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首页> 外文期刊>International journal of geomechanics >Physico-Chemical Effects on Shrinkage Behavior of Compacted Expansive Clay
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Physico-Chemical Effects on Shrinkage Behavior of Compacted Expansive Clay

机译:理化效应对压实膨胀土收缩特性的影响

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摘要

Physico-chemical effects have a significant impact on the behavior of clay barriers due to the interactions between the pore fluid and clay particles, and they pose a great challenge because the efficiency of clay barriers and cover systems may be altered. Therefore, this paper highlights the effect of physico-chemical factors on shrinkage behavior of compacted expansive clay. To achieve this, the compacted clay specimens were inundated with distilled water, NaCl, and CaCl2 salt solutions in separate oedometer cells at a vertical pressure of 6.25kPa and allowed to swell. The swollen specimens were gradually shrunk until the specimens attained constant mass, and the changes in void ratio and water content were monitored during drying. The experimental results showed that magnitude of induced osmotic suction and type of pore fluid had a significant impact on shrinkage behavior of compacted clay specimens due to the changes in soil structure. The average pore size of compacted specimens significantly decreased with the induced osmotic suction due to the reduction in size of micropores owing to the suppression of double layers. The discussions are supported by scanning electron microscopy images. Also, the experimental shrinkage data were fitted using modified van Genuchten and Fermi mathematical models, and the results showed that these models fit well with an adjusted R-2 higher than 0.9962.
机译:由于孔隙流体和黏土颗粒之间的相互作用,物理化学效应对黏土屏障的行为产生了重大影响,并且由于黏土屏障和覆盖系统的效率可能会发生变化,因此它们也带来了巨大的挑战。因此,本文重点介绍了理化因素对压实膨胀粘土的收缩行为的影响。为了达到这个目的,在6.25kPa的垂直压力下,在单独的里程表池中用蒸馏水,NaCl和CaCl2盐溶液淹没压实的粘土样品,并使其溶胀。逐渐使溶胀的样品收缩,直到样品达到恒定质量,并在干燥过程中监测空隙率和含水量的变化。实验结果表明,由于土壤结构的变化,诱导的渗透力的大小和孔隙流体的类型对压实黏土样品的收缩行为有显着影响。由于双层的抑制,由于微孔尺寸的减小,致密样品的平均孔径随着诱导的渗透吸引而显着减小。讨论得到扫描电子显微镜图像的支持。此外,使用改良的van Genuchten和Fermi数学模型拟合了实验收缩率数据,结果表明,这些模型与调整后的R-2高于0.9962很好地拟合。

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