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Re-examination of Undrained Strength at Atterberg Limits Water Contents

机译:重新检查阿特伯格的排水强度会限制水含量

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Most of the testing procedures to determine liquid limit and plastic limit are strength based with the assumption that, irrespective of the soil type, the strengths at these limiting water contents are considered to be unique, being equal to 1.7 and 170 kN/ m~2, respectively. Based on this, the plastic limit has been redefined as the water content at which there is a 100-fold increase in undrained strength as compared to that of liquid limit water content, and the range of water contents producing this strength variation as the plasticity index. However, published data from the various literature sources clearly show that the variation of undrained shear strength at the liquid limit water content is observed to be nearly sixty times, and that at plastic limit is more than seventeen times, and hence, no.unique value of undrained strength can be assigned either at the liquid limit or plastic limit of soils. The variation of undrained strength with water content has been well documented in literature. Thus, uniqueness of strength at liquid limit or plastic limit, which is nothing but water holding capacity of soils at different state of consistencies, is not tenable.
机译:确定液体极限和塑性极限的大多数测试程序都是基于以下假设得出的强度:与土壤类型无关,这些极限含水量的强度被认为是唯一的,分别等于1.7和170 kN / m〜2 , 分别。基于此,塑性极限被重新定义为与液态极限水含量相比不排水强度增加100倍的含水量,而产生该强度变化的含水量范围作为可塑性指标。但是,来自各种文献来源的公开数据清楚地表明,在液体极限含水量下不排水的剪切强度的变化约为60倍,在塑性极限处则大于17倍,因此没有唯一值不排水强度的最大值可以指定为土壤的液体极限或塑性极限。不排水强度随含水量的变化已在文献中有充分的文献记载。因此,在液体极限或塑性极限下强度的唯一性,即在不同稠度状态下的土壤的持水能力,是站不住脚的。

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