Soil Organic Carbon Pools and Stocks in Permafrost-Affected Soils on the Tibetan Plateau

The Tibetan Plateau reacts particularly sensitively to possible effects of climate change. Approximately two thirds of the total area is affected by permafrost. To get a better understanding of the role of permafrost on soil organic carbon pools and stocks, investigations were carried out including...

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Bibliographic Details
Published in:PLoS ONE
Main Authors: Doerfer, Corina, Kuehn, Peter, Baumann, Frank, He, Jin-Sheng, Scholten, Thomas
Other Authors: Dorfer, C (reprint author), Univ Tubingen, Dept Geosci Phys Geog & Soil Sci, Tubingen, Germany., Univ Tubingen, Dept Geosci Phys Geog & Soil Sci, Tubingen, Germany., Peking Univ, Coll Urban & Environm Sci, Dept Ecol, Beijing 100871, Peoples R China.
Format: Journal/Newspaper
Language:English
Published: plos one 2013
Subjects:
C-13 NMR-SPECTROSCOPY
QINGHAI-TIBET
DENSITY FRACTIONS
TEMPERATURE-DEPENDENCE
MATTER DECOMPOSITION
CLIMATIC-CHANGE
ALPINE MEADOW
TUNDRA SOILS
FOREST SOILS
CHINA
Active layer thickness
permafrost
Tundra
Online Access:https://hdl.handle.net/20.500.11897/391957
https://doi.org/10.1371/journal.pone.0057024
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Summary:The Tibetan Plateau reacts particularly sensitively to possible effects of climate change. Approximately two thirds of the total area is affected by permafrost. To get a better understanding of the role of permafrost on soil organic carbon pools and stocks, investigations were carried out including both discontinuous (site Huashixia, HUA) and continuous permafrost (site Wudaoliang, WUD). Three organic carbon fractions were isolated using density separation combined with ultrasonic dispersion: the light fractions (<1.6 g cm(-3)) of free particulate organic matter (FPOM) and occluded particulate organic matter (OPOM), plus a heavy fraction (>1.6 g cm(-3)) of mineral associated organic matter (MOM). The fractions were analyzed for C, N, and their portion of organic C. FPOM contained an average SOC content of 252 g kg(-1). Higher SOC contents (320 g kg(-1)) were found in OPOM while MOM had the lowest SOC contents (29 g kg(-1)). Due to their lower density the easily decomposable fractions FPOM and OPOM contribute 27% (HUA) and 22% (WUD) to the total SOC stocks. In HUA mean SOC stocks (0-30 cm depth) account for 10.4 kg m(-2), compared to 3.4 kg m(-2) in WUD. 53% of the SOC is stored in the upper 10 cm in WUD, in HUA only 39%. Highest POM values of 36% occurred in profiles with high soil moisture content. SOC stocks, soil moisture and active layer thickness correlated strongly in discontinuous permafrost while no correlation between SOC stocks and active layer thickness and only a weak relation between soil moisture and SOC stocks could be found in continuous permafrost. Consequently, permafrost-affected soils in discontinuous permafrost environments are susceptible to soil moisture changes due to alterations in quantity and seasonal distribution of precipitation, increasing temperature and therefore evaporation. Multidisciplinary Sciences SCI(E) 9 ARTICLE 2 null 8

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