风化砂岩构建低渗透屏障以隔离煤矿垃圾的潜在用途

M. Rosa, C. Agouridis, R. Warner
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引用次数: 0

摘要

比电导和硒(Se)是阿巴拉契亚煤田新近受到关注的两个水质参数。利用低渗透屏障将高比电导和产硒渣滓从环境水流中隔离开来,是减少这些成分从煤矿渣滓中浸出的一种方法。理想情况下,用于形成屏障的材料应该易于接近,具有低水平的比电导和硒,并且能够通过适当的湿度调节实现低渗透率。棕色和灰色风化砂岩通常很容易在阿巴拉契亚煤田的矿区找到。来自肯塔基州派克维尔附近的肯塔基大学本特山研究中心的废渣样本和水质样本表明,这些废渣类型有望满足低比电导生产材料的标准。然而,这些砂岩的含沙量往往高于垃圾填埋场中通常用于压实屏障或衬垫的砂岩。本研究的目的是评估使用棕色和/或灰色风化砂岩创建低渗透屏障的潜力。为达到研究目的,2012年共收集了4个废土样本(确定为M1-M4)。每个废石样本都是从肯塔基州东部不同的矿井中获得的。样品M1和M2由棕色砂岩组成;M3为灰色砂岩;样品M4是棕色和灰色砂岩的混合物。对每个废土样品进行筛选和土壤质地分析。利用双环渗透仪对每个样品建立了废土含水率-密度关系和废土饱和水力导电性-含水率关系。在实验室中,对于小于2mm的部分,最大饱和水力导电性值在低5.9 × 10 -8 cm s -1到高3.1 × 10 -7 cm s -1之间。这些饱和水力导电性值与垃圾填埋场中用于建造衬垫的土壤相当,特别是在废物中细粒百分比约为50%或更高的情况下。然而,在现场,由于岩石碎片的影响,这些饱和水力导电性值通常会高出1-3个数量级。这些结果表明,与灰色砂岩相比,具有较高细粒含量的棕色砂岩可能更适合用于构建低渗透屏障,以隔离高比电导产生和/或产硒的碎屑。根据这些实验室结果,建议对这种应用的棕色风化砂岩进行现场评估。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
POTENTIAL USE OF WEATHERED SANDSTONES TO CONSTRUCT A LOW PERMEABILITY BARRIER TO ISOLATE PROBLEMATIC COAL MINE SPOILS 1
Specific conductance and selenium (Se) are two water quality parameters of emerging concern in the Appalachian coalfields. Isolation of high specific conductance and Se producing spoils from environmental water flows using a low permeability barrier is one method of minimizing the leaching of these constituents from coal mine spoils. Ideally, the material used to form the barrier should be readily accessible, have low levels of specific conductance and Se, and be capable of achieving a low permeability with the proper moisture adjustment. Brown and gray weathered sandstones are often readily available at mine sites in the Appalachian coalfields. Spoil samples and water quality samples from the University of Kentucky Bent Mountain Research Complex near Pikeville, Kentucky indicated that these spoil types hold promise in meeting the criteria of being a low specific conductance producing material. However, these sandstones tend to have higher sand contents than those typically used in compacted barriers or liners in landfills. The objective of this study was to assess the potential of using brown and/or gray weathered sandstones to create a low permeability barrier. To meet the objective of the study, a total of four spoil samples (identified as M1-M4) were collected in 2012. Each spoil sample was obtained from a different mine in eastern Kentucky. Samples M1 and M2 consisted of brown sandstone; sample M3 was gray sandstone; and sample M4 was a mixture of brown and gray sandstones. Each spoil sample was screened and analyzed for soil texture. Spoil moisture content-density relationships and spoil saturated hydraulic conductivity-moisture content relationships were developed for each sample using double ring permeameters. Maximum saturated hydraulic conductivity values ranged between a low of 5.9 x 10 -8 cm s -1 to a high of 3.1 x 10 -7 cm s -1 in the laboratory for the <2mm fraction. These saturated hydraulic conductivity values were comparable to soils used to construct liners in landfills, particularly in instances where the percentage of fines in the spoils were about 50% or greater. When in the field, however, it is expected that these saturated hydraulic conductivity values will typically be 1-3 orders of magnitude higher due to rock fragments. These results demonstrate that brown sandstone, with its higher fines content, is likely a more suitable media than gray sandstone for constructing a low permeability barrier to isolate high specific conductance producing and/or Se generating spoils. Based on these laboratory results, field assessments of brown weathered sandstones for this application are recommended.
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