of the system remains unchanged under 24 These points are explored in more detail in, for example, Chapter 4 of Ma97. 25 Eugene Wigner shared the 1963 Nobel Prize in Physics, principally for his work on symmetries. 10 CH1 BASIC CONCEPTS
  • 24. a parity transformation on the position vectors of all particles in the system. Parity is therefore conserved, by which we mean that the total parity quantum number remains unchanged in the interaction. Compelling evidence for parity conservation in the strong and electromagnetic interactions comes from the absence of transitions between nuclear states and atomic states, respectively, that would violate parity conservation. The evidence for non-conservation of parity in the weak interaction will be discussed in detail in Chapter 6. There is also a contribution to the total parity if the particle has an orbital angular momentum l. In this case its wave function is a product of a radial part Rnl and an angular part Ym l ð ; Þ: lmnðxÞ ¼ RnlYm l ð ; Þ; ð1:9Þ where n and m are the principal and magnetic quantum numbers and Ym l ð ; Þ is a spherical harmonic. It is straightforward to show from the relations between Cartesian ðx; y; zÞ and spherical polar co-ordinates ðr; ; Þ, i.e. x ¼ r sin cos ; y ¼ r sin sin ; z ¼ r cos ; ð1:10Þ that the parity transformation x ! x implies r ! r; ! ; ! þ ; ð1:11Þ and from this it can be shown that Ym l ð ; Þ ! Ym l ð ; þ Þ ¼ ðÞl Ym l ð ; Þ: ð1:12Þ Equation (1.12) may easily be verified directly for specific cases; for example, for the first three spherical harmonics, Y0 0 ¼ 1 4 1 2 ; Y0 1 ¼ 3 4 1 2 cos ; Y 1 1 ¼ 3 8 1 2 sin e i : ð1:13Þ Hence ^ P P lmnðxÞ ¼ P lmnðxÞ ¼ PðÞl lmnðxÞ; ð1:14Þ i.e. lmnðxÞ is an eigenstate of parity with eigenvalue Pð1Þl . An analysis of the Dirac Equation (1.1) for relativistic electrons, shows that it is invariant under a parity transformation only if Pðeþ e Þ ¼ 1. This is a general result for all fermion–antifermion pairs, so it is a convention to assign P ¼ þ1 to all leptons and P ¼ 1 to their antiparticles. We will see in Chapter 3 that in strong interactions quarks can only be created as part of a quark–antiquark pair, so the intrinsic parity of a single quark cannot be measured. For this reason, it is also SYMMETRIES AND CONSERVATION LAWS 11
  • 25. a convention to assign P ¼ þ1 to quarks. Since quarks are fermions, it follows from the Dirac result that P ¼ 1 for antiquarks. The intrinsic parities of hadrons then follow from their structure in terms of quarks and the orbital angular momentum between the constituent quarks, using Equation (1.14). This will be explored in Chapter 3 as part of the discussion of the quark model. 1.3.2 Charge conjugation Charge conjugation is the operation of changing a particle into its antiparticle. Like parity, it gives rise to a multiplicative quantum number that is conserved in strong and electromagnetic interactions, but violated in the weak interaction. In discussing charge conjugation, we will need to distinguish between states such as the photon and the neutral pion 0 that do not have distinct antiparticles and those such as the þ and the neutron, which do. Particles in the former class we will collectively denote by a and those of the latter type will be denoted by b. It is also convenient at this point to extend our notation for states. Thus we will represent a state of type a having a wavefunction a by ja; ai and similarly for a state of type b. Then under the charge conjugation operator, ^ C C, ^ C Cja; ai ¼ Caja; ai; ð1:15aÞ and ^ C Cjb; bi ¼ j b b; b bi; ð1:15bÞ where Ca is a phase factor analogous to the phase factor in Equation (1.5).26 Applying the operator twice, in the same way as for parity, leads to Ca ¼ 1. From Equation (1.15a), we see that states of type a are eigenstates of ^ C C with eigenvalues 1, called their C-parities. States with distinct antiparticles can only form eigenstates of ^ C C as linear combinations. As an example of the latter, consider a þ pair with orbital angular momentum L between them. In this case ^ C Cjþ ; Li ¼ ð1ÞL jþ ; Li; ð1:16Þ because interchanging the pions reverses their relative positions in the spatial wavefunction. The same factor occurs for spin-1 2 fermion pairs f f f, but in addition there are two other factors. The first is ð1ÞSþ1 , where S is the total spin of the pair. 26 A phase factor could have been inserted in Equation (1.15b), but it is straightforward to show that the relative phase of the two states b and b b cannot be measured and so a phase introduced in this way would have no physical consequences. 12 CH1 BASIC CONCEPTS
  • 26. This follows directly from the structure of the spin wavefunctions: 12 Sz ¼ 1 1ffiffi 2 p ð1#2 þ #12Þ Sz ¼ 0 #1#2 Sz ¼ 1 9 = ; S ¼ 1 ð1:17aÞ and 1ffiffi 2 p ð1#2 #12Þ Sz ¼ 0 S ¼ 0; ð1:17bÞ where i ð#iÞ represents particle i having spin ‘up’ (‘down’) in the z-direction. A second factor ð1Þ arises whenever fermions and antifermions are interchanged. This has its origins in quantum field theory.27 Combining these factors, finally we have ^ C Cj f f f; J; L; Si ¼ ð1ÞLþS j f f f; J; L; Si; ð1:18Þ for fermion–antifermion pairs having total, orbital and spin angular momentum quantum numbers J, L and S, respectively. 1.4 Interactions and Feynman Diagrams We now turn to a discussion of particle interactions and how they can be described by the very useful pictorial methods of Feynman diagrams. 1.4.1 Interactions Interactions involving elementary particles and/or hadrons are conveniently summarized by ‘equations’ by analogy with chemical reactions, in which the different particles are represented by symbols which usually – but not always – have a superscript to denote their electric charge. In the interaction e þ n ! e þ p; ð1:19Þ for example, an electron neutrino e collides with a neutron n to produce an electron e and a proton p, whereas the equation e þ p ! e þ p ð1:20Þ 27 See, for example, pp. 249–250 of Go86. INTERACTIONS AND FEYNMAN DIAGRAMS 13
