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Title pageLife on Mars?Using Geant4 to model the subsurface
radiation environment
Lewis DartnellCoMPLEX (Centre for Mathematics and Physics in the
Life Sciences and Experimental Biology)
University College London, UK
Supervisors: Andrew Coates, MSSL John Ward, Biochemistry
SPENVIS-GEANT4 workshop. Leuven, 3-7 October 2005
Why Mars?
• Most Earth-like body in the solar system• Known to have once been warm and
wet, with a thick atmosphere andmagnetic field
• The original home of life?
Mars today• 6 mbar atmosphere, freezing surface temperatures, bone-dry
surface sterilised by UV, bathed in solar energetic and cosmicradiation particles
Refugial Life
• Could extremophile life persist beneaththe surface, within pockets of liquidwater…?
• Deep hot Biosphere on Earth.• Methane plumes detected seeping out of
ground.
ExtremophilesMicrobes on Earth survive extremes of:
Temperature:113ºC superheated water --> -18ºC ice pockets
pH:pH 0 sulphuric acid --> pH 11 soda lakes
Salinity:saturated brine --> pure distilled water
Pressure:1,000 atm --> vacuum
As well as entire ecosystems independentof energy from the sun - 5km deep ‘rock-eaters’ and hydrothermal ventcommunities
Radioresistant bacteria
Survival curves of D. radiodurans, B. subtilis, and E. coliDeinococcus radiodurans
Crustal Anomalies
• Failure of global magnetic field ~4Gya, withsubsequent loss of atmosphere and environmentalcollapse.
• Remnant magnetism stored in rocks. Effect onincoming radiation?