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废弃矿山场地中金属元素(Cu、Zn、As(V)、Cd 和 Pb)渗流潜能的土壤阻滞:批量平衡吸附和渗流柱研究。

Soil attenuation of the seepage potential of metallic elements (Cu, Zn, As(V), Cd, and Pb) at abandoned mine sites: A batch equilibrium sorption and seepage column study.

机构信息

Department of Environmental Science and Ecological Engineering, Korea University, Seoul, 02841 South Korea.

Department of Environmental Science and Ecological Engineering, Korea University, Seoul, 02841 South Korea.

出版信息

J Hazard Mater. 2017 Oct 5;339:292-300. doi: 10.1016/j.jhazmat.2017.05.054. Epub 2017 Jun 20.

DOI:10.1016/j.jhazmat.2017.05.054
PMID:28658638
Abstract

Soil attenuation of off-site leaching potential of metallic elements at the two abandoned mine sites was investigated using batch sorption and layered column studies. In batch study, the leachate concentration-specific sorption (K) by downgradient clean soils was in the order of Pb>Cu>Cd>Zn>As for DY site and Pb>As>Cu>Cd>Zn for BS site. In the layered (mine+clean) soil column, element elution was significantly reduced (e.g., no initial flush, retarded peak arrival, and lower peak concentration) while sulfate elution can be an indicator of the dissolution of sulfur-bearing minerals in mine soils. The greatest reduction was observed for Pb and Cu while the lowest was for Cd (2-19%) and Zn (6-51%), consistent with the batch data. Both the reduced elution at slow seepage and concentration drop after flow interruption support the time-limited propensity. In column segments, the sorptive elements (Cu, Pb, and As) were dominantly found in the inlet while less sorptive ones (Zn and Cd) in the outlet. Both batch and column data suggest that the element leaching with mine leachate movement can be greatly attenuated by the interactions with the surrounding downgradient soil during the seepage process.

摘要

采用批量吸附和层状柱状研究,研究了两个废弃矿山场地中金属元素场外浸出潜力的土壤衰减。在批量研究中,下游清洁土壤对浸出液浓度特异性吸附(K)的顺序为:DY 场地为 Pb>Cu>Cd>Zn>As,BS 场地为 Pb>As>Cu>Cd>Zn。在分层(矿山+清洁)土壤柱中,元素洗脱显著减少(例如,没有初始冲洗,峰到达延迟和峰浓度降低),而硫酸盐洗脱可以指示矿山土壤中含硫矿物的溶解。Pb 和 Cu 的减少最大,而 Cd(2-19%)和 Zn(6-51%)的减少最小,与批量数据一致。缓慢渗流中的洗脱减少和流动中断后的浓度下降都支持时间限制倾向。在柱状段中,吸附元素(Cu、Pb 和 As)主要存在于入口处,而吸附性较弱的元素(Zn 和 Cd)则存在于出口处。批量和柱状数据均表明,在渗流过程中,与周围下游土壤的相互作用可大大衰减随矿山浸出液迁移的元素浸出。

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