
Chemical processes in protoplanetary disks that influence planet formation and composition.Protoplanetary disk chemistry refers to the complex network of chemical reactions occurring in the rotating disks of gas and dust around young stars, from which planets form. These processes determine the initial composition of planets, including their water content, organic molecules, and volatile elements. The chemistry is driven by radiation from the central star, cosmic rays, and the thermal history of the disk, leading to a rich variety of molecular species in both gas and solid phases.
The field emerged in the 1970s with the first observations of molecules in disks, but advanced significantly with the advent of ALMA in the 2010s, which resolved chemical structures in disks.
In the disk, gas-phase reactions, grain-surface reactions, and ice formation occur at different temperatures and pressures. Ultraviolet radiation from the star photodissociates molecules, while cosmic rays ionize gas, driving ion-molecule reactions. As material moves inward and heats up, ices sublimate, releasing molecules into the gas phase. The final composition of planetesimals and planets is set by the balance between these processes, which can be traced in meteorites and observed in disk spectra.
Understanding disk chemistry helps predict the composition of exoplanets and the availability of water and organics for potential life, guiding the search for habitable worlds.
Some complex organic molecules, like methanol, can form on ice grains at temperatures as low as 10 K, without needing energetic radiation.





















