SlideShare a Scribd company logo
1 of 29
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Origin of the Solar System
Our theory must explain the data
1. Large bodies in the Solar System have
orderly motions.
2. There are two types of planets.
– small, rocky terrestrial planets
– large, hydrogen-rich Jovian planets
3. Asteroids & comets exist in certain regions
of the Solar System
4. There are exceptions to these patterns.
© 2005 Pearson Education Inc., publishing as Addison-Wesley
The Solar Nebula
• The nebular theory holds that
our Solar System formed out
of a nebula which collapsed
under its own gravity.
• observational evidence
– We observe stars in the
process of forming today.
– The are always found within
interstellar clouds of gas.
– This image shows the Orion
Nebula..newborn solar
systems within!
solar nebula – name given to
the cloud of gas from which our
own Solar System formed
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Gravitational Collapse
• The solar nebular was initially somewhat spherical and a
few light years in diameter.
– very cold
– rotating slightly
• It was given a “push” by some event.
– perhaps the shock wave from a nearby supernova
• As the nebula shrank, gravity increased, causing collapse.
• As the nebula “falls” inward, gravitational potential
energy is converted to heat.
– Conservation of Energy
• As the nebula’s radius decreases, it rotates faster
– Conservation of Angular Momentum
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Flattening of the Solar Nebula
• As the nebula collapses, clumps of gas collide & merge.
• Their random velocities average out into the nebula’s
direction of rotation.
• The spinning nebula assumes the shape of a disk.
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Why does the cloud spin?
• Its part of a spinning galaxy—lots of angular
momentum avaialble
• Particles closer to the center of galaxy move more
rapily than particles farther away..speed decreases
with radial distance.
• As a shock wave and then gravity compress the
cloud, angular momentum must be conserved, so
toques transfer some angular momentum from the
galactic disk to the interstellar cloud.
• This is similar to the formation of cyclones and
hurricanes in our atmosphere.
© 2005 Pearson Education Inc., publishing as Addison-Wesley
The Coriolis effect
• Air moves fastest at the equator due to the Earths
Spin
• As temp differences causes air currents to move
North south, the result is a whilpool of air
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Rotating disk with collapsing cloud
Imagine disk of Galaxy seen from above
Note:
Speed decreases With radial
distance
Stars in Galaxy
orbit about
center of galaxy
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Rotating disk with collapsing cloud
Centripital force (gravity) makes particles orbit center
of cloud, while cloud orbits center of galaxy.
Particles on outside rotate more slowly about galactic
center
Stars on inside rotate more rapidly
Collisions occur
Faster particles will win!
Disk begins to swirl!
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Collapse of the Solar Nebula
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Orderly Motions in the Solar System
• The Sun formed in the very center of the nebula.
– temperature & density were high enough for nuclear fusion
reactions to begin
• The planets formed in the rest of the disk.
• This would explain the following:
– all planets lie along one plane (in the disk)
– all planets orbit in one direction (the spin direction of the disk)
– the Sun rotates in the same direction
– the planets would tend to rotate in this same direction
– most moons orbit in this direction
– most planetary orbits are near circular (collisions in the disk)
© 2005 Pearson Education Inc., publishing as Addison-Wesley
More Support for the Nebular Theory
• We have observed disks around other stars.
• These could be new planetary systems in formation.
 Pictoris
AB Aurigae
Proto-Solar
systems in the
Orion Nebula!
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Building the Planets
Condensation – elements & compounds began to
condense (i.e. solidify) out of the nebula…. depending
on temperature!
Imagine atoms and molecules coming together atom by
atom—electric force and ionization is main mechanism
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Building the Planets
…and temperature in the Solar nebula
depended on distance from the Sun!
© 2005 Pearson Education Inc., publishing as Addison-Wesley
The Young Sun emitted pulses of
UV and X-rays
• These photons ionized some atoms in the
solar nebula and deposited charge on others
• These made the atoms and molecules
“sticky”
• Try to slide down a plastic slide on a dry,
sunny day. Your hair will stand up!
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Building the Planets
So only rocks & metals condensed within 3.5 AU
of the Sun… the so-called frost line.
Hydrogen compounds (ices) condensed beyond the
