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Geochemical dispersal of thallium and accompanying metals in sediment profiles from a smelter-impacted area in South China

机译:南方冶炼区沉积物沉积物沉积物铊和伴随金属的地球化学分散

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Thallium is a trace metal with a toxicity greater than that of Pb, Cd and Hg. This study complements the authors' previous research, with main focus on contamination by Tl and accompanying metals (Pb, Zn, Cd, and Cu) in sediments from an area historically affected by Pb-Zn smelting in Shaoguan city (northern Guangdong Province, South China). In order to provide complex data on the geochemistry of anthropogenic Tl in sediments, total contents and geochemical fractionation of Tl and the other metals were comparatively studied for two different sediment profiles, core A from the Pb-Zn smelter outlet (a major Tl pollution point-source) and core B from the inlet of the North River (natural water courses near the smelter). Surprisingly high enrichment of Tl was observed across both depth profiles, with varying distribution patterns versus depth. Further comparison of Tl contents and its geochemical fractions in the upper, middle and bottom horizons of core A and core B, in combination with mineralogical phases of the sediments, clearly demonstrated both lateral and vertical mobility of Tl, due to complex processes such as mechanical disturbance/mixing, long-term alteration/dissolution of smelter-derived particles, and vertical migration of Tl through colloidal (or microparticle) transport with alumino-phyllosilicates and Fe/Mn (hydr) oxides. Relatively high abundance of Tl in the labile fractions of all selected sediments from both locations highlights a potentially significant environmental risk to the local ecological system in the near future. (C) 2017 Published by Elsevier Ltd.
机译:铊是一种痕量金属,毒性大于Pb,Cd和Hg。本研究补充了提交人之前的研究,主要关注TL和伴随的金属(Pb,Zn,Cd和Cd)在历史上受到韶关市PB-ZN冶炼(南部北部)的沉积物中的沉积物中的沉积物(Pb,Zn,Cd和Cd)污染中国)。为了提供关于沉积物中的人为T1地球化学的复杂数据,对于两种不同的沉积物曲线,来自PB-Zn冶炼厂出口的核心A,核心A的总含量和地球化学分馏,来自PB-Zn冶炼厂出口(主要TL污染点 - 来自北河的入口(冶炼厂附近的自然水课程)和核心B.在深度型材上观察到令人惊讶地高的T1富集,不同的分布模式与深度相比。进一步比较T1含量及其地球化学级分在核心A和核心B的上部,中间地平线中,与沉积物的矿物学相结合,显然表现出T1的横向和垂直迁移率,这是由于机械的复杂工艺干扰/混合,冶炼颗粒的长期改变/溶解,以及通过胶体(或微粒)输送与氧化铝(或微粒)和Fe / Mn(氢)氧化物的垂直迁移T1。两个地点的所有选定沉积物的不稳定部分中的相对高的TL丰富的TL凸显了对当地生态系统在不久的将来的潜在重大环境风险。 (c)2017年由elestvier有限公司出版

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