survey of the solar system 2 introduction the solar system is occupied by a variety of objects, all...
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Survey of the Solar Survey of the Solar SystemSystem
Survey of the Solar System 2
IntroductionIntroductionThe The Solar SystemSolar System is occupied by a is occupied by a
variety of objects, all maintaining order variety of objects, all maintaining order around the sun around the sun
The planets in the solar system form The planets in the solar system form two main families: solid rocky inner two main families: solid rocky inner planets and gaseous/liquid outer planets and gaseous/liquid outer planetsplanets
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Origin of the Solar SystemOrigin of the Solar SystemAge of the Solar SystemAge of the Solar System
All objects in the Solar System seem to All objects in the Solar System seem to have formed at nearly the same timehave formed at nearly the same time
Radioactive dating of rocks from the Radioactive dating of rocks from the Earth, Moon, and some asteroids Earth, Moon, and some asteroids suggests an age of about 4.5 billion yrssuggests an age of about 4.5 billion yrs
A similar age is found for the Sun based A similar age is found for the Sun based on current observations and nuclear on current observations and nuclear reaction ratesreaction rates
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Origin of the Solar SystemOrigin of the Solar System IntroductionIntroduction
Solar nebula hypothesisSolar nebula hypothesis - currently - currently favored theory for the Solar System’s originfavored theory for the Solar System’s origin
Solar System evolved from a rotating, flattened Solar System evolved from a rotating, flattened disk of gas and dust (an disk of gas and dust (an interstellar cloudinterstellar cloud), ), the outer part of the disk becoming the planets the outer part of the disk becoming the planets and the inner part becoming the Sunand the inner part becoming the Sun
This hypothesis naturally explains the Solar This hypothesis naturally explains the Solar System’s flatness and the common direction of System’s flatness and the common direction of motion of the planets around the Sunmotion of the planets around the Sun
Interstellar clouds are common between Interstellar clouds are common between the stars in our galaxy and this suggests the stars in our galaxy and this suggests that most stars may have planets around that most stars may have planets around them them
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Origin of the Solar SystemOrigin of the Solar SystemFormation of the Solar NebulaFormation of the Solar Nebula
A few million years passes for a cloud to A few million years passes for a cloud to collapse into a rotating disk with a bulge in collapse into a rotating disk with a bulge in the centerthe center
This disk is called the This disk is called the solar nebulasolar nebula with the with the bulge becoming the Sun and the disk bulge becoming the Sun and the disk condensing into planetscondensing into planets
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Origin of the Solar SystemOrigin of the Solar SystemPlanetesimalsPlanetesimals
Next step is for tiny particles to stick Next step is for tiny particles to stick together into bigger pieces through together into bigger pieces through collisions collisions
As long as collision are not too violent, As long as collision are not too violent, objects, called objects, called planetesimalsplanetesimals, ranging in , ranging in size from millimeters to kilometers, may size from millimeters to kilometers, may formform
Formation of the PlanetsFormation of the Planets Planets formed from “gentle” collisions of Planets formed from “gentle” collisions of
the planetesimals, which dominated over the planetesimals, which dominated over more violent shattering collisionsmore violent shattering collisions
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Origin of the Solar SystemOrigin of the Solar SystemFormation of the PlanetsFormation of the Planets
Simulations show that planetesimal Simulations show that planetesimal collisions gradually lead to collisions gradually lead to approximately circular planetary approximately circular planetary orbitsorbits
As planetesimals grew in size and As planetesimals grew in size and mass their increased gravitational mass their increased gravitational attraction helped them grow faster attraction helped them grow faster into clumps and rings surrounding into clumps and rings surrounding the Sunthe Sun
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Origin of the Solar SystemOrigin of the Solar System Direct Formation of Giant PlanetsDirect Formation of Giant Planets
It is possible the outer regions of the solar nebula It is possible the outer regions of the solar nebula were cold and dense enough for gravity to pull gas were cold and dense enough for gravity to pull gas together into the giant planets without the need to together into the giant planets without the need to first form cores from planetesimalsfirst form cores from planetesimals
Formation of MoonsFormation of Moons Moons of the outer planets were probably formed Moons of the outer planets were probably formed
from planetesimals orbiting the growing planetsfrom planetesimals orbiting the growing planets
Final Stages of Planet FormationFinal Stages of Planet Formation Rain of planetesimals cratered surfacesRain of planetesimals cratered surfaces Remaining planetesimals became small moons, Remaining planetesimals became small moons,
comets, and asteroidscomets, and asteroids
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Origin of the Solar SystemOrigin of the Solar System Formation of AtmospheresFormation of Atmospheres