frost line.
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Building the Planets
accretion -- small grains stick to one another via
electromagnetic force until they are massive enough to
attract via gravity to form...acretion is mostly a
gravitational effect..macroscopic objects attracting one
another
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Acretion continues today!
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Building the Planets
…After condensation produces macrosopic objects
These will:• combine near the Sun to form rocky planets
• combine beyond the frostline to form icy planetesimals
which…
• capture H/He far from Sun to form gas planets
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Building the Planets
• Each gas (Jovian) planet formed its own “miniature”
solar nebula.
• Moons formed out of the disk.
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Building the Planets
solar wind --- charged particles streaming out from
the Sun cleared away the leftover gas—this might be
a relatively rare event!
Other solar systems show evidence that their nebulae
weren’t cleared out!
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Origin of the Asteroids
• The Solar wind cleared the leftover gas, but not the
leftover planetesimals.
• Those leftover rocky planetesimals which did not
accrete onto a planet are the present-day asteroids.
• Most inhabit the asteroid belt between Mars & Jupiter.
– Jupiter’s gravity prevented a planet from forming there.
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Origin of the Comets
• The leftover icy
planetesimals are the
present-day comets.
• Those which were
located between the
Jovian planets, if not
captured, were
gravitationally flung in
all directions into the
Oort cloud.
• Those beyond
Neptune’s orbit
remained in the ecliptic
plane in what we call
the Kuiper belt.
The nebular theory predicted the existence
of the Kuiper belt 40 years before it was
discovered!
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Exceptions to the Rules
• There were many more leftover planetesimals than we
see today.
• Most of them collided with the newly-formed planets
& moons during the first few 108 years of the Solar
System.
• We call this the heavy bombardment period.
So how does the nebular theory deal with exceptions,
i.e. data which do not fit the model’s predictions?
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Exceptions to the Rules
• Why some moons orbit opposite their planet’s rotation
– captured moons (e.g. Triton)
• Why rotation axes of some planets are tilted
– impacts “knock them over” (extreme example: Uranus)
• Why some planets rotate more quickly than others
– impacts “spin them up”
• Why Earth is the only terrestrial planet with a large
Moon
– giant impact
Close encounters with and impacts by planetesimals could explain:
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Formation of the Moon
(Giant Impact Theory)
• The Earth was struck by a
Mars-sized planetesimal
• A part of Earth’s mantle
was ejected
• This coalesced in the
Moon.
– it orbits in same direction as
Earth rotates
– lower density than Earth
– Earth was “spun up”
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Formation of Moon
(illustration from Joe Tucciarone
http://www.monkeytime.com/sciencemaster/
galleries/jt_space/gallery.php)
See: move at:
http://yso.mtk.nao.ac.jp/~kokubo/
moon/kit/movie.html
© 2005 Pearson Education Inc., publishing as Addison-Wesley
9.5 How Old is the Solar System?
• How do we measure the age of a rock?
• How old is the Solar System and how do we
know?
© 2005 Pearson Education Inc., publishing as Addison-Wesley
Radiometric Dating
• Isotopes which are unstable are
said to be radioactive.
• They spontaneously change in
to another isotope in a process
called radioactive decay.
– protons convert to neutrons
– neutrons convert to protons
• The time it takes half the
amount of a radioactive isotope
to decay is called its half life.
• By knowing rock chemistry, we chose a stable isotope which does
not form with the rock…its presence is due solely to decay.
• Measuring the relative amounts of the two isotopes and knowing
the half life of the radioactive isotope tells us the age of the rock.
© 2005 Pearson Education Inc., publishing as Addison-Wesley
The Age of our Solar System
• Radiometric dating can only measure the age of a rock
since it solidified.
• Geologic processes on Earth cause rock to melt and
resolidify.
 Earth rocks can’t be used to measure the Solar System’s age.
• We must find rocks which have not melted or vaporized
since the condensed from the Solar nebula.
– meteorites imply an age of 4.6 billion years for Solar System
– This value is consistent with the age of the oldest moon rocks (4.4
billion years)
• Radioactive isotopes are formed in stars & supernovae
– suggests that Solar System formation was triggered by supernova
– short half lives suggest the supernova was nearby