  • 27. represents an electron and proton interacting to give the same particles in the final state, but in general travelling in different directions. In such equations, conserved quantum numbers must have the same total values in initial and final states. Particles may be transferred from initial to final states and vice versa, when they become antiparticles. Thus the process þ p ! þ p; ð1:21aÞ also implies the reaction p þ p p ! þ þ ; ð1:22Þ which is obtained by taking the proton from the final state to an antiproton in the initial state and the negatively charged pion in the initial state to a positively charged pion in the final state. The interactions in Equations (1.20) and (1.21a), in which the particles remain unchanged, are examples of elastic scattering, in contrast to the reactions in Equations (1.19) and (1.22), where the final-state particles differ from those in the initial state. Collisions between a given pair of initial particles do not always lead to the same final state, but can lead to different final states with different probabilities. For example, the collision of a negatively charged pion and a proton can give rise to elastic scattering (Equation (1.21a)) and a variety of other reactions, such as þ p ! n þ 0 and þ p ! p þ þ þ þ ; ð1:21bÞ depending on the initial energy. In particle physics it is common to refer (rather imprecisely) to such interactions as ‘inelastic’ scattering. Similar considerations apply to nuclear physics, but the term inelastic scattering is reserved for the case where the final state is an excited state of the parent nucleus A, that subsequently decays, for example via photon emission, i.e. a þ A ! a þ A ; A ! A þ ; ð1:23Þ where a is a projectile and A is an excited state of A. A useful shorthand notation used in nuclear physics for the general reaction a þ A ! b þ B is Aða; bÞB. It is usual in nuclear physics to further subdivide types of interactions according to the underlying mechanism that produced them. We will return to this in Section 2.9, as part of a more general discussion of nuclear reactions. Finally, many particles are unstable and spontaneously decay to other, lighter (i.e. having less mass) particles. An example of this is the free neutron (i.e. one not bound in a nucleus), which decays by the -decay reaction n ! p þ e þ e; ð1:24Þ 14 CH1 BASIC CONCEPTS
  • 28. with a mean lifetime of about 900 s.28 The same notation can also be used in nuclear physics. For example, many nuclei decay via the -decay reaction. Thus, denoting a nucleus with Z protons and N nucleons as (Z, N ), we have ðZ; NÞ ! ðZ 1; NÞ þ eþ þ e: ð1:25Þ This is also a weak interaction. This reaction is effectively the decay of a proton bound in a nucleus. Although a free proton cannot decay by the -decay p ! n þ eþ þ e because it violates energy conservation (the final-state particles have greater total mass than the proton), a proton bound in a nucleus can decay because of its binding energy. This will be explained in Chapter 2. 1.4.2 Feynman diagrams The forces producing all the above interactions are due to the exchange of particles and a convenient way of illustrating this is to use Feynman diagrams. There are mathematical rules and techniques associated with these that enable them to be used to calculate the quantum mechanical probabilities for given reactions to occur, but in this book Feynman diagrams will only be used as a convenient very useful pictorial description of reaction mechanisms. We first illustrate them at the level of elementary particles for the case of electromagnetic interactions, which arise from the emission and/or absorption of photons. For example, the dominant interaction between two electrons is due to the exchange of a single photon, which is emitted by one electron and absorbed by the other. This mechanism, which gives rise to the familiar Coulomb interaction at large distances, is illustrated in the Feynman diagram Figure 1.1(a). In such diagrams, we will use the convention that particles in the initial state are shown on the left and particles in the final state are shown on the right. (Some authors take time to run along the y-axis.) Spin-1 2 fermions (such as the electron) 28 The reason that this decay involves an antineutrino rather than a neutrino will become clear in Chapter 3. Figure 1.1 One-photon exchange in (a) e þ e ! e þ e and (b) eþ þ eþ ! eþ þ eþ INTERACTIONS AND FEYNMAN DIAGRAMS 15
  • 29. are drawn as solid lines and photons are drawn as wiggly lines. Arrowheads pointing to the right indicate that the solid lines represent electrons. In the case of photon exchange between two positrons, which is shown in Figure 1.1(b), the arrowheads on the antiparticle (positron) lines are conventionally shown as pointing to the left. In interpreting these diagrams, it is important to remember: (1) that the direction of the arrows on fermion lines does not indicate the particle’s direction of motion, but merely whether the fermions are particles or antiparticles, and (2) that particles in the initial state are always to the left and particles in the final state are always to the right. A feature of the above diagrams is that they are constructed from combinations of simple three-line vertices. This is characteristic of electromagnetic processes. Each vertex has a line corresponding to a single photon being emitted or absorbed, while one fermion line has the arrow pointing toward the vertex and the other away from the vertex, guaranteeing charge conservation at the vertex, which is one of the rules of Feynman diagrams.29 For example, a vertex like Figure 1.2 would correspond to a process in which an electron emitted a photon and turned into a positron. This would violate charge conservation and is therefore forbidden. Feynman diagrams can also be used to describe the fundamental weak and strong interactions. This is illustrated by Figure 1.3(a), which shows contributions to the elastic weak scattering reaction e þ e ! e þ e due to the exchange of a Z0 , and by Figure 1.3(b), which shows the exchange of a gluon g (represented by a coiled line) between two quarks, which is a strong interaction. Feynman diagrams can also be drawn at the level of hadrons. As an illustration, Figure 1.4 shows the exchange of a charged pion (shown as a dashed line) between a proton and a neutron. We shall see later that this mechanism is a major contribution to the strong nuclear force between a proton and a neutron. We turn now to consider in more detail the relation between exchanged particles and forces. 29 Compare Kirchhoff’s laws in electromagnetism. e– e+ γ Figure 1.2 The forbidden vertex e ! eþ þ 16 CH1 BASIC CONCEPTS
  • 30. 1.5 Particle Exchange: Forces and Potentials This section starts with a discussion of the important relationship between forces and particle exchanges and then relates this to potentials. Although the idea of a potential has its greatest use in non-relativistic physics, nevertheless it is useful to illustrate concepts and is used in later sections as an intermediate step in relating theoretical Feynman diagrams to measurable quantities. The results can easily be extended to more general situations. 1.5.1 Range of forces At each vertex of a Feynman diagram, charge is conserved by construction. We will see later that, depending on the nature of the interaction (strong, weak or electromagnetic), other quantum numbers are also conserved. However, it is easy to show that energy and momentum cannot be conserved simultaneously. Consider the general case of a reaction A þ B ! A þ B mediated by the exchange of a particle X, as shown in Figure 1.5. In the rest frame of the incident Figure 1.3 (a) Contributions of (a) Z0 exchange to the elastic weak scattering reaction e þ e ! e þ e, and (b) gluon exchange contribution to the strong interaction q þ q ! q þ q Figure 1.4 Single-pion exchange in the reaction p þ n ! n þ p PARTICLE EXCHANGE: FORCES AND POTENTIALS 17
