Winter 2012

Origin of the most basic properties: planets revolve around the Sun in the same plane
Laplace's solar nebula hypothesis: co-planar motion
Astrophysical disks around Saturn, binary stars, and galaxies
Comparative studies of protostellar disks
properties:
comparable size, mass, temperature, as the solar nebula
disk life span is around a few Myr
condensation of ice and silicate grains
meteorites carry same fractional amount of elements as the Sun's atmosphere
Isotopic anomaly
daughter nuclei in chondrule meteorites
decay, half life, radiometric dating
range of isotopic chronometers
supernova precursor and different meteoritic byproduct
Putting together terrestrial planets:
planetesimals collision and coagulation
impact growth and craters
giant impacts, lunar formation
radiometric dating of terrestrial planet formation
Putting together gas giant planets:
sufficiently massive core to initiate gas accretion
preferred location for Jovian planet formation
heat transfer during accretion
environmental impact: multiple gas giants, perturbation on terrestrial planets and Kuiper Belt Objects
clearing up the solar system: disk depletion