More Related Content

What's hot

What's hot (20)

What is Solar system? FORMATION OF SOLAR SYSTEM. SOLAR SYSTEM: Structure
What is Solar system? FORMATION OF SOLAR SYSTEM. SOLAR SYSTEM: StructureWhat is Solar system? FORMATION OF SOLAR SYSTEM. SOLAR SYSTEM: Structure
What is Solar system? FORMATION OF SOLAR SYSTEM. SOLAR SYSTEM: Structure
 
The Solar System (Space)
The Solar System (Space)The Solar System (Space)
The Solar System (Space)
 
Solar System Planets
Solar System PlanetsSolar System Planets
Solar System Planets
 
Lesson 7 solar system
Lesson 7 solar systemLesson 7 solar system
Lesson 7 solar system
 
Touring our solar system (astronomy)
Touring  our solar system (astronomy)Touring  our solar system (astronomy)
Touring our solar system (astronomy)
 
The solar system
The solar systemThe solar system
The solar system
 
Astronamy in quran.ppt saleel@hira
Astronamy in quran.ppt saleel@hiraAstronamy in quran.ppt saleel@hira
Astronamy in quran.ppt saleel@hira
 
Planets and Moon
Planets and MoonPlanets and Moon
Planets and Moon
 
Earth and Life Science - The Solar System
Earth and Life Science - The Solar SystemEarth and Life Science - The Solar System
Earth and Life Science - The Solar System
 
Solar system
Solar systemSolar system
Solar system
 
Amber
AmberAmber
Amber
 
Presentation on solar system
Presentation on solar systemPresentation on solar system
Presentation on solar system
 
The Solar System
The Solar SystemThe Solar System
The Solar System
 
Moon's Properties and Characteristics
Moon's Properties and CharacteristicsMoon's Properties and Characteristics
Moon's Properties and Characteristics
 
PSunit3notes
PSunit3notesPSunit3notes
PSunit3notes
 
SOLAR SYSTEM PPT CLASS 8
SOLAR SYSTEM  PPT CLASS 8 SOLAR SYSTEM  PPT CLASS 8
SOLAR SYSTEM PPT CLASS 8
 
Beyond the solar system
Beyond the solar systemBeyond the solar system
Beyond the solar system
 
Presentation earth and space
Presentation   earth and space Presentation   earth and space
Presentation earth and space
 
Beyond Our Solar System
Beyond Our Solar SystemBeyond Our Solar System
Beyond Our Solar System
 
4th Grade Solar System PowerPoint Project
4th Grade Solar System PowerPoint Project4th Grade Solar System PowerPoint Project
4th Grade Solar System PowerPoint Project
 

Similar to Solar System Formation

Astonishing Astronomy 101 - Chapter 6
Astonishing Astronomy 101 - Chapter 6Astonishing Astronomy 101 - Chapter 6
Astonishing Astronomy 101 - Chapter 6Don R. Mueller, Ph.D.
 
Sophie & char formation of the solar system
Sophie & char formation of the solar systemSophie & char formation of the solar system
Sophie & char formation of the solar systemwhitmers
 
Solar System Formation/Sun/Comets/Meteors
Solar System Formation/Sun/Comets/MeteorsSolar System Formation/Sun/Comets/Meteors
Solar System Formation/Sun/Comets/MeteorsBantay's Earth Science!
 
The Sun and our Solar System
The Sun and our Solar System The Sun and our Solar System
The Sun and our Solar System Jeanie Lacob
 
Solar system PPT
Solar system PPTSolar system PPT
Solar system PPTNamisha2001
 
Solar system PPT
Solar system PPT Solar system PPT
Solar system PPT Namisha2001
 
The Universe, the eight planets, The sun
The Universe, the eight planets, The sunThe Universe, the eight planets, The sun
The Universe, the eight planets, The sunprinceexplore0
 
Apes earth systems
Apes  earth systemsApes  earth systems
Apes earth systemsBobby Lewis
 
Lesson 13 the earth in the solar system
Lesson 13  the earth in the solar systemLesson 13  the earth in the solar system
Lesson 13 the earth in the solar systemPRIYANKA ABRAHAM
 
2017 Formation of Solar System.ppt
2017 Formation of Solar System.ppt2017 Formation of Solar System.ppt
2017 Formation of Solar System.pptCharlesBuale1
 
THEORIES OF EARTH’S FORMATION.pptx
THEORIES OF EARTH’S FORMATION.pptxTHEORIES OF EARTH’S FORMATION.pptx
THEORIES OF EARTH’S FORMATION.pptxlevi0417
 
Solar system & planets
Solar system & planetsSolar system & planets
Solar system & planetsSanyam Gandotra
 
COMETS, ASTEROIDS AND METEORS.pptx
COMETS, ASTEROIDS AND METEORS.pptxCOMETS, ASTEROIDS AND METEORS.pptx
COMETS, ASTEROIDS AND METEORS.pptxsayfranco
 
Solar system & planets
Solar system & planetsSolar system & planets
Solar system & planetsshanoofsharaf
 
Solar system p0wer point presentation
Solar system p0wer point presentationSolar system p0wer point presentation
Solar system p0wer point presentationsarithaspr
 

Similar to Solar System Formation (20)

Astonishing Astronomy 101 - Chapter 6
Astonishing Astronomy 101 - Chapter 6Astonishing Astronomy 101 - Chapter 6
Astonishing Astronomy 101 - Chapter 6
 
