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DOI10.1126/science.1147039
A sulfur dioxide climate feedback on early Mars
Halevy I.; Zuber M.T.; Schrag D.P.
发表日期2007
ISSN0036-8075
起始页码1903
结束页码1907
卷号318期号:5858
英文摘要Ancient Mars had liquid water on its surface and a CO2-rich atmosphere. Despite the implication that massive carbonate deposits should have formed, these have not been detected. On the basis of fundamental chemical and physical principles, we propose that climatic conditions enabling the existence of liquid water were maintained by appreciable atmospheric concentrations of volcanically degassed SO2 and H2S. The geochemistry resulting from equilibration of this atmosphere with the hydrological cycle is shown to inhibit the formation of carbonates. We propose an early martian climate feedback involving SO2, much like that maintained by CO 2 on Earth.
英文关键词carbon dioxide; carbonic acid; hydrogen sulfide; mineral; silicate; sulfur dioxide; water; atmospheric chemistry; carbon dioxide; carbonate; climate conditions; climate feedback; concentration (composition); geochemistry; Mars; sulfur dioxide; article; astronomy; atmosphere; climate; environmental temperature; geochemistry; liquid; magnetic field; precipitation; priority journal; sediment; weather; Atmosphere; Carbon Dioxide; Carbonates; Climate; Extraterrestrial Environment; Hydrogen Sulfide; Mars; Oxidation-Reduction; Photolysis; Precipitation; Sulfites; Sulfur Dioxide; Temperature; Water
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/243920
作者单位Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, United States; Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, United States
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Halevy I.,Zuber M.T.,Schrag D.P.. A sulfur dioxide climate feedback on early Mars[J],2007,318(5858).
APA Halevy I.,Zuber M.T.,&Schrag D.P..(2007).A sulfur dioxide climate feedback on early Mars.Science,318(5858).
MLA Halevy I.,et al."A sulfur dioxide climate feedback on early Mars".Science 318.5858(2007).
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