火星探测计划
甲烷
火星人
火星大气层
天体生物学
大气(单位)
大气甲烷
环境科学
沉积岩
大气科学
地球科学
地质学
化学
地球化学
地理
气象学
物理
有机化学
作者
Christopher R. Webster,P. R. Mahaffy,S. K. Atreya,John E. Moores,Gregory J. Flesch,C. A. Malespin,Christopher P. McKay,Germán Martínez,C. L. Smith,Javier Martín‐Torres,Javier Gómez‐Elvira,María‐Paz Zorzano,Michael H. Wong,M. G. Trainer,A. Steele,Doug Archer,B. Sutter,Patrice Coll,Caroline Freissinet,Pierre‐Yves Meslin
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:2018-06-07
卷期号:360 (6393): 1093-1096
被引量:292
标识
DOI:10.1126/science.aaq0131
摘要
Variable levels of methane in the martian atmosphere have eluded explanation partly because the measurements are not repeatable in time or location. We report in situ measurements at Gale crater made over a 5-year period by the Tunable Laser Spectrometer on the Curiosity rover. The background levels of methane have a mean value 0.41 ± 0.16 parts per billion by volume (ppbv) (95% confidence interval) and exhibit a strong, repeatable seasonal variation (0.24 to 0.65 ppbv). This variation is greater than that predicted from either ultraviolet degradation of impact-delivered organics on the surface or from the annual surface pressure cycle. The large seasonal variation in the background and occurrences of higher temporary spikes (~7 ppbv) are consistent with small localized sources of methane released from martian surface or subsurface reservoirs.
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