
How stellar properties and processes determine the chemical makeup and location of forming planets.Planetary composition and formation is the study of how the chemical makeup of planets is determined by the properties of their host star and the processes occurring in the protoplanetary disk — the swirling disk of gas and dust from which planets form. The star's mass, temperature, luminosity, and metallicity (its abundance of elements heavier than hydrogen and helium) dictate the conditions in the disk, including temperature gradients and radiation pressure, which in turn influence which materials can condense and accrete into planets. This explains why some planets are rocky, some are gas giants, and why certain elements like sulfur or carbon are enriched or depleted in different planetary systems.
The modern understanding emerged in the 1970s–1980s with the nebular hypothesis refined by researchers like Viktor Safronov and George Wetherill, who developed planetesimal accretion models. The first confirmed exoplanet in 1992 and subsequent surveys like Kepler in the 2000s provided observational constraints that reshaped the field.
The star's radiation and stellar wind sculpt the disk, creating a temperature gradient: closer to the star, only refractory materials like silicates and metals can solidify, while volatile compounds like water and methane remain gaseous. Farther out, ices condense, allowing the formation of massive cores that can accrete gas. The star's composition also matters — a star rich in heavy elements seeds the disk with more solid material, promoting the formation of rocky planets. Processes like photoevaporation (the star's radiation stripping gas from the disk) and radial drift of solid particles further sort materials by location, leaving a chemical fingerprint in the planets that form.
This knowledge guides the search for habitable exoplanets by predicting which stars and orbital distances are likely to host Earth-like compositions, and it informs models of our own solar system's formation.
A star's sulfur abundance can act as a 'fossil record' of the building blocks that formed its planets, because sulfur is volatile enough to be lost from hot inner regions but preserved in cooler outer zones.
| ΔH_f | variable | Formation enthalpy change — enthalpy joule per mole |
| H_compound | variable | Enthalpy of the compound — enthalpy joule per mole |
| x_i | variable | Stoichiometric coefficient of element i — stoichiometric coefficient |
| H_i^element | variable | Enthalpy of element i in its standard state — enthalpy joule per mole |
| Σ | operator | Sum over constituent elements — summation |





















