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有证据表明火星土壤的反应活性是由超氧离子引起的。

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

作者信息

Yen A S, Kim S S, Hecht M H, Frant M S, Murray B

机构信息

Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, USA.

出版信息

Science. 2000 Sep 15;289(5486):1909-12. doi: 10.1126/science.289.5486.1909.

Abstract

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 (O2-) 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.

摘要

海盗号着陆器未能探测到火星上存在生命的证据,相反,却发现了一种具有化学反应活性、能够分解有机分子的土壤。这种反应活性归因于火星土壤中存在一种或多种尚未确认的无机超氧化物或过氧化物。利用电子顺磁共振光谱,我们表明,在模拟火星大气条件下,暴露于紫外线辐射的类火星矿物表面会直接形成超氧自由基离子(O2-)。这些氧自由基可以解释土壤的反应特性以及火星表面明显缺乏有机物质的现象。

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