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Predicted performance of clay-barrier landfill covers in arid and semi-arid environments

机译:干旱和半干旱环境下粘土屏障垃圾填埋场的预测性能

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摘要

Conventional landfill cover systems for municipal solid waste include low-permeability compacted clay barriers to minimize infiltration into the landfilled waste. Such layers are vulnerable in climates where arid to semi-arid conditions prevail, whereby the clay cover tends to desiccate and crack, resulting in drastically higher infiltration, i.e., lower cover efficiency. To date, this phenomenon, which has been reported in field observations, has not been adequately assessed. In this paper, the performance of a cover system solely relying on a clay barrier was simulated using a numerical finite element formulation to capture changes in the clay layer and the corresponding modified hydraulic characteristics. The cover system was guided by USEPA Subtitle-D minimum requirements and consisted of a clay layer underlying a protective vegetated soil. The intrinsic characteristics of the clay barrier and vegetative soil cover, including their saturated hydraulic conductivities and their soil-water characteristic curves, were varied as warranted to simulate intact or "cracked" conditions as determined through the numerical analyses within the proposed methodology. The results indicate that the levels of percolation through the compromised or cracked cover were up to two times greater than those obtained for intact covers, starting with an intact clay hydraulic conductivity of 10~(-5) cm/s.
机译:用于城市固体废物的常规垃圾掩埋覆盖系统包括低渗透性的压实粘土屏障,以最大程度地减少渗入垃圾中。这种层在干旱至半干旱条件普遍的气候中是脆弱的,由此粘土覆盖层趋于干燥和破裂,从而导致渗透率大大提高,即覆盖效率降低。迄今为止,尚未在野外观察中报告这种现象。在本文中,使用数值有限元公式捕获粘土层的变化和相应的修改后的水力特性,模拟了仅依靠粘土屏障的覆盖系统的性能。覆盖系统遵循USEPA Subtitle-D最低要求,由保护性植被土壤下面的粘土层组成。黏土屏障和植物性土壤覆盖物的内在特征,包括其饱和的水力传导率和土壤-水特征曲线,根据所提议的方法中的数值分析确定,可以模拟完整或“开裂”的条件。结果表明,从完好无损的覆盖层或破裂的覆盖层渗透的水平是完整覆盖层的渗透水平的两倍,从完整的粘土水力传导率为10〜(-5)cm / s开始。

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