Swindle Timothy D, Pack Andreas, Schwenzer Susanne P, Young Edward D
Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721.
Georg-August-Universitāt, Geowissenschaftliches Zentrum, Department of Geochemistry and Isotope Geology, Goldschmidtstraße 1, Göttingen D-37073, Germany.
Proc Natl Acad Sci U S A. 2025 Jan 14;122(2):e2404258121. doi: 10.1073/pnas.2404258121. Epub 2025 Jan 6.
The elemental and isotopic abundances of major species in the Martian atmosphere have been determined, but analyses often lack sufficient precision, and those of minor and trace species are frequently not well known. Many important questions about the evolution and current state of Mars require the kind of knowledge that can be gained from analysis of a returned sample of the Martian atmosphere. Key target species include the noble gases, nitrogen, and various species containing carbon, hydrogen, and oxygen, such as methane. More detailed analyses will no doubt provide measurements of other species that will allow insights of their own. These volatiles can constrain the origin of the Martian atmosphere, exchange of volatiles between the surface and interior, polar processes, and (in the case of methane) the possibility of extant biology on Mars.
火星大气中主要成分的元素丰度和同位素丰度已被测定,但分析往往缺乏足够的精度,而次要和痕量成分的丰度通常并不为人熟知。许多关于火星演化和当前状态的重要问题需要通过对返回的火星大气样本进行分析才能获得相关知识。关键目标成分包括稀有气体、氮以及各种含碳、氢和氧的成分,如甲烷。更详细的分析无疑将提供对其他成分的测量结果,这些结果也将带来各自的见解。这些挥发性物质可以限制火星大气的起源、表面与内部之间挥发性物质的交换、极地过程,以及(就甲烷而言)火星上现存生物存在的可能性。