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稻麦轮作体系中生物炭施用对土壤氧化亚氮浓度剖面及扩散与排放的影响。

Soil concentration profiles and diffusion and emission of nitrous oxide influenced by the application of biochar in a rice-wheat annual rotation system.

作者信息

Zhou Ziqiang, Xu Xin, Bi Zhichao, Li Lu, Li Bo, Xiong Zhengqin

机构信息

Jiangsu Key Laboratory of Low Carbon Agriculture and GHG Mitigation, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing, 210095, China.

出版信息

Environ Sci Pollut Res Int. 2016 Apr;23(8):7949-61. doi: 10.1007/s11356-015-5929-x. Epub 2016 Jan 15.

Abstract

Field experiments were carried out to determine biochar effects on nitrous oxide (N2O) concentration profiles, diffusion, and emissions in paddy soil under rice-wheat annual rotation in southeastern China. An in situ soil gas device was adapted to measure N2O concentrations at depths of 7, 15, 30, and 50 cm. Five treatments were installed as N0B0, N0B1, N1B0, N1B1, and N1B2 (B0, B1, and B2 designated as biochar at 0, 20, and 40 t ha(-1), respectively, while N0 and N1 as nitrogen at 0 and 250 kg N ha(-1) crop(-1), respectively). The results showed that N2O concentrations were higher in the 15 and 30 cm depths than other depths. With positive diffusive fluxes, the 7 cm in the rice season and 15 cm in the wheat season were main production sites. The surface N2O emissions and topsoil diffusive fluxes showed good agreement. N application strongly increased soil N2O profiles and surface emissions. Relative to N1B0, N1B1 decreased N2O concentration, surface emissions, and diffusive fluxes by 25.2, 31.8, and 26.5 %, respectively, while N1B2 decreased them averagely by 40.7, 43.2, and 44.2 %, correspondingly. Therefore, the gas gradient method is effective for estimating N2O emissions, and biochar can decrease N2O production when N was applied.

摘要

在中国东南部稻麦轮作的稻田土壤中进行了田间试验,以确定生物炭对一氧化二氮(N₂O)浓度剖面、扩散及排放的影响。采用原位土壤气体装置测量7、15、30和50厘米深度处的N₂O浓度。设置了五个处理,分别为N0B0、N0B1、N1B0、N1B1和N1B2(B0、B1和B2分别表示生物炭施用量为0、20和40吨·公顷⁻¹,而N0和N1分别表示氮肥施用量为0和250千克·氮·公顷⁻¹·作物⁻¹)。结果表明,15和30厘米深度处的N₂O浓度高于其他深度。在正扩散通量下,水稻季的7厘米深度处和小麦季的15厘米深度处是主要产生位点。地表N₂O排放与表土扩散通量表现出良好的一致性。施氮显著增加了土壤N₂O剖面和地表排放。相对于N1B0,N1B1使N₂O浓度、地表排放和扩散通量分别降低了25.2%、31.8%和26.5%,而N1B2相应地平均降低了40.7%、43.2%和44.2%。因此,气体梯度法对于估算N₂O排放是有效的,并且在施氮时生物炭可以减少N₂O的产生。

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