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EXO-/ASTROBIOLOGY WITH A DARWIN/TPF MISSION

机译:DARWIN / TPF任务的EXO //生物生物学

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摘要

The spectroscopic characterization of Earth-like ex-oplanets is one of the goals shared by two major projects: Darwin (ESA) and TPF-Terrestrial Planet Finder (NASA). By producing low resolution spectra of the planetary thermal emission, they will be able to detect the 9.6 μm band of O_3 which may be the signature of an O_2-rich atmosphere sustained by a biological activity. In this paper, we review several studies focusing on the possible use of this ozone signature as a biomarker for terrestrial exoplanets. First, we stress the risk of false positive detection produced by abiotic photochemical production of O_2 and O_3 and we show how to filter these imposters out by selecting only the simultaneous detection of O_3-CO_2-H_2O (triple signature). In a second part, we investigate the false, negative, cases: when O_2-rich atmospheres do not exhibit the O_3 feature. This happens when the partial pressure of CO_2 is too high or, unexpectedly, when the O_3 layer is too dense. Eventually, we present other eventual biomarkers that could trace life where O_3 fails.
机译:像地球系外行星的光谱表征是两个主要项目共有的目标之一:达尔文(ESA)和TPF-地面行星搜索器(NASA)。通过产生行星热辐射的低分辨率光谱,他们将能够检测到9.6μm的O_3带,这可能是生物活动所维持的富含O_2的大气的特征。在本文中,我们回顾了几项研究,重点研究了可能将这种臭氧特征用作陆地系外行星的生物标记的可能性。首先,我们强调由非生物光化学生产O_2和O_3产生假阳性检测的风险,并且我们展示了如何通过仅选择同时检测O_3-CO_2-H_2O(三重签名)来过滤掉这些冒名顶替者。在第二部分中,我们调查了错误的,否定的情况:当富含O_2的大气不表现出O_3特征时。当CO_2的分压太高或O_3层太稠密时,就会发生这种情况。最终,我们提出了其他可能追踪O_3失效的生物标记物。

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