Abiotic Reduction of Mercury(II) in the Presence of Sulfidic Mineral Suspensions
Abiotic Reduction of Mercury(II) in the Presence of Sulfidic Mineral Suspensions
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DOI:
10.3389/fenvc.2021.660058
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发表时间:
2021-06-14
影响因子:
--
通讯作者:
Mason, Robert P.
中科院分区:
文献类型:
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作者:
Coulibaly, Mariame;Mazrui, Nashaat M.;Mason, Robert P.
Monomethylmercury (CH3Hg) is a neurotoxic pollutant that biomagnifies in aquatic food webs. In sediments, the production of CH3Hg depends on the bacterial activity of mercury (Hg) methylating bacteria and the amount of bioavailable inorganic divalent mercury (Hg-II). Biotic and abiotic reduction of Hg-II to elemental mercury (Hg-0) may limit the pool of Hg-II available for methylation in sediments, and thus the amount of CH3Hg produced. Knowledge about the transformation of Hg-II is therefore primordial to the understanding of the production of toxic and bioaccumulative CH3Hg. Here, we examined the reduction of Hg-II by sulfidic minerals (FeS(s) and CdS(s)) in the presence of dissolved iron and dissolved organic matter (DOM) using low, environmentally relevant concentrations of Hg and ratio of Hg-II:FeS(s). Our results show that the reduction of Hg-II by Mackinawite (FeS(s)) was lower (