Atmospheres were the last planet-forming processAtmospheres were the last planet-forming process Outer planets gravitationally captured their Outer planets gravitationally captured their
atmospheres from the solar nebulaatmospheres from the solar nebula Inner planets created their atmospheres by Inner planets created their atmospheres by
volcanic activity and perhaps from comets and volcanic activity and perhaps from comets and asteroids that vaporized on impactasteroids that vaporized on impact
Cleaning up the Solar SystemCleaning up the Solar System Residual gas and dust swept out of the Solar Residual gas and dust swept out of the Solar
System by young Sun’s intense solar windSystem by young Sun’s intense solar wind
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Components of the Solar SystemComponents of the Solar SystemThe SunThe Sun
The Sun is a star, a ball of incandescent The Sun is a star, a ball of incandescent gas whose output is generated by nuclear gas whose output is generated by nuclear fusion in its corefusion in its core
Composed mainly of hydrogen (71%) and Composed mainly of hydrogen (71%) and helium (27%), it also contains traces of helium (27%), it also contains traces of nearly all the other chemical elementsnearly all the other chemical elements
It is the most massive object in the Solar It is the most massive object in the Solar System – 700 times the mass of the rest of System – 700 times the mass of the rest of the Solar System combinedthe Solar System combined
It’s large mass provides the gravitational It’s large mass provides the gravitational force to hold all the Solar System bodies in force to hold all the Solar System bodies in their orbits around the Suntheir orbits around the Sun
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Components of the Solar SystemComponents of the Solar SystemThe planetsThe planets
Planets shine primarily by reflected Planets shine primarily by reflected sunlightsunlight
Orbits are elliptical, lying in nearly the Orbits are elliptical, lying in nearly the same plane – Pluto is the exception with a same plane – Pluto is the exception with a high (17high (17°) inclination of its orbit) inclination of its orbit
All the planets travel (revolve) All the planets travel (revolve) counterclockwise around the Sun counterclockwise around the Sun
Six planets rotate counterclockwise; Venus Six planets rotate counterclockwise; Venus rotates clockwise, and Uranus and Pluto rotates clockwise, and Uranus and Pluto appear to rotate on their sidesappear to rotate on their sides
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Components of the Solar SystemComponents of the Solar SystemTwo types of planetsTwo types of planets
Inner planetsInner planets Mercury, Venus, Earth, MarsMercury, Venus, Earth, Mars Small rocky (mainly silicon and oxygen) bodies Small rocky (mainly silicon and oxygen) bodies
with relatively thin or no atmospheres with relatively thin or no atmospheres Also referred to as Also referred to as terrestrial planetsterrestrial planets
Outer planetsOuter planets Jupiter, Saturn, Uranus, Neptune, and PlutoJupiter, Saturn, Uranus, Neptune, and Pluto Gaseous, liquid, or icy (HGaseous, liquid, or icy (H22O, COO, CO22, CH, CH44, NH, NH33)) Excluding Pluto, also referred to as Excluding Pluto, also referred to as Jovian Jovian
planetsplanets Jovian planets are much larger than terrestrial Jovian planets are much larger than terrestrial
planets and do not have a well-defined surfaceplanets and do not have a well-defined surface
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Fig. co_14b
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Components of the Solar SystemComponents of the Solar SystemSatellitesSatellites
The number of planetary satellites has The number of planetary satellites has changed frequently over the last several changed frequently over the last several years; years;
Most recent count is broken down as follows: Most recent count is broken down as follows: Jupiter 63, Saturn 60, Uranus 27, Neptune 13, Jupiter 63, Saturn 60, Uranus 27, Neptune 13, Mars 2, Pluto 3, Earth 1, and Mercury and Mars 2, Pluto 3, Earth 1, and Mercury and Venus are moonlessVenus are moonless
The moons generally follow approximately The moons generally follow approximately circular orbits that are roughly in the circular orbits that are roughly in the planet’s equatorial plane, thus resembling planet’s equatorial plane, thus resembling miniature solar systemsminiature solar systems
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Components of the Solar SystemComponents of the Solar SystemAsteroids and cometsAsteroids and comets
Their composition and sizeTheir composition and size AsteroidsAsteroids are rocky or metallic bodies ranging are rocky or metallic bodies ranging
in size from a few meters to 1000 km across in size from a few meters to 1000 km across (about 1/10 the Earth’s diameter)(about 1/10 the Earth’s diameter)
Comets Comets are icy bodies about 10 km or less are icy bodies about 10 km or less across that can grow very long tails of gas and across that can grow very long tails of gas and dust as they near the Sun and are vaporized dust as they near the Sun and are vaporized by its heatby its heat
Their location within Solar SystemTheir location within Solar System Most asteroids are in Most asteroids are in asteroid beltasteroid belt between between
Mars and Jupiter indicating that these Mars and Jupiter indicating that these asteroids are the failed building-blocks of a asteroids are the failed building-blocks of a planetplanet
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Fig. 14.4