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首页> 外文期刊>The Science of the Total Environment >Molecular characteristics of sedimentary organic matter in controlling mercury (Hg) and elemental mercury (Hg~0) distribution in tropical estuarine sediments
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Molecular characteristics of sedimentary organic matter in controlling mercury (Hg) and elemental mercury (Hg~0) distribution in tropical estuarine sediments

机译:控制河口沉积物中汞(Hg)和元素汞(Hg〜0)分布的沉积有机物的分子特征

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Sedimentary organic matter (SOM) plays an important role in hosting and reducing Hg-II in marine/estuarine sediment. This study provides a better understanding on the influence of nature of SOM, in regulating sedimentary mercury (Hg) and elemental mercury (Hg-0) distribution, and speciation in the Zuari and Mandovi Estuaries that are representative of monsoon fed tropical estuaries, located in the central west coast of India. Salinity of the overlying water column controlled the physical and chemical characteristics of SOM in the estuarine systems. The high molecular weight (MW) SOM dominated at the mid and upstream (low salinity region) of the estuaries, whereas, the low MW SOM prevailed at the downstream (high salinity region). Sediment Hg showed more affinity towards the SOM of high MW. Increasing MW of SOM increased total sedimentary Hg-T in both the estuaries. SOM with low MW in the estuarine sediment displayed a negative relationship with the sediment Hg concentration. Distribution of Hg(0)concentration in the estuarine sediment suggests that reduction of Hg-II in presence low MW SOM was a dominant process. It was also found that distribution and speciation of Hg(0 )in the estuarine sediment depends on the quantity, quality of the SOM, and the total sediment Hg loading. This study demonstrated that the competition between Hg-SOM complexation and Hg-II reduction by SOM controls Hg-II/Hg-0 distribution in tropical estuarine sediment systems. (C) 2019 Elsevier B.V. All rights reserved.
机译:沉积有机物(SOM)在海洋和河口沉积物中的Hg-II吸收和减少中起着重要作用。这项研究可以更好地了解SOM的性质对调节沉积汞(Hg)和元素汞(Hg-0)的分布以及位于季风喂养的热带河口代表的Zuari和Mandovi河口中的物种形成的影响。印度中西部海岸。上方水柱的盐度控制着河口系统中SOM的物理和化学特性。在河口的中上游(低盐度区),高分子量(SOM)占主导地位,而在下游(高盐度区),低分子量(SOM)占主导地位。沉积物汞对高MW的SOM表现出更大的亲和力。 SOM MW的增加使两个河口的总沉积Hg-T增加。河口沉积物中低分子量的SOM与沉积物中的汞浓度呈负相关。 Hg(0)浓度在河口沉积物中的分布表明,在低MW SOM存在下降低Hg-II是一个主要过程。还发现,河口沉积物中Hg(0)的分布和形态取决于SOM的数量,质量和沉积物中Hg的总量。这项研究表明,SOM对Hg-SOM络合和Hg-II还原的竞争控制着热带河口沉积物系统中Hg-II / Hg-0的分布。 (C)2019 Elsevier B.V.保留所有权利。

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