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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Geochemical signatures and processes in a stream contaminated by heavy mineral processing near Ipoh city, Malaysia
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Geochemical signatures and processes in a stream contaminated by heavy mineral processing near Ipoh city, Malaysia

机译:马来西亚伊富努市附近重型矿物加工污染的地球化学签名及流程

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摘要

The environmental impacts of a heavy mineral processing involving rare earth elements (REEs) in the Kinta River and its tributaries near Ipoh city in Malaysia is investigated using geochemical and isotopic signatures and geochemical modeling. Analysis of water, sediment, suspended particulate matter, and rock samples reveals that stream waters close to the heavy mineral processing plant site are anthropogenically influenced, as indicated by slightly low pH (4.98-6.24) and elevated concentrations of Fe (up to 129 mg/L), Cl- (1540 mg/L), total REEs (1580 mu g/L), U (17.2 mu g/L), and Th (0.33 mu g/L). REE patterns and Pb isotope ratios of waters and sediments from a tributary are similar to those of tailings pond seepage and sediments, suggesting that not only these elements but also U and Th are derived from heavy mineral processing. The delta Fe-56 values of water in the tributary decrease downstream, accompanied by a decrease in Fe concentration, which is likely due to isotope fractionation via oxidative precipitation of Fe hydroxides. The concentrations of REEs, U, and Th decrease downstream, accompanied by an increase in pH, with different removal factors (Th > U > REEs). The influence of contamination is confined to within similar to 1.5 km downstream of the source. Tamm's acid oxalate extraction (to dissolve only low crystalline phases) showed that Th and Al concentrations were lower while U and Fe concentrations were higher in downstream suspended particulate samples, suggesting that Th and U may be removed by different mechanisms from stream water. The results of geochemical modeling suggest that Th precipitated as a solid phase, such as an intermediate between ThO2 and Th(OH)(4), with increasing stream water pH. In contrast, U may have been removed by adsorption onto Fe hydroxides, as supported by surface complexation modeling. The geochemical signatures and processes discussed in this study may be applicable for environmental assessment of REE processing. (C) 2017 Elsevier Ltd. All rights reserved.
机译:利用地球化学和同位素签名和地球化学建模,研究了克林塔河及其在马来西亚怡保市附近的稀土元素(REEE)的重型矿物处理的环境影响。水,沉积物,悬浮颗粒物和岩石样品的分析表明,靠近重型矿物加工植物部位的溪流水域是人为影响,如略微低pH(4.98-6.24)和升高的Fe浓度(高达129毫克)所示/ L),Cl-(1540mg / L),总重量(1580 mu g / l),U(17.2μg/ L),Th(0.33μg/ l)。 REE模式和支流的PB同位素比率与支流的水域和沉积物类似于尾矿池塘渗流和沉积物,这表明不仅仅是这些元素,而且源于U和TH源自重型矿物加工。在下游的支流减少的水中的ΔFE-56值伴随着Fe浓度的降低,这可能是由于二氧化碳沉淀的同位素分馏。 Rees,U和Th降低下游的浓度伴随着pH的增加,具有不同的去除因子(Th> U> Rees)。污染的影响被限制在源下游的1.5公里。 TAMM的酸性萃取(仅溶解低结晶相)表明,在下游悬浮的颗粒样品中较低的u和Fe浓度较低时Th和Al浓度较低,表明Th和U可以通过流水的不同机制除去。地球化学建模的结果表明,Th沉淀为固相,例如ThO2和Th(OH)(4)之间的中间体,随着物流水pH增加。相反,U可以通过吸附到Fe氢氧化物上而被除去,如表面络合建模所支持。本研究中讨论的地球化学签名和过程可适用于REE处理的环境评估。 (c)2017 Elsevier Ltd.保留所有权利。

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