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Shear strength of granitic residual soil in saturated and unsaturated conditions

机译:饱和和不饱和条件下花岗岩残留土壤的剪切强度

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Over the last 40 years there has been increasing interest in the mechanical behaviour (i.e. the shear strength and volume change behaviour) of unsaturated soils. However, there is still a lack of a good representative and comprehensive shear strength analytical model. Researchers have been trying to link the volume change behaviour to the shear strength; however there are still shortcomings in the existing frameworks. They have been developed from the standpoint of stress-strain behaviour. Thus, an experimental procedure for the laboratory test were performed by carrying out series of consolidated drained triaxial tests on saturated and unsaturated specimens of diameter 50mm and 100mm height. The test equipment involved a conventional and a double-walled triaxial cell, and the test material was granitic residual soil grade V. The results underlined the shear strength behaviour of the test material with respect to net stress and suction and showed a good match with the proposed shear strength model. It has been found that the apparent shear strength for unsaturated soil due to the force of suction exists and thus can increase the strength of the whole soil skeleton as shown and prove in the tabulated tables.
机译:在过去的40年中,不饱和土壤的机械行为(即剪切强度和体积变化行为)越来越兴趣。但是,仍然缺乏良好的代表性和综合剪切力量分析模型。研究人员一直试图将体积变化行为联系起来的剪切力量;然而,现有框架中仍有缺点。它们是从压力 - 应变行为的观点发展的。因此,通过在直径为50mm和100mm高度的饱和和不饱和标本上进行一系列固结的排水三轴试验来进行实验室试验的实验程序。测试设备涉及常规和双壁三轴细胞,测试材料是花岗岩残留的土壤级V.结果强调了测试材料相对于净应力和吸力的剪切强度行为,并与之匹配提出剪切强度模型。已经发现,由于抽吸力而导致的不饱和土的表观剪切强度存在,因此可以增加整个土壤骨架的强度,如图所示,并在制表的表中证明。

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