Abstract
The freeze–thaw process can significantly affect soil physicochemical properties and microbial activity as well as elemental cycling. Dynamics of the concentrations of dissolved carbon and nitrogen in wetland soil during the freeze–thaw period comprehensively reflect these processes.
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References
Grogan P, Michelsen A, Ambus P, Jonasson S. Freeze–thaw regime effects on carbon and nitrogen dynamics in sub–arctic heath tundra mesocosms. Soil Biol Biochem. 2004;36:641–54.
Henry HAL. Soil freeze–thaw cycle experiments: trends, methodological weaknesses and suggested improvements. Soil Biol Biochem. 2007;39:977–86.
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© 2013 Springer-Verlag Berlin Heidelberg
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Yu, X. (2013). Dynamics of Dissolved Carbon and Nitrogen in Wetland Soil and its Overlying Ice and Water During the Freeze–Thaw Period. 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_4
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DOI: https://doi.org/10.1007/978-3-642-34465-7_4
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Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-34464-0
Online ISBN: 978-3-642-34465-7
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