Transient Liquid Water as a Mechanism for Induration of Soil Crusts on Mars

Details Transient Liquid Water as a Mechanism for Induration of Soil Crusts on Mars Transient Liquid Water as a Mechanism for Induration of Soil Crusts on Mars

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.2188l&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.2188

Physics

3

Scientific paper

We propose two alternative models to account for the origin of cemented
Martian soils, or duricrusts, involving the action of transient liquid
water films to mediate adhesion and cementation of grains.

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