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硝态氮和铵态氮对淹水水稻土中汞的甲基化、去甲基化和还原作用的差异。

The divergent effects of nitrate and ammonium application on mercury methylation, demethylation, and reduction in flooded paddy slurries.

机构信息

College of Chemical Engineering, Huaqiao University, Xiamen 361021, China; State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China.

College of Chemical Engineering, Huaqiao University, Xiamen 361021, China.

出版信息

J Hazard Mater. 2023 Oct 15;460:132457. doi: 10.1016/j.jhazmat.2023.132457. Epub 2023 Sep 1.

Abstract

The production of methylmercury (MeHg) in flooded paddy fields determines its accumulation in rice grains; this, in turn, results in MeHg exposure risks for not only rice-eating humans but also wildlife. Nitrogen (N) fertilizers have been widely applied in rice cultivation fields to supply essential nutrients. However, the effects of N fertilizer addition on mercury (Hg) transformations are not unclear. This limits our understanding of MeHg formation in rice paddy ecosystems. In this study, we spiked three Hg tracers (Hg, MeHg, and Hg) in paddy slurries fertilized with urea, ammonium, and nitrate. The influences of N fertilization on Hg methylation, demethylation, and reduction and the underlying mechanisms were elucidated. The results revealed that dissimilatory nitrate reduction was the dominant process in the incubated paddy slurries. Nitrate addition inhibited Hg reduction, Hg methylation, and MeHg demethylation. Competition between nitrates and other electron acceptors (e.g., Hg, sulfate, or carbon dioxide) under dark conditions was the mechanism underlying nitrate-regulated Hg transformation. Ammonium and urea additions promoted Hg reduction, and anaerobic ammonium oxidation coupled with Hg reduction (Hgammox) was likely the reason. This work highlighted that nitrate addition not only inhibited Hg methylation but also reduced the demethylation of MeHg and therefore may generate more accumulation of MeHg in the incubated paddy slurries. Findings from this study link the biogeochemical cycling of N and Hg and provide crucial knowledge for assessing Hg risks in intermittently flooded wetland ecosystems.

摘要

在淹水的稻田中,甲基汞(MeHg)的生成决定了其在稻米中的积累,这反过来又使食用稻米的人类和野生动物面临 MeHg 暴露的风险。氮肥已广泛应用于稻田,以提供必需的营养。然而,氮肥料的添加对汞(Hg)转化的影响尚不清楚。这限制了我们对水稻田生态系统中 MeHg 形成的理解。在这项研究中,我们在添加尿素、铵和硝酸盐的稻田泥浆中添加了三种 Hg 示踪剂(Hg、MeHg 和 Hg)。阐明了 N 施肥对 Hg 甲基化、去甲基化和还原的影响及其潜在机制。结果表明,异化硝酸盐还原是培养的稻田泥浆中的主要过程。硝酸盐的添加抑制了 Hg 的还原、甲基化和 MeHg 的去甲基化。黑暗条件下硝酸盐与其他电子受体(如 Hg、硫酸盐或二氧化碳)之间的竞争是硝酸盐调控 Hg 转化的机制。铵和尿素的添加促进了 Hg 的还原,而与 Hg 还原偶联的厌氧铵氧化(Hgammox)可能是原因。这项工作强调了硝酸盐的添加不仅抑制了 Hg 的甲基化,而且降低了 MeHg 的去甲基化,因此可能会导致培养的稻田泥浆中 MeHg 的积累增加。本研究将氮和汞的生物地球化学循环联系起来,为评估间歇性淹水湿地生态系统中的 Hg 风险提供了重要知识。

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