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Understanding the relation of As and Mn biogeochemistry within Fe-rich sediments in southeast Asian aquifers

机译:了解东南亚含水层Fe富含Fe富含Fe沉积物中的和Mn生物地球化学的关系

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Aquifer sediments were collected from varying depths from selected villages in Murshidabad, India. Hydrological and physico-chemical parameters of groundwater were measured and aquifer cores were collected. Solid phase analysis includes X-Ray Diffraction (XRD), X-ray Absorption Spectroscopy (XAS) and x-ray imaging. Primary focus of this work was to understand the inter-relation of As and Mn biogeochemistry in presence of Fe-rich minerals. Mechanism of As and Mn release is controlled by the oxidation-reduction of Fe bearing minerals in these subsurface aquifers. With our spectroscopy data, we have observed reduced As and Mn species in aquifer sediment as the depth increased relating directly to elevated concentration of As and Mn observed in groundwater. These observations are vital in understanding the inter-depending behavior of As and Mn in subsurface sediments.
机译:从印度Murshidabad的选定村庄的不同深度收集含水层沉积物。测量地下水的水文和物理化学参数,收集含水层核心。固相分析包括X射线衍射(XRD),X射线吸收光谱(XAs)和X射线成像。这项工作的主要重点是了解在Fe富含Fe矿物质中的AS和Mn生物地球化学的关系。作为和Mn释放的机制由这些地下含水层中的Fe轴承矿物的氧化还原控制。利用我们的光谱数据,我们已经观察到含水层沉积物中的含量和Mn种类,因为深度增加直接与地下水中观察到的升高的浓度和MN升高。这些观察结果对于理解地下沉积物中的互补性行为至关重要。

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