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津巴布韦马佐韦大坝痕量金属形态趋势分析,该大坝为典型的亚热带水坝生态系统,受到金矿开采和农业活动的影响。

Trace metal speciation trends in Mazowe dam, Zimbabwe, a typical sub-tropical dam ecosystem impacted by gold mining and agriculture.

机构信息

Department of Chemistry and Earth Sciences, University of Zimbabwe, Harare, Zimbabwe.

Tegwani Farm, Jumbo Road, Mazowe, Zimbabwe.

出版信息

Environ Geochem Health. 2024 Jul 29;46(9):348. doi: 10.1007/s10653-024-02117-w.

Abstract

The present study aimed to assess trace metal speciation trends in the water and sediments of Mazowe Dam, a typical sub-tropical dam ecosystem impacted by gold mining and agriculture in Zimbabwe. The elements studied include Al, As, Cd, Co, Cr, Cu, Hg, Fe, Mn, Ni, Pb, and Zn. Elemental speciation in the water column was determined using Visual MINTEQ version 3.1 geochemical computer modelling, while speciation in the sediment phase was determined using sequential extraction techniques. For each element, the data obtained were subjected to extensive correlation analysis to identify intra- and inter-metal species interactions in the water column and the sediment phase, as well as across the water-sediment interface. Possible mechanisms to account for the observed species interactions are proposed. In the water column, Co was predicted to have the highest number of chemical species (9), Cd and Zn (8), Mn and Fe (7), Ni (6), Pb (5), Al and Cu (3), Cr, Hg, and As have the least (2). In the sediment, Al, As, Co, Cr, Cu, Fe, Ni and Fe mainly exist in the residual fraction, while Zn and Mn concentrations in fractions vary per sampling site, with no fraction that is dominant across the sampling sites. Equilibrium exchange reactions across the water-sediment interface were observed e.g., for Cd species /FACd (aq) and Co species /FACoG (aq), and /FACo (aq). This study is valuable in highlighting trace metal speciation in a tropical dam ecosystem in Africa and adds to the growing knowledge about the behaviour of trace metals in aquatic ecosystems in the region and globally.

摘要

本研究旨在评估津巴布韦马佐韦大坝受金矿开采和农业影响的典型亚热带大坝生态系统中的痕量金属形态趋势。研究的元素包括 Al、As、Cd、Co、Cr、Cu、Hg、Fe、Mn、Ni、Pb 和 Zn。使用 Visual MINTEQ 版本 3.1 地球化学计算机建模来确定水柱中的元素形态,而使用连续提取技术来确定沉积物相中的形态。对于每个元素,获得的数据都经过广泛的相关分析,以确定水柱和沉积物相中以及水-沉积物界面上的金属内和金属间物种相互作用。提出了可能的机制来解释观察到的物种相互作用。在水柱中,预测 Co 将具有最高数量的化学物质(9 种),Cd 和 Zn(8 种),Mn 和 Fe(7 种),Ni(6 种),Pb(5 种),Al 和 Cu(3 种),Cr、Hg 和 As(2 种)最少。在沉积物中,Al、As、Co、Cr、Cu、Fe、Ni 和 Fe 主要以残余形式存在,而 Zn 和 Mn 浓度在各采样点的分数中变化,没有一个分数在整个采样点中占主导地位。观察到水-沉积物界面上的平衡交换反应,例如 Cd 物种/FACd(aq)和 Co 物种/FACoG(aq),以及/FACo(aq)。这项研究对于突出非洲热带大坝生态系统中的痕量金属形态具有重要价值,并增加了有关该地区和全球水生生态系统中痕量金属行为的不断增长的知识。

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