  • 31. particle A, the lower vertex represents the virtual process (‘virtual’ because X does not appear as a real particle in the final state), AðMAc2 ; 0Þ ! AðEA; pAcÞ þ XðEX; pAcÞ; ð1:26Þ where EA is the total energy of particle A and pA is its three-momentum.30 Thus, if we denote by PA the four-vector for particle A, PA ¼ ðEA=c; pAÞ ð1:27Þ and P2 A ¼ E2 A=c2 p2 A ¼ M2 Ac2 : ð1:28Þ Applying this to the diagram and imposing momentum conservation, gives EA ¼ ðp2 c2 þ M2 Ac4 Þ1=2 ; EX ¼ ðp2 c2 þ M2 Xc4 Þ1=2 ; ð1:29Þ where p ¼ jpj. The energy difference between the final and initial states is given by E ¼ EX þ EA MAc2 ! 2pc; p ! 1 ! MXc2 ; p ! 0 ð1:30Þ and thus E MXc2 for all p, i.e. energy is not conserved. However, by the Heisenberg uncertainty principle, such an energy violation is allowed, but only for a time h=E, so we immediately obtain r R h=MXc ð1:31Þ 30 A resumé of relativistic kinematics is given in Appendix B. Figure 1.5 Exchange of a particle X in the reaction A þ B ! A þ B 18 CH1 BASIC CONCEPTS
  • 32. as the maximum distance over which X can propagate before being absorbed by particle B. This maximum distance is called the range of the interaction and this was the sense of the word used in Section 1.1.1. The electromagnetic interaction has an infinite range, because the exchanged particle is a massless photon. In contrast, the weak interaction is associated with the exchange of very heavy particles – the W and Z bosons. These lead to ranges that from Equation (1.31) are of the order of RW;Z 2 1018 m. The funda- mental strong interaction has infinite range because, like the photon, gluons have zero mass. On the other hand, the strong nuclear force, as exemplified by Figure 1.4 for example, has a much shorter range of approximately (1–2) 1015 m. We will comment briefly on the relation between these two different manifestations of the strong interaction in Section 7.1. 1.5.2 The Yukawa potential In the limit that MA becomes large, we can regard B as being scattered by a static potential of which A is the source. This potential will in general be spin dependent, but its main features can be obtained by neglecting spin and considering X to be a spin-0 boson, in which case it will obey the Klein–Gordon equation h2 @2 ðx; tÞ @t2 ¼ h2 c2 r2 ðx; tÞ þ M2 Xc4 ðx; tÞ: ð1:32Þ The static solution of this equation satisfies r2 ðxÞ ¼ M2 Xc4 h2 ðxÞ; ð1:33Þ where ðxÞ is interpreted as a static potential. For MX ¼ 0 this equation is the same as that obeyed by the electrostatic potential, and for a point charge e interacting with a point charge þe at the origin, the appropriate solution is the Coulomb potential VðrÞ ¼ eðrÞ ¼ e2 40 1 r ; ð1:34Þ where r ¼ jxj and 0 is the dielectric constant. The corresponding solution in the case where M2 X 6¼ 0 is easily verified by substitution to be VðrÞ ¼ g2 4 er=R r ; ð1:35Þ where R is the range defined earlier and g, the so-called coupling constant, is a parameter associated with each vertex of a Feynman diagram and represents the PARTICLE EXCHANGE: FORCES AND POTENTIALS 19
  • 33. basic strength of the interaction.31 For simplicity, we have assumed equal strengths for the couplings of particle X to the particles A and B. The form of VðrÞ in Equation (1.35) is called a Yukawa potential, after the physicist who first introduced the idea of forces due to massive particle exchange in 1935.32 As MX ! 0, R ! 1 and the Coulomb potential is recovered from the Yukawa potential, while for very large masses the interaction is approximately point-like (zero range). It is conventional to introduce a dimensionless parameter X by X ¼ g2 4 hc ; ð1:36Þ that characterizes the strength of the interaction at short distances r R. For the electromagnetic interaction this is the fine structure constant e2 =40 hc 1=137 ð1:37Þ that governs the splittings of atom energy levels.33 The forces between hadrons are also generated by the exchange of particles. Thus, in addition to the electromagnetic interaction between charged hadrons, all hadrons, whether charged or neutral, experience a strong short-range interaction, which in the case of two nucleons, for example, has a range of about 1015 m, corresponding to the exchange of a particle with an effective mass of about 1 7th the mass of the proton. The dominant contribution to this force is the exchange of a single pion, as shown in Figure 1.4. This nuclear strong interaction is a complicated effect that has its origins in the fundamental strong interactions between the quark distributions within the two hadrons. Two neutral atoms also experience an electromagnetic interaction (the van der Waals force), which has its origins in the fundamental Coulomb forces, but is of much shorter range. Although an analogous mechanism is not in fact responsible for the nuclear strong interaction, it is a useful reminder that the force between two distributions of particles can be much more complicated than the forces between their components. We will return to this point when we discuss the nature of the nuclear potential in more detail in Section 7.1. 1.6 Observable Quantities: Cross Sections and Decay Rates We have mentioned earlier that Feynman diagrams can be turned into probabilities for a process by a set of mathematical rules (the Feynman Rules) that can be 31 Although we call g a (point) coupling constant, in general it will have a dependence on the momentum carried by the exchanged particle. We ignore this in what follows. 32 For this insight, Hideki Yukawa received the 1949 Nobel Prize in Physics. 33 Like g, the coupling X will in general have a dependence on the momentum carried by particle X. In the case of the electromagnetic interaction, this dependence is relatively weak. 20 CH1 BASIC CONCEPTS
