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.
Textile Pollution Controlling Engineering Center of Ministry of Environmental Protection, College of Environmental Science and Engineering, Donghua University, Shanghai 201620, China.
Sci Total Environ. 2020 Apr 20;714:136769. doi: 10.1016/j.scitotenv.2020.136769. Epub 2020 Jan 17.
Directly returning rice straw to the paddy soil would significantly stimulate methane emission, and hydrochar has potential to be used as soil conditioner. However, the effects of hydrochar on the methane emission from paddy soil and the related mechanisms are still unclear. In the present study, straw-based hydrochar obtained at 200 °C (HC200), 250 °C (HC250) and 300 °C (HC300) and hydrochar after removal of bio-oil at these temperatures (CHC200, CHC250, and CHC300) were prepared and added to the paddy soil. The application of HC200, HC250 and HC300 resulted in the enhanced methane production compared to the control, showing 4.3, 1.6 and 1.5-fold higher methane production, respectively. It was related to the large amount of dissolved organic matter (DOM) released from hydrochar. Excitation-emission matrix fluorescence spectroscopy with parallel factor analysis (EEM-PARAFAC) showed that the hydrochar-derived DOM mainly included humic-like, phenolic and less aromatic structures, and with the increase of hydrothermal temperature, the content of humic-like substances and phenols increased, while biodegradable organics decreased. This was consistent with the maximum methane production by HC200. After incubation, there was no low-aromatic structures observed in the soil leachate, and the residual organics were mainly humus. The EEM-PARAFAC results were supported by compositional characterization of soil leachate by high-resolution mass spectrometry, and the refractory organics released from hydrochar was mainly lignins or (CRAM)-like structures in the range of H/C = 0.8-1.6 and O/C = 0.1-0.5. The organics dissolved from the washed hydrochar was significantly reduced, and some washed hydrochar (CHC250 and CHC300) even inhibited methane emission possibly due to their ability to adsorb organics. Microbial analysis further showed that the increased methane production resulted from hydrochar was associated with the enrichment of Janibacter, Anaeromyxobacter, Anaerolinea and Sporacetigenium. This present study provided a better understanding to the effect of hydrochar on methanogenesis in paddy soil.
直接将稻草还田会显著刺激甲烷排放,而水热炭有潜力用作土壤调理剂。然而,水热炭对稻田甲烷排放的影响及其相关机制仍不清楚。在本研究中,制备了在 200°C(HC200)、250°C(HC250)和 300°C(HC300)下获得的基于稻草的水热炭和在这些温度下去除生物油后的水热炭(CHC200、CHC250 和 CHC300),并将其添加到稻田土壤中。与对照相比,HC200、HC250 和 HC300 的应用导致甲烷产量增加,分别提高了 4.3、1.6 和 1.5 倍。这与水热炭释放的大量溶解有机物质(DOM)有关。平行因子分析(EEM-PARAFAC)的激发-发射矩阵荧光光谱表明,水热炭衍生的 DOM 主要包括腐殖质样、酚类和较少的芳香结构,随着水热温度的升高,腐殖质样物质和酚类物质的含量增加,而可生物降解的有机物减少。这与 HC200 的最大甲烷产量一致。孵育后,土壤浸出液中没有观察到低芳香结构,残留有机物主要是腐殖质。土壤浸出液的高分辨质谱组成特征分析支持 EEM-PARAFAC 结果,水热炭释放的难降解有机物主要为木质素或(CRAM)样结构,范围为 H/C=0.8-1.6 和 O/C=0.1-0.5。从洗涤水热炭中溶解的有机物明显减少,一些洗涤水热炭(CHC250 和 CHC300)甚至可能由于其吸附有机物的能力而抑制甲烷排放。微生物分析进一步表明,水热炭对甲烷生成的增加与 Janibacter、Anaeromyxobacter、Anaerolinea 和 Sporacetigenium 的富集有关。本研究为水热炭对稻田甲烷生成的影响提供了更好的理解。