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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Mineralogical and geochemical characterization of a chromium contamination in an aquifer - A combined analytical and modeling approach
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Mineralogical and geochemical characterization of a chromium contamination in an aquifer - A combined analytical and modeling approach

机译:含水层中铬污染的矿物学和地球化学表征 - 一种分析与建模方法

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摘要

This study presents a detailed mineralogical and chemical characterization of a chromium contamination in alluvial deposits underlying a leather tannery in Austria. Drill cores revealed that the contamination is represented by a black layer that exhibits sharp boundaries with adjacent brown alluvial sediments. This black layer is located below the groundwater table and begins at the source of the contamination. The black layer thickens with increasing distance from the source and the depth of the upper boundary remains at the same level relative to the surface. Mineralogical and chemical investigations showed that the black layer contains reduced Cr phases, a Cr(III) hydroxide and a Cr(III)-Ca-containing hydrocalcite, which are present as discrete grains, in vein-like pore spaces and/or as a coating around mineral grains. Cr(VI) is nearly only present above the groundwater table. Our 2-D model predicts a longitudinal spread of the black layer of approximately 37 m downgradient from the source and a maximum transversal spread of approximately 10 m. This study shows that, if the source of the contamination is not eliminated, the plume will increase continuously farther downgradient.
机译:本研究介绍了奥地利皮革制革厂底层沉积物中铬污染的详细矿物学和化学特征。钻孔透露,污染物由黑色层表示,黑层与相邻的棕色冲积沉积物表现出尖锐的边界。该黑色层位于地下水位下方,并在污染源开始。黑层随着距离源的增加而变厚,并且上边界的深度保持在相对于表面的相同水平。矿物学和化学研究表明,黑色层含有还原的Cr相,Cr(III)氢氧化物和含Cr(III)-CA的含氢物,其作为离散颗粒在静脉状的孔隙空间和/或作为一个矿物质覆盖。 Cr(vi)几乎仅在地下水位上方存在。我们的二进制模型预测了从源极约37米的黑色层的纵向扩散,最大横向扩散约为10米。本研究表明,如果没有消除污染的来源,羽流将持续增加更远的降级。

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