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Water in the upper martian surface at mid- and low-latitudes: presence, state, and consequences

Möhlmann, Diedrich T.F. (2004) Water in the upper martian surface at mid- and low-latitudes: presence, state, and consequences. Virtual Journal of Geobiology, 3 (4), 3C. Elsevier.

Full text not available from this repository.

Official URL: http://earth.elsevier.com/geobiology/

Abstract

Sublimation of water ice is more effective than evaporation of spoprtion water at the same temperature. Therefore, water in the form of ice, must, over geological time-scales, have left in the upper martian surface (m-scale) at mid- and low-latitudes, leaving sorption water as a possible physical form of unstable subsurface water. Adsorption water is "liquid-like" at these temperatures (in the sense of a 2D-liquid). This property is the reason for the specific importance of physioabsorbed water under martian conditions. It is shown that unfrozen adsorption water can cause numerous physical, chemical, and possible also biological processes in the upper martian surface and may be responsible for a number of its properties.

Item URL in elib:https://elib.dlr.de/22944/
Document Type:Article
Additional Information: LIDO-Berichtsjahr=2004,
Title:Water in the upper martian surface at mid- and low-latitudes: presence, state, and consequences
Authors:
AuthorsInstitution or Email of AuthorsAuthors ORCID iD
Möhlmann, Diedrich T.F.UNSPECIFIEDUNSPECIFIED
Date:2004
Journal or Publication Title:Virtual Journal of Geobiology
Refereed publication:Yes
Open Access:No
Gold Open Access:No
In SCOPUS:No
In ISI Web of Science:No
Volume:3
Page Range:3C
Publisher:Elsevier
Status:Published
Keywords:Mars, surface, ice, cosmochemistry
HGF - Research field:Aeronautics, Space and Transport (old)
HGF - Program:Space (old)
HGF - Program Themes:W - no assignment
DLR - Research area:Space
DLR - Program:W - no assignment
DLR - Research theme (Project):W - no assignment (old)
Location: Berlin-Adlershof
Institutes and Institutions:Institute of Planetary Research
Deposited By: Pieth, Susanne
Deposited On:29 Mar 2006
Last Modified:27 Apr 2009 05:05

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