Sophie & char formation of the solar system
Sophie & char formation of the solar systemSophie & char formation of the solar system
Sophie & char formation of the solar system
 
Solar system
Solar systemSolar system
Solar system
 
Solar System Formation/Sun/Comets/Meteors
Solar System Formation/Sun/Comets/MeteorsSolar System Formation/Sun/Comets/Meteors
Solar System Formation/Sun/Comets/Meteors
 
The Sun and our Solar System
The Sun and our Solar System The Sun and our Solar System
The Sun and our Solar System
 
Solar system PPT
Solar system PPTSolar system PPT
Solar system PPT
 
12 lecture outline
12 lecture outline12 lecture outline
12 lecture outline
 
Solar system PPT
Solar system PPT Solar system PPT
Solar system PPT
 
The Universe, the eight planets, The sun
The Universe, the eight planets, The sunThe Universe, the eight planets, The sun
The Universe, the eight planets, The sun
 
Apes earth systems
Apes  earth systemsApes  earth systems
Apes earth systems
 
Lesson 13 the earth in the solar system
Lesson 13  the earth in the solar systemLesson 13  the earth in the solar system
Lesson 13 the earth in the solar system
 
2017 Formation of Solar System.ppt
2017 Formation of Solar System.ppt2017 Formation of Solar System.ppt
2017 Formation of Solar System.ppt
 
GEO610 Module I.pdf
GEO610 Module I.pdfGEO610 Module I.pdf
GEO610 Module I.pdf
 
THEORIES OF EARTH’S FORMATION.pptx
THEORIES OF EARTH’S FORMATION.pptxTHEORIES OF EARTH’S FORMATION.pptx
THEORIES OF EARTH’S FORMATION.pptx
 
Solar system & planets
Solar system & planetsSolar system & planets
Solar system & planets
 
COMETS, ASTEROIDS AND METEORS.pptx
COMETS, ASTEROIDS AND METEORS.pptxCOMETS, ASTEROIDS AND METEORS.pptx
COMETS, ASTEROIDS AND METEORS.pptx
 
Solar system & planets
Solar system & planetsSolar system & planets
Solar system & planets
 
The Universe
The UniverseThe Universe
The Universe
 
Astronomy
AstronomyAstronomy
Astronomy
 
Solar system p0wer point presentation
Solar system p0wer point presentationSolar system p0wer point presentation
Solar system p0wer point presentation
 

Recently uploaded

Unlocking the Potential: Deep dive into ocean of Ceramic Magnets.pptx
Unlocking  the Potential: Deep dive into ocean of Ceramic Magnets.pptxUnlocking  the Potential: Deep dive into ocean of Ceramic Magnets.pptx
Unlocking the Potential: Deep dive into ocean of Ceramic Magnets.pptxanandsmhk
 
Chemistry 4th semester series (krishna).pdf
Chemistry 4th semester series (krishna).pdfChemistry 4th semester series (krishna).pdf
Chemistry 4th semester series (krishna).pdfSumit Kumar yadav
 
Asymmetry in the atmosphere of the ultra-hot Jupiter WASP-76 b
Asymmetry in the atmosphere of the ultra-hot Jupiter WASP-76 bAsymmetry in the atmosphere of the ultra-hot Jupiter WASP-76 b
Asymmetry in the atmosphere of the ultra-hot Jupiter WASP-76 bSérgio Sacani
 
Recombination DNA Technology (Nucleic Acid Hybridization )
Recombination DNA Technology (Nucleic Acid Hybridization )Recombination DNA Technology (Nucleic Acid Hybridization )
Recombination DNA Technology (Nucleic Acid Hybridization )aarthirajkumar25
 
Formation of low mass protostars and their circumstellar disks
Formation of low mass protostars and their circumstellar disksFormation of low mass protostars and their circumstellar disks
Formation of low mass protostars and their circumstellar disksSérgio Sacani
 
Animal Communication- Auditory and Visual.pptx
Animal Communication- Auditory and Visual.pptxAnimal Communication- Auditory and Visual.pptx
Animal Communication- Auditory and Visual.pptxUmerFayaz5
 
Natural Polymer Based Nanomaterials
Natural Polymer Based NanomaterialsNatural Polymer Based Nanomaterials
Natural Polymer Based NanomaterialsAArockiyaNisha
 
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCR
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCRStunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCR
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCRDelhi Call girls
 
DIFFERENCE IN BACK CROSS AND TEST CROSS
DIFFERENCE IN  BACK CROSS AND TEST CROSSDIFFERENCE IN  BACK CROSS AND TEST CROSS
DIFFERENCE IN BACK CROSS AND TEST CROSSLeenakshiTyagi
 
