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.
Sci Total Environ. 2020 Nov 15;743:140725. doi: 10.1016/j.scitotenv.2020.140725. Epub 2020 Jul 6.
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.
生物炭可用作土壤改良剂。然而,它通常具有独特的物理化学性质和复杂的有机物,这可能会影响土壤产甲烷作用。在这项研究中,将在 300°C(BC300)、500°C(BC500)和 700°C(BC700)下获得的秸秆基生物炭添加到稻田土壤中。与空白组相比,BC300 显著增加了约 38%的稻田甲烷排放。然而,随着热解温度的升高,这种促进作用逐渐消失,甚至在 BC700 组中出现了 18.2%的甲烷减少。这可能与生物炭释放的有机物有关。范·克里夫伦(VK)图显示,BC700 和 BC500 的芳香度明显高于 BC300。荧光分析进一步表明,BC300 增加了土壤中可降解荧光有机物的数量,为甲烷产生提供了更多的底物。此外,随着热解温度的升高,释放的荧光有机物更有可能是不可生物降解的腐殖质。此外,研究表明,BC700 可以吸附土壤中一些固有的有机物,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,产甲烷作用与同型产乙酸菌(如脱硫菌和梭菌)的丰度呈正相关,同型产乙酸菌具有进一步降解各种类型有机物的能力,并为产甲烷菌提供底物。本文从有机物和微生物角度,为生物炭对稻田甲烷排放的影响提供了更深入的认识。