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Introduction to Atoms

       CHAPTER 4
       SECTION 1
History of Atom

 All atoms share the same basic structure
 During past 200 years, scientists have proposed
  different models.
 An atom is the smallest particle of an element.
 Atomic theory grew as a series of models that
  developed from experimental evidence. As more
  evidence was collected, the theory and models were
  revised.
Dalton’s Model

 Based on experiments, Dalton developed a theory
  of structure of matter
 4 main concepts:
    All matter is composed of tiny, indivisible particles called
     atoms
    Atoms of each element are exactly alike
    Atoms of different elements have different masses
    Atoms of different elements can join to form compounds
Dalton’s Model
Thomson’s Model

 End of 1800s
 Thomson discovered that atoms were not
  simple, solid spheres
 Atoms contained subatomic particles
    Very small, negatively charged
    Called them electrons
Discovery of the Electron

In 1897, J.J. Thomson used a cathode ray
tube to deduce the presence of a negatively
charged particle: the electron
Modern Cathode Ray Tubes




     Television       Computer Monitor

Cathode ray tubes pass electricity
through a gas that is contained at a
very low pressure.
Thomson’s Model

 Also knew that atoms were electrically neutral
   Must contain enough positive charge to balance negative
    charge of electrons
 Developed model where electrons were stuck into a
  positively charged sphere
     Like chocolate chips in cookie dough
Thomson’s Model
Rutherford’s Model

 By early 1900s, scientists knew that positive charge
  of atom comes from subatomic particles called
  protons
 A proton is a positive charged particle in the
  nucleus of an atom.
 1911—Rutherford begins to test theory
 His experiments led him to believe that protons are
  concentrated in a small area at center of atom
    Called this area the nucleus
Rutherford’s Model

 Rutherford’s model describes an atom as mostly
 empty space, with a center nucleus that contains
 nearly all the mass
    Like the pit in a peach
Bohr’s Model

 Modified Rutherford’s model in 1913
 Proposed that each electron has a certain amount of
 energy
    Helped electron move around nucleus
 Electrons move around nucleus in region called
  energy levels
 The energy level is the specific amount of energy
  an electron has.
 Energy levels surround nucleus in rings, like layers of
  onion
Bohr’s Model

 Has been called planetary model
   Energy levels occupied by electrons are like orbits of planets at
    different distances from the sun (nucleus)
Electron Cloud Model

 Model accepted today
 Electrons dart around in an energy level
 Rapid, random motion creates a “cloud” of negative
  charge around nucleus
 Electron cloud gives atom its size and shape
Electron Cloud Model
Findings


 Eugen Goldstein in 1886 observed
  what is now called the “proton” -
  particles with a positive charge, and
  a relative mass of 1 (or 1840 times
  that of an electron)
 1932 – James Chadwick confirmed
  the existence of the “neutron” – a
  particle with no charge, but a mass
  nearly equal to a proton
Atomic Number
 Atoms are composed of identical
 protons, neutrons, and electrons
  How then are atoms of one element different
  from another element?
 Elements are different because they
  contain different numbers of PROTONS
 The “atomic number” of an element is
  the number of protons in the nucleus
 # protons in an atom = # electrons
Atomic Number

Atomic number (Z) of an element is
the number of protons in the nucleus
of each atom of that element.
   Element      # of protons   Atomic # (Z)

   Carbon            6              6

 Phosphorus         15             15

    Gold            79             79
Mass Number

Mass number is the number of
protons and neutrons in the nucleus
of an isotope: Mass # = p+ + n0
Nuclide              p+   n0   e- Mass #
Oxygen - 18          8    10   8    18

Arsenic - 75         33   42   33   75

Phosphorus - 31      15   16   15   31
The Complete Set-UP

  Contain the symbol of the
   element, the mass number and the
   atomic number.
Superscript →
              Mass
              number


Subscript →
                Atomic
                number
                         X
Isotopes

Dalton was wrong about all
 elements of the same type being
 identical
Atoms of the same element can
 have different numbers of
 neutrons.
Thus, different mass numbers.
These are called isotopes.
Isotopes

 Frederick Soddy (1877-1956)
 proposed the idea of isotopes in
 1912
 Isotopes are atoms of the same element having
 different masses, due to varying numbers of
 neutrons.
 Soddy won the Nobel Prize in Chemistry
 in 1921 for his work with isotopes and
 radioactive materials.
Naming Isotopes

We can also put the mass
number after the name of the
element:
carbon-12

carbon-14

uranium-235
Isotopes are atoms of the same element having
different masses, due to varying numbers of
neutrons.
  Isotope     Protons Electrons   Neutrons   Nucleus
Hydrogen–1
 (protium)      1         1          0
Hydrogen-2
(deuterium)     1         1          1

Hydrogen-3      1         1          2
 (tritium)
Isotopes
Elements
occur in
nature as
mixtures of
isotopes.
Isotopes are
atoms of the
same element
that differ in
the number of
neutrons.