  • 34. derived from the quantum theory of the underlying interaction.34 We will not pursue this in detail in this book, but rather will show in principle their relation to observables, i.e. things that can be measured, concentrating on the cases of two- body scattering reactions and decays of unstable states. 1.6.1 Amplitudes The intermediate step is the amplitude f, the modulus squared of which is directly related to the probability of the process occurring. It is also called the invariant amplitude because, as we shall show, it is directly related to observable quantities and these have to be the same in all inertial frames of reference. To get some qualitative idea of the structure of f, we will use non-relativistic quantum mechanics and assume that the coupling constant g2 is small compared with 4 hc, so that the interaction is a small perturbation on the free particle solution, which will be taken as plane waves. If we expand the amplitude in a power series in g2 and keep just the first term (i.e. lowest-order perturbation theory), then the amplitude for a particle in an initial state with momentum qi to be scattered to a final state with momentum qf by a potential VðxÞ is proportional to fðq2 Þ ¼ ð d3 xVðxÞ exp½iq x= h; ð1:38Þ i.e. the Fourier transform of the potential, where q qi qf is the momentum transfer.35 The integration may be done using polar co-ordinates. Taking q in the x- direction, gives q x ¼ jqjr cos ð1:39Þ and d3 x ¼ r2 sin d dr d; ð1:40Þ where r ¼ jxj. For the Yukawa potential, the integral in Equation (1.38) gives fðq2 Þ ¼ g2 h2 q2 þ M2 Xc2 : ð1:41Þ 34 In the case of the electromagnetic interaction, the theory is called Quantum Electrodynamics (QED) and is spectacularly successful in explaining experimental results. Richard Feynman shared the 1965 Nobel Prize in Physics with Sin-Itiro Tomonoga and Julian Schwinger for their work on formulating quantum electro- dynamics. The Feynman Rules are discussed in an accessible way in Gr87. 35 See, for example, Chapter 11 of Ma92. OBSERVABLE QUANTITIES: CROSS SECTIONS AND DECAY RATES 21
  • 35. This amplitude corresponds to the exchange of a single particle, as shown for example in Figures 1.3 and 1.4. The structure of the amplitude, which is quite general, is a numerator proportional to the product of the couplings at the two vertices (or equivalently X in this case), and a denominator that depends on the mass of the exchanged particle and its momentum transfer squared. The denomi- nator is called the propagator for particle X. In a relativistic calculation, the term q2 becomes q2 , where q is the four-momentum transfer. Returning to the zero-range approximation, one area where it is used extensively is in weak interactions, particularly applied to nuclear decay processes. In these situations, MX ¼ MW;Z and f ! GF, where GF, the so-called Fermi coupling constant, is given from Equation (1.36) by GF ð hcÞ3 ¼ 4W ðMW c2Þ2 ¼ 1:166 105 GeV2 : ð1:42Þ The numerical value is obtained from analyses of decay processes, including that of the neutron and a heavier version of the electron called the muon, whose properties will be discussed in Chapter 3. All the above is for the exchange of a single particle. It is also possible to draw more complicated Feynman diagrams that correspond to the exchange of more than one particle. An example of such a diagram for elastic e e scattering, where two photons are exchanged, is shown in Figure 1.6. The number of vertices in any diagram is called the order n, and when the amplitude associated with any given Feynman diagram is calculated, it always contains a factor of ð ffiffiffiffi p Þn . Since the probability is proportional to the square of the modulus of the amplitude, the former will contain a factor n . The probability associated with the single-photon exchange diagrams of Figure 1.1 thus contain a factor of 2 and the contribution from two-photon exchange is of the order of 4 . Figure 1.6 Two-photon exchange in the reaction e þ e ! e þ e 22 CH1 BASIC CONCEPTS
  • 36. As 1=137, the latter is usually very small compared with the contribution from single-photon exchange. This is a general feature of electromagnetic interactions: because the fine structure constant is very small, in most cases only the lowest-order diagrams that contribute to a given process need be taken into account, and more complicated higher-order diagrams with more vertices can (to a good approximation) be ignored in many applications. 1.6.2 Cross-sections The next step is to relate the amplitude to measurables. For scattering reactions, the appropriate observable is the cross-section. In a typical scattering experiment, a beam of particles is allowed to hit a target and the rates of production of various particles in the final state are counted.36 It is clear that the rates will be proportional to: (a) the number N of particles in the target illuminated by the beam, and (b) the rate per unit area at which beam particles cross a small surface placed in the beam at rest with respect to the target and perpendicular to the beam direction. The latter is called the flux and is given by J ¼ nbvi; ð1:43Þ where nb is the number density of particles in the beam and vi their velocity in the rest frame of the target. Hence the rate Wr at which a specific reaction r occurs in a particular experiment can be written in the form Wr ¼ JNr; ð1:44aÞ where r, the constant of proportionality, is called the cross-section for reaction r. If the beam has a cross-sectional area S, its intensity is I ¼ JS and so an alternative expression for the rate is Wr ¼ NrI=S ¼ Irntt; ð1:44bÞ where nt is the number of target particles per unit volume and t is the thickness of the target. If the target consists of an isotopic species of atomic mass MA (in atomic mass units-defined in Section 1.7 below), then nt ¼ NA=MA, where is the density of the target and NA is Avogadro’s constant. Thus, Equation (1.44b) may be written Wr ¼ IrðtÞNA=MA; ð1:44cÞ 36 The practical aspects of experiments are discussed in Chapter 4. OBSERVABLE QUANTITIES: CROSS SECTIONS AND DECAY RATES 23
  • 37. where ðtÞ is a measure of the amount of material in the target, expressed in units of mass per unit area. The form of Equation (1.44c) is particularly useful for the case of thin targets, commonly used in experiments. In the above, the product JN is called the luminosity L, i.e. L JN ð1:45Þ and contains all the dependencies on the densities and geometries of the beam and target. The cross-section is independent of these factors. It can be seen from the above equations that the cross-section has the dimensions of an area; the rate per target particle Jr at which the reaction occurs is equal to the rate at which beam particles would hit a surface of area r, placed in the beam at rest with respect to the target and perpendicular to the beam direction. Since the area of such a surface is unchanged by a Lorentz transformation in the beam direction, the cross-section is the same in all inertial frames of reference, i.e. it is a Lorentz invariant. The quantity r is better named the partial cross-section, because it is the cross- section for a particular reaction r. The total cross-section is defined by X r r: ð1:46Þ Another useful quantity is the differential cross-section, drð ; Þ=d, which is defined by dWr JN drð ; Þ d d; ð1:47Þ where dWr is the measured rate for the particles to be emitted into an element of solid angle d ¼ d cos d in the direction ð ; Þ, as shown in Figure 1.7. The total cross-section is obtained by integrating the partial cross-section over all angles, i.e. r ¼ ð2 0 d ð1 1 d cos drð ; Þ d : ð1:48Þ The final step is to write these formulae in terms of the scattering amplitude fðq2 Þ appropriate for describing the scattering of a non-relativistic spinless particle from a potential. To do this it is convenient to consider a single beam particle interacting with a single target particle and to confine the whole system in an arbitrary volume V (which cancels in the final result). The incident flux is then given by J ¼ nbvi ¼ vi=V ð1:49Þ 24 CH1 BASIC CONCEPTS
