Effects of Freeze-thaw on Soil Nitrogen Conversion: Research Progress

doi:10.11924/j.issn.1000-6850.casb2021-0121

Abstract

Abstract:

Nitrogen is one of the important nutrients limiting plant growth, and its transformation degree in soil is affected by many factors. As an important driving force for soil N transformation in mid, high latitude or high altitude areas, the effects of freeze-thaw also has a great impact on the process of soil N transformation. Based on existing research results at home and abroad, this paper summarized the effects of soil freeze-thaw cycles, freeze duration and freeze intensity on the process of soil N transformation. We summed up the general rules of soil N transformation caused by the changes of freeze-thaw patterns: changes in freezing and thawing patterns were all conducive to the mineralization of soil N. The increase of freeze-thaw intensity could significantly increase the content of soil nitrate N. Changes in freeze-thaw patterns will also increase N₂O emissions.

Key words: effect of freeze-thaw, freeze-thaw frequency, freeze-thaw duration, freeze-thaw strength, nitrogen mineralization

CLC Number:

S158.5

Yu He, Xie Hongbao, Chen Yimin, Wang Yao, Sui Yueyu, Jiao Xiaoguang. Effects of Freeze-thaw on Soil Nitrogen Conversion: Research Progress[J]. Chinese Agricultural Science Bulletin, 2021, 37(26): 88-92.

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