Physiochemical properties of nanomaterials and its nanotoxicity.pptx
Physiochemical properties of nanomaterials and its nanotoxicity.pptxPhysiochemical properties of nanomaterials and its nanotoxicity.pptx
Physiochemical properties of nanomaterials and its nanotoxicity.pptxAArockiyaNisha
 
All-domain Anomaly Resolution Office U.S. Department of Defense (U) Case: “Eg...
All-domain Anomaly Resolution Office U.S. Department of Defense (U) Case: “Eg...All-domain Anomaly Resolution Office U.S. Department of Defense (U) Case: “Eg...
All-domain Anomaly Resolution Office U.S. Department of Defense (U) Case: “Eg...Sérgio Sacani
 
Nanoparticles synthesis and characterization​ ​
Nanoparticles synthesis and characterization​  ​Nanoparticles synthesis and characterization​  ​
Nanoparticles synthesis and characterization​ ​kaibalyasahoo82800
 
Pulmonary drug delivery system M.pharm -2nd sem P'ceutics
Pulmonary drug delivery system M.pharm -2nd sem P'ceuticsPulmonary drug delivery system M.pharm -2nd sem P'ceutics
Pulmonary drug delivery system M.pharm -2nd sem P'ceuticssakshisoni2385
 
Botany 4th semester file By Sumit Kumar yadav.pdf
Botany 4th semester file By Sumit Kumar yadav.pdfBotany 4th semester file By Sumit Kumar yadav.pdf
Botany 4th semester file By Sumit Kumar yadav.pdfSumit Kumar yadav
 
Discovery of an Accretion Streamer and a Slow Wide-angle Outflow around FUOri...
Discovery of an Accretion Streamer and a Slow Wide-angle Outflow around FUOri...Discovery of an Accretion Streamer and a Slow Wide-angle Outflow around FUOri...
Discovery of an Accretion Streamer and a Slow Wide-angle Outflow around FUOri...Sérgio Sacani
 
Raman spectroscopy.pptx M Pharm, M Sc, Advanced Spectral Analysis
Raman spectroscopy.pptx M Pharm, M Sc, Advanced Spectral AnalysisRaman spectroscopy.pptx M Pharm, M Sc, Advanced Spectral Analysis
Raman spectroscopy.pptx M Pharm, M Sc, Advanced Spectral AnalysisDiwakar Mishra
 
fundamental of entomology all in one topics of entomology
fundamental of entomology all in one topics of entomologyfundamental of entomology all in one topics of entomology
fundamental of entomology all in one topics of entomologyDrAnita Sharma
 
GBSN - Microbiology (Unit 1)
GBSN - Microbiology (Unit 1)GBSN - Microbiology (Unit 1)
GBSN - Microbiology (Unit 1)Areesha Ahmad
 
PossibleEoarcheanRecordsoftheGeomagneticFieldPreservedintheIsuaSupracrustalBe...
PossibleEoarcheanRecordsoftheGeomagneticFieldPreservedintheIsuaSupracrustalBe...PossibleEoarcheanRecordsoftheGeomagneticFieldPreservedintheIsuaSupracrustalBe...
PossibleEoarcheanRecordsoftheGeomagneticFieldPreservedintheIsuaSupracrustalBe...Sérgio Sacani
 
Zoology 4th semester series (krishna).pdf
Zoology 4th semester series (krishna).pdfZoology 4th semester series (krishna).pdf
Zoology 4th semester series (krishna).pdfSumit Kumar yadav
 

Recently uploaded (20)

Unlocking the Potential: Deep dive into ocean of Ceramic Magnets.pptx
Unlocking  the Potential: Deep dive into ocean of Ceramic Magnets.pptxUnlocking  the Potential: Deep dive into ocean of Ceramic Magnets.pptx
Unlocking the Potential: Deep dive into ocean of Ceramic Magnets.pptx
 
Chemistry 4th semester series (krishna).pdf
Chemistry 4th semester series (krishna).pdfChemistry 4th semester series (krishna).pdf
Chemistry 4th semester series (krishna).pdf
 
Asymmetry in the atmosphere of the ultra-hot Jupiter WASP-76 b
Asymmetry in the atmosphere of the ultra-hot Jupiter WASP-76 bAsymmetry in the atmosphere of the ultra-hot Jupiter WASP-76 b
Asymmetry in the atmosphere of the ultra-hot Jupiter WASP-76 b
 
Recombination DNA Technology (Nucleic Acid Hybridization )
Recombination DNA Technology (Nucleic Acid Hybridization )Recombination DNA Technology (Nucleic Acid Hybridization )
Recombination DNA Technology (Nucleic Acid Hybridization )
 
