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Crack Characteristic and Permeability Change of Compacted Clay Liners with Different Liquid Limits under Dry-Wet Cycles

机译:干湿循环下不同液体限制的压实粘土衬垫的裂纹特性和渗透性变化

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摘要

The crack characteristic and permeability change in six compacted clay liners (CCLs) under dry-wet cycles were studied. Results show that as soil liquid limit (LL) increases, the crack block (CB) number, crack ratio (CR), and crack length (CL) of the CCLs increase under the dry state. The CB sizes of all the six CCLs correspond to normal distribution. A piecewise linear relationship exists between crack parameters and soil LL, and the slope at LL 50. The size of the representative elementary volume (REV) of cracked CCL decreases linearly with the increase in soil LL when LL 50. The sample size of the CCLs for the permeability test must be larger than REV. Before and after three dry-wet cycles, the permeability ratio (K3/k0) initially increases and eventually decreases as soil LL increases, and LL at the peak value of K3/k0 is 36.1%. However, linear relationships exist between permeability D-value (K3 − k0) and soil LL in a semilog coordinate system when LL 50%. The volume and mean width of unclosed cracks are two main factors that determine the increase in permeability after dry-wet cycles. After three dry-wet cycles, these factors decrease as soil LL increases, thereby reducing the permeability D-value.
机译:研究了干湿循环下六个压实粘土衬里(CCLS)的裂纹特性和渗透性变化。结果表明,由于土壤液体限制(LL)增加,CCLS在干燥状态下增加的裂缝块(Cb)数,裂缝率(Cr)和裂缝长度(Cl)增加。所有六个CCLS的CB尺寸对应于正态分布。在裂纹参数和土壤L1之间存在分段线性关系,以及L10的斜率。裂化CCL的代表性基本体积(Rev)的尺寸随着L150时的土壤L1的增加而导入线性降低。CCLS的样品大小对于渗透性测试必须大于Rev。在三次干湿循环之前和之后,渗透率(K3 / K0)最初增加,并且最终随着土壤LL的增加而降低,K3 / K0峰值的LL为36.1%。然而,当LL 50%时,在半径坐标系中的渗透性D值(K3-k0)和土壤LL之间存在线性关系。未缩减裂缝的体积和平均宽度是确定干湿循环后渗透性增加的两个主要因素。在三个干湿循环之后,随着土壤LL的增加,这些因子降低,从而降低渗透性D值。

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