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Lecture 31: The Family of the Sun Astronomy 161 – Winter 2004
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Key Ideas: The Solar System contains: The Sun Terrestrial Planets Jovian Planets Pluto Giant Moons Asteroids, Icy Bodies, Comets, & Meteoroids The planets all lie in nearly the same plane and orbit in the same general direction.
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The Golden Age of Exploration The Solar System has been explored with robotic spacecraft & astronauts: Landed men on the Moon Robotic landers on Moon, Venus, & Mars Returned rocks from the Moon (~382 kg) Probed Atmospheres of Venus, Mars, & Jupiter Flown spacecraft by all planets except Pluto Mapped Venus with radar Flown by asteroids & comets, landing on one asteroid
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Magellan Venus Cassini & Huygens Mars Sojourner Pioneer 10 & 11 Voyager 1 & 2 Apollo 11-17
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The Family of the Sun The Sun: a middle-aged, average sized star The Terrestrial Planets: Rocky Planets: Mercury, Venus, Earth & Mars The Jovian Planets: Gas Giants: Jupiter, Saturn, Uranus & Neptune Pluto: fits into neither category Small Icy & Rocky Bodies: Icy: Icy Moons, Kuiper Belt Objects, & Comets Rocky: Giant Moons, Asteroids & Meteoroids
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The 9 Planets, in order: Planets: Mercury Venus Earth Mars Jupiter Saturn Uranus Neptune Pluto Mnemonic: My Very Educated Mother Just Served Us Nine Pizzas
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Relative Sizes of the Planets
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Basic Properties of the Planets Locations: Terrestrial in the inner solar system: 0.4-1.5AU Jovian in the outer solar system: 5-30 AU All orbit in the same direction & same plane: Orbit counterclockwise, in the same sense as the rotation of the Sun. All except Pluto orbit very near the Ecliptic plane. Provides clues to Solar System formation.
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Pluto Neptune Uranus Saturn Jupiter Mars Earth Venus Mercury
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Pluto Ecliptic Plane
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The Solar System, by mass The contents of the Solar System, ordered by their total mass in Earth masses: Sun: 330,000 M Earth 4 Jovian Planets: 447 M Earth total 4 Terrestrial Planets: 1.985 M Earth total Giant Moons: 0.105 M Earth total Pluto, the icy oddball planet: 0.002 M Earth Rest of the contents make a tiny contribution.
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The Sun The Sun is a middle-aged, average-sized star. Mostly Hydrogen & Helium Contains 99.8% the mass of the Solar System about 4.6 Gyr old The Sun shines because it is hot: Surface (photosphere) is ~6000 K Radiates mostly Visible light plus UV & IR Kept hot by nuclear fusion in its core: Builds Helium from Hydrogen fusion.
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The Jovian Planets Jupiter, Saturn, Uranus & Neptune Largest Planets: at least 15 times mass of Earth. Jupiter, largest, is 318 Earth Masses Only in the outer solar system (5 to 30 AU) Gas Giants (“Jupiter-like”): No Solid Surfaces (mostly atmosphere) Mostly Hydrogen & Helium Rocky/icy inner cores Low density: 0.7 to 1.7 g/cc (water is 1 g/cc)
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The Jovian Planets Jupiter (318 M ) Uranus (15 M ) Saturn (95 M ) Neptune (17 M )
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Terrestrial Planets Mercury, Venus, Earth & Mars “Earth-Like” Rocky Planets Largest is Earth Only in the inner solar system (0.4 to 1.5 AU) Rocky Planets: Solid Surfaces Mostly silicates and iron High Density: 3.9-5.5 g/cc (rock & metal) Earth, Venus, & Mars have atmospheres
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The Terrestrial Planets Earth (1 M ) Mars (0.11 M ) Venus (0.82 M ) Mercury (0.055 M )
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Solid inner core Liquid outer core
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The Giant Moons Natural satellites orbiting planets. Giant Moons: Earth: The Moon Jupiter: Io, Europa, Ganymede, & Callisto (the Galilean moons) Saturn: Titan Neptune: Triton Many smaller moons, both rocky & icy. Only Mercury & Venus have no moons.
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The Giant Moons
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Pluto: The Planet that Doesn’t Fit Pluto is neither a Terrestrial nor Jovian Planet. Smallest of the planets Intermediate Density: 1.8 g/cc (mostly icy) Pluto’s orbit is also odd: The most elliptical orbit of all the planets The most highly inclined: ~17º from the Ecliptic. Largest of a distinct class of objects, but still a “planet”.
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Distant Pluto Pluto Charon Pluto’s Moon Hubble Reconstruction of Pluto
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Small Icy Bodies Pluto is the largest of a class of icy bodies: Found only in the outer solar system Densities of 1.2 to 2 g/cc (like ices) Examples: Triton, large moon of Neptune Charon, Pluto’s large moon Trans-Neptunian Objects (Kuiper Belt Objects & Plutinos)
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Triton
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The Leftovers (Minor Bodies) Asteroids: Range from 500km (Ceres) to large boulders Made of rock (density 2-3 g/cc) Meteoroids: Bits of rock and metal Range in size from grains of sand to boulders Comets: Composite rock & ice “dirty snowballs” Longs tails of gas & dust are swept off them when they pass near the Sun.
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Asteroids 253 Mathilde 951 Gaspra 243 Ida
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Meteor burning up in the atmosphere.
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Comet Hale-Bopp
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5 km Nucleus of Comet Halley
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