Wang Yongjie, Dang Fei, Zhong Huan, Wei Zhongbo, Li Ping
State Key Laboratory of Pollution Control and Resources Reuse, School of the Environment, Nanjing University, Nanjing, 210023, People's Republic of China.
Key Laboratory of Soil Environment and Pollution Remediation, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, 210008, People's Republic of China.
Environ Sci Pollut Res Int. 2016 Mar;23(5):4602-8. doi: 10.1007/s11356-015-5696-8. Epub 2015 Oct 31.
Biogeochemical cycling of sulfur and selenium (Se) could play an important role in methylmercury (MeHg) dynamics in soil, while their potential effects on MeHg production in rice paddy soil are less understood. The main objective of this study was to explore the effects of sulfate and selenite on net MeHg production in contaminated rice paddy soil, characterized with massive MeHg production and thus MeHg accumulation in rice. A series of microcosm incubation experiments were conducted using a contaminated paddy soil amended with sulfate and/or selenite, in which sulfate-reducing bacteria were mainly responsible for MeHg production. Our results demonstrated that sulfate addition reduced solid and dissolved MeHg levels in soils by ≤18 and ≤25 %, respectively. Compared to sulfate, selenite was more effective in inhibiting net MeHg production, and the inhibitory effect depended largely on amended selenite doses. Moreover, sulfate input played a dual role in affecting Hg-Se interactions in soil, which could be explained by the dynamics of sulfate under anoxic conditions. Therefore, the effects of sulfate and selenium input should be carefully considered when assessing risk of Hg in anoxic environments (e.g., rice paddy field and wetland).
硫和硒(Se)的生物地球化学循环可能在土壤甲基汞(MeHg)动态中发挥重要作用,然而它们对稻田土壤中甲基汞产生的潜在影响却鲜为人知。本研究的主要目的是探究硫酸盐和亚硒酸盐对受污染稻田土壤中甲基汞净产量的影响,该稻田土壤具有大量甲基汞产生以及由此导致的水稻中甲基汞积累的特征。使用添加了硫酸盐和/或亚硒酸盐的受污染稻田土壤进行了一系列微观培养实验,其中硫酸盐还原菌是甲基汞产生的主要原因。我们的结果表明,添加硫酸盐分别使土壤中固态和溶解态甲基汞水平降低了≤18%和≤25%。与硫酸盐相比,亚硒酸盐在抑制甲基汞净产量方面更有效,且抑制效果在很大程度上取决于添加的亚硒酸盐剂量。此外,硫酸盐输入在影响土壤中汞 - 硒相互作用方面具有双重作用,这可以通过缺氧条件下硫酸盐的动态变化来解释。因此,在评估缺氧环境(如稻田和湿地)中汞的风险时,应仔细考虑硫酸盐和硒输入的影响。