Perchlorate Radiolysis on Mars and the Origin of Martian Soil Reactivity

被引:113
作者
Quinn, Richard C. [1 ]
Martucci, Hana F. H. [2 ]
Miller, Stephanie R. [3 ]
Bryson, Charles E. [4 ]
Grunthaner, Frank J. [5 ]
Grunthaner, Paula J. [5 ]
机构
[1] NASA, Ames Res Ctr, Carl Sagan Ctr, SETI Inst, Moffett Field, CA 94035 USA
[2] San Jose State Univ, Dept Chem, San Jose, CA 95192 USA
[3] NASA, Ames Educ Associates Program, Moffett Field, CA USA
[4] Apparati Inc, Mountain View, CA USA
[5] NASA, Jet Prop Lab, Pasadena, CA USA
关键词
Mars; Radiolysis; Organic degradation; in situ measurement; Planetary habitability and biosignatures; GAS-EXCHANGE EXPERIMENT; VIKING; MODEL; DECOMPOSITION; SIMULATIONS; CHEMISTRY;
D O I
10.1089/ast.2013.0999
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Results from the Viking biology experiments indicate the presence of reactive oxidants in martian soils that have previously been attributed to peroxide and superoxide. Instruments on the Mars Phoenix Lander and the Mars Science Laboratory detected perchlorate in martian soil, which is nonreactive under the conditions of the Viking biology experiments. We show that calcium perchlorate exposed to gamma rays decomposes in a CO2 atmosphere to form hypochlorite (ClO-), trapped oxygen (O-2), and chlorine dioxide (ClO2). Our results show that the release of trapped O-2 (g) from radiation-damaged perchlorate salts and the reaction of ClO- with amino acids that were added to the martian soils can explain the results of the Viking biology experiments. We conclude that neither hydrogen peroxide nor superoxide is required to explain the results of the Viking biology experiments.
引用
收藏
页码:515 / 520
页数:6
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