Diffuse hydrothermal methane output and evidence of methanotrophic activity within the soils at Sousaki (Greece)
Identifieur interne : 000058 ( Main/Exploration ); précédent : 000057; suivant : 000059Diffuse hydrothermal methane output and evidence of methanotrophic activity within the soils at Sousaki (Greece)
Auteurs : W. D Lessandro [Italie] ; L. Brusca [Italie] ; K. Kyriakopoulos [Grèce] ; M. Martelli [Italie] ; G. Michas [Grèce] ; G. Papadakis [Grèce] ; F. Salerno [Italie]Source :
- Geofluids [ 1468-8115 ] ; 2011-02.
Descripteurs français
- Wicri :
- topic : Changement climatique, Micro-organisme.
English descriptors
- KwdEn :
- Atmospheric gases, Atmospheric methane, Bender conrad, Biological activity, Blackwell publishing, Carbon dioxide, Castaldi, Castaldi tedesco, Chamber method, Climate change, Concentration ratio, Consumption experiments, Consumption rate, Consumption rates, Deeper levels, Degassing, Diffuse hydrothermal methane output, Endogenous gases, Environmental microbiology, Etiope, Gaseous manifestations, Geogenic gases, Geophysical research letters, Geothermal, Geothermal areas, Geothermal research, Geothermal system, Global biogeochemical cycles, Global change biology, Harsh conditions, High consumption rates, High values, Hydrothermal, Hydrothermal alteration, Hydrothermal system, Hydrothermal systems, Intergovernmental panel, Laboratory incubation experiments, Lmol, Measurement campaigns, Measurement site, Mediterranean area, Methane, Methane emissions, Methane oxidation, Methanotrophic, Methanotrophic activity, Methanotrophic activity decreases, Methanotrophic bacteria, Methanotrophic microorganisms, Microorganism, Negative values, Ophiolithic rocks, Oxidation activity, Pantelleria island, Phylum verrucomicrobia, Pmolch4, Positive values, Present study, Previous estimates, Previous studies, Recent studies, Same order, Sampling sites, Soil gases, Soil sample, Soil samples, Sousaki, Southern italy, Study area, Such conditions, Such environments, Thermophilic methanotrophic bacteria, Uxes, Volcanic, Vulcanologia sezione, Water vapour, Water vapour output data.
- Teeft :
- Atmospheric gases, Atmospheric methane, Bender conrad, Biological activity, Blackwell publishing, Carbon dioxide, Castaldi, Castaldi tedesco, Chamber method, Climate change, Concentration ratio, Consumption experiments, Consumption rate, Consumption rates, Deeper levels, Degassing, Diffuse hydrothermal methane output, Endogenous gases, Environmental microbiology, Etiope, Gaseous manifestations, Geogenic gases, Geophysical research letters, Geothermal, Geothermal areas, Geothermal research, Geothermal system, Global biogeochemical cycles, Global change biology, Harsh conditions, High consumption rates, High values, Hydrothermal, Hydrothermal alteration, Hydrothermal system, Hydrothermal systems, Intergovernmental panel, Laboratory incubation experiments, Lmol, Measurement campaigns, Measurement site, Mediterranean area, Methane, Methane emissions, Methane oxidation, Methanotrophic, Methanotrophic activity, Methanotrophic activity decreases, Methanotrophic bacteria, Methanotrophic microorganisms, Microorganism, Negative values, Ophiolithic rocks, Oxidation activity, Pantelleria island, Phylum verrucomicrobia, Pmolch4, Positive values, Present study, Previous estimates, Previous studies, Recent studies, Same order, Sampling sites, Soil gases, Soil sample, Soil samples, Sousaki, Southern italy, Study area, Such conditions, Such environments, Thermophilic methanotrophic bacteria, Uxes, Volcanic, Vulcanologia sezione, Water vapour, Water vapour output data.
Abstract
Methane soil flux measurements have been made in 38 sites at the geothermal system of Sousaki (Greece) with the closed chamber method. Fluxes range from −47.6 to 29 150 mg m−2 day−1, and the diffuse CH4 output of the system has been estimated at 19 t a−1. Contemporaneous CO2 flux measurements showed a moderate positive correlation between CO2 and CH4 fluxes. Comparison of the CO2/CH4 soil flux ratios with the CO2/CH4 ratio of the gases of the main gas manifestations provided evidence for methanotrophic activity within the soil. Laboratory CH4 consumption experiments confirmed the presence of methanotrophic microorganisms in soil samples collected at Sousaki. Consumption was generally in the range from −4.9 to −38.9 pmolCH4 h−1 g−1 but could sometimes reach extremely high values (−33 000 pmolCH4 h−1 g−1). These results are consistent with recent studies on other geothermal systems that revealed the existence of thermoacidophilic bacteria exerting methanotrophic activity in hot, acid soils, thereby reducing methane emissions to the atmosphere.
Url:
DOI: 10.1111/j.1468-8123.2010.00322.x
Affiliations:
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<front><div type="abstract" xml:lang="en">Methane soil flux measurements have been made in 38 sites at the geothermal system of Sousaki (Greece) with the closed chamber method. Fluxes range from −47.6 to 29 150 mg m−2 day−1, and the diffuse CH4 output of the system has been estimated at 19 t a−1. Contemporaneous CO2 flux measurements showed a moderate positive correlation between CO2 and CH4 fluxes. Comparison of the CO2/CH4 soil flux ratios with the CO2/CH4 ratio of the gases of the main gas manifestations provided evidence for methanotrophic activity within the soil. Laboratory CH4 consumption experiments confirmed the presence of methanotrophic microorganisms in soil samples collected at Sousaki. Consumption was generally in the range from −4.9 to −38.9 pmolCH4 h−1 g−1 but could sometimes reach extremely high values (−33 000 pmolCH4 h−1 g−1). These results are consistent with recent studies on other geothermal systems that revealed the existence of thermoacidophilic bacteria exerting methanotrophic activity in hot, acid soils, thereby reducing methane emissions to the atmosphere.</div>
</front>
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