  • 38. and since the number of target particles is N ¼ 1, the differential rate is dWr ¼ vi V drð ; Þ d d: ð1:50Þ In quantum mechanics, provided the interaction is not too strong, the transition rate for any process is given in perturbation theory by the Born approximation37 dWr ¼ 2 h ð d3 x f VðxÞ i 2 ðEfÞ: ð1:51Þ The term ðEfÞ is the density-of-states factor (see below) and we take the initial and final state wavefunctions to be plane waves: i ¼ 1 ffiffiffiffi V p exp½iqi x= h; f ¼ 1 ffiffiffiffi V p exp½iqf x= h; ð1:52Þ 37 This equation is a form of the Second Golden Rule. It is discussed in Appendix A. Figure 1.7 Geometry of the differential cross-section: a beam of particles is incident along the z-axis and collides with a stationary target at the origin; the differential cross-section is proportional to the rate for particles to be scattered into a small solid angle d in the direction ð ; Þ OBSERVABLE QUANTITIES: CROSS SECTIONS AND DECAY RATES 25
  • 39. where the final momentum qf lies within a small solid angle d located in the direction ð ; Þ (see Figure 1.7.). Then, by direct integration, dWr ¼ 2 hV2 j fðq2 Þj2 ðEfÞ; ð1:53Þ where fðq2 Þ is the scattering amplitude defined in Equation (1.38). The density of states ðEfÞ that appears in Equation (1.51) is the number of possible final states with energy lying between Ef and Ef þ dEf and is given by38 ðEfÞ ¼ V ð2 hÞ3 q2 f vf d: ð1:54Þ If we use this and Equation (1.53) in Equation (1.50), we have d d ¼ 1 42 h4 q2 f vivf j fðq2 Þj2 : ð1:55Þ Although this result has been derived in the laboratory system, because we have taken a massive target it is also valid in the centre-of-mass system. For a finite mass target it would be necessary to make a Lorentz transformation on Equation (1.55). The expression is also true for the general two-body relativistic scattering process a þ b ! c þ d. All the above is for spinless particles, so finally we have to generalize Equation (1.55) to include the effects of spin. Suppose the initial-state particles a and b, have spins sa and sb and the final-state particles c and d have spins sc and sd. The total numbers of spin substates available to the initial and final states are gi and gf, respectively, given by gi ¼ ð2sa þ 1Þð2sb þ 1Þ and gf ¼ ð2sc þ 1Þ ð2sd þ 1Þ: ð1:56Þ If the initial particles are unpolarized (which is the most common case in practice), then we must average over all possible initial spin configurations (because each is equally likely) and sum over the final configurations. Thus, Equation (1.55) becomes d d ¼ gf 42 h4 q2 f vivf jMfij2 ; ð1:57Þ where jMfij2 j fðq2Þj2 ð1:58Þ and the bar over the amplitude denotes a spin-average of the squared matrix element. 38 The derivation is given in detail in Appendix A. 26 CH1 BASIC CONCEPTS
  • 40. 1.6.3 Unstable states In the case of an unstable state, the observable of interest is its lifetime at rest , or equivalently its natural decay width, given by ¼ h=, which is a measure of the rate of the decay reaction. In general, an initial unstable state will decay to several final states and in this case we define f as the partial width for channel f and ¼ X f f ð1:59Þ as the total decay width, while Bf f = ð1:60Þ is defined as the branching ratio for decay to channel f. The energy distribution of an unstable state to a final state f has the Breit–Wigner form Nf ðWÞ / f ðW MÞ2 c4 þ 2=4 ; ð1:61Þ where M is the mass of the decaying state and W is the invariant mass of the decay products.39 The Breit–Wigner formula is shown in Figure 1.8 and is the same formula that describes the widths of atomic and nuclear spectral lines. (The overall factor depends on the spins of the particles involved.) It is a symmetrical bell- shaped curve with a maximum at W ¼ M and a full width at half the maximum height of the curve. It is proportional to the number of events with invariant mass W. If an unstable state is produced in a scattering reaction, then the cross section for that reaction will show an enhancement described by the same Breit–Wigner formula. In this case we say we have produced a resonance state. In the vicinity of a resonance of mass M, and width , the cross-section for the reaction i ! f has the form fi / if ðE Mc2Þ2 þ 2=4 ; ð1:62Þ where E is the total energy of the system. Again, the form of the overall constant will depend on the spins of the particles involved. Thus, for example, if the resonance particle has spin j and the spins of the initial particles are s1 and s2, then fi ¼ h2 q2 i 2j þ 1 ð2s1 þ 1Þð2s2 þ 1Þ if ðE Mc2Þ2 þ 2=4 : ð1:63Þ 39 This form arises from a state that decays exponentially with time, although a proper proof of this is quite lengthy. See, for example, Appendix B of Ma97. OBSERVABLE QUANTITIES: CROSS SECTIONS AND DECAY RATES 27
  • 41. In practice there will also be kinematical and angular momentum effects that will distort this formula from its perfectly symmetric shape. An example of resonance formation in p interactions is given in Figure 1.9, which shows the p total cross-section in the centre-of-mass energy range Figure 1.8 The Breit--Wigner formula (Equation (1.61)) Figure 1.9 Total cross-sections for p interactions (data from Ca68) 28 CH1 BASIC CONCEPTS
