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长期添加生物炭对稻田土壤细菌和真菌反硝化一氧化氮排放的影响

[Effects of Long-term Biochar Addition on Denitrification NO Emissions from Bacteria and Fungi in Paddy Soil].

作者信息

Wang Meng-Jie, Jiang Wen-Ting, Xu You-Xiang, Liu Yu-Xue, Lü Hao-Hao, Wang Yu-Ying, Yang Sheng-Mao, He Li-Li, Cai Yan-Jiang

机构信息

State Key Laboratory of Subtropical Silviculture, College of Environment and Resources, College of Carbon Neutrality, Zhejiang A&F University, Hangzhou 311300, China.

Zhejiang Engineering Research Center of Biochar, Institute of Environment Resources and Soi Fertilizer, Zhejiang Academy of Agricultural Sciences, Hangzhou 310021, China.

出版信息

Huan Jing Ke Xue. 2024 Aug 8;45(8):4923-4931. doi: 10.13227/j.hjkx.202309176.

Abstract

Denitrification driven by bacteria and fungi is the main source of nitrous oxide (NO) emissions from paddy soil. It is generally believed that biochar reduces NO emissions by influencing the bacterial denitrification process, but the relevant mechanism of its impact on fungal denitrification is still unclear. In this study, the long-term straw carbonization returning experimental field in Changshu Agricultural Ecological Experimental Base of the Chinese Academy of Sciences was taken as the object. Through indoor anaerobic culture and molecular biology technology, the relative contributions of bacteria and fungi to denitrifying NO production in paddy soil and the related microorganism mechanism were studied under different long-term biochar application amounts (blank, 2.25 t·hm, and 22.5 t·hm, respectively, expressed by BC0, BC1, and BC10). The results showed that compared with that in BC0, biochar treatment significantly reduced NO emission rate, denitrification potential, and cumulative NO emissions, and the contribution of bacterial denitrification was greater than that of fungal denitrification in all three treatments. Among them, the relative contribution rate of bacterial denitrification in BC10 (62.9%) was significantly increased compared to BC0 (50.8%), whereas the relative contribution rate of fungal denitrification in BC10 (37.1%) was significantly lower than that in BC0 (49.2%). The application of biochar significantly increased the abundance of bacterial denitrification functional genes (, , and ) but reduced the abundance of fungal genes. The contribution rate of fungal denitrification was significantly positively correlated with the NO emission rate and negatively correlated with soil pH, TN, SOM, and DOC. Biochar may have inhibited the growth of denitrifying fungi by increasing pH and carbon and nitrogen content, reducing the abundance of related functional genes, thereby weakening the reduction ability of NO to NO during fungal denitrification process. This significantly reduces the contribution rate of NO production during the fungal denitrification process and the denitrification NO emissions from paddy soil. This study helps to broaden our understanding of the denitrification process in paddy soil and provides a theoretical basis for further regulating fungal denitrification NO emissions.

摘要

细菌和真菌驱动的反硝化作用是稻田土壤氧化亚氮(N₂O)排放的主要来源。一般认为,生物炭通过影响细菌反硝化过程来减少N₂O排放,但其对真菌反硝化作用影响的相关机制仍不清楚。本研究以中国科学院常熟农业生态试验基地的长期秸秆炭化还田试验田为研究对象,通过室内厌氧培养和分子生物学技术,研究了不同长期生物炭施用量(分别以BC0、BC1和BC10表示空白、2.25 t·hm⁻²和22.5 t·hm⁻²)下,细菌和真菌对稻田土壤反硝化产生N₂O的相对贡献及相关微生物机制。结果表明,与BC0相比,生物炭处理显著降低了N₂O排放速率、反硝化潜力和累积N₂O排放量,且在所有三种处理中细菌反硝化的贡献均大于真菌反硝化。其中,BC10中细菌反硝化的相对贡献率(62.9%)相较于BC0(50.8%)显著增加,而BC10中真菌反硝化的相对贡献率(37.1%)显著低于BC0(49.2%)。生物炭的施用显著增加了细菌反硝化功能基因(nirS、nirK和nosZ)的丰度,但降低了真菌nirK基因的丰度。真菌反硝化贡献率与N₂O排放速率显著正相关,与土壤pH、TN、SOM和DOC显著负相关。生物炭可能通过提高pH值以及碳氮含量,降低相关功能基因丰度,从而抑制了反硝化真菌的生长,进而削弱了真菌反硝化过程中N₂O还原为N₂的能力。这显著降低了真菌反硝化过程中N₂O产生的贡献率以及稻田土壤反硝化N₂O排放量。本研究有助于拓宽我们对稻田土壤反硝化过程的理解,并为进一步调控真菌反硝化N₂O排放提供理论依据。

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