Faculty of Engineering Department of Environmental Engineering, Dokuz Eylul University, Kaynaklar Campus, 35160, Buca, Izmir, Turkey.
Environ Monit Assess. 2018 Dec 19;191(1):25. doi: 10.1007/s10661-018-7158-5.
The natural soil, processing products, and wastes generated in a colemanite mining site were studied according to their mineral structures, contents of As, Cr, Cu, Ni, Mn, Zn, Al, and Fe. The possible sources, chemical distributions, and the mobilization behaviors of the metals and the correlations between the metal mobilization ratios and their chemical partitioning were also examined and evaluated. The mineralogical composition of the materials was determined, and the correlations between the mineralogical sources of the determined metals with each other were investigated by using principal component analysis. The results showed that mica and smectite were considered to be the source of Cr, Cu, Ni, and Zn, and As was found in the mineral structure of the colemanite. On the other hand, the distributions of the metals in the binding forms indicated that Cr, Ni, Zn, Al, and Fe were mostly bound on the residual fraction, while Cu, Mn, and As were distributed in labile forms. Arsenic was recognized as the most mobile element with 10.37% mobility. Fe mobilization was originated from exchangeable fraction, where As mobilization was significantly correlated with its reducible and organic fractions.
对科尔曼石矿区的天然土壤、加工产品和废物进行了研究,根据其矿物结构、砷、铬、铜、镍、锰、锌、铝和铁的含量进行了研究。还检查和评估了金属的可能来源、化学分布以及金属的迁移行为及其与化学分配的关系。确定了材料的矿物成分,并通过主成分分析研究了所确定金属的矿物来源之间的相关性。结果表明,云母和蒙脱石被认为是 Cr、Cu、Ni 和 Zn 的来源,而砷存在于科尔曼石的矿物结构中。另一方面,金属在结合形式中的分布表明,Cr、Ni、Zn、Al 和 Fe 主要结合在残余部分,而 Cu、Mn 和 As 分布在不稳定形式中。砷被认为是最具迁移性的元素,迁移率为 10.37%。铁的迁移是由可交换部分引起的,砷的迁移与可还原和有机部分显著相关。