4.4 Article

On Detecting Biospheres from Chemical Thermodynamic Disequilibrium in Planetary Atmospheres

期刊

ASTROBIOLOGY
卷 16, 期 1, 页码 39-67

出版社

MARY ANN LIEBERT, INC
DOI: 10.1089/ast.2015.1327

关键词

-

资金

  1. Exobiology Program grant [NNX10AQ90G]
  2. NASA Earth and Space Sciences Fellowship [NNX15AR63H]
  3. NASA Astrobiology Institute's Virtual Planetary Laboratory [NNA13AA93A]
  4. NASA Washington Space Grant

向作者/读者索取更多资源

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.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.4
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据