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The Origin and Evolution of the Solar System

The Origin and Evolution of the Solar System

The Origin and Evolution of the Solar System

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30 <strong>The</strong> structure <strong>of</strong> <strong>the</strong> <strong>Solar</strong> <strong>System</strong>Table 1.10. Characteristics <strong>of</strong> some important asteroids. <strong>The</strong> ones given are: , <strong>the</strong>semi-major axis; , <strong>the</strong> eccentricity; , <strong>the</strong> inclination; <strong>and</strong> , <strong>the</strong> diameter (U = unknown).Year <strong>of</strong> Name discovery (AU) ( Æ ) (km)Ceres 1801 2.75 0.079 10.6 1003Pallas 1802 2.77 0.237 34.9 608Juno 1804 2.67 0.257 13.0 250Vesta 1807 2.58 0.089 7.1 538Hygeia 1849 3.15 0.100 3.8 450Undina 1867 3.20 0.072 9.9 250Eros 1898 1.46 0.223 10.8 UHildago 1920 5.81 0.657 42.5 15Apollo 1932 1.47 0.566 6.4 UIcarus 1949 1.08 0.827 22.9 2Chiron 1977 13.50 0.378 6.9 Usynchronization is found for all <strong>the</strong> satellites in <strong>the</strong> <strong>Solar</strong> <strong>System</strong>. Ano<strong>the</strong>r effectis to cause a precession <strong>of</strong> <strong>the</strong> spin axis <strong>of</strong> <strong>the</strong> Earth. <strong>The</strong> spin <strong>of</strong> <strong>the</strong> Earth doesnot contribute to tides but it does create an equatorial bulge distorting it fromspherical symmetry. <strong>The</strong> equatorial radius <strong>of</strong> <strong>the</strong> Earth is about 22 km greaterthan <strong>the</strong> polar radius. <strong>The</strong> spinning Earth acts like a gyroscope <strong>and</strong> <strong>the</strong> Moonexerts a torque on it due to <strong>the</strong> differential pull on <strong>the</strong> near <strong>and</strong> far regions <strong>of</strong> <strong>the</strong>equatorial bulge. It is this torque which gives a spin-axis precession period <strong>of</strong>about 26 000 years.1.5 AsteroidsIt was seen in table 1.2 that to fill a gap in Bode’s law it was necessary to introducea body between Mars <strong>and</strong> Jupiter. <strong>The</strong> small body Ceres, discovered in1801, filled <strong>the</strong> gap admirably but <strong>the</strong> pattern was made more complicated by <strong>the</strong>discovery <strong>of</strong> many o<strong>the</strong>r bodies, all smaller than Ceres, in <strong>the</strong> same region <strong>of</strong> <strong>the</strong><strong>Solar</strong> <strong>System</strong>. <strong>The</strong>se bodies, called asteroids, raise many questions as to <strong>the</strong>irorigin but here we shall just consider <strong>the</strong>ir characteristics.1.5.1 Characteristics <strong>of</strong> <strong>the</strong> major asteroidsIn table 1.10 <strong>the</strong> data for a number <strong>of</strong> asteroids, chosen because <strong>the</strong>y span <strong>the</strong>period from <strong>the</strong> first discovery to recent times <strong>and</strong> because <strong>the</strong>y illustrate differentorbital characteristics, are shown.<strong>The</strong> sizes <strong>of</strong> asteroids are best measured by stellar occultation. By timingan occultation <strong>and</strong> knowing <strong>the</strong> orbit <strong>of</strong> <strong>the</strong> asteroid it is possible to obtain quite

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