  • 42. 1.2–2.4 GeV. (The units used in the plots will become clear after the next section.) Two enhancements can be seen that are of the approximate Breit–Wigner resonance form and there are two other maxima at higher energies. In principle, the mass and width of a resonance may be obtained by using a Breit–Wigner formula and varying M and to fit the cross-section in the region of the enhancement. In practice, more sophisticated methods are used that fit a wide range of data, including differential cross-sections, simultaneously and also take account of non-resonant contributions to the scattering. The widths obtained from such analyses are of the order of 100 MeV, with corresponding interaction times of order 1023 s, which is consistent with the time taken for a relativistic pion to transit the dimension of a proton. Resonances are also a feature of interactions in nuclear physics and we will return to this in Section 2.9 when we discuss nuclear reaction mechanisms. 1.7 Units: Length, Mass and Energy Most branches of science introduce special units that are convenient for their own purposes. Nuclear and particle physics are no exceptions. Distances tend to be measured in femtometres (fm) or, equivalently fermis, with 1 fm 1015 m. In these units, the radius of the proton is about 0.8 fm. The range of the strong nuclear force between protons and neutrons is of the order of 1–2 fm, while the range of theweak force is of the order of 103 fm. For comparison, the radii of atoms are of the order of 105 fm. A common unit for area is the barn (b) defined by 1 b ¼ 1028 m2 . For example, the total cross-section for pp scattering (a strong interaction) is a few tens of millibarns (mb) (compare also the p total cross-section in Figure 1.9), whereas the same quantity for p scattering (a weak interaction) is a few tens of femtobarns (fb), depending on the energies involved. Nuclear cross-sections are very much larger and increase approxi- mately like A2=3 , where A is the total number of nucleons in the nucleus. Energies are invariably specified in terms of the electron volt (eV) defined as the energy required to raise the electric potential of an electron or proton by 1 V. In SI units, 1 eV ¼ 1:6 1019 J. The units 1 keV ¼ 103 eV, 1 MeV ¼ 106 eV, 1 GeV ¼ 109 eV and 1 TeV ¼ 1012 eV are also in general use. In terms of these units, atomic ionization energies are typically a few eV, the energies needed to bind nucleons in heavy nuclei are typically 7–8 MeV per particle, and the highest particle energies produced in the laboratory are of the order of 1 TeV for protons. Momenta are specified in eV=c, MeV=c, etc.. In order to create a new particle of mass M, an energy at least as great as its rest energy Mc2 must be supplied. The rest energies of the electron and proton are 0.51 MeV and 0.94 GeV respectively, whereas the W and Z0 bosons have rest energies of 80 GeV and 91 GeV, respectively. Correspondingly, their masses are conveniently measured in MeV=c2 or GeV=c2 , so that, for example, Me ¼ 0:51 MeV=c2 ; Mp ¼ 0:94 GeV=c2 ; MW ¼ 80:3 GeV=c2 ; MZ ¼ 91:2 GeV=c2 ð1:64Þ UNITS: LENGTH, MASS AND ENERGY 29
  • 43. In SI units, 1 MeV=c2 ¼ 1:78 1030 kg. In nuclear physics it is also common to express masses in atomic mass units (u), where 1 u ¼ 1:661 1027 kg ¼ 931:5 MeV=c2 . Although practical calculations are expressed in the above units, it is usual in particle physics to make theoretical calculations in units chosen such that h h=2 ¼ 1 and c ¼ 1 (called natural units) and many books do this. However, as this book is about both nuclear and particle physics, only practical units will be used. A table giving numerical values of fundamental and derived constants, together with some useful conversion factors is given on page XV. Problems 1.1 ‘Derive’ the Klein–Gordon equation using the information in Footnote 21 and verify that Equation (1.35) is a static solution of the equation. 1.2 Verify that the spherical harmonic Y1 1 ¼ ffiffi 3 8 q sin ei is an eigenfunction of parity with eigenvalue P ¼ 1. 1.3 A proton and antiproton at rest in an S-state annihilate to produce 0 0 pairs. Show that this reaction cannot be a strong interaction. 1.4 Suppose that an intrinsic C-parity factor is introduced into Equation (1.15b), which then becomes ^ C Cjb; bi ¼ Cbj b b; b bi. Show that the eigenvalue corresponding to any eigenstate of ^ C C is independent of Cb, so that Cb cannot be measured. 1.5 Consider the reaction d ! nn, where d is a spin-1 S-wave bound state of a proton and a neutron called the deuteron and the initial pion is at rest. Deduce the intrinsic parity of the negative pion. 1.6 Write down equations in symbol form that describe the following interactions: (a) elastic scattering of an electron antineutrino and a positron; (b) inelastic production of a pair of neutral pions in proton–proton interactions; (c) the annihilation of an antiproton with a neutron to produce three pions. 1.7 Draw a lowest-order Feynman diagram for the following processes: (a) e elastic scattering; (b) n ! p þ e þ e; 30 CH1 BASIC CONCEPTS
  • 44. (c) eþ e ! eþ e ; (d) a fourth-order diagram for the reaction þ ! eþ þ e . 1.8 Calculate the energy–momentum transfer between two particles equivalent to a distance of approach of (a) 1fm and (b) 103 fm. Assuming that the intrinsic strengths of the fundamental weak and electromagnetic interactions are approxi- mately equal, compare the relative sizes of the invariant (scattering) amplitudes for weak and electromagnetic processes at these two energy–momentum transfers. 1.9 Verify by explicit integration that fðqÞ ¼ g2 h2 ½q2 þ m2 c2 1 is the amplitude corresponding to the Yukawa potential VðrÞ ¼ g2 4 er=R r ; where R ¼ h=mc is the range and r ¼ jxj. 1.10 Two beams of particles consisting of n bunches with Niði ¼ 1; 2Þ particles in each, traverse circular paths and collide ‘head-on’. Show that in this case the general expression Equation (1.45) for the luminosity reduces to L ¼ nN1N2f =A, where A is the cross-sectional area of the beam and f is the frequency, i.e. f ¼ 1=T, where T is the time taken for the particles to make one traversal of the ring. 1.11 A thin (density 1 mg cm2 ) target of 24 Mg (MA ¼ 24:3 atomic mass units) is bombarded with a 10 nA beam of alpha particles. A detector subtending a solid angle of 2 103 sr, records 20 protons/s. If the scattering is isotropic, determine the cross-section for the 24 Mgð; pÞ reaction. PROBLEMS 31
  • 45. 2 Nuclear Phenomenology In this chapter we start to examine some of the things that can be learned from experiments, beginning with basic facts about nuclei, including what can be deduced about their shapes and sizes. Then we discuss the important topic of nuclear stability and the phenomenology of the various ways that unstable nuclei decay to stable states. Finally, we briefly review the classification of reactions in nuclear physics. Before that we need to introduce some notation. 2.1 Mass Spectroscopy and Binding Energies Nuclei are specified by: Z – atomic number ¼ the number of protons, N – neutron number ¼ the number of neutrons, A – mass number ¼ the number of nucleons, so that A ¼ Z þ N. We will also refer to A as the nucleon number. The charge on the nucleus is þZe, where e is the absolute value of the electric charge on the electron. Nuclei with combinations of these three numbers are also called nuclides and are written A Y or A ZY, where Y is the chemical symbol for the element. Some other common nomenclature is: nuclides with the same mass number are called isobars, nuclides with the same atomic number are called isotopes, nuclides with the same neutron number are called isotones. Nuclear and Particle Physics B. R. Martin # 2006 John Wiley Sons, Ltd. ISBN: 0-470-01999-9
