Protoplanetary core formation by rain-out of minerals

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Gas Giant Planets, Minerals, Planetary Cores, Planetary Evolution, Protoplanets, Brownian Movements, Drops (Liquids), Liquid Metals, Long Term Effects

Scientific paper

Models of giant protoplanets computed by DeCampli and Cameron (1979) show that Fe and other minerals in the planet interior are in a liquid state during one of the stages of protoplanet evolution. A model of coalescence of liquid drops was developed using the 'stochastic' collection equation of Slattery (1978); the growth times to droplets was much shorter than the period during which the drops are in a liquid state. Brownian collection quickly coalesced the tiny droplets to a radius of 0.005 cm; gravitational collection was required to form droplets of radii greater than 0.005 cm.

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