We are inviting applications for one fully-funded, full-time Ph.D. position lasting three years. The successful candidate will engage in innovative research exploring water instability under reduced atmospheric pressure, as part of effusive cryovolcanism processes, using methods of both analogue and numerical modelling.
See details here (open until 4th of January 2025)
Overview of the low-pressure Mars Chamber at The Open University, UK, where the mud experiments are conducted. The chamber allows to reduce the atmospheric pressure to the average values present on the surface of Mars. (Photo: Petr Brož)