Sublimation of Water Ice in Low Pressure Environments: Isotopic Effects and Implications for the Martian Paleoclimate Record

Details Sublimation of Water Ice in Low Pressure Environments: Isotopic Effects and Implications for the Martian Paleoclimate Record Sublimation of Water Ice in Low Pressure Environments: Isotopic Effects and Implications for the Martian Paleoclimate Record

Oct 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpico1323.8031m&link_type=abstract

Fourth International Conference on Mars Polar Science and Exploration, October 2-6, 2006, Davos, Switzerland. LPI Contribution

Physics

Scientific paper

Following recent laboratory sublimation fractionation experiments
conducted on dusty water ice we examine the role played by D/H in
recording past martian climate change. We consider both the size and
duration of isotopic signals preserved in the northern polar layered
deposits.

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