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REAPPRAISAL OF THE ACTIVITY OF CLAYS. ACTIVITY CHART

机译:重新评估粘土的活性。活动表

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References(34) The proposed activity chart, which aims to classify soils (425 μm) using the Atterberg limits, differs from the plasticity chart recently proposed by the author because the inorganic soils with platey clay minerals are classified (in addition to clay percentage) on the basis of their activity rather than on the degree of plasticity as a function of the liquid limit value, currently used by the standards. This is because soils that have the same liquid limit value may have very different characteristics because of both the amount and type of clay minerals contained in the soils. On the activity chart, the silt and the clay zones are subdivided (by two straight lines) in three new groups (low activity, medium activity and high activity) making it possible to classify inorganic soils with platey clay minerals (or their fraction) 425 μm on the basis of the amount and type of clay minerals they contain. The activity chart adapted to predict residual shear behaviour of cohesive soils is also shown. Finally, the distinction between coarse-grained soils and fine-grained soils based on their percentage of clay (2 μm), might be useful in characterizing and predicting soils' engineering behaviour.
机译:参考文献(34)拟议的活动图旨在利用Atterberg限值对土壤(<425μm)进行分类,它与作者最近提出的可塑性图不同,因为对具有板状粘土矿物的无机土壤进行了分类(除了粘土百分比)是根据其活性而不是根据标准当前使用的液体极限值决定其可塑性程度。这是因为具有相同的液体极限值的土壤可能具有非常不同的特性,因为土壤中所含的粘土矿物的数量和类型都如此。在活动图表上,粉砂和黏土区域(通过两条直线)细分为三个新的组(低活性,中活性和高活性),从而可以用板状粘土矿物(或其分数)对无机土壤进行分类。根据其所含粘土矿物的数量和类型为425μm。还显示了适用于预测粘性土壤残余剪切行为的活性图。最后,根据粗粒土和细粒土的粘土含量(<2μm)进行区分,可能有助于表征和预测土壤的工程行为。

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