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Investigation of the swelling behaviour of compacted bentonite-sand mixture by mock-up tests

机译:通过模拟试验研究压实膨润土-砂混合物的溶胀行为

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Two small-scale mock-up tests were carried out on a compacted mixture of bentonite and sand, one with saturation from the bottom only and the other with saturation from the top and bottom. Swelling pressure was monitored at different positions of the soil sample in both axial and radial directions. Results showed that the two-side saturation accelerates the swelling pressure kinetics by a factor of 4. The radial swelling pressure kinetics depends on the soil swelling, soil collapse, and interaction between the soil layers. Further analysis based on the relative humidity measurements in an infiltration test performed previously showed that the variations of swelling pressure with suction are similar to those found in literature, and that threshold points exist indicating the initiation of soil collapse. These threshold points appeared at higher suction when the soil was farther from the wetting face. The failure of the axial confining elements in the storage galleries was also simulated by releasing the piston and allowing a limited axial swelling of 20%. The radial swelling pressures decreased sharply upon the piston release and during the free axial swelling. A swelling pressure gradient was found from the bottom to the top with a higher value at the bottom. The density gradient was estimated based on the swelling pressure profile.
机译:在膨润土和沙子的密实混合物上进行了两次小规模的模型测试,一个仅从底部开始饱和,另一个从顶部和底部开始饱和。在轴向和径向上在土壤样品的不同位置处监测膨胀压力。结果表明,两侧饱和度使溶胀压力动力学加快了4倍。径向溶胀动力学取决于土壤溶胀,土壤塌陷和土壤层之间的相互作用。根据先前进行的渗透测试中的相对湿度测量结果进行的进一步分析表明,吸力引起的溶胀压力变化与文献中的变化类似,并且存在指示土壤崩塌开始的阈值点。当土壤距离润湿面较远时,这些阈值点出现在较高的吸力下。还通过释放活塞并允许20%的有限轴向膨胀模拟了储藏通道中轴向约束元件的失效。在活塞释放时和在自由轴向膨胀期间,径向膨胀压力急剧下降。发现从底部到顶部的溶胀压力梯度在底部具有较高的值。基于溶胀压力曲线估计密度梯度。

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