Abiotic Production of Methane in Terrestrial Planets
Abiotic Production of Methane in Terrestrial Planets
复制标题
DOI:
10.1089/ast.2012.0817
复制
发表时间:
2013-06-01
期刊:
影响因子:
4.2
通讯作者:
Escobar-Briones, Elva
中科院分区:
文献类型:
--
作者:
Guzman-Marmolejo, Andres;Segura, Antigona;Escobar-Briones, Elva
On Earth, methane is produced mainly by life, and it has been proposed that, under certain conditions, methane detected in an exoplanetary spectrum may be considered a biosignature. Here, we estimate how much methane may be produced in hydrothermal vent systems by serpentinization, its main geological source, using the kinetic properties of the main reactions involved in methane production by serpentinization. Hydrogen production by serpentinization was calculated as a function of the available FeO in the crust, given the current spreading rates. Carbon dioxide is the limiting reactant for methane formation because it is highly depleted in aqueous form in hydrothermal vent systems. We estimated maximum CH4 surface fluxes of 6.8 x 10(8) and 1.3 x 10(9) molecules cm(-2) s(-1) for rocky planets with 1 and 5 M-circle plus, respectively. Using a 1-D photochemical model, we simulated atmospheres with volume mixing ratios of 0.03 and 0.1 CO2 to calculate atmospheric methane concentrations for the maximum production of this compound by serpentinization. The resulting abundances were 2.5 and 2.1 ppmv for 1 M-circle plus planets and 4.1 and 3.7ppmv for 5 M-circle plus planets. Therefore, low atmospheric concentrations of methane may be produced by serpentinization. For habitable planets around Sun-like stars with N-2-CO2 atmospheres, methane concentrations larger than 10 ppmv may indicate the presence of life.