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Effects of nitrogen and biochar amendment on soil methane concentration profiles and diffusion in a rice-wheat annual rotation system

The CH(4) emissions from soil were influenced by the changeable CH(4) concentrations and diffusions in soil profiles, but that have been subjected to nitrogen (N) and biochar amendment over seasonal and annual time frames. Accordingly, a two-year field experiment was conducted in southeastern China...

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Detalles Bibliográficos
Autores principales: Xu, Xin, Wu, Zhen, Dong, Yubing, Zhou, Ziqiang, Xiong, Zhengqin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5144129/
https://www.ncbi.nlm.nih.gov/pubmed/27929052
http://dx.doi.org/10.1038/srep38688
Descripción
Sumario:The CH(4) emissions from soil were influenced by the changeable CH(4) concentrations and diffusions in soil profiles, but that have been subjected to nitrogen (N) and biochar amendment over seasonal and annual time frames. Accordingly, a two-year field experiment was conducted in southeastern China to determine the amendment effects on CH(4) concentrations and diffusive effluxes as measured by a multilevel sampling probe in paddy soil during two cycles of rice-wheat rotations. The results showed that the top 7-cm soil layers were the primary CH(4) production sites during the rice-growing seasons. This layer acted as the source of CH(4) generation and diffusion, and the deeper soil layers and the wheat season soil acted as the sink. N fertilization significantly increased the CH(4) concentration and diffusive effluxes in the top 7-cm layers during the 2013 and 2014 rice seasons. Following biochar amendment, the soil CH(4) concentrations significantly decreased during the rice season in 2014, relative to the single N treatment. Moreover, 40 t ha(−1) biochar significantly decreased the diffusive effluxes during the rice seasons in both years. Therefore, our results showed that biochar amendment is a good strategy for reducing the soil profile CH(4) concentrations and diffusive effluxes induced by N in paddy fields.