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Material Cycling of Wetland Soils Driven by Freeze-Thaw Effects pp 57–66Cite as

Freeze–Thaw Effects on Sorption/Desorption of Dissolved Organic Carbon in Wetland Soils

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Abstract

Dissolved organic carbon (DOC) is a major controlling factor in soil formation (Dawson et al. 1978), mineral weathering (Raulund–Rasmussen et al. 1998), nutrient cycling, microbial activity, and organic matter decomposition and transformation in soils (Magill and Aber 2000; Williams et al. 2000). The sorption of DOC is the dominant factor in DOC concentration in soil solutions, transport and transformation and the microbial availability of DOC. It is not only the major control for organic matter (OM) and OM–assisted transport (Kaiser and Zech 1999); it also contributes to the stabilization and accumulation of organic matter in soils (Guggenberger and Kaiser 2003).

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Authors and Affiliations

  1. Northeast Institute of Geography, Chinese Academy of Sciences, Changchun, People’s Republic of China

    Xiaofei Yu

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Yu, X. (2013). Freeze–Thaw Effects on Sorption/Desorption of Dissolved Organic Carbon in Wetland Soils. In: Material Cycling of Wetland Soils Driven by Freeze-Thaw Effects. Springer Theses. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-34465-7_5

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