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电渗析效应作为一种控制稻田土壤镉再迁移的新机制。

The Voltaic Effect as a Novel Mechanism Controlling the Remobilization of Cadmium in Paddy Soils during Drainage.

机构信息

College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, China.

School of Agriculture and Food Sciences, The University of Queensland, St Lucia, Queensland 4072, Australia.

出版信息

Environ Sci Technol. 2021 Feb 2;55(3):1750-1758. doi: 10.1021/acs.est.0c06561. Epub 2021 Jan 25.

DOI:10.1021/acs.est.0c06561
PMID:33492945
Abstract

Excessive cadmium (Cd) accumulation in rice grain is a global issue that affects human health. The drainage of paddy soils during the grain filling period leads to the remobilization of Cd in soils, resulting in most of the Cd accumulated in rice grain. The rate of Cd remobilization during drainage differs markedly among soils, but the mechanisms underlying these differences remain largely unknown. Using microcosm soil incubation, electrochemical experiments, isotope labeling, and microscopic and spectroscopic analyses, here, we discover the voltaic effect as a novel mechanism controlling the remobilization of Cd during soil drainage. During soil flooding, microbial sulfate reduction results in the formation of various metal sulfides. When the soils are subsequently drained, the various metal sulfides can form within sulfide voltaic cells. The metal sulfides with a lower electrochemical potential act as anodes and are prone to oxidative dissolution, whereas the metal sulfides with a higher potential act as cathodes and are protected from oxidation. This voltaic effect explains why the presence of ZnS (with a low potential) suppresses the oxidative dissolution of Cd sulfides, whereas the presence of CuS (with a high potential) promotes the oxidative dissolution of Cd sulfides. The voltaic effect is applicable to all chalcophile trace metals coupled with the sulfur redox cycle in periodically anoxic-oxic environments, thus playing an important role in the biogeochemistry of trace metals.

摘要

过量的镉(Cd)在稻米中的积累是一个全球性的问题,会影响人类健康。在灌浆期排干稻田土壤会导致土壤中 Cd 的再移动,从而导致大部分 Cd 积累在稻米中。在排水过程中 Cd 再移动的速度在不同土壤中差异显著,但这些差异的机制在很大程度上仍不清楚。通过微宇宙土壤培养、电化学实验、同位素标记以及微观和光谱分析,我们在这里发现了一种新的机制,即伏特效应,它控制着土壤排水过程中 Cd 的再移动。在土壤淹没期间,微生物硫酸盐还原导致各种金属硫化物的形成。当随后排干土壤时,各种金属硫化物可以在硫化物伏特电池内形成。具有较低电化学势的金属硫化物充当阳极,容易发生氧化溶解,而具有较高电势的金属硫化物充当阴极,受到氧化的保护。这种伏特效应解释了为什么 ZnS(具有低电势)的存在会抑制 Cd 硫化物的氧化溶解,而 CuS(具有高电势)的存在会促进 Cd 硫化物的氧化溶解。伏特效应适用于所有与硫氧化还原循环偶联的亲硫痕量金属,在周期性缺氧-好氧环境中,因此在痕量金属的生物地球化学中发挥着重要作用。

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