Comparative Planetology • Comparative Planetology is the comparing and contrasting of different worlds to describe and categorize them • Important Properties: – – – – – – Distance to the Sun Orbital Period Radius Mass Rotation Period Density Solar System Layout • All planets travel in elliptical orbits with the Sun at one focus • Most eccentricities are low • Most lay in the same orbital plane • Mercury and Pluto are the exceptions – Each has significant eccentricity and don’t lie in the orbital plane Terrestrial Planets • Properties of all terrestrial planets – – – – – Within about 1.5 AU of the Sun Relatively small Relatively high density Rocky Composition Solid Surfaces • Some Differences – Atmospheres are very different – Some have moons – Surface conditions very different Jovian Planets • Properties of Jovian planets – – – – – – Farther away from the Sun Made almost entirely of gas Relatively Large Strong Magnetic Fields Many Moons All have Rings • Some Differences – Compositions different – Inner Structure differences Terrestrial vs. Jovian Pluto • What is Pluto? Interstellar Matter Interstellar Matter Interstellar Matter • Interstellar matter is made of gas and dust – The gas is mostly individual atoms and small molecules – 0.1 – 1.0 nanometers in size – Gas does not account for all the obscuration of light • Interstellar dust is made of clumps of atoms and molecules – Dust absorbs or scatters light (like headlights in fog) – Obscuration increases with decreasing wavelength Interstellar Matter • Interstellar dust is typically about 100 nm in size – This makes the dust invisible to radio waves – The dust is opaque to shorter wavelengths – “Extinction” is the term for the dimming out of light • Because dust blocks the shorter wavelengths more than the longer wavelengths, visible light loses some of its blue component – Makes the light appear more red – “Reddening” Interstellar Matter • Notice dust cloud edges • Cloud blocks some of the blue light intensity Interstellar Matter • Space is an empty place? A dirty place? • Average gas density ~ 9 billion atoms per m3 – Better than any vacuum created on Earth – Earth’s gas density is approximately 1x1025 atoms per m3 – That is a million – billion times more! • Average dust distribution ~ 1000 particles per km3 • Volume the size of Earth would not fill a coffee cup Interstellar Matter • Earth’s atmosphere has 1 dust particle per 1018 gas atoms • Space has 1 dust particle per 1012 gas atoms • If the gas density of space was equal to Earth, we couldn’t see our hand in front of our face • As we look over large distances, this is significant Interstellar Matter Interstellar Medium • Nebula: “Fuzzy” patches in the sky • Emission Nebulae: gas clouds hot enough (thousands of Kelvins) to emit visible light • Dark Dust Cloud: Cold and dense (relatively) clouds of dust and gas Nebulae Nebulae Dark Dust Clouds 21-cm Radiation • How do you observe nebula that are too dense or cool to emit usable radiation? • 21-cm wavelength radiation is emitted from cool atomic Hydrogen • This long wavelength allows the radiation to penetrate dust Nebular Theory • The solar system started as a cloud of hot gas • The cloud’s gravity started to pull it inward • As it pulled inward it started to rotate Nebular Theory • Because of the rotation it started to flatten out • It started to spin faster as the cloud shrunk • Planets formed in cooler outer regions Condensation Theory • Condensation theory adds to the nebular theory by introducing DUST • Models show that gas alone would not clump together • Dust particles act as the nucleus for larger object formation Condensation Theory Condensation Theory Angular Momentum • When objects spin, Newton says they should keep spinning • Spinning objects have momentum • This momentum must be conserved Angular Momentum • Angular momentum: L = Iω • For Conservation of Momentum: Ii ωi = If ωf • I is the moment of inertia – For spheres I = 2/5 MR2 • ω = angular velocity (how fast it rotates) • If the moment of inertia goes down, then the angular momentum must go up Angular Momentum • A Star in the final stages of its life will shrink and turn into a neutron star • The mass of the star is 5x1035 kg • Its initial radius is 1x109 m • Its initial ω is 3x10-6 rad/sec (1 revolution in 25 days) • As it becomes a neutron star, it shrinks to a radius of 20,000 m • What is it’s new rotation rate? Angular Momentum Ii ωi = If ωf 2/5 M Ri2 ωi = 2/5 M Rf2 ωf Ri2 ωi = Rf2 ωf ωf = Ri2 ωi / Rf2 ωf = (1x109 m)2 (3x10-6 rad/s) / (2x104 m)2 ωf = 7,500 rad/s 4,300,000 revolutions per hour Angular Momentum • A new planet is forming much like ours did • Its initial mass is 5x1025 kg • It is initially spinning at a rate of once every 50 hours • Fast-forward a million years • Due to collisions with other things, it’s mass has increased to 7.5x1025 kg • However, because some of the planet has cooled (and therefore shrunk) its radius has not changed • What is the new rate of rotation? Angular Momentum Ii ωi = If ωf 2/5 Mi R2 ωi = 2/5 Mf R2 ωf Mi ωi = Mf ωf ωf = Mi ωi / Mf ωf = (5x1025 kg)(1rev/50hr) / (7.5x1025 kg) ωf = 0.0133 rev/hr 1 revolution every 75 hours Angular Momentum Ii ωi = If ωf • Everything else being equal: • Rotation slows if: – Mass Increases – Radius Increases • Rotation speeds up if: – Mass Decreases – Radius Decreases