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生物炭改良剂缓解了冬小麦生长季稻田中的 NO 排放。

Biochar amendment mitigated NO emissions from paddy field during the wheat growing season.

机构信息

Jiangsu Key Laboratory of Low Carbon Agriculture and GHGs Mitigation, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing, 210095, China; Georg-August University of Göttingen, Department of Soil Science of Temperate Ecosystems, Department of Agricultural Soil Science, Büsgenweg 2, 37077, Göttingen, Germany.

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

出版信息

Environ Pollut. 2021 Jul 15;281:117026. doi: 10.1016/j.envpol.2021.117026. Epub 2021 Mar 27.

Abstract

Biochar may variably impact nitrogen (N) transformation and N-cycle-related microbial activities. Yet the mechanism of biochar amendment on nitrous oxide (NO) emissions from agricultural ecosystems remains unclear. Based on a 6-year long-term biochar amendment experiment, we applied a dual isotope (N-O) labeling technique with tracing transcriptional genes to differentiate the contribution of nitrifier nitrification (NN), nitrifier denitrification (ND), nitrification-coupled denitrification (NCD) and heterotrophic denitrification (HD) pathway to NO production. Then the field experiment provided quantitative data on dynamic NO emissions, soil mineral N and key functional marker gene abundances during the wheat growing season. By using N-O isotope, biochar decreased NO emission derived from ND (by 45-94%), HD (by 35-46%) and NCD (by 30-64%) compared to the values under N application. Biochar increased the relative contribution of NN to total NO production as evidenced by the increase in ammonia-oxidizing bacteria, but did not influence the cumulative NN-derived NO. The field experiment found that the majority of the NO emissions peaked following fertilization, in parallel with soil NH and nitrite dynamics. Soil NO emissions during the wheat growing stage were effectively decreased (by 38-48%) by biochar amendment. Based on the correlation analyses and random forest analysis in both microcosm and field experiments, the decrease in nitrite concentration (by 62-65%) and increase in NO consumption were mainly responsible for net NO mitigation, as evidenced by the decrease in the ratios of nitrite reductase genes/transcripts (nirS, nirK and fungal nirK) and NO reductase gene/transcripts (nosZI and nosZII). Based on the extrapolation from microcosm to field, biochar significantly mitigated NO emissions by weakening the ND processes, since NCD and HD contributed little during the NO emission "peaks" following urea fertilization. Therefore, emphasis should be put on the ND process and nitrite accumulation during NO emission peaks and extrapolated to all agroecosystems.

摘要

生物炭可能会对氮(N)转化和与 N 循环相关的微生物活性产生不同的影响。然而,生物炭改良对农业生态系统中一氧化二氮(NO)排放的机制仍不清楚。基于一项为期 6 年的生物炭改良长期试验,我们应用双同位素(N-O)标记技术和追踪转录基因,以区分硝化作用(NN)、硝化反硝化(ND)、硝化耦合反硝化(NCD)和异养反硝化(HD)途径对 NO 生成的贡献。然后,田间试验提供了小麦生长季节动态 NO 排放、土壤矿质 N 和关键功能标记基因丰度的定量数据。通过使用 N-O 同位素,与 N 应用相比,生物炭使 ND(减少 45-94%)、HD(减少 35-46%)和 NCD(减少 30-64%)产生的 NO 排放量减少。生物炭增加了氨氧化细菌的相对贡献,从而增加了 NN 对总 NO 生成的贡献,但不影响累积的 NN 衍生的 NO。田间试验发现,大部分 NO 排放紧随施肥后达到峰值,与土壤 NH 和亚硝酸盐动态平行。通过生物炭改良,有效地减少了小麦生长阶段的土壤 NO 排放(减少 38-48%)。基于微宇宙和田间试验的相关分析和随机森林分析,亚硝酸盐浓度的降低(降低 62-65%)和 NO 消耗的增加是净 NO 缓解的主要原因,这表现为亚硝酸盐还原酶基因/转录物(nirS、nirK 和真菌 nirK)和 NO 还原酶基因/转录物(nosZI 和 nosZII)的比值降低。基于从微宇宙到田间的外推,由于在尿素施肥后 NO 排放“高峰”期间 NCD 和 HD 贡献较小,因此生物炭通过削弱 ND 过程显著减轻了 NO 排放。因此,应在所有农业生态系统中重视 ND 过程和亚硝酸盐积累,尤其是在 NO 排放高峰期。

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