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Carbon sequestration potential of soils in southeast Germany derived from stable soil organic carbon saturation
Authors:Martin Wiesmeier  Rico Hübner  Peter Spörlein  Uwe Geuß  Edzard Hangen  Arthur Reischl  Bernd Schilling  Margit von Lützow  Ingrid Kögel‐Knabner
Affiliation:1. Lehrstuhl für Bodenkunde, Department für ?kologie und ?kosystemmanagement, Wissenschaftszentrum Weihenstephan für Ern?hrung, Landnutzung und Umwelt, Technische Universit?t München, , Freising‐Weihenstephan, 85350 Germany;2. Lehrstuhl für Wirtschaftslehre des Landbaues, Wissenschaftszentrum Weihenstephan für Ern?hrung, Landnutzung und Umwelt, Technische Universit?t München, , Freising‐Weihenstephan, 85350 Germany;3. Bavarian Environment Agency, , Hof, 95030 Germany;4. Institute for Advanced Study, Technische Universit?t München, , Garching, 85748 Germany
Abstract:Sequestration of atmospheric carbon (C) in soils through improved management of forest and agricultural land is considered to have high potential for global CO2 mitigation. However, the potential of soils to sequester soil organic carbon (SOC) in a stable form, which is limited by the stabilization of SOC against microbial mineralization, is largely unknown. In this study, we estimated the C sequestration potential of soils in southeast Germany by calculating the potential SOC saturation of silt and clay particles according to Hassink [Plant and Soil 191 (1997) 77] on the basis of 516 soil profiles. The determination of the current SOC content of silt and clay fractions for major soil units and land uses allowed an estimation of the C saturation deficit corresponding to the long‐term C sequestration potential. The results showed that cropland soils have a low level of C saturation of around 50% and could store considerable amounts of additional SOC. A relatively high C sequestration potential was also determined for grassland soils. In contrast, forest soils had a low C sequestration potential as they were almost C saturated. A high proportion of sites with a high degree of apparent oversaturation revealed that in acidic, coarse‐textured soils the relation to silt and clay is not suitable to estimate the stable C saturation. A strong correlation of the C saturation deficit with temperature and precipitation allowed a spatial estimation of the C sequestration potential for Bavaria. In total, about 395 Mt CO2‐equivalents could theoretically be stored in A horizons of cultivated soils – four times the annual emission of greenhouse gases in Bavaria. Although achieving the entire estimated C storage capacity is unrealistic, improved management of cultivated land could contribute significantly to CO2 mitigation. Moreover, increasing SOC stocks have additional benefits with respect to enhanced soil fertility and agricultural productivity.
Keywords:agricultural management  climate change  CO2 mitigation  soil organic carbon stocks  soil fractionation  stabilization of soil organic matter
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