Biochar Amendments Facilitate Methane Production by Regulating the Abundances of Methanogens and Methanotrophs in Flooded Paddy Soil

IF 2.1 Q3 SOIL SCIENCE Frontiers in soil science Pub Date : 2022-07-01 DOI:10.3389/fsoil.2022.801227
Jiakai Gao, Ling Liu, Z. Shi, J. Lv
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引用次数: 1

Abstract

The application of biochar in conjunction with fertilizer in agricultural production is one of the most promising types of management to improve soil quality. However, the effects on the soil microbial community and methane (CH4) emissions from the interactive mechanisms of biochar combined with fertilizer are unclear. In this study, soil column trial was conducted to monitor the surface water nitrogen, dissolved organic carbon (DOC) and CH4 emission dynamics during the process of leaching. Additionally, bacterial and archaeal communities of the soil (0-10 cm) amended with biochar derived from different pyrolysis temperatures (300°C, 500°C, and 700°C) were also analyzed. High-throughput sequencing revealed that the soil archaeal and bacterial community diversities increased under the biochar amendments. The CH4 emission flux of all the treatments in the whole leaching period ranged from 0.0001 to 2.04 μg m-2 h-1, and the DOC ranged from 1.86 to 24.4 mg L-1. Our results showed that biochar amendments significantly increase the soil pH, total nitrogen (TN), and DOC contents, while inhibiting the loss of NO 3 − N during leaching. In addition, biochar addition increased the paddy soil CH4 emissions, which ascribed to the increasing ratio of the abundances of methanogens to methanotrophs. Consequently, the higher CH4 emissions were probably caused by the stimulation of methanogenic archaea under the biochar amendments. Thus, the results obtained in this study can be applied to guide the application of biochar on greenhouse gas emissions in paddy soil.
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生物炭改良剂通过调节淹水稻田土壤中产甲烷菌和脱甲烷菌的丰度来促进甲烷的产生
将生物炭与肥料结合应用于农业生产是改善土壤质量最有前景的管理类型之一。然而,生物炭与肥料的相互作用机制对土壤微生物群落和甲烷(CH4)排放的影响尚不清楚。本研究采用土柱试验方法监测了浸出过程中地表水氮、溶解有机碳(DOC)和CH4的排放动态。此外,还分析了用不同热解温度(300°C、500°C和700°C)的生物炭改良的土壤(0-10 cm)的细菌和古菌群落。高通量测序显示,在生物炭改良剂的作用下,土壤古菌和细菌群落的多样性增加。在整个浸出期内,所有处理的CH4排放通量在0.0001-2.04μg m-2 h-1之间,DOC在1.86-24.4 mg L-1之间。我们的研究结果表明,生物炭改良剂显著提高了土壤pH值、总氮(TN)和DOC含量,同时抑制了NO3−N在浸出过程中的损失。此外,生物炭的添加增加了稻田土壤CH4的排放,这归因于产甲烷菌与产甲烷菌的丰度比的增加。因此,较高的CH4排放可能是由生物炭改良剂刺激产甲烷古菌引起的。因此,本研究结果可用于指导生物炭在水稻土温室气体排放方面的应用。
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