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首页> 外文期刊>Water, Air, and Soil Pollution >A Geochemical and Geophysical Characterization of Sulfide Mine Ponds at the Iberian Pyrite Belt (Spain)
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A Geochemical and Geophysical Characterization of Sulfide Mine Ponds at the Iberian Pyrite Belt (Spain)

机译:伊比利亚黄铁矿带(西班牙)硫化矿池的地球化学和地球物理特征

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摘要

This work presents the results of a geochemical and geophysical characterization of the Monte Romero and La Naya mine ponds, belonging to the Cueva de la Mora and Riotinto mine districts, respectively, based on mineralogical, geochemical and geophysical techniques. In order to obtain a representative environmental characterization, two deposits showing different mineralogies, physico-chemical parameters, chemical compositions of tailings and pond conditions were selected. Monte Romero mine tailings showed an upper level mainly composed of silicates and a deeper level mainly composed of sulfides and barite. The toxic metal content was different in both levels but high enough to exceed the regional legal concentration limits for agricultural soils. An electrical resistivity tomography survey revealed a homogeneous upper unit (3 m thickness), which displayed low resistivity values, corresponding to water-saturated silt and clay materials with an abundance of sulfides which was interpreted as the pond infilling. The La Naya mine pond presented a homogeneous mineralogical composition made up of quartz as the main mineral and chlorite-smectite and jarosite as accessory phases. The absence of sulfide phases and the low contents of metal elements are directly related to the reworking processes of the sludge dumped in this pond. The geophysical survey revealed that the pond infilling did not have a constant thickness, but ranged between 15 and 20 m. An inner groundwater flow in the infilling was recognized. The low resistivity values allowed the presence of acid waters and related subsurface flows to be identified in both mine ponds, but no acid water drainage occurred across their vessels. When compared to the Aznalcollar tailings spill, the La Naya pond is large enough to release a similar amount of sludge, but of a very low metal content. The Monte Romero sludge displays a similar, potentially toxic metal content to the Aznalcollar sludge, but its size is significantly smaller.
机译:这项工作基于矿物学,地球化学和地球物理技术,对分别属于Cueva de la Mora和Riotinto矿区的Monte Romero和La Naya矿池进行了地球化学和地球物理特征的描述。为了获得代表性的环境特征,选择了两个具有不同矿物学,理化参数,尾矿化学成分和池塘条件的矿床。 Monte Romero矿的尾矿表现出较高的水平,主要由硅酸盐组成,而较深的水平主要由硫化物和重晶石组成。有毒金属含量在两个水平上均不同,但高到足以超过农业土壤的区域法定浓度极限。电阻层析成像调查显示,上部均质(3 m厚),显示较低的电阻率值,对应于水饱和的粉砂和粘土材料,并带有大量的硫化物,被解释为池塘填充物。拉纳亚(La Naya)矿池呈现出均一的矿物学组成,其组成为石英为主要矿物,绿泥石-蒙脱石和黄钾铁石为辅助相。硫化物相的缺乏和金属元素的低含量直接与该池中倾倒的污泥的再加工过程有关。地球物理调查表明,池塘填充物的厚度不是恒定的,而是在15至20 m之间。识别出填充物中的内部地下水流。低电阻率值可以在两个矿池中识别出酸性水和相关的地下流的存在,但是整个容器中都没有酸性水的排出。与Aznalcollar尾矿溢流相比,La Naya池塘足够大,可以释放出类似量的污泥,但金属含量非常低。 Monte Romero污泥显示出与Aznalcollar污泥相似的,可能有毒的金属含量,但其尺寸要小得多。

著录项

  • 来源
    《Water, Air, and Soil Pollution》 |2011年第4期|p.387-405|共19页
  • 作者单位

    D. Gomez-Ortiz • J. Lillo-RamosDpt. Biologia y Geologia, ESCET,Universidad Rey Juan Carlos,C/Tulipan s,28933 Mostoles, Madrid, Spain;

    D. Gomez-Ortiz • J. Lillo-RamosDpt. Biologia y Geologia, ESCET,Universidad Rey Juan Carlos,C/Tulipan s,28933 Mostoles, Madrid, Spain;

    D. Gomez-Ortiz • J. Lillo-RamosDpt. Biologia y Geologia, ESCET,Universidad Rey Juan Carlos,C/Tulipan s,28933 Mostoles, Madrid, Spain;

    D. Gomez-Ortiz • J. Lillo-RamosDpt. Biologia y Geologia, ESCET,Universidad Rey Juan Carlos,C/Tulipan s,28933 Mostoles, Madrid, Spain;

    D. Gomez-Ortiz • J. Lillo-RamosDpt. Biologia y Geologia, ESCET,Universidad Rey Juan Carlos,C/Tulipan s,28933 Mostoles, Madrid, Spain;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    mine pond; metals; acid mine drainage; electrical resistivity tomography; iberian pyrite belt;

    机译:矿池金属;酸性矿山排水电阻层析成像伊比利亚黄铁矿带;

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