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Using stable and radioactive isotopes for the investigation of contaminant metal mobilization in a metal mining district

机译:使用稳定的放射性同位素调查金属矿区中的污染物金属迁移

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Naturally occurring stable and radioactive isotopes were used as environmental tracers to investigate contaminant metal mobilization processes in a metal smelter dump mainly consisting of slag. Water emerging from the dump at a spring is heavily contaminated by metals. The smelter dump contains minor amounts of flue dust, a material which shows a high potential for metal mobilization. Nearby dumps mainly consist of low-grade ore. Concentration patterns of U-238. Ra-226 and Pb-210 determined in sediment deposited close to the contaminated spring reveal the flue dust to be the major local metal source rather than the slag or the low-grade ore. Contamination pathways inside the dump were investigated using hydrological, chemical and isotopic data. Strong negative correlation between water discharge and metal concentration in the spring water suggests, besides short-term dilution of the metal concentration by direct rainwater runoff, distinct long-term dilution of the spring water by groundwater being discharged at a significantly increased rate as a result of heavy rains. delta O-18 and delta D signatures of rain, local groundwater and spring water confirm the importance of groundwater derived from the local aquifer. Another hydrological component with importance for metal mobilization was found to be water that is recharged in the dump itself. Tritium analysis allowed an assessment of the probable residence time of that water component in the smelter dump. Since that water component seems to represent a major local contamination pathway the findings of the study are of substantial importance for site remediation planning. As a primary result it could be stated that covering the dump would not result in any noteworthy short-term improvement of the spring water quality. First significant effects would only be visible after 2-3 decades at the earliest. (c) 2008 Elsevier Ltd. All rights reserved.
机译:天然存在的稳定同位素和放射性同位素被用作环境示踪剂,以研究主要由矿渣组成的金属冶炼厂废料中的污染物金属迁移过程。春季从垃圾场流出的水被金属严重污染。冶炼厂的废料场含有少量的烟道粉尘,这种材料显示出很高的金属动员潜力。附近的垃圾场主要由低品位矿石组成。 U-238的浓度模式。在靠近受污染的春季沉积物中测定的Ra-226和Pb-210表明,烟道粉尘是主要的本地金属来源,而不是矿渣或低品位矿石。使用水文,化学和同位素数据调查了垃圾场内部的污染途径。废水排放与泉水中金属浓度之间的强烈负相关性表明,除了直接雨水径流对金属浓度的短期稀释以外,地下水排放对泉水的明显长期稀释也因此以显着增加的速率发生。大雨。雨水,当地地下水和泉水的三角洲O-18和三角洲D标志证实了从当地含水层中提取的地下水的重要性。发现对金属动员非常重要的另一个水文要素是在垃圾场本身补充的水。 t分析可以评估该水成分在冶炼厂垃圾场中的可能停留时间。由于该水成分似乎代表了主要的局部污染途径,因此该研究的结果对于场地修复计划具有至关重要的意义。可以得出的主要结果是,对垃圾场进行覆盖不会在短期内显着改善泉水水质。最早的重大影响最早要到2-3年后才能看到。 (c)2008 Elsevier Ltd.保留所有权利。

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