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尼日利亚西南部一座废弃金矿的尾矿和岩芯样本中的重金属污染。

Heavy metal contamination in tailings and rocksamples from an abandoned goldminein Southwestern Nigeria.

机构信息

Department of Environmental Management and Toxicology, Federal University of Agriculture, Abeokuta, Abeokuta, Ogun State, Nigeria.

出版信息

Environ Monit Assess. 2014 Jan;186(1):165-74. doi: 10.1007/s10661-013-3363-4. Epub 2013 Aug 16.

DOI:10.1007/s10661-013-3363-4
PMID:23949700
Abstract

Active and abandoned primary and secondary goldmines have been observed to be major sources of metals into the environment. This study assessed the level of metal concentrations in rock and tailing samples collected from the abandoned primary goldmine site at Iperindo. A total of five rock and ten tailing samples were collected for this study. The tailing samples were subjected to physicochemical analysis using standard methods. The samples were analyzed for metals using inductively coupled plasma/optical emission spectrometry technique. The results obtained indicated that tailings were acidic (pH 5.02), with electrical conductivity 133.4 μS/cm, cation exchange capacity 8.95 meq/100 g, available phosphorus was 4.74 mg/L, organic carbon 5.58 %, and organic matter 9.63 %. The trends for metal concentrations within the samples were in the order: Zn > Cu > Co > Pb > Cr > As > Cd for rock samples, Cu > Zn > Cr > Pb > As > Co > Cd in tailing samples. Cd, Pb, and Zn in the rock were above the Abundance of Elements in Average Crustal Rocks standards. Principal component analysis showed higher variations among samples in Iperindo. Cd, Pb, Cr, Co, Cu, As, and Zn were strongly loaded to principal component 1, with these metals significantly contributing to variations in 65.76 % of rock and 53.24 % of tailing. This study suggests that the metal concentration in tailings is a reflection of the metal composition of the rocks.

摘要

已观察到活跃和废弃的主要和次要金矿是金属进入环境的主要来源。本研究评估了从 Iperindo 废弃的主要金矿现场采集的岩石和尾矿样本中金属的浓度水平。本研究共采集了五块岩石和十份尾矿样本。对尾矿样品进行了标准方法的物理化学分析。使用电感耦合等离子体/发射光谱技术对样品进行了金属分析。所得结果表明,尾矿呈酸性(pH 5.02),电导率为 133.4 μS/cm,阳离子交换量为 8.95 meq/100 g,有效磷为 4.74 mg/L,有机碳为 5.58%,有机物质为 9.63%。样品中金属浓度的趋势为:岩石样品中 Zn > Cu > Co > Pb > Cr > As > Cd,尾矿样品中 Cu > Zn > Cr > Pb > As > Co > Cd。岩石中的 Cd、Pb 和 Zn 均高于平均地壳岩石中元素的丰度标准。主成分分析显示 Iperindo 样品之间的变化较大。Cd、Pb、Cr、Co、Cu、As 和 Zn 强烈加载到主成分 1 中,这些金属对岩石的 65.76%和尾矿的 53.24%的变化有显著贡献。本研究表明,尾矿中的金属浓度反映了岩石的金属组成。

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