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首页> 外文期刊>The Science of the Total Environment >Effects of biochar on methane emission from paddy soil: Focusing on DOM and microbial communities
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Effects of biochar on methane emission from paddy soil: Focusing on DOM and microbial communities

机译:生物炭对水稻土甲烷排放的影响:专注于DOM和微生物社区

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摘要

Biochar can be used as a soil amendment. However, it generally possesses unique physicochemical properties and complex organics, which could affect soil methanogenesis. In this study, straw-based biochars obtained at 300 °C (BC300), 500 °C (BC500) and 700 °C (BC700) were added to the paddy soil. Compared with the blank group, BC300 significantly increased paddy soil methane emissions by about 38%. However, this promoting effect gradually disappeared with the increase of pyrolysis temperature, and the inhibition even appeared in the BC700 group with the methane reduction by 18.2%. This might be related to the organics released from biochar. Van Krevelen (VK) diagram showed that the aromaticity of BC700 and BC500 were significantly higher than BC300. Fluorescent analysis further revealed that BC300 increased the amount of degradable fluorescent organics in the soil, which could provide more substrate for methane production. Moreover, as pyrolysis temperature increased, the fluorescent organics released were more likely to be non-biodegradable humus. In addition, it was shown that BC700 could adsorb some inherent organics in the soil, and thus reduced the total organic content and inhibited soil methane emissions. Microbial analysis showed that methanogenesis had a positive correlation with the abundance of syntrophic bacteria (e.g. Desulfobacca and Clostridium) which had ability to further degrade various types of organics and provided substrates to the methanogens. This article provides a deeper understanding regarding for the effects of biochar on methane emission from paddy soil in terms of organics and microbial perspectives.
机译:生物炭可以用作土壤修正案。然而,它通常具有独特的物理化学性质和复杂的有机物,这可能影响土壤甲烷化。在该研究中,在300℃(BC300),500℃(BC500)和700℃(BC700)中获得的基于秸秆的生物谱系被添加到水稻土中。与空白组相比,BC300显着提高了水稻土壤甲烷排放量约为38%。然而,这种促进效果随着热解温的增加而逐渐消失,并且抑制甚至在BC700组中出现,甲烷降低18.2%。这可能与生物炭释放的有机物有关。 Van Krevelen(VK)图显示BC700和BC500的芳香性显着高于BC300。荧光分析进一步揭示了BC300增加了土壤中可降解的荧光有机物量,这可以为甲烷生产提供更多的基材。此外,随着热解温增加,释放的荧光有机物更可能是不可生物降解的腐殖质。此外,显示BC700可以吸收土壤中的一些固有物质,从而降低了总有机含量并抑制了土壤甲烷排放。微生物分析表明,甲烷发生与具有进一步降解各种类型的有机物并向甲烷基因提供的能力的能力进一步降解各种类型的阳性相关性(例如Desulfobacca和Clostridium)。本文对生物炭对有机物和微生物观点来说,对生物炭对水稻土甲烷排放的影响提供了更深入的了解。

著录项

  • 来源
    《The Science of the Total Environment 》 |2020年第15期| 140725.1-140725.9| 共9页
  • 作者单位

    Textile Pollution Controlling Engineering Center of Ministry of Environmental Protection College of Environmental Science and Engineering Donghua University Shanghai 201620 China;

    Textile Pollution Controlling Engineering Center of Ministry of Environmental Protection College of Environmental Science and Engineering Donghua University Shanghai 201620 China;

    Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3) Department of Environmental Science and Engineering Fudan University Shanghai 200433 China;

    Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3) Department of Environmental Science and Engineering Fudan University Shanghai 200433 China;

    Textile Pollution Controlling Engineering Center of Ministry of Environmental Protection College of Environmental Science and Engineering Donghua University Shanghai 201620 China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Straw biochar; Methanogens; Microbial communities;

    机译:稻草生物炭;甲烷;微生物群落;

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