Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia

LS Shirokova, OS Pokrovsky, SN Kirpotin, C Desmukh… - Biogeochemistry, 2013 - Springer
Active processes of permafrost thaw in Western Siberia increase the number of soil
subsidencies, thermokarst lakes and thaw ponds. In continuous permafrost zones, this …
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[引用][C] Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia

LS Shirokova, OS Pokrovsky, SN Kirpotin… - …, 2013 - ui.adsabs.harvard.edu
Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies
in discontinuous permafrost zones of Western Siberia - NASA/ADS Now on home page ads icon …

[引用][C] Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia

OS Pokrovsky, SN Kirpotin, C Desmukh… - … . 2013. Vol. 113. P …, 2013 - openrepository.ru
Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies
in discontinuous permafrost zones of Western Siberia - «Национальный агрегатор открытых …

Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia

LS Shirokova, OS Pokrovsky, S Audry, J Viers… - Biogeochemistry, 2013 - elibrary.ru
Active processes of permafrost thaw in Western Siberia increase the number of soil
subsidencies, thermokarst lakes and thaw ponds. In continuous permafrost zones, this …
[PDF] researchgate.net

[PDF][PDF] Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia

LS Shirokova, OS Pokrovsky, SN Kirpotin… - …, 2013 - researchgate.net
Active processes of permafrost thaw in Western Siberia increase the number of soil
subsidencies, thermokarst lakes and thaw ponds. In continuous permafrost zones, this …

Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia.

LS Shirokova, OS Pokrovsky, SN Kirpotin, C Desmukh… - 2013 - cabidigitallibrary.org
Active processes of permafrost thaw in Western Siberia increase the number of soil
subsidencies, thermokarst lakes and thaw ponds. In continuous permafrost zones, this …

[引用][C] Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia

LS SHIROKOVA, OS POKROVSKY… - Biogeochemistry …, 2013 - pascal-francis.inist.fr
Keyword (en) atmosphere biodegradation organic carbon concentration carbon dioxide
depressions ecosystems trace elements ponds forests lakes bogs colloidal materials …

Biogeochemistry of organic carbon, CO, CH, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia.

L Shirokova, O Pokrovsky, S Kirpotin… - …, 2013 - search.ebscohost.com
Active processes of permafrost thaw in Western Siberia increase the number of soil
subsidencies, thermokarst lakes and thaw ponds. In continuous permafrost zones, this …

[引用][C] Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia

OS Pokrovsky, SN Kirpotin, C Desmukh, BG Pokrovsky… - 2013 - vital.lib.tsu.ru
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[引用][C] Biogeochemistry of organic carbon, CO2, CH4, and trace elements in thermokarst water bodies in discontinuous permafrost zones of Western Siberia

LS Shirokova, OS Pokrovsky, SN Kirpotin, C Desmukh… - 2013