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Fe(II) Oxidation and Sources of Acidity on MarsThere is an apparent paradox be-tween the evidence that aqueous environments on Mars were predominantly acidic, and the fact that Mars is predominantly a basaltic (and olivine-rich) planet. The problem being that basalt and olivine will act to neutralize acidic solutions they come into contact with, and that there is a lot more basaltic crust on Mars than water or acid. This is especially true if there is an appreciable amount of water available to bring the acid in contact with the basaltic crust. Several hypotheses for ancient mar-tian environments call on long lived groundwater and aqueous systems.
Document ID
20170002052
Document Type
Conference Paper
Authors
Niles, P. B. (NASA Johnson Space Center Houston, TX, United States)
Peretyazkho, T. S. (Jacobs Technology, Inc. Houston, TX, United States)
Sutter, B. (Jacobs Technology, Inc. Houston, TX, United States)
Date Acquired
March 8, 2017
Publication Date
March 20, 2017
Subject Category
Lunar and Planetary Science and Exploration
Report/Patent Number
JSC-CN-38859
Meeting Information
Lunar and Planetary Science Conference(The Woodlands, TX)
Distribution Limits
Public
Copyright
Public Use Permitted.

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