中国农业气象 ›› 2018, Vol. 39 ›› Issue (07): 442-452.doi: 10.3969/j.issn.1000-6362.2018.07.002
赵光昕,张晴雯,刘杏认,田秀平
出版日期:
2018-07-20
发布日期:
2018-07-17
作者简介:
赵光昕(1991?),硕士生,主要研究方向为农业生态系统碳氮循环。E-mail:zgxzhao@126.com
基金资助:
ZHAO Guang-xin, ZHANG Qing-wen, LIU Xing-ren, TIAN Xiu-ping
Online:
2018-07-20
Published:
2018-07-17
摘要: 氧化亚氮(N2O)是重要的温室气体之一,还会破坏大气臭氧层,影响全球气候变化。农田土壤是N2O最主要的排放源,由微生物主导的硝化和反硝化作用是其最主要的排放途径,因此,土壤的硝化和反硝化作用备受关注。在综合国内外相关研究的基础上,就区分硝化和反硝化作用对N2O排放贡献的研究方法、土壤N2O产生途径及其影响因素以及施用生物炭对N2O排放的影响机理进行归纳总结。结果表明:硝化和反硝化作用对生物炭的响应不同,在N2O减排效应上也存在很大的不确定性,其内在机理尚不明确。在此基础上,提出区分硝化和反硝化作用对N2O排放贡献的最佳研究方法,并就农田土壤硝化反硝化作用的影响因素以及对生物炭的响应机制进行研究展望。
赵光昕,张晴雯,刘杏认,田秀平. 农田土壤硝化反硝化作用及其对生物炭添加响应的研究进展[J]. 中国农业气象, 2018, 39(07): 442-452.
ZHAO Guang-xin, ZHANG Qing-wen, LIU Xing-ren, TIAN Xiu-ping. Nitrification and Denitrification and its Response to Biochar Addition in Agricultural Soil:A Review[J]. Chinese Journal of Agrometeorology, 2018, 39(07): 442-452.
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