Lower temp (H, He, CH4, H2O, N2, ice) - outer edges
Planetary Compositions
Slide 11
How Did We Get a Solar System?
Inner Planets:
Hot Silicate minerals, metals, no light elements, ice
Begin to stick together with dust clumps
Slide 12
How Did We Get a Solar System?
Accretion - particles collide and stick together or break apart gravity not involved if small pieces
Form planetesimals, up to a few km across
Slide 13
How Did We Get a Solar System?
Gravitational accretion: planetesimals attract stuff
Large protoplanets dominate, grow rapidly, clean up area ( takes ~10 to 25 My)
Slide 14
How Did We Get a Solar System?
Outer Solar System
Cold ices, gases 10x more particles than inner
May have formed icy center, then captured lighter gases (Jupiter and Saturn first? Took H and He?)
Slide 15
How Did We Get a Solar System?
Early burst of solar wind - sweeps debris out of system
Gravitational accretion of gas for protoplanets in the coolest nebular parts
Slide 16
? Should have been a planet instead of a debris belt? Jupiter kept it from forming
How Did We Get a Solar System?
Eros image at
Slide 17
Beyond the Gas Giants - Pluto, Charon and the Kuiper Belt objects
Chunks of ice and rock material
Little time / debris available to make a planet slower!!
How Did We Get a Solar System?
Slide 18
Slide 19
Planetesimals swept up debris
Accretion + Impacts = HEAT
Eventually begin to melt materials
Iron, silica melt at different temperatures
Iron sank density layering
Slide 20
Differentiation
Separation of homogenous interior into layers of different compositions
Early hottest time dense iron-rich material core
Releases additional heat
Leaves mantle with molten ocean enriched in silica