Sublimation rate of ice under simulated Mars conditions and the effect of layers of mock regolith JSC Mars-1
We have studied the sublimation of ice buried beneath ≤200 mm of JSC Mars‐1 model regolith under simulated Mars conditions. As expected, even thin layers of regolith cause large decreases in sublimation rate, up to one order of magnitude at 50 mm. When the depth of the regolith was 50 to 200 mm we d...
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Veröffentlicht in: | Geophysical research letters 2007-01, Vol.34 (2), p.n/a |
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Sprache: | eng |
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