Formation of low mass protostars and their circumstellar disks
Formation of low mass protostars and their circumstellar disksFormation of low mass protostars and their circumstellar disks
Formation of low mass protostars and their circumstellar disks
 
Animal Communication- Auditory and Visual.pptx
Animal Communication- Auditory and Visual.pptxAnimal Communication- Auditory and Visual.pptx
Animal Communication- Auditory and Visual.pptx
 
Natural Polymer Based Nanomaterials
Natural Polymer Based NanomaterialsNatural Polymer Based Nanomaterials
Natural Polymer Based Nanomaterials
 
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCR
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCRStunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCR
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCR
 
DIFFERENCE IN BACK CROSS AND TEST CROSS
DIFFERENCE IN  BACK CROSS AND TEST CROSSDIFFERENCE IN  BACK CROSS AND TEST CROSS
DIFFERENCE IN BACK CROSS AND TEST CROSS
 
Physiochemical properties of nanomaterials and its nanotoxicity.pptx
Physiochemical properties of nanomaterials and its nanotoxicity.pptxPhysiochemical properties of nanomaterials and its nanotoxicity.pptx
Physiochemical properties of nanomaterials and its nanotoxicity.pptx
 
All-domain Anomaly Resolution Office U.S. Department of Defense (U) Case: “Eg...
All-domain Anomaly Resolution Office U.S. Department of Defense (U) Case: “Eg...All-domain Anomaly Resolution Office U.S. Department of Defense (U) Case: “Eg...
All-domain Anomaly Resolution Office U.S. Department of Defense (U) Case: “Eg...
 
Nanoparticles synthesis and characterization​ ​
Nanoparticles synthesis and characterization​  ​Nanoparticles synthesis and characterization​  ​
Nanoparticles synthesis and characterization​ ​
 
Pulmonary drug delivery system M.pharm -2nd sem P'ceutics
Pulmonary drug delivery system M.pharm -2nd sem P'ceuticsPulmonary drug delivery system M.pharm -2nd sem P'ceutics
Pulmonary drug delivery system M.pharm -2nd sem P'ceutics
 
Botany 4th semester file By Sumit Kumar yadav.pdf
Botany 4th semester file By Sumit Kumar yadav.pdfBotany 4th semester file By Sumit Kumar yadav.pdf
Botany 4th semester file By Sumit Kumar yadav.pdf
 
Discovery of an Accretion Streamer and a Slow Wide-angle Outflow around FUOri...
Discovery of an Accretion Streamer and a Slow Wide-angle Outflow around FUOri...Discovery of an Accretion Streamer and a Slow Wide-angle Outflow around FUOri...
Discovery of an Accretion Streamer and a Slow Wide-angle Outflow around FUOri...
 
Raman spectroscopy.pptx M Pharm, M Sc, Advanced Spectral Analysis
Raman spectroscopy.pptx M Pharm, M Sc, Advanced Spectral AnalysisRaman spectroscopy.pptx M Pharm, M Sc, Advanced Spectral Analysis
Raman spectroscopy.pptx M Pharm, M Sc, Advanced Spectral Analysis
 
fundamental of entomology all in one topics of entomology
fundamental of entomology all in one topics of entomologyfundamental of entomology all in one topics of entomology
fundamental of entomology all in one topics of entomology
 
GBSN - Microbiology (Unit 1)
GBSN - Microbiology (Unit 1)GBSN - Microbiology (Unit 1)
GBSN - Microbiology (Unit 1)
 
PossibleEoarcheanRecordsoftheGeomagneticFieldPreservedintheIsuaSupracrustalBe...
PossibleEoarcheanRecordsoftheGeomagneticFieldPreservedintheIsuaSupracrustalBe...PossibleEoarcheanRecordsoftheGeomagneticFieldPreservedintheIsuaSupracrustalBe...
PossibleEoarcheanRecordsoftheGeomagneticFieldPreservedintheIsuaSupracrustalBe...
 
