
Chemical processes and material recycling during planet formation from protoplanetary disks.Planetary accretion chemistry is the study of the chemical processes that occur during the formation of planets from protoplanetary disks. It encompasses the condensation of solids from gas, the accretion of these solids into planetesimals and protoplanets, and the subsequent chemical differentiation and processing within these bodies. This field explains the composition of planets, including the origin of water and organic molecules, and why different planets have different volatile content.
The field developed in the mid-20th century with the analysis of meteorites and the formulation of condensation sequences by John Larimer and others in the 1960s-70s. The discovery of exoplanets has since provided new constraints on the diversity of planetary compositions.
The process begins with the cooling of the protoplanetary disk, where different minerals condense at different temperatures, creating a radial chemical gradient. Dust grains collide and stick together, forming larger bodies. Heating from radioactive decay and impacts causes melting and differentiation, leading to the formation of a metallic core and silicate mantle. Volatile elements, including water, can be delivered by icy planetesimals from the outer disk, while chemical reactions between the atmosphere and magma ocean can generate additional water and organics.
Understanding accretion chemistry is essential for interpreting exoplanet observations, such as the composition of their atmospheres, and for assessing the habitability of rocky worlds.
Water on Earth may have been partly generated by chemical reactions between hydrogen and magma in the planet's early molten interior, not solely delivered by icy comets.
| T(r) | variable | disk temperature at radius r — temperature kelvin |
| r | variable | radial distance from the central object — radius metre |
| M | variable | mass of the central object — mass kilogram |
| \dot{M} | variable | mass accretion rate — mass flow rate kilogram per second |
| G | constant | Constant of universal gravitation. — gravitational constant = 6.67430e-11 cubic metre per kilogram per second squared |
| \sigma | constant | Constant relating blackbody radiated power to temperature. — stefan boltzmann constant = 5.670374419e-8 watt per square metre per kelvin to the fourth |

