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4.1

  • 1. Introduction to Atoms CHAPTER 4 SECTION 1
  • 2. History of Atom  All atoms share the same basic structure  During past 200 years, scientists have proposed different models.  An atom is the smallest particle of an element.  Atomic theory grew as a series of models that developed from experimental evidence. As more evidence was collected, the theory and models were revised.
  • 3. Dalton’s Model  Based on experiments, Dalton developed a theory of structure of matter  4 main concepts:  All matter is composed of tiny, indivisible particles called atoms  Atoms of each element are exactly alike  Atoms of different elements have different masses  Atoms of different elements can join to form compounds
  • 5. Thomson’s Model  End of 1800s  Thomson discovered that atoms were not simple, solid spheres  Atoms contained subatomic particles  Very small, negatively charged  Called them electrons
  • 6. Discovery of the Electron In 1897, J.J. Thomson used a cathode ray tube to deduce the presence of a negatively charged particle: the electron
  • 7. Modern Cathode Ray Tubes Television Computer Monitor Cathode ray tubes pass electricity through a gas that is contained at a very low pressure.
  • 8. Thomson’s Model  Also knew that atoms were electrically neutral  Must contain enough positive charge to balance negative charge of electrons  Developed model where electrons were stuck into a positively charged sphere  Like chocolate chips in cookie dough
  • 10. Rutherford’s Model  By early 1900s, scientists knew that positive charge of atom comes from subatomic particles called protons  A proton is a positive charged particle in the nucleus of an atom.  1911—Rutherford begins to test theory  His experiments led him to believe that protons are concentrated in a small area at center of atom  Called this area the nucleus
  • 11. Rutherford’s Model  Rutherford’s model describes an atom as mostly empty space, with a center nucleus that contains nearly all the mass  Like the pit in a peach
  • 12. Bohr’s Model  Modified Rutherford’s model in 1913  Proposed that each electron has a certain amount of energy  Helped electron move around nucleus  Electrons move around nucleus in region called energy levels  The energy level is the specific amount of energy an electron has.  Energy levels surround nucleus in rings, like layers of onion
  • 13. Bohr’s Model  Has been called planetary model  Energy levels occupied by electrons are like orbits of planets at different distances from the sun (nucleus)
  • 14. Electron Cloud Model  Model accepted today  Electrons dart around in an energy level  Rapid, random motion creates a “cloud” of negative charge around nucleus  Electron cloud gives atom its size and shape
  • 16. Findings  Eugen Goldstein in 1886 observed what is now called the “proton” - particles with a positive charge, and a relative mass of 1 (or 1840 times that of an electron)  1932 – James Chadwick confirmed the existence of the “neutron” – a particle with no charge, but a mass nearly equal to a proton
  • 17. Atomic Number  Atoms are composed of identical protons, neutrons, and electrons  How then are atoms of one element different from another element?  Elements are different because they contain different numbers of PROTONS  The “atomic number” of an element is the number of protons in the nucleus  # protons in an atom = # electrons
  • 18. Atomic Number Atomic number (Z) of an element is the number of protons in the nucleus of each atom of that element. Element # of protons Atomic # (Z) Carbon 6 6 Phosphorus 15 15 Gold 79 79
  • 19. Mass Number Mass number is the number of protons and neutrons in the nucleus of an isotope: Mass # = p+ + n0 Nuclide p+ n0 e- Mass # Oxygen - 18 8 10 8 18 Arsenic - 75 33 42 33 75 Phosphorus - 31 15 16 15 31
  • 20. The Complete Set-UP  Contain the symbol of the element, the mass number and the atomic number. Superscript → Mass number Subscript → Atomic number X
  • 21. Isotopes Dalton was wrong about all elements of the same type being identical Atoms of the same element can have different numbers of neutrons. Thus, different mass numbers. These are called isotopes.
  • 22. Isotopes  Frederick Soddy (1877-1956) proposed the idea of isotopes in 1912  Isotopes are atoms of the same element having different masses, due to varying numbers of neutrons.  Soddy won the Nobel Prize in Chemistry in 1921 for his work with isotopes and radioactive materials.
  • 23. Naming Isotopes We can also put the mass number after the name of the element: carbon-12 carbon-14 uranium-235
  • 24. Isotopes are atoms of the same element having different masses, due to varying numbers of neutrons. Isotope Protons Electrons Neutrons Nucleus Hydrogen–1 (protium) 1 1 0 Hydrogen-2 (deuterium) 1 1 1 Hydrogen-3 1 1 2 (tritium)
  • 25. Isotopes Elements occur in nature as mixtures of isotopes. Isotopes are atoms of the same element that differ in the number of neutrons.