Zoology 4th semester series (krishna).pdf
Zoology 4th semester series (krishna).pdfZoology 4th semester series (krishna).pdf
Zoology 4th semester series (krishna).pdf
 

Solar System Formation

  • 1. © 2005 Pearson Education Inc., publishing as Addison-Wesley Origin of the Solar System Our theory must explain the data 1. Large bodies in the Solar System have orderly motions. 2. There are two types of planets. – small, rocky terrestrial planets – large, hydrogen-rich Jovian planets 3. Asteroids & comets exist in certain regions of the Solar System 4. There are exceptions to these patterns.
  • 2. © 2005 Pearson Education Inc., publishing as Addison-Wesley The Solar Nebula • The nebular theory holds that our Solar System formed out of a nebula which collapsed under its own gravity. • observational evidence – We observe stars in the process of forming today. – The are always found within interstellar clouds of gas. – This image shows the Orion Nebula..newborn solar systems within! solar nebula – name given to the cloud of gas from which our own Solar System formed
  • 3. © 2005 Pearson Education Inc., publishing as Addison-Wesley Gravitational Collapse • The solar nebular was initially somewhat spherical and a few light years in diameter. – very cold – rotating slightly • It was given a “push” by some event. – perhaps the shock wave from a nearby supernova • As the nebula shrank, gravity increased, causing collapse. • As the nebula “falls” inward, gravitational potential energy is converted to heat. – Conservation of Energy • As the nebula’s radius decreases, it rotates faster – Conservation of Angular Momentum
  • 4. © 2005 Pearson Education Inc., publishing as Addison-Wesley Flattening of the Solar Nebula • As the nebula collapses, clumps of gas collide & merge. • Their random velocities average out into the nebula’s direction of rotation. • The spinning nebula assumes the shape of a disk.
  • 5. © 2005 Pearson Education Inc., publishing as Addison-Wesley Why does the cloud spin? • Its part of a spinning galaxy—lots of angular momentum avaialble • Particles closer to the center of galaxy move more rapily than particles farther away..speed decreases with radial distance. • As a shock wave and then gravity compress the cloud, angular momentum must be conserved, so toques transfer some angular momentum from the galactic disk to the interstellar cloud. • This is similar to the formation of cyclones and hurricanes in our atmosphere.
  • 6. © 2005 Pearson Education Inc., publishing as Addison-Wesley The Coriolis effect • Air moves fastest at the equator due to the Earths Spin • As temp differences causes air currents to move North south, the result is a whilpool of air
  • 7. © 2005 Pearson Education Inc., publishing as Addison-Wesley Rotating disk with collapsing cloud Imagine disk of Galaxy seen from above Note: Speed decreases With radial distance Stars in Galaxy orbit about center of galaxy
  • 8. © 2005 Pearson Education Inc., publishing as Addison-Wesley Rotating disk with collapsing cloud Centripital force (gravity) makes particles orbit center of cloud, while cloud orbits center of galaxy. Particles on outside rotate more slowly about galactic center Stars on inside rotate more rapidly Collisions occur Faster particles will win! Disk begins to swirl!
  • 9. © 2005 Pearson Education Inc., publishing as Addison-Wesley Collapse of the Solar Nebula
  • 10. © 2005 Pearson Education Inc., publishing as Addison-Wesley Orderly Motions in the Solar System • The Sun formed in the very center of the nebula. – temperature & density were high enough for nuclear fusion reactions to begin • The planets formed in the rest of the disk. • This would explain the following: – all planets lie along one plane (in the disk) – all planets orbit in one direction (the spin direction of the disk) – the Sun rotates in the same direction – the planets would tend to rotate in this same direction – most moons orbit in this direction – most planetary orbits are near circular (collisions in the disk)
  • 11. © 2005 Pearson Education Inc., publishing as Addison-Wesley More Support for the Nebular Theory • We have observed disks around other stars. • These could be new planetary systems in formation.  Pictoris AB Aurigae Proto-Solar systems in the Orion Nebula!
  • 12. © 2005 Pearson Education Inc., publishing as Addison-Wesley Building the Planets Condensation – elements & compounds began to condense (i.e. solidify) out of the nebula…. depending on temperature! Imagine atoms and molecules coming together atom by atom—electric force and ionization is main mechanism
  • 13. © 2005 Pearson Education Inc., publishing as Addison-Wesley Building the Planets …and temperature in the Solar nebula depended on distance from the Sun!
  • 14. © 2005 Pearson Education Inc., publishing as Addison-Wesley The Young Sun emitted pulses of UV and X-rays • These photons ionized some atoms in the solar nebula and deposited charge on others • These made the atoms and molecules “sticky” • Try to slide down a plastic slide on a dry, sunny day. Your hair will stand up!
  • 15. © 2005 Pearson Education Inc., publishing as Addison-Wesley Building the Planets So only rocks & metals condensed within 3.5 AU of the Sun… the so-called frost line. Hydrogen compounds (ices) condensed beyond the frost line.
