首页> 美国卫生研究院文献>Astrobiology >Response of Atmospheric Biomarkers to NOx-Induced Photochemistry Generated by Stellar Cosmic Rays for Earth-like Planets in the Habitable Zone of M Dwarf Stars
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Response of Atmospheric Biomarkers to NOx-Induced Photochemistry Generated by Stellar Cosmic Rays for Earth-like Planets in the Habitable Zone of M Dwarf Stars

机译:大气生物标志物对M型矮星宜居区域中类地行星恒星宇宙射线产生的NOx诱导的光化学的响应

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摘要

Understanding whether M dwarf stars may host habitable planets with Earth-like atmospheres and biospheres is a major goal in exoplanet research. If such planets exist, the question remains as to whether they could be identified via spectral signatures of biomarkers. Such planets may be exposed to extreme intensities of cosmic rays that could perturb their atmospheric photochemistry. Here, we consider stellar activity of M dwarfs ranging from quiet up to strong flaring conditions and investigate one particular effect upon biomarkers, namely, the ability of secondary electrons caused by stellar cosmic rays to break up atmospheric molecular nitrogen (N2), which leads to production of nitrogen oxides (NOx) in the planetary atmosphere, hence affecting biomarkers such as ozone (O3). We apply a stationary model, that is, without a time dependence; hence we are calculating the limiting case where the atmospheric chemistry response time of the biomarkers is assumed to be slow and remains constant compared with rapid forcing by the impinging stellar flares. This point should be further explored in future work with time-dependent models. We estimate the NOx production using an air shower approach and evaluate the implications using a climate-chemical model of the planetary atmosphere. O3 formation proceeds via the reaction O+O2+M→O3+M. At high NOx abundances, the O atoms arise mainly from NO2 photolysis, whereas on Earth this occurs via the photolysis of molecular oxygen (O2). For the flaring case, O3 is mainly destroyed via direct titration, NO+O3→NO2+O2, and not via the familiar catalytic cycle photochemistry, which occurs on Earth. For scenarios with low O3, Rayleigh scattering by the main atmospheric gases (O2, N2, and CO2) became more important for shielding the planetary surface from UV radiation. A major result of this work is that the biomarker O3 survived all the stellar-activity scenarios considered except for the strong case, whereas the biomarker nitrous oxide (N2O) could survive in the planetary atmosphere under all conditions of stellar activity considered here, which clearly has important implications for missions that aim to detect spectroscopic biomarkers. Key Words: M dwarf—Atmosphere—Earth-like—Biomarkers—Stellar cosmic rays. Astrobiology 12, 1109–1122.
机译:系外行星研究的一个主要目标是了解M矮星是否可能拥有具有类似地球的大气层和生物圈的宜居行星。如果存在这样的行星,那么是否可以通过生物标记的光谱特征识别它们的问题仍然存在。这样的行星可能会暴露于极端强度的宇宙射线中,这可能会扰乱其大气的光化学反应。在这里,我们考虑了M个矮星的恒星活动,从安静到强烈的爆发条件,并研究了对生物标记的一种特殊影响,即恒星宇宙射线引起的二次电子分解大气分子氮(N2)的能力,从而导致在行星大气中产生氮氧化物(NOx),从而影响生物标记物,例如臭氧(O3)。我们应用固定模型,即没有时间依赖性;因此,我们正在计算极限情况,其中假设生物标志物的大气化学响应时间较慢,并且与撞击恒星耀斑的快速强迫相比保持恒定。在以后的工作中,应使用时间相关模型进一步探讨这一点。我们使用风淋方法估算NOx的产生,并使用行星大气的气候化学模型评估其影响。 O3的生成通过O + O2 + M→O3 + M反应进行。在高NOx含量下,O原子主要来自NO2的光解作用,而在地球上,这是通过分子氧(O2)的光解作用发生的。对于扩口情况,O3主要通过直接滴定法(NO + O3→NO2 + O2)而不是通过地球上常见的催化循环光化学来破坏。对于O3含量较低的场景,主要大气气体(O2,N 2 和CO 2 )的瑞利散射对于屏蔽行星表面免受紫外线辐射变得更为重要。这项工作的主要结果是,除了强烈的情况外,生物标记物O 3 在所有考虑的恒星活动场景中都幸免于难,而生物标记物一氧化二氮(N 2 O)可以在这里考虑的所有恒星活动条件下在行星大气中生存,这显然对旨在探测光谱生物标志物的任务具有重要意义。关键词:矮人-大气-类地球-生物标记物-恒星宇宙射线。天体生物学12,1109-1122。

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