4.4 Article

Perchlorate Radiolysis on Mars and the Origin of Martian Soil Reactivity

期刊

ASTROBIOLOGY
卷 13, 期 6, 页码 515-520

出版社

MARY ANN LIEBERT, INC
DOI: 10.1089/ast.2013.0999

关键词

Mars; Radiolysis; Organic degradation; in situ measurement; Planetary habitability and biosignatures

资金

  1. NASA [NNX09AM93G]
  2. NASA [110787, NNX09AM93G] Funding Source: Federal RePORTER

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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.

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