1. Source, distribution, and geochemical processes of geogenic high chromium groundwater around the world: A critical review.
- Author
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Guo, Huaming, Liu, Chao, Yan, Song, Yin, Jiahong, and Shan, Jun
- Subjects
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GROUNDWATER , *ULTRABASIC rocks , *HEXAVALENT chromium , *BEDROCK , *CHROMIUM - Abstract
[Display omitted] • High Cr groundwater widely occurred in the world, with Cr(VI) as the major species. • Oxidation of Cr(III) and Cr(VI) desorption resulted in groundwater Cr enrichment. • Oxidation of dissolved Cr(III) by Mn oxides led to Cr(VI) formation in bedrock aquifers. • Oxidation of adsorbed Cr(III) and direct oxidation of Cr(III) occurred in sediment aquifers. • Relative contribution of the two oxidations in the sediment aquifers are still open. Due to the high toxicity of hexavalent chromium (Cr), dissolved Cr(VI) in groundwater used for drinking poses serious risk on human health. Here we systematically summarized distribution, hydrogeological settings, and geochemical characteristics of high Cr groundwater, and evaluated Cr source and geochemical processes controlling Cr distribution in typical groundwater throughout the world. High Cr groundwater (Cr > 10 μg/L), generally characterized by high Eh, HCO 3 –, and SO 4 2-, mainly occurred in oxic conditions of bedrock aquifers and sediment aquifers composed of ultramafic rocks and ultramafic rock-sourced sediments, respectively. Chromium(VI) was the predominant Cr species. Groundwater Cr was directly sourced from exchangeable and silicate-bound forms in aquifer solids. In the bedrock aquifers with high dissolved oxygen (DO) and relatively low pH, oxidation of dissolved Cr(III) by Mn oxides during silicate weathering led to the formation of Cr(VI). In the sedimentary aquifers, both oxidation of adsorbed Cr(III) by newly formed Mn oxides and direct oxidation of Cr(III) by DO during silicate weathering due to the presence of dissolved Mn and DO and the long residence time contributed to Cr(VI) generation. The low flow rates promoted Cr(VI) enrichment in groundwater from those aquifers. However, we highlight that the relative contribution of those two reactions to Cr(III) oxidation in the sedimentary aquifers and the effect of groundwater age on Cr concentration in different hydrogeological settings are still open and need to be evaluated, which help in better understanding mechanisms of Cr enrichment in groundwater. [ABSTRACT FROM AUTHOR]
- Published
- 2024
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