  • 46. The concept of isotopes was introduced in Chapter 1. For example, stable isotopes of carbon are 12 C and 13 C, and the unstable isotope used in dating ancient objects (see later in this chapter) is 14 C; all three have Z ¼ 6. Just as in the case of electrons in atoms, the forces that bind the nucleons in nuclei contribute to the total mass of an atom M(Z, A) and in terms of the masses of the proton Mp and neutron Mn MðZ; AÞ Z ðMp þ meÞ þ N Mn: ð2:1Þ The mass deficit is defined as MðZ; AÞ MðZ; AÞ Z ðMp þ meÞ N Mn ð2:2Þ and Mc2 is called the binding energy B. Binding energies may be calculated if masses are measured accurately. One way of doing this is by using the techniques of mass spectroscopy. The principle of the method is shown in Figure 2.1. A source of ions of charge q, containing various isotopes passes through a region where there are uniform electric (E) and magnetic (B1) fields at right angles. The electric field will exert a force qE in one direction and the magnetic field will exert a force qvB1 in the opposite direction, where v is the speed of the ions. By balancing these forces, ions of a specific speed v ¼ E=B1 can be selected and allowed to pass through a collimating slit. Ions with other velocities (shown as dashed lines) are deflected. The beam is then allowed to continue through a second Figure 2.1 Schematic diagram of a mass spectrometer (adapted from Kr88 Copyright John Wiley Sons, Inc.) 34 CH2 NUCLEAR PHENOMENOLOGY
  • 47. uniform magnetic field B2 where it will be bent into a circular path of radius , given by mv ¼ qB2 ð2:3Þ and since q, B2 and v are fixed, particles with a fixed ratio q=m will bend in a path with a unique radius. Hence isotopes may be separated and focused onto a detector (e.g. a photographic plate). In the common case where B1 ¼ B2 ¼ B, q m ¼ E B2 : ð2:4Þ In practice, to achieve high accuracy, the device is used to measure mass differences rather than absolute values of mass.1 Conventional mass spectroscopy cannot be used to find the masses of very short- lived nuclei and in these cases the masses are determined from kinematic analysis of nuclear reactions as follows. Consider the inelastic reaction Aða; aÞA , where A is the short-lived nucleus whose mass is to be determined. The kinematics of this are: aðEi; piÞ þ AðmAc2 ; 0Þ ! aðEf ; pf Þ þ A ð~ E E; p ~Þ; ð2:5Þ where we use tilded quantities to denote the energy, mass, etc. of A . Equating the total energy before the collision EtotðinitialÞ ¼ Ei þ mac2 þ mAc2 ð2:6aÞ to the total energy after the collision EtotðfinalÞ ¼ Ef þ ~ E E þ mac2 þ ~ m m c2 ð2:6bÞ gives the following expression for the change in energy of the nucleus: E ð~ m m mAÞc2 ¼ Ei Ef ~ E E ¼ p2 i 2ma p2 f 2ma ~ p p2 2~ m m ; ð2:7Þ where we have assumed non-relativistic kinematics. If the initial momentum of the projectile is along the x-direction and the scattering angle is , then from momentum conservation, ð~ p pÞx ¼ pi pf cos ; ð~ p pÞy ¼ pf sin ð2:8Þ 1 Practical details of mass spectroscopy may be found in, for example, Chapter 3 of Kr88. MASS SPECTROSCOPY AND BINDING ENERGIES 35
  • 48. and using these in Equation (2.7) gives E ¼ Ei 1 ma ~ m m Ef 1 þ ma ~ m m þ 2ma ~ m m EiEf 1=2 cos : ð2:9Þ This formula can be used iteratively to deduce E and hence the mass of the excited nucleus A , from measurements of the initial and final energy of the projectile by initially setting ~ m m ¼ mA on the right-hand side because E is small in comparison with mA. One final point is that the energies in Equation (2.9) are measured in the laboratory system, whereas the final energies (masses) will be needed in the centre-of- mass system.2 The necessary transformation is easily found to be ECM ¼ Elab 1 þ ma=mA ð Þ1 : ð2:10Þ A similar formula to Equation (2.9) may be derived for the general reaction A(a,b)B: E ¼ Ei 1 ma mB Ef 1 þ mb mB þ 2 mB mambEiEf 1=2 cos þ Q; ð2:11Þ where Q is the kinetic energy released in the reaction. A commonly used quantity of interest is the binding energy per nucleon B=A. This is shown schematically in Figure 2.2 for nuclei that are stable or long-lived. 2 A discussion of these two systems is given in Appendix C. Figure 2.2 Binding energy per nucleon as a function of mass number A for stable and long- lived nuclei 36 CH2 NUCLEAR PHENOMENOLOGY
  • 49. This shows that B=A peaks at a value of 8.7 MeV for a mass number of about 56 (close to iron) and thereafter falls very slowly. Excluding very light nuclei, the binding energy per nucleon is between 7 and 9 MeV over a wide range of the periodic table. In Section 2.5 we will discuss a model that provides an explanation for the shape of this curve. 2.2 Nuclear Shapes and Sizes The shape and size of a nucleus may be found from scattering experiments; i.e. a projectile is scattered from the nucleus and the angular distribution of the scattered particles examined, as was done by Rutherford and his collaborators when they deduced the existence of the nucleus. The interpretation is simplest in those cases where the projectile itself has no internal structure, i.e. it is an elementary particle, and electrons are often used. In this case the relevant force is electromagnetic and we learn about the charge distribution in the nucleus. The first experiments of this type were performed by Hofstader and his collaborators in the late 1950s.3 If instead of an electron a hadron is used as the projectile, the force is dominantly the nuclear strong interaction and we find information about the matter density. Neutrons are com- monly used so that Coulomb effects are absent. We discuss these two cases in turn. 2.2.1 Charge distribution To find the amplitude for electron–nucleus scattering, we should in principle solve the Schrödinger (or Dirac) equation using a Hamiltonian that includes the full electromagnetic interaction and use nuclear wavefunctions. This can only be done numerically. However, in Appendix C we derive a simple formula that describes the electromagnetic scattering of a charged particle in the so-called Born approxima- tion, which assumes Z 1 and uses plane waves for the initial and final states. This leads to the Rutherford cross-section, which in its relativistic form may be written d dO Rutherford ¼ Z2 2 ð hcÞ2 4E2 sin4 ð=2Þ ; ð2:12Þ where E is the total initial energy of the projectile and is the angle through which it is scattered. Note that Equation (2.12) is of order 2 because it corresponds to the exchange of a single photon. Although Equation (2.12) has a limited range of applicability, it is useful to discuss the general features of electron scattering. Equation (2.12) actually describes the scattering of a spin-0 point-like projectile of unit charge from a fixed point-like target with electric charge Ze, i.e. the charge 3 Robert Hofstader shared the 1961 Nobel Prize in Physics for his pioneering electron scattering experiments. NUCLEAR SHAPES AND SIZES 37
