Abstract
Freeze–thaw can promote the production and fixation of DOC, NH4 +–N and NO3 −–N in wetland soils, and promote the depletion and release of wetland soil organic carbon and organic nitrogen. The DOC, NH4 +–N and NO3 −–N concentrations in the water overlying wetland and downstream water bodies will increase in the freeze–thaw period. As a result of global warming, fixation of DOC and NH4 +–N and the release of organic carbon in wetland soils may be weakened. Wetland reclamation also promotes the release of DOC and NH4 +–N from wetland soils.
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© 2013 Springer-Verlag Berlin Heidelberg
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Yu, X. (2013). Conclusions and Prospect. 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_9
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DOI: https://doi.org/10.1007/978-3-642-34465-7_9
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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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