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DOI10.1126/science.abc7717
Long-term drying of Mars by sequestration of ocean-scale volumes of water in the crust
Scheller E.L.; Ehlmann B.L.; Hu R.; Adams D.J.; Yung Y.L.
发表日期2021
ISSN0036-8075
起始页码56
结束页码62
卷号372期号:6537
英文摘要Geological evidence shows that ancient Mars had large volumes of liquid water. Models of past hydrogen escape to space, calibrated with observations of the current escape rate, cannot explain the present-day deuterium-to-hydrogen isotope ratio (D/H). We simulated volcanic degassing, atmospheric escape, and crustal hydration on Mars, incorporating observational constraints from spacecraft, rovers, and meteorites. We found that ancient water volumes equivalent to a 100 to 1500 meter global layer are simultaneously compatible with the geological evidence, loss rate estimates, and D/H measurements. In our model, the volume of water participating in the hydrological cycle decreased by 40 to 95% over the Noachian period (~3.7 billion to 4.1 billion years ago), reaching present-day values by ~3.0 billion years ago. Between 30 and 99% of martian water was sequestered through crustal hydration, demonstrating that irreversible chemical weathering can increase the aridity of terrestrial planets. © 2021 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works
英文关键词chemical weathering; crust; deuterium; hydration; hydrogen isotope; hydrological cycle; isotopic ratio; Mars; Article; astronomy; atmospheric diffusion; deuterium hydrogen exchange; evolution; geological time; historical period; hydration; hydrology; priority journal; sea; volcano; water content; water loss; weathering; Emmelichthyidae
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/245365
作者单位Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, United States; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, United States
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Scheller E.L.,Ehlmann B.L.,Hu R.,et al. Long-term drying of Mars by sequestration of ocean-scale volumes of water in the crust[J],2021,372(6537).
APA Scheller E.L.,Ehlmann B.L.,Hu R.,Adams D.J.,&Yung Y.L..(2021).Long-term drying of Mars by sequestration of ocean-scale volumes of water in the crust.Science,372(6537).
MLA Scheller E.L.,et al."Long-term drying of Mars by sequestration of ocean-scale volumes of water in the crust".Science 372.6537(2021).
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