Evidence that the reactivity of the martian soil is due to superoxide ions

被引:206
作者
Yen, AS
Kim, SS
Hecht, MH
Frant, MS
Murray, B
机构
[1] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[2] Chemot Consulting, Newton, MA 02458 USA
[3] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
关键词
D O I
10.1126/science.289.5486.1909
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The Viking Landers were unable to detect evidence of Life on Mars but, instead, found a chemically reactive soil capable of decomposing organic molecules. This reactivity was attributed to the presence of one or more as-yet-unidentified inorganic superoxides or peroxides in the martian soil. Using electron paramagnetic resonance spectroscopy, we show that superoxide radical ions (O-2(-)) form directly on Mars-analog mineral surfaces exposed to ultraviolet radiation under a simulated martian atmosphere. These oxygen radicals can explain the reactive nature of the soil and the apparent absence of organic material at the martian surface.
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收藏
页码:1909 / 1912
页数:4
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