The Large Dirty Mars Chamber is a large, adaptable, environmental simulation chamber suitable for a wide range of scientific and engineering investigations. This facility is unique in its application to materials and processes not usually associated with vacuum chambers. Many studies involve the use of up to several kilograms of regolith simulants, as well as large volumes of water, brines and CO2 ice. George is also suitable for testing large instruments and structures (e.g., rover mechanisms) under martian environmental conditions.
Ongoing research includes simulations of mud-volcanism, surface runoff of both water and brine solutions on sediment slopes, CO2 sublimation-driven mass wasting on sediment slopes and CO2 sublimation-drivenaraneiform and dust plume simulations, all under Mars atmospheric conditions.
George is 1.8 m long and 0.9 m in diameter, with 11 large (20 cm diameter), adaptable ports used for feedthroughs and viewports. Temperatures inside the chamber can be controlled by a cryogenic sleeve down to -70°C. Lower temperatures (~-180°C) can be maintained using a 1.2 m long, 50 cm wide cryogenic cooling plate. Pressure is automatically controllable, between 0.8 mbar - 1000 mbar.
Length | 1.8 m |
Diameter | 0.9 m |
Pressure | 1 mbar - 1000 mbar |
Temperature | ~-180°C - +20°C |
If you are interested in conducting experiments with us, please see our Client Project Process for more information.
For all enquiries please Contact us!
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Open University PhD student Jessie Hogan - Jessie is looking at how ice grains of different concentrations, relevant to Enceladus, form under low pressure conditions. Her work is ongoing, so come back later for more details.
Academy of Sciences of the Czech Republic Researcher Dr. Petr Brož - Petr has a three-year project investigating cryovolcanic features on the surface of icy worlds such as Europa, Titan, Enceladus, Triton and Ceres. They aim to investigate several aspects of freezing water under near-vacuum environments that remain unsolved in the community. Keep an eye out on upcoming publications for their results!
Utrecht University, Netherlands, PhD student Lonneke Roelofs & Université Nantes, France, research scientist Dr. Susan Conway - Experiments to investigate how sublimation of H2O ice changes the mobility of dry granular flows under Martian pressures. Keep an eye out for future publications!
Arizona State University's Prof. Jacob Adler and Georgia Institute of Technology's PhD student Sharissa Thompson - A continuation from their work in 2022 remotely pouring slurries of different concentrations of water and Mars regolith simulants down slopes under Martian atmospheric pressures to investigate changes in sediment flow dynamics. See their AGU abstract here and some images on our X, Instagram or LinkedIn pages.
Utecht University, Netherlands, PhD student Lonneke Roelofs and Simone Visschers & Université Nantes, France, research scientist Dr. Susan Conway - Simulated the formation of Martian Linear Dune Gullies with burrowing blocks of CO2 ice by explosive sublimation-induced particle transport. Check out some impressive videos of this process on our Instagram or LinkedIn pages. Also see their publications & conference abstracts:
Academy of Sciences of the Czech Republic Researcher Dr. Petr Brož and Dr, Ondrej Krýza - ran experiments investigating whether the volume of mud changes when exposed to martian atmospheric pressures depending of pressure, thickness and presence of salts. See their publications for more information:
Arizona State University's Prof. Jacob Adler - They remotely poured slurries of water and Mars-like materials (basalt, kaolinite, bentonite, and MGS-1 regolith simulant) down slopes of different angles under Martian atmospheric pressures to investigate changes in sediment flow dynamics. See their AGU abstract here.
Academy of Sciences of the Czech Republic Researcher Dr. Petr Brož and Dr, Ondrej Krýza - Investigated how low viscosity mud propogates under Martian atmospheric pressures with rapid freezing and formation of ice crusts. See their publications for more information: