首页> 外文OA文献 >Physico-chemical Processes In Acid Mine Drainage In Coal Mining South Brazil [processos Físico-químicos Em Drenagem ácida De Mina Em Mineração De Carvão No Sul Do Brasil]
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Physico-chemical Processes In Acid Mine Drainage In Coal Mining South Brazil [processos Físico-químicos Em Drenagem ácida De Mina Em Mineração De Carvão No Sul Do Brasil]

机译:巴西南部煤矿开采中酸性矿山的物理化学过程[巴西南部煤矿开采中酸性矿山的物理化学过程]

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摘要

Acid mine drainage generated from coal mine showed a pH of 3.2, high concentrations of SO42-, Al, Fe, Mn, Zn and minor As, Cd, Co, Cr, Cu, Ni and Pb. The major reduction in the concentration occurred for Al, As, Cr, Fe and Pb after the treatment with CaO. The evolution of these acid waters within the tributary stream showed decreasing concentration for all soluble constituents, except Al. This natural attenuation was controlled by pH (6.4 to 10.8) as a result of concurrent mixing with tributary stream and reaction with local bedrock that contains limestone. Aluminum increasing concentration during this evolution seems to be related to an input of Al-enriched waters due to the leaching of silicate minerals in alkaline conditions.
机译:煤矿产生的酸性矿山排水显示pH为3.2,高浓度的SO42-,Al,Fe,Mn,Zn和微量的As,Cd,Co,Cr,Cu,Ni和Pb。用CaO处理后,Al,As,Cr,Fe和Pb的浓度发生了最大程度的降低。这些酸水在支流中的逸出表明,除Al外,所有可溶性成分的浓度均降低。由于与支流同时混合并与含有石灰石的局部基岩反应,这种自然衰减受到pH的控制(6.4至10.8)。由于在碱性条件下硅酸盐矿物的浸出,在这种演变过程中铝浓度的增加似乎与富铝水的输入有关。

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  • 作者

    Campaner V.P.; Luiz-Silva W.;

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  • 年度 2015
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  • 原文格式 PDF
  • 正文语种 por
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