Direct evidence of helium rain in Jupiter and Saturn

The immiscibility of hydrogen-helium mixture under the temperature and pressure conditions of planetary interiors is crucial for understanding the structures of gas giant planets (e.g., Jupiter and Saturn). While the experimental probe at such extreme conditions is challenging, theoretical simulation is heavily relied in an effort to unravel the mixing behavior of hydrogen and helium. Here we develop a method via a machine learning accelerated molecular dynamics simulation to quantify the physical separation of hydrogen and helium under the conditions of planetary interiors. The immiscibility line achieved with the developed method yields substantially higher demixing temperatures at pressure above 1.5 Mbar than earlier theoretical data, but matches better to the experimental estimate. Our results revise the structures of Jupiter and Saturn where H-He demixing takes place in a large fraction of the interior radii, i.e., 27.5% in Jupiter and 48.3% in Saturn. This direct evidence of an H-He immiscible layer supports the formation of helium rain and explains the helium reduction in atmosphere of Jupiter and Saturn.