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首页> 外文期刊>Environmental Earth Sciences >Delineation of compaction criteria for acceptable hydraulic conductivity of lateritic soil-bentonite mixtures designed as landfill liners
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Delineation of compaction criteria for acceptable hydraulic conductivity of lateritic soil-bentonite mixtures designed as landfill liners

机译:划定设计为垃圾填埋场衬层的红土土-膨润土混合物可接受的水力传导率的压实标准

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In current geoenvironmental practice, design engineers usually require that soil liners in waste landfills be compacted within a specified range of water content and dry unit weight. This specification is based primarily on the need to achieve a minimum dry unit weight for factors controlling the performance of compacted soil liners most especially the hydraulic conductivity, k. In this study, lateritic soil treated with up to 10% bentonite, prepared at various compaction states (dry of optimum, optimum and wet of optimum moisture content) was compacted with four compactive efforts (i.e., the reduced British Standard Light, British Standard Light, West African Standard, and British Standard Heavy) to simulate the range of compaction energies expected in the field. Prepared soil mixtures were permeated with water and specimens that yielded the permissible limit of k ≤ 1 × 10−9 m/s were enclosed in an envelope (known as the acceptable zone) on the water content–dry unit weight curve. It was observed that compaction conditions resulting in moisture content slightly wet of optimum led to the lowest values of k and that the shapes and boundaries of the acceptable zones gradually increased in extent, shifting to wet side of optimum moisture content as the bentonite content increased to 10%. This approach provides good control over the quality of compacted soils and has great potential for field application.
机译:在当前的地球环境实践中,设计工程师通常要求将垃圾填埋场中的土壤衬层压实在规定的含水量和单位干重范围内。该规范主要基于对控制压实土壤衬砌性能(尤其是水力传导系数k)的因素实现最小干重的要求。在这项研究中,用四种压实方法(即还原的英国标准光,英国标准光)用各种压实状态(最佳干度,最佳干度和最佳水分含量的湿润状态)制备的经高达10%膨润土处理的红土土壤进行压实。 ,西非标准和英国标准重型)来模拟现场预期的压实能量范围。将准备好的土壤混合物用水浸透,将达到k≤1×10 −9 m / s的允许极限的标本封闭在含水量干燥的包膜(称为可接受区域)中单位重量曲线。观察到,压实条件导致水分含量稍为最佳湿润状态时,k值最低,可接受区域的形状和边界逐渐扩大,随着膨润土含量的增加,湿润侧移至最佳水分含量湿侧。 10%。这种方法可以很好地控制压实土壤的质量,在野外应用中具有很大的潜力。

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