Interdisciplinary Research Centre for Agriculture Green Development in Yangtze River Basin, Department of Environmental Sciences and Engineering, College of Resources and Environment, Southwest University, Chongqing 400716, China.
State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China.
J Environ Sci (China). 2022 Sep;119:68-77. doi: 10.1016/j.jes.2022.02.011. Epub 2022 Feb 19.
Biochar has been used increasingly as a soil additive to control mercury (Hg) pollution in paddy rice fields. As the most active component of soil organic matter, soil dissolved organic matter (DOM) plays a vital role in the environmental fate of contaminants. However, there are very few studies to determine the impact of biochar on the Hg cycle in rice paddies using insights from DOM. This study used original and modified biochar to investigate their effect on DOM dynamics and their potential impact on methylmercury (MeHg) production and bioaccumulation in rice plants. Porewater DOM was collected to analyze the variations in soil-derived DOM in paddy soils. The results showed that the addition of biochar, whether in original or modified form, significantly reduced the bioaccumulation of MeHg in rice plants, especially in hulls and grains (p<0.05). However, MeHg production in soils was only inhibited by the modified biochar. Biochar addition induced a significant increase in DOM's aromaticity and molecular weight (p<0.05), which decreased Hg bioavailability. Furthermore, enhanced microbial activity was also observed in DOM (p<0.05), further increasing MeHg production in the soil. Thus, the effect of biochar on the fate of Hg cycle involves competition between the two different roles of DOM. This study identified a specific mechanism by which biochar affects Hg behavior in rice paddy soil and contributes to understanding the more general influence of biochar in agriculture and contaminant remediation.
生物炭作为一种土壤添加剂,已被越来越多地用于控制稻田中汞(Hg)污染。作为土壤有机质中最活跃的成分,土壤溶解有机质(DOM)在污染物的环境归宿中起着至关重要的作用。然而,利用 DOM 的见解来确定生物炭对稻田汞循环的影响的研究却很少。本研究使用原始和改性生物炭来研究它们对 DOM 动力学的影响及其对水稻植株中甲基汞(MeHg)生成和生物累积的潜在影响。采集了孔隙水 DOM,以分析稻田土壤中土壤衍生 DOM 的变化。结果表明,添加生物炭,无论是原始形式还是改性形式,都能显著降低水稻植株对 MeHg 的生物累积,特别是在壳和谷粒中(p<0.05)。然而,只有改性生物炭抑制了土壤中 MeHg 的生成。生物炭的添加会导致 DOM 的芳香度和分子量显著增加(p<0.05),从而降低 Hg 的生物利用度。此外,还观察到 DOM 中的微生物活性增强(p<0.05),进一步增加了土壤中 MeHg 的生成。因此,生物炭对 Hg 循环命运的影响涉及 DOM 的两个不同作用之间的竞争。本研究确定了生物炭影响水稻土中 Hg 行为的特定机制,有助于理解生物炭在农业和污染物修复中的更普遍影响。