Candeias Carla, Ávila Paula F, Ferreira da Silva Eduardo, Teixeira João Paulo
GeoBioTec-Geobiosciences, Geotechnologies e Geoengineering Research Center, Geosciences Department, University of Aveiro, Campus de Santiago, 3810-193, Aveiro, Portugal,
Environ Monit Assess. 2015 Mar;187(3):135. doi: 10.1007/s10661-015-4343-7. Epub 2015 Feb 22.
Through the years, mining and beneficiation processes in Panasqueira Sn-W mine (Central Portugal) produced large amounts of As-rich mine wastes laid up in huge tailings and open-air impoundments (Barroca Grande and Rio tailings) that are the main source of pollution in the surrounding area once they are exposed to the weathering conditions leading to the formation of acid mine drainage (AMD) and consequently to the contamination of the surrounding environments, particularly soils. The active mine started the exploration during the nineteenth century. This study aims to look at the extension of the soil pollution due to mining activities and tailing erosion by combining data on the degree of soil contamination that allows a better understanding of the dynamics inherent to leaching, transport, and accumulation of some potential toxic elements in soil and their environmental relevance. Soil samples were collected in the surrounding soils of the mine, were digested in aqua regia, and were analyzed for 36 elements by inductively coupled plasma mass spectrometry (ICP-MS). Selected results are that (a) an association of elements like Ag, As, Bi, Cd, Cu, W, and Zn strongly correlated and controlled by the local sulfide mineralization geochemical signature was revealed; (b) the global area discloses significant concentrations of As, Bi, Cd, and W linked to the exchangeable and acid-soluble bearing phases; and (c) wind promotes the mechanical dispersion of the rejected materials, from the milled waste rocks and the mineral processing plant, with subsequent deposition on soils and waters. Arsenic- and sulfide-related heavy metals (such as Cu and Cd) are associated to the fine materials that are transported in suspension by surface waters or associated to the acidic waters, draining these sites and contaminating the local soils. Part of this fraction, especially for As, Cd, and Cu, is temporally retained in solid phases by precipitation of soluble secondary minerals (through the precipitation of hydrated metal sulfates) in warm, dry periods, but such minerals are easily dissolved during rainy periods. Climate is an important instability factor, and the hot and dry summers and cold, rainy, and windy winters in this region are physical phenomena that enhance the good receptivity of these soils to retain some of the metals present in the primary and also the secondary mineralogy. Considering the obtained results from both the sequential chemical extraction and the environmental risk assessment according to the risk assessment code, Ag, Cd, Cu, and Zn are classified with very high risk while As is classified with medium risk.
多年来,葡萄牙中部的帕纳谢拉锡钨矿的采矿和选矿过程产生了大量富含砷的矿山废料,这些废料堆积在巨大的尾矿库和露天蓄水池(巴罗卡格兰德尾矿库和里奥尾矿库)中,一旦暴露在风化条件下,就会成为周边地区的主要污染源,导致酸性矿山排水(AMD)的形成,进而污染周边环境,尤其是土壤。这座活跃的矿山于19世纪开始勘探。本研究旨在通过结合土壤污染程度数据,研究采矿活动和尾矿侵蚀造成的土壤污染范围,以便更好地理解土壤中一些潜在有毒元素的淋溶、迁移和积累的内在动态及其环境相关性。在矿山周边土壤采集土壤样本,用王水消解,并用电感耦合等离子体质谱仪(ICP-MS)分析了36种元素。选定的结果是:(a)揭示了银、砷、铋、镉、铜、钨和锌等元素的组合具有很强的相关性,并受当地硫化物矿化地球化学特征的控制;(b)整个区域显示出与可交换和酸溶性赋存相相关的高浓度砷、铋、镉和钨;(c)风促进了废弃物料的机械扩散,这些物料来自磨碎的废石和选矿厂,随后沉积在土壤和水体上。与砷和硫化物相关的重金属(如铜和镉)与细颗粒物质有关,这些细颗粒物质通过地表水以悬浮状态运输,或与酸性水有关,这些酸性水从这些场地排出并污染当地土壤。这部分物质,特别是砷、镉和铜,在温暖干燥时期通过可溶性次生矿物(通过水合金属硫酸盐的沉淀)沉淀而暂时保留在固相中,但这些矿物在雨季很容易溶解。气候是一个重要的不稳定因素,该地区炎热干燥的夏季和寒冷、多雨、多风的冬季是增强这些土壤对原生和次生矿物学中存在的一些金属良好吸附性的物理现象。根据风险评估代码,综合顺序化学提取和环境风险评估的结果,银、镉、铜和锌被归类为极高风险,而砷被归类为中等风险。