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首页> 外文期刊>Engineering Geology >Geoenvironmental characterization of unstable abandoned mine tailings combining geophysical and geochemical methods (Cartagena-La Union district, Spain)
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Geoenvironmental characterization of unstable abandoned mine tailings combining geophysical and geochemical methods (Cartagena-La Union district, Spain)

机译:地球物理和地球化学方法(Cartagena-La Union District)的不稳定废弃矿山尾矿地板环境特征

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AbstractThis study presents the results of the geoenvironmental characterization of the Brunita mine pond in the Cartagena-La Unión mining district, Murcia (SE Spain). The main objective was to evaluate the present conditions of the mine tailings in order to identify related environmental hazards. Since 1956, the Brunita mine tailings were being stored in four stepped ponds at the watercourse of a NNO-SSE trending ravine. Subsequently, they were stored in a single, large pond. After the closure of the pond operations, certain work on dike stabilization was performed and debris from the Brunita mine started to accumulate. The mining works for >50years have led to the complete burial of the surrounding valleys and hills by mine waste material. Electrical resistivity tomography (ERT) has allowed the determining of both the general geometry of the pond base and the thickness of the mine tailings. Surveys along a total of 6 ERT profiles, 3 longitudinal and 3 transverse profiles to the largest dimension of the pond were carried out. The strong resistivity contrast between the infilling and the bedrock is high enough to clearly define the bottom pond boundary. Low resistivity values (<10Ω·m) characterize the infilling of the pond, whereas resistivity values>200Ω·m correspond to the Paleozoic rocks that constitute the base of the deposit. Vertical steps have been recognized defining strong variations in the thickness of the deposit. This geometry results from the interaction between the paleotopography of the previous valley and the different growth stages of the deposit. The depth of the pond's base obtained from two boreholes has confirmed the results obtained from ERT profiles. Significant amounts of pyrite and siderite and an appreciable presence of sphalerite and galena were determined by XRD of representative samples. Accordingly, high contents of toxic metals (Cd, Cu, Pb, Sn and Zn) and As were detected in chemical analyses, which show the potential of the tailings to release substantial amounts of these pollutants into the surrounding soils and watercourses. AMD has been identified and percolation through the base of the pond could occur at its northeast sector, where a low resistivity area is recognized. The manifest instability of the tailings pond makes it necessary to include physical stabilization in remediation and monitoring in order to minimize the environmental impact of the tailings on the areas affected, which is located in one of the most popular tourist areas in SE Spain.Highlights?Joint use of geophysical and geochemical methods for environmental characterization?Resistivity data reveals ~8m thick mine deposits with significant acid water leakage.?Significant toxic metal and metalloid content have been measured.?The pond instability makes it necessary to work on remediation and monitoring.?
机译:<![cdata [ 抽象 本研究显示了Brunita-LaUnión矿区的Brunita Mine Pond的地理环境表征结果,穆尔西亚(西班牙)。主要目标是评估矿山尾矿的现状,以确定相关的环境危害。自1956年以来,Brunita Mine尾矿正在储存在一个NNO-SSE趋势峡谷的水道中的四个阶梯式池塘中。随后,它们存放在一个大型池塘中。在关闭池塘运营之后,对堤防稳定化的某些作品进行了,并且来自Brunita Mine的碎片开始积累。 50年的采矿工程导致矿井废料完全埋葬周围的山谷和山丘。电阻率断层扫描(ERT)允许确定池塘底座的一般几何形状和矿井尾矿的厚度。沿着总共6个ERT型材,3个纵向和3个横向剖面进行了调查,以池塘的最大尺寸。 infilling和基岩之间的强电阻率对比足够高,以清楚地限定底部池塘边界。低电阻率值(<10Ω·m)表征池塘的infilling,而电阻率值>200Ω·m对应于构成沉积物底部的古生代岩石。已经认识到垂直步骤限定了沉积物厚度的强变化。这种几何形状由前谷的古图谱和沉积物的不同生长阶段之间的相互作用产生。从两个钻孔获得的池塘的深度已经确认了从ert型材获得的结果。通过代表性样本的XRD确定了大量的黄铁矿和散热岩和明显存在的斯巴尔氏酒和加勒纳。因此,在化学分析中检测到毒性金属(CD,Cu,Pb,Sn,Sn和Zn)的高含量,显示尾矿的潜力,以将大量这些污染物释放到周围的土壤和水道中。通过池塘的底座确定了AMD,可以在其东北部门出现,在其东北部门被认可低电阻率区域。尾矿池的清单不稳定使得有必要在修复和监测中包括物理稳定,以最大限度地减少尾矿对受影响地区的环境影响,该区域位于西班牙最受欢迎的旅游区域之一。 突出显示 联合使用地球物理和地球化学方法对于环境特征 电阻率数据显示〜8M厚矿山沉积物,具有重要的酸性扫管液呃泄漏。 已经测量了显着的有毒金属和金属体含量。 池塘不稳定性使得有必要在修复和监控上工作。

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