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Tropical Soils–Acid Mine Drainage Interactions: Breakthrough Curves and Some Transport Parameters

机译:热带土壤与酸性矿山排水的相互作用:突破曲线和一些运输参数

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The interactions between acid mine drainage (AMD) and three tropical clayey soils have been studied through hydraulic conductivity and batch sorption/dissolution testing. After 19–24 pore volumes of AMD flow through the soils, the measured final hydraulic conductivity ranged between 1.1×10?11 and 3.3×10?11 m/s. The pH, electrical conductivity, and solute breakthrough curves obtained suggested the soils had low acid-buffering capacities. Also, several chemical species were released from the soils due to AMD attack of soil grains and mineral. The batch tests revealed high dissolution of species such as sodium, cobalt, and sulfate from the soils by AMD. The results also indicated dissolution of metals from soil constituents, desorption of chemical species, and transformation and dissolution of soil minerals due to AMD attack. The results of the study showed that, in general, the soils were not effective in attenuating contaminants present in the AMD. Thus, they may not be used alone to construct liners for acid-generating waste mine containment facilities.
机译:通过水力传导率和分批吸附/溶解测试研究了酸性矿山排水(AMD)与三种热带黏性土壤之间的相互作用。在19–24孔隙体积的AMD流过土壤后,测得的最终水力传导率介于1.1×10?11和3.3×10?11 m / s之间。 pH,电导率和溶质穿透曲线表明土壤具有较低的酸缓冲能力。此外,由于AMD对土壤谷物和矿物质的侵蚀,几种化学物质也从土壤中释放出来。批处理测试表明,AMD从土壤中高度溶解了钠,钴和硫酸盐等物质。结果还表明,由于AMD的侵蚀,金属从土壤成分中溶解,化学物质的解吸以及土壤矿物的转化和溶解。研究结果表明,总的来说,土壤不能有效减轻AMD中存在的污染物。因此,它们不能单独用于构造用于产酸废矿围堵设施的衬里。

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