P086-05
Thermal and chemical evolution of small, shallow water bodies on Europa
Abstract:
To quantify the longevity of small bodies of water in Europa’s ice shell and understand their chemical evolution to constrain how shallow water impacts the ice shell composition, and regional surface geology over time, we developed a multiphase, two-dimensional, finite difference model that describes the thermal and chemical evolution of small bodies of liquid water after they are emplaced in the ice shell of Europa. Using sea ice as an analog at the roof of the sill and terrestrial magma chambers at the floor, a conservative parameterization of salt entrainment and rejection is implemented using constitutive equations relating bulk salinity in the ice to its thermochemical formation environment.
We find that lenticulae are more geologically transient than previously described. Our results imply that lenticulae may be actively forming, suggesting liquid water may still be present in Europa’s shallow ice shell. If salts are present in the liquid, meters-thick layers of salt may precipitate out of solution during freezing creating distinct mechanical, thermal, and dielectric layers in the shell. Finally, we suggest how both active and refrozen lenticulae may be detectable with the upcoming Europa Clipper mission providing a window into the ice shell’s history and habitability.