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Potential of coal mine waste rock for generating acid mine drainage

机译:煤矿waste石产生酸性矿山排水的潜力

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Acid mine drainage (AMD) due to the oxidation of sulphide bearing waste rock (WR) is a common environmental problem associated with coal extraction. Therefore, WRs from the Lakhra coal field in Pakistan, were studied to i) perform a mineralogical and chemical characterisation, ii) determine the AMD generating potential and iii) estimate the leachability of elements. The chemical and mineralogical composition was studied using ICP, XRF, XRD and SEM. Acid base accounting and weathering cell test determined the acid producing potential of WRs. Besides organic material, the WRs were composed of quartz, pyrite, kaolinite, hematite and gypsum with varying amounts of calcite, lime, malladerite, spangolite, franklinite and birnessite. The major elements Si, Al, Ca and Fe were in the range (wt.%) of 8-12, 6-9, 0.3-3 and 1-10, respectively, with high S concentrations (19.4-113.3 g/kg). Trace elements were in the range (mg/kg) As (0.3-8), Cd (0.2-0.4), Co (15-75), Cr (67-111), Cu (25-101), Hg (0.1-0.2), Ni (50-107), Pb (8-20) and Zn (75-135). The AMD potential of WRs ranged from -70 to -492 kg CaCO3/tonne. During the test period of 192 days, the pH of leachates from very acidic WRs was maintained from 1 to 2.5, whereas, the less acidic WRs produced leachates of mildly acidic (2.7) to neutral (7.3) pH. The leachates from very acidic WRs ranged in the element concentrations of Fe, SO42- and Al from mg/L to g/L and As, B, Co, Cu, Mn, Ni and Zn from mu g/L to mg/L. However, the leachates from less acidic WRs contained all major elements in mg/L and trace elements in mu g/L concentrations except for B and Mn that ranged from mu g/L to mg/L. The results show that the studied WRs have mild to strong acid producing potential and have the capacity to deteriorate natural water quality significantly. Therefore, necessary preventive or/and acid neutralising measures are strongly suggested. (C) 2015 Elsevier B.V. All rights reserved.
机译:由于含硫化物的废石(WR)的氧化而导致的酸性矿山排水(AMD)是与煤炭开采相关的常见环境问题。因此,对巴基斯坦Lakhra煤田的WRs进行了以下研究:i)进行矿物学和化学表征,ii)确定AMD的产生潜力,iii)估算元素的浸出性。使用ICP,XRF,XRD和SEM研究了化学和矿物组成。酸碱计算和风化室测试确定了WR的产酸潜力。除有机材料外,WR包括石英,黄铁矿,高岭石,赤铁矿和石膏,以及不同数量的方解石,石灰,绿宝石,斯潘戈石,富兰克林石和水钠锰矿。 Si,Al,Ca和Fe的主要元素分别在8-12、6-9、0.3-3和1-10的重量百分比范围内,并且具有较高的S浓度(19.4-113.3 g / kg) 。微量元素的范围为(mg / kg)As(0.3-8),Cd(0.2-0.4),Co(15-75),Cr(67-111),Cu(25-101),Hg(0.1- 0.2),镍(50-107),铅(8-20)和锌(75-135)。 WR的AMD潜力为-70至-492 kg CaCO3 /吨。在192天的测试期间,来自极酸性WR的渗滤液的pH值保持在1至2.5,而酸性较低的WR则产生了弱酸性(2.7)到中性(7.3)pH的渗滤液。来自极酸性WRs的浸出液中,Fe,SO42-和Al的元素浓度从mg / L到g / L,而As,B,Co,Cu,Mn,Ni和Zn的元素浓度从μg/ L到mg / L。但是,来自酸性较低的WR的浸出液中所有主要元素(mg / L)和痕量元素(μg/ L)除外,B和Mn的范围从μg/ L至mg / L。结果表明,所研究的WR具有中等至强酸产生潜力,并且具有显着降低天然水质的能力。因此,强烈建议采取必要的预防或/和酸中和措施。 (C)2015 Elsevier B.V.保留所有权利。

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