Instituto Politécnico de Castelo Branco and CERENA/FEUP Centre, Portugal.
Department of Geology, University of Trás-os-Montes e Alto Douro and CEMUC Centre, Portugal.
Ecotoxicol Environ Saf. 2016 Nov;133:135-45. doi: 10.1016/j.ecoenv.2016.06.045. Epub 2016 Jul 20.
The mining complex of Murçós belongs to the Terras de Cavaleiros Geopark, located in Trás-os-Montes region, northeast Portugal. A stockwork of NW-SE-trending W>Sn quartz veins intruded Silurian metamorphic rocks and a Variscan biotite granite. The mineralized veins contain mainly quartz, cassiterite, wolframite, scheelite, arsenopyrite, pyrite, sphalerite, chalcopyrite, galena, rare pyrrhotite, stannite, native bismuth and also later bismuthinite, matildite, joseite, roosveltite, anglesite, scorodite, zavaritskite and covellite. The exploitation produced 335t of a concentrate with 70% of W and 150t of another concentrate with 70% of Sn between 1948 and 1976. The exploitation took place mainly in four open pit mines as well as underground. Three lakes were left in the area. Remediation processes of confination and control of tailings and rejected materials and phytoremediation with macrophytes from three lakes were carried out between 2005 and 2007. Stream sediments, soils and water samples were collected in 2008 and 2009, after the remediation process. Most stream sediments showed deficiency or minimum enrichment for metals. The sequential enrichment factor in stream sediments W>Bi>As>U>Cd>Sn=Ag>Cu>Sb>Pb>Be>Zn is mainly associated with the W>Sn mineralizations. Stream sediments receiving drainage of a mine dump were found to be significantly to extremely enriched with W, while stream sediments and soils were found to be contaminated with As. Two soil samples collected around mine dumps and an open pit lake were also found to be contaminated with U. The waters from the Murçós W>Sn mine area were acidic to neutral. After the remediation, the surface waters were contaminated with F(-), Al, As, Mn and Ni and must not be used for human consumption, while open pit lake waters must also not be used for agriculture because of contamination with F(-), Al, Mn and Ni. In most waters, the As occurred as As (III), which is toxic and is easily mobilized in the drainage system. The remediation promoted a decrease in metals and As concentrations of soils and waters, however the applied processes were not enough to rehabilitate the area.
摩尔科斯矿区属于葡萄牙东北部特拉斯-奥斯-蒙蒂斯地区的卡斯凯什大地质公园。NW-SE 走向的锡石石英脉侵入了志留纪变质岩和华力西期黑云母花岗岩。矿化脉主要含有石英、锡石、黑钨矿、白钨矿、毒砂、黄铁矿、闪锌矿、黄铜矿、方铅矿、硫锑铅矿、辉铋矿、黝铜矿、辉碲铋矿、自然铋,以及后来的辉铋矿、硅镁镍矿、硒锌矿、银铅矿、硫砷银矿和铜蓝。1948 年至 1976 年期间,该矿区开采了 335 吨含 70%钨的精矿和 150 吨含 70%锡的精矿。开采主要在四个露天矿和地下进行。矿区留下了三个湖泊。2005 年至 2007 年间,对三个湖泊的尾矿和废弃物料的限制和控制以及利用大型水生植物进行的植物修复进行了修复。2008 年和 2009 年,在修复过程之后,收集了溪流沉积物、土壤和水样。大多数溪流沉积物显示出对金属的缺乏或最小富集。溪流沉积物中锡>铋>砷>铀>镉>锡=银>铜>锑>铅>铍>锌的顺序富集因子主要与 W>Sn 矿化有关。接收矿山废料排水的溪流沉积物被发现明显到极度富集 W,而溪流沉积物和土壤被发现受到砷的污染。在矿山废料堆和一个露天矿湖周围采集的两个土壤样本也被发现受到铀的污染。摩尔科斯 W>Sn 矿区的水呈酸性至中性。修复后,地表水受到 F(-)、Al、As、Mn 和 Ni 的污染,不得用于人类消费,而露天矿湖的水也因受到 F(-)、Al、Mn 和 Ni 的污染而不得用于农业。在大多数水中,砷以 As(III)的形式存在,As(III)具有毒性,在排水系统中很容易迁移。修复促进了土壤和水中金属和砷浓度的降低,但所采用的过程不足以恢复该地区。