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On Detecting Biospheres from Chemical Thermodynamic Disequilibrium in Planetary Atmospheres

机译:从行星大气化学热力学不平衡中检测生物圈的研究

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Atmospheric chemical disequilibrium has been proposed as a method for detecting extraterrestrial biospheres from exoplanet observations. Chemical disequilibrium is potentially a generalized biosignature since it makes no assumptions about particular biogenic gases or metabolisms. Here, we present the first rigorous calculations of the thermodynamic chemical disequilibrium in Solar System atmospheres, in which we quantify the available Gibbs energy: the Gibbs free energy of an observed atmosphere minus that of atmospheric gases reacted to equilibrium. The purely gas phase disequilibrium in Earth's atmosphere is mostly attributable to O-2 and CH4. The available Gibbs energy is not unusual compared to other Solar System atmospheres and smaller than that of Mars. However, Earth's fluid envelope contains an ocean, allowing gases to react with water and requiring a multiphase calculation with aqueous species. The disequilibrium in Earth's atmosphere-ocean system (in joules per mole of atmosphere) ranges from approximate to 20 to 2x10(6) times larger than the disequilibria of other atmospheres in the Solar System, where Mars is second to Earth. Only on Earth is the chemical disequilibrium energy comparable to the thermal energy per mole of atmosphere (excluding comparison to Titan with lakes, where quantification is precluded because the mean lake composition is unknown). Earth's disequilibrium is biogenic, mainly caused by the coexistence of N-2, O-2, and liquid water instead of more stable nitrate. In comparison, the O-2-CH4 disequilibrium is minor, although kinetics requires a large CH4 flux into the atmosphere. We identify abiotic processes that cause disequilibrium in the other atmospheres. Our metric requires minimal assumptions and could potentially be calculated from observations of exoplanet atmospheres. However, further work is needed to establish whether thermodynamic disequilibrium is a practical exoplanet biosignature, requiring an assessment of false positives, noisy observations, and other detection challenges. Our Matlab code and databases for these calculations are available, open source. Key Words: BiosignaturesDisequilibriumPlanetary atmospheresGibbs free energyExoplanetsEquilibriumThermodynamics. Astrobiology 16, 39-67.
机译:大气化学不平衡已被提议作为一种从系外行星观测中探测地外生物圈的方法。化学不平衡可能是普遍的生物特征,因为它不对特定的生物气体或代谢做出任何假设。在这里,我们对太阳系大气中的热力学化学不平衡进行了首次严格的计算,在其中我们量化了可用的吉布斯能量:观测到的大气中的吉布斯自由能减去反应达到平衡的大气气体的吉布斯自由能。地球大气中的纯气相不平衡主要归因于O-2和CH4。与其他太阳系大气相比,可用的吉布斯能量并不罕见,比火星还小。但是,地球的流体包裹层包含海洋,使气体与水发生反应,并需要对含水物种进行多相计算。地球大气-海洋系统中的不平衡(以每摩尔大气焦耳为单位)的范围约为火星次于地球的太阳系中其他大气的不平衡的20到2x10(6)倍。仅在地球上,化学不平衡能与每摩尔大气的热能相当(不包括与泰坦湖的比较,由于不知道平均湖组成,因此无法进行量化)。地球的不平衡是生物成因的,主要是由N-2,O-2和液态水(而不是更稳定的硝酸盐)共存引起的。相比之下,O-2-CH4的不平衡很小,尽管动力学需要大量的CH4通入大气。我们确定了导致其他环境不平衡的非生物过程。我们的度量标准仅需极少的假设,并且有可能根据对系外行星大气的观测来计算。但是,需要进一步的工作来确定热力学不平衡是否是实际的系外行星生物特征,这需要评估假阳性,嘈杂的观测结果和其他检测挑战。我们用于这些计算的Matlab代码和数据库是可用的,开源的。关键词:生物签名失衡行星大气吉布斯自由能系外行星平衡热力学。天体生物学16,39-67。

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  • 来源
    《Astrobiology》 |2016年第1期|39-67|共29页
  • 作者单位

    Univ Washington, Dept Earth & Space Sci, Astrobiol Program, Seattle, WA 98195 USA;

    Stanford Univ, Dept Chem Engn, Stanford, CA 94305 USA;

    Univ Washington, Dept Earth & Space Sci, Astrobiol Program, Seattle, WA 98195 USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 13:05:34

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