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WP 4a. Gaseous carbon flux from permafrost soils
WP 4 Team:
- Svetlana Evgrafova (PhD, Senior Researcher) – PI
- Oxana Masyagina (PhD, Research scientist)
- Sergey Syrtcov (Research scientist)
- Valentina Kholodilova (PhD-student)
WP 4 Motivation:
- Small changes in the stock of organic carbon in the permafrost soil by net emission of CO2 (or CH4) into the atmosphere will have a profound impact on the
atmosphere's CO2 (and CH4) concentration and with that very likely on the Earth's climate
- Landscape affects the fate of organic carbon in permafrost soils:
- aerobic conditions – release of CO2
- anaerobic conditions - microbial production of CH4
WP 4 Research questions:
- How much of CO2 and CH4 release from soil depending on the actual permafrost regime, and the soil temperature and soil moisture in the active layer?
- What the sources (biotic or abiotic) of the two gases?
WP 4 Approaches:
- Closed chamber technique for soil CO2 efflux and CH4 exchange measurements
- Analysis of stable carbon isotopic composition of gases with Picarro G213i
Expected outcome:
To relate results to the carbon stocks as determined in WP 2 in order to quantify the carbon release from soil depending on the permafrost regime
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