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Critical Masses for Various Terrestrial Planet Atmospheric Gases and Water in/on Mars
Lin-gun Liu
2014
Source PublicationTERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES
Volume25Issue:5Pages:703-707
AbstractThe lower critical mass boundaries (CM) for various atmospheric gas species on terrestrial planets are estimated. The CM is different for different gas molecules. Except for He, the observed atmospheric compositions of the terrestrial planets are consistent with these estimates. The lower CM boundary for gaseous H2O is calculated as 8.06 x 10(26) g, which is significantly greater than the Martian mass (6.419 x 10(26) g). Thus, Mars is not capable of retaining H2O in its atmosphere. If the speculated ocean on Mars and the claimed H2O ice in the Martian soil are true, both the ocean and ice had to be derived earlier from H2O degassed from the Martian interior after the surface temperature cooled much below 100 degrees C. These watery bodies cannot be sustained for long durations because evaporation and sublimation would turn them into gaseous H2O, which would be lost to outer-space. It is concluded that H2O in/on Mars is inherent and that the primordial planetesimals that formed Mars must have contained appreciable amounts of hydrous minerals, if the oceans and/or H2O ice on Mars are true.
KeywordCritical Mass Atmospheric Composition Water Mars
Subject Area地球深部物质与流体作用地球化学
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/5279
Collection地球内部物质高温高压实验室_地球内部物质高温高压实验室_期刊论文
Recommended Citation
GB/T 7714
Lin-gun Liu. Critical Masses for Various Terrestrial Planet Atmospheric Gases and Water in/on Mars[J]. TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES,2014,25(5):703-707.
APA Lin-gun Liu.(2014).Critical Masses for Various Terrestrial Planet Atmospheric Gases and Water in/on Mars.TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES,25(5),703-707.
MLA Lin-gun Liu."Critical Masses for Various Terrestrial Planet Atmospheric Gases and Water in/on Mars".TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES 25.5(2014):703-707.
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