非均质土壤特性的实验观测

D. Muir Wood, G. V. Kumar
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引用次数: 38

摘要

对高岭土和粗粒均匀砂(d50~2mm)的混合物进行了三轴试验。对各向同性正常固结和超固结样品进行了排水和不排水压缩试验。已经发现,混合物的机械行为由粘土基质的机械行为主导,直到粘土含量降至40%以下,颗粒成分的体积分数达到约0.45。不排水试验中的孔隙压力不受沙子存在的影响。排水试验中粘土基质的体积应变与纯粘土中的体积应变几乎相同。使用为复合材料性能开发的理论分析计算了混合物的机械响应:发现该分析高估了颗粒材料的影响。使用有限元程序进行的数值分析更接近实验观测,但仍然高估了沙子的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Experimental observations of behaviour of heterogeneous soils

Triaxial tests have been performed on mixtures of kaolin clay and a coarse uniform sand (d50∼2 mm). Drained and undrained compression tests have been performed on isotropically normally consolidated and overconsolidated samples. It has been found that the mechanical behaviour of the mixture is dominated by the mechanical behaviour of the clay matrix until the clay content falls below 40 per cent and the volume fraction of the granular constituent reaches about 0.45. Pore pressures in undrained tests are unaffected by the presence of the sand. Volumetric strains in the clay matrix in drained tests are virtually identical to those seen in pure clay.

Calculations of mechanical response of mixtures have been made using a theoretical analysis, developed for the behaviour of composites: it is found that this analysis overestimates the effect of the granular material. Numerical analyses using a finite element program lie closer to the experimental observations but still overestimate the influence of the sand.

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