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Numerical interpretation of the coupled hydromechanical behaviour of expansive clays in constant volume column tests

机译:定容柱试验中膨胀土的耦合流变力学行为的数值解释

摘要

© The authors and ICE Publishing: All rights reserved, 2015.Experimental and numerical studies of the behaviour of expansive clays have been attracting increasing interest, due to their good sealing properties, which render them ideal to be used as engineered barriers (buffers) in both active (e.g. nuclear) and non-active waste disposal facilities. Both large scale and laboratory scaled experiments indicate that the sealing capabilities of the buffer are fundamentally governed by its volumetric behaviour when wetted. In this paper, a constant volume column infiltration test, performed under isothermal conditions on compacted MX80 bentonite, is modelled numerically using the Imperial College Finite Element Program (ICFEP). A modified version of the Barcelona Basic Model is used to simulate the behaviour of the buffer, which is inherently partly saturated. The numerical results agree well with the observed experimental data, especially with regard to the advancement of the wetting front. A detailed interpretation of the computed evolutions with time of stress state, suction and void ratio at different elevations along the samples axis is carried out, providing insight into the complex hydro-mechanical response of the buffer during the experiment. Indeed, even though the overall volume of the sample was kept constant, a region of localised dilation, which induced the contraction of other zones of the material, was observed to advance simultaneously with the wetting front along the height of the soil column.
机译:©作者和ICE Publishing版权所有:保留所有权利,2015年。由于膨胀土的良好密封性能,对膨胀土性能的实验和数值研究引起了越来越多的关注,这使其成为理想的可作为工程隔离层(缓冲层)的材料。主动(例如核能)和非主动废物处理设施。大规模和实验室规模的实验均表明,缓冲液的密封能力从润湿时的体积行为基本决定。在本文中,使用帝国大学有限元程序(ICFEP)对等压条件下在密实MX80膨润土上进行的等体积柱渗透试验进行了数值模拟。使用巴塞罗那基本模型的修改版来模拟缓冲区的行为,缓冲区的本质是部分饱和的。数值结果与观察到的实验数据非常吻合,特别是在润湿前沿方面。沿着样品轴在不同高度上对应力状态,吸力和空隙比随时间变化的计算演化进行了详细的解释,从而提供了对实验过程中缓冲液复杂的水力响应的深入了解。实际上,即使样品的总体积保持恒定,也观察到局部膨胀的区域会引起材料其他区域的收缩,并随着润湿前沿沿着土壤柱的高度同时前进。

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