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Experimental Study on Volume Change Indices of Bentonite Soils

机译:膨润土土壤体积变化指标的试验研究

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This paper reports experimental results regarding statically compacted clay specimens to study the volume change behavior of bentonites. The volume change indices such as the coefficients of compressibility, volume compressibility, and consolidation (i. e. a_v, m_v and c_v respectively) and the saturated coefficient of permeability k at different surcharge pressures were determined with the commonly adopted procedures. The swell potentials, swelling pressures, different phases of the swollen specimens were analyzed for the volume change behavior during compression. Experimental results revealed that the swell potential is dependent on the initial dry density, the initial water content and the vertical pressure at which the clay specimens were allowed to swell. The swelling pressure was found to be similar for the specimens with varying water content, showing strong dependency on the initial void ratio. The compression indices (viz. m_v and a_v ) of saturated specimens decreased with an increase in the vertical pressure. About 80% to 90% of the volume change occurred in the primary compression phase under any given vertical pressure. The coefficient of consolidation c_v and the saturated coefficient of permeability k decreased with an increase in the vertical pressure.
机译:本文报道了有关静态压实粘土样品的实验结果,以研究膨润土的体积变化行为。体积变化指数,例如可压缩性,体积可压缩性和固结系数(分别为a_v,m_v和c_v)和在不同附加压力下的渗透率饱和系数k是通过常用程序确定的。分析了膨胀电位,膨胀压力,溶胀样品的不同相在压缩期间的体积变化行为。实验结果表明,膨胀势取决于初始干密度,初始含水量和允许粘土试样膨胀的垂直压力。发现具有变化的水含量的样品的溶胀压力相似,显示出对初始空隙率的强烈依赖性。饱和试样的压缩指数(即m_v和a_v)随垂直压力的增加而降低。在任何给定的垂直压力下,大约80%至90%的体积变化发生在主压缩阶段。固结系数c_v和饱和渗透系数k随着垂直压力的增加而减小。

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