  • 50. distribution of the target is neglected. It therefore needs to be modified in a number of ways before it can be used in practice. We will state the modifications without proof. Firstly, taking account of the electron spin leads to the so-called Mott cross- section d dO Mott ¼ d dO Rutherford 1 2 sin2 ð=2Þ ; ð2:13Þ where ¼ v=c and v is the velocity of the initial electron. At higher energies, the recoil of the target needs to be taken into account and this introduces a factor E0 =E on the right-hand side of Equation (2.13), where E0 is the final energy of the electron. At higher energies we also need to take account of the interaction with the magnetic moment of the target in addition to its charge. The final form for the differential cross-section is d dO spin 1 2 ¼ d dO Mott E0 E 1 þ 2 tan2 2 ; ð2:14Þ where ¼ q2 4M2c2 ð2:15Þ and M is the target mass. Because the energy loss of the electron to the recoiling nucleus is no longer negligible, q, the previous momentum transfer, has been replaced by the four-momentum transfer q, whose square is q2 ¼ ðp p0 Þ2 ¼ 2m2 ec2 2ðEE0 c2 p j j p0 j j cos Þ 4EE0 c2 sin2 ð=2Þ; ð2:16Þ where pð p0 Þ is the four-momentum of the initial (final) electron. (Because q2 0, it is common practice to replace it with Q2 ¼ q2 , so as to work with positive quantities.4 ) For the rest of this discussion it will be sufficient to ignore the magnetic interaction, although we will use a variant of the full form (2.16) in Chapter 6. The final modification is due to the spatial extension of the nucleus. If the spatial charge distribution within the nucleus is written f (x) then we define the form factor F(q2 ) by Fðq2 Þ 1 Ze ð eiqx= h fðxÞ d3 x with Ze ¼ ð fðxÞ d3 x; ð2:17Þ 4 To remove any confusion, in the non-relativistic case, which we use in the rest of this chapter, q is interpreted to be q ¼ jqj 0 where q p p0 , as was used in Section 1.6.1. We will need the four- momentum definition of q in Chapter 6. 38 CH2 NUCLEAR PHENOMENOLOGY
  • 51. i.e. the Fourier transform of the charge distribution.5 In the case of a spherically symmetric charge distribution, the angular integrations in Equations (2.17) may be done using spherical polar coordinates to give Fðq2 Þ ¼ 4 h Zeq ð 1 0 rðrÞsin qr h dr; ð2:18Þ where q ¼ jqj and ðrÞ is the radial charge distribution. The final form of the experimental cross-section in this approximation is given by6 d dO expt ¼ d dO Mott Fðq2 Þ 2 : ð2:19Þ Two examples of measured cross-sections are shown in Figure 2.3. Striking features are the presence of a number of well-defined minima superimposed on a Figure 2.3 Elastic differential cross-sections as a function of the scattering angle for 450 MeV electrons from 58 Ni and 758 MeV electrons from 48 Ca; the solid lines are fits as described in the text (adapted from Si75 (58 Ni data) and Be67 (48 Ca data), Copyright American Physical Society) 5 Strictly this formula assumes that the recoil of the target nucleus is negligible and the interaction is relatively weak, so that perturbation theory may be used. 6 If the magnetic interaction were included, another form factor would be necessary, as is the case in high- energy electron scattering discussed in Chapter 6. NUCLEAR SHAPES AND SIZES 39 Publisher's Note: Permission to reproduce this image online was not granted by the copyright holder. Readers are kindly requested to refer to the printed version of this chapter.
  • 52. rapid decrease in the cross-section with angle. These features are common to all elastic data, although not all nuclei show so many minima as those shown. The minima are due to the form factor and we can make this plausible by taking the simple case where the nuclear charge distribution is represented by a hard sphere such that ðrÞ ¼ constant; r a ¼ 0 r a ð2:20Þ where a is a constant. In this case, evaluation of Equation (2.18) gives Fðq2 Þ ¼ 3 sinðbÞ bcosðbÞ ½ b3 ; ð2:21Þ where b qa= h. Thus Fðq2 Þ will be zero at values of b for which b ¼ tanðbÞ. In practice, as we will see below, ðrÞ is not a hard sphere, and although it is approximately constant for much of the nuclear volume, it falls smoothly to zero at the surface. Smoothing the edges of the radial charge distribution (2.20) modifies the positions of the zeros, but does not alter the argument that the minima in the cross-sections are due to the spatial distribution of the nucleus. Their actual positions and depths result from a combination of the form factor and the form of the point-like amplitude. We shall see below that the minima can tell us about the size of the nucleus. If one measures the cross-section for a fixed energy at various angles (and hence various q2 ), the form factor can in principle be extracted using Equation (2.19) and one might attempt to find the charge distribution from the inverse Fourier transform fðxÞ ¼ Ze ð2 Þ3 ð Fðq2 Þ eiqx= h d3 q: ð2:22Þ However, q2 only has a finite range for a fixed initial electron energy and even within this range the rapid fall in the cross-section means that in practice measurements cannot be made over a sufficiently wide range of angles for the integral in Equation (2.22) to be evaluated accurately. Thus, even within the approximations used, reliable charge distributions cannot be found from Equation (2.22). Therefore different strategies must be used to deduce the charge distribution. In one approach, plausible – but very general – parameterized forms (for example a sum of Gaussians) are chosen for the charge distribution and are used to modify the point-like electromagnetic interaction. The resulting Schrödinger (or Dirac) equation is solved numerically to produce an amplitude, and hence a cross-section, for electron– nucleus scattering. The parameters of the charge distribution are then varied to give a good fit of the experimental data. The solid curves in Figure 2.3 are obtained in this way. 40 CH2 NUCLEAR PHENOMENOLOGY
  • 53. Some radial charge distributions for various nuclei obtained by these methods are shown in Figure 2.4. They are well represented by the form chðrÞ ¼ 0 ch 1 þ eðraÞ=b ; ð2:23Þ where a and b for medium and heavy nuclei are found to be a 1:07A1=3 fm and b 0:54 fm: ð2:24Þ From this we can deduce that the charge density is approximately constant in the nuclear interior and falls fairly rapidly to zero at the nuclear surface, as anticipated above. The value of 0 ch is in the range 0.06–0.08 for medium to heavy nuclei and decreases slowly with increasing mass number. Figure 2.4 Radial charge distributions ch of various nuclei, in units of e fm3 ; the thickness of the curves near r ¼ 0 is a measure of the uncertaintity in ch (adapted from Fr83) NUCLEAR SHAPES AND SIZES 41