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Laboratory Column Experiment to Evaluate Oxygen Diffusion through Covers with Capillary Barrier Effects Subjected to Freeze-Thaw Cycles

机译:实验室柱实验,通过冻结-融化循环评估通过毛细屏障效应覆盖的氧气扩散

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Environmental reclamation of mine waste disposal facilities often requires their confinement under engineered soil covers to control gas migration and water infiltration. In temperate climates, covers with capillary barrier effects (CCBE) are successfully used to control oxygen flux; these covers require a fine-grained material that acts as a moisture-retaining layer. In Nordic environments, where such natural fine-grained soils are not always available, soil or crushed rock-bentonite mixtures could be used instead. A key parameter in the design and performance evaluation of CCBE is the effective diffusion coefficient of oxygen (D_e) of the moisture-retaining layer. This paper aims at presenting the development of a laboratory column testing and interpretation method to evaluate the D_e of a crushed rock-bentonite moisture-retaining layer in a CCBE and the effect of freeze-thaw cycles on D_e. The numerical approach used to analyze the experimental diffusion test results allowed obtaining D_e for various saturation conditions observed in the moisture-retaining layer. Preliminary results show that the initial measured value of D_e increased by two orders of magnitude after 3 freeze-thaw cycles. Steady-state flux calculations based on the obtained D_e showed that despite a good initial cover performance, the capacity of the tested cover to act as an oxygen barrier is reduced in the longer term. This study demonstrates that the proposed laboratory column oxygen diffusion test could be an effective tool to assess the performance of CCBE to control oxygen migration when exposed to cold climate conditions.
机译:矿山废物处理设施的环境开垦通常需要将其限制在工程土壤覆盖下,以控制气体迁移和水的渗透。在温带气候下,具有毛细屏障效应(CCBE)的覆盖层已成功用于控制氧气通量。这些覆盖层需要细颗粒的材料作为保湿层。在北欧环境中,此类天然细粒土壤并不总是可用,可以使用土壤或碎石-膨润土混合物代替。 CCBE设计和性能评估中的关键参数是保水层中氧气的有效扩散系数(D_e)。本文旨在介绍一种实验室柱测试和解释方法的开发,以评估CCBE中破碎的膨润土保水层的D_e以及冻融循环对D_e的影响。用于分析实验性扩散测试结果的数值方法允许获得在保水层中观察到的各种饱和条件下的D_e。初步结果表明,D_e的初始测量值在3次冻融循环后增加了两个数量级。根据获得的D_e进行的稳态通量计算表明,尽管初始覆盖层性能良好,但从长远来看,被测覆盖层充当氧气屏障的能力会降低。这项研究表明,拟议的实验室色谱柱氧气扩散测试可能是评估CCBE在暴露于寒冷气候条件下控制氧气迁移的性能的有效工具。

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