  • 16. © 2005 Pearson Education Inc., publishing as Addison-Wesley Building the Planets accretion -- small grains stick to one another via electromagnetic force until they are massive enough to attract via gravity to form...acretion is mostly a gravitational effect..macroscopic objects attracting one another
  • 17. © 2005 Pearson Education Inc., publishing as Addison-Wesley Acretion continues today!
  • 18. © 2005 Pearson Education Inc., publishing as Addison-Wesley Building the Planets …After condensation produces macrosopic objects These will:• combine near the Sun to form rocky planets • combine beyond the frostline to form icy planetesimals which… • capture H/He far from Sun to form gas planets
  • 19. © 2005 Pearson Education Inc., publishing as Addison-Wesley Building the Planets • Each gas (Jovian) planet formed its own “miniature” solar nebula. • Moons formed out of the disk.
  • 20. © 2005 Pearson Education Inc., publishing as Addison-Wesley Building the Planets solar wind --- charged particles streaming out from the Sun cleared away the leftover gas—this might be a relatively rare event! Other solar systems show evidence that their nebulae weren’t cleared out!
  • 21. © 2005 Pearson Education Inc., publishing as Addison-Wesley Origin of the Asteroids • The Solar wind cleared the leftover gas, but not the leftover planetesimals. • Those leftover rocky planetesimals which did not accrete onto a planet are the present-day asteroids. • Most inhabit the asteroid belt between Mars & Jupiter. – Jupiter’s gravity prevented a planet from forming there.
  • 22. © 2005 Pearson Education Inc., publishing as Addison-Wesley Origin of the Comets • The leftover icy planetesimals are the present-day comets. • Those which were located between the Jovian planets, if not captured, were gravitationally flung in all directions into the Oort cloud. • Those beyond Neptune’s orbit remained in the ecliptic plane in what we call the Kuiper belt. The nebular theory predicted the existence of the Kuiper belt 40 years before it was discovered!
  • 23. © 2005 Pearson Education Inc., publishing as Addison-Wesley Exceptions to the Rules • There were many more leftover planetesimals than we see today. • Most of them collided with the newly-formed planets & moons during the first few 108 years of the Solar System. • We call this the heavy bombardment period. So how does the nebular theory deal with exceptions, i.e. data which do not fit the model’s predictions?
  • 24. © 2005 Pearson Education Inc., publishing as Addison-Wesley Exceptions to the Rules • Why some moons orbit opposite their planet’s rotation – captured moons (e.g. Triton) • Why rotation axes of some planets are tilted – impacts “knock them over” (extreme example: Uranus) • Why some planets rotate more quickly than others – impacts “spin them up” • Why Earth is the only terrestrial planet with a large Moon – giant impact Close encounters with and impacts by planetesimals could explain:
  • 25. © 2005 Pearson Education Inc., publishing as Addison-Wesley Formation of the Moon (Giant Impact Theory) • The Earth was struck by a Mars-sized planetesimal • A part of Earth’s mantle was ejected • This coalesced in the Moon. – it orbits in same direction as Earth rotates – lower density than Earth – Earth was “spun up”
  • 26. © 2005 Pearson Education Inc., publishing as Addison-Wesley Formation of Moon (illustration from Joe Tucciarone http://www.monkeytime.com/sciencemaster/ galleries/jt_space/gallery.php) See: move at: http://yso.mtk.nao.ac.jp/~kokubo/ moon/kit/movie.html
  • 27. © 2005 Pearson Education Inc., publishing as Addison-Wesley 9.5 How Old is the Solar System? • How do we measure the age of a rock? • How old is the Solar System and how do we know?
  • 28. © 2005 Pearson Education Inc., publishing as Addison-Wesley Radiometric Dating • Isotopes which are unstable are said to be radioactive. • They spontaneously change in to another isotope in a process called radioactive decay. – protons convert to neutrons – neutrons convert to protons • The time it takes half the amount of a radioactive isotope to decay is called its half life. • By knowing rock chemistry, we chose a stable isotope which does not form with the rock…its presence is due solely to decay. • Measuring the relative amounts of the two isotopes and knowing the half life of the radioactive isotope tells us the age of the rock.
  • 29. © 2005 Pearson Education Inc., publishing as Addison-Wesley The Age of our Solar System • Radiometric dating can only measure the age of a rock since it solidified. • Geologic processes on Earth cause rock to melt and resolidify.  Earth rocks can’t be used to measure the Solar System’s age. • We must find rocks which have not melted or vaporized since the condensed from the Solar nebula. – meteorites imply an age of 4.6 billion years for Solar System – This value is consistent with the age of the oldest moon rocks (4.4 billion years) • Radioactive isotopes are formed in stars & supernovae – suggests that Solar System formation was triggered by supernova – short half lives suggest the supernova was nearby