首页> 外文学位 >Geochemical characterization of coal-combustion byproducts and adjacent pore waters fifteen years after emplacement in an abandoned mine land site in southwestern Indiana.
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Geochemical characterization of coal-combustion byproducts and adjacent pore waters fifteen years after emplacement in an abandoned mine land site in southwestern Indiana.

机译:煤燃烧副产物和邻近孔隙水在印第安纳州西南部废弃矿场中放置后十五年的地球化学特征。

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摘要

Coal-combustion byproducts (CCBs) have potential as structural fill and capping materials in coal mine reclamation because of their abundance, engineering properties, and acid-neutralization capacity. However, the potential to leach constituents of concern (COCs) into groundwater hinders their widespread utilization. In 1996, an abandoned mine land (AML) Site in southwestern Indiana was reclaimed using a Fixated Scrubber Sludge (FSS) cap composed of flue gas desulphurization sludge, fly ash, and lime. The cap was placed over pyritic refuse, overburden spoil, and ponded ash. In 2011, 45 samples of FSS and ponded ash extracted from six sediment cores were subjected to laboratory analyses to identify evidence of chemical weathering. Also, samples of groundwater and pore water from the unsaturated and shallow saturated zone were collected during the 2012 water year to find potential leaching of CCBs and calculate mineral saturation indices. X-ray diffractometry indicated that oxidation of hannebachite to gypsum and calcite was restricted to the upper one-to-four centimeters of the FSS cap. Samples of the ponded ash revealed no alteration with depth. Elemental analysis indicated there was no significant change in major oxide or trace element concentrations in FSS or ponded ash. Water chemistry data confirmed historical Site data exhibiting decreasing concentrations of COCs and neutralizing conditions. Calculated saturation indices show that soluble minerals in FSS and ponded ash are in equilibrium with groundwater. The results of this study support previous research indicating that COCs which were initially leached from the CCBs quickly, reached equilibrium with the impacted water and that there was little or no additional alteration of CCBs.
机译:煤燃烧副产物(CCBs)由于其含量丰富,工程特性和酸中和能力而具有作为煤矿填海中的结构填充和封盖材料的潜力。但是,将关注的成分(COC)浸入地下水的潜力阻碍了它们的广泛利用。 1996年,印第安纳州西南部的一块废弃矿山(AML)场址被固定的洗涤器污泥(FSS)帽回收,该帽由烟气脱硫污泥,粉煤灰和石灰组成。将帽子放在黄铁矿垃圾,覆盖的土壤和灰烬上。 2011年,对从六个沉积物岩心中提取的45种FSS和池灰进行了实验室分析,以确定化学风化的证据。此外,在2012供水年度收集了非饱和和浅层饱和带的地下水和孔隙水的样本,以发现潜在的CCB浸出并计算矿物饱和指数。 X射线衍射法表明,锰锌铁矿氧化成石膏和方解石仅限于FSS帽的上部1-4厘米。积灰的样品显示其深度没有变化。元素分析表明,FSS或积灰中的主要氧化物或微量元素浓度没有显着变化。水化学数据证实了历史现场数据显示出降低的COC浓度和中和条件。计算得出的饱和指数表明,FSS和池灰中的可溶性矿物质与地下水处于平衡状态。这项研究的结果支持以前的研究,表明最初从CCB中浸出的COC很快与受影响的水达到平衡,而且CCB很少或没有其他变化。

著录项

  • 作者

    Martin, Luke Cameron.;

  • 作者单位

    Indiana University.;

  • 授予单位 Indiana University.;
  • 学科 Geochemistry.;Mining engineering.;Mineralogy.
  • 学位 M.S.
  • 年度 2015
  • 页码 89 p.
  • 总页数 89
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:52:25

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