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Stress induced time dependent behavior of clayey soils

机译:黏土的应力诱导时间相关行为

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It is shown that time compression curve obtained from one-dimensional consolidation curve in the laboratory may include six phases. These are initial compression, first primary compression, transition from first primary compression to second primary compression, second primary compression, and transition from second primary compression to creep and lastly creep. This paper attempts to identify the quantitative beginnings and characteristics of these phases. A mathematical characteristic of all the soils that follow primary consolidation as per Terzaghi's one dimensional consolidation theoryrnis derived. It is known as the constant of primary consolidation. It is used to study the beginning of secondary consolidation and its effects on primary consolidation. Another characteristic of soils for creep and total absence of primary compression is derived. Methods are suggested for the determination of coefficients of Primary and Secondary consolidations and the compression index.
机译:结果表明,在实验室中从一维固结曲线获得的时间压缩曲线可能包括六个阶段。这些是初始压缩,第一主压缩,从第一主压缩到第二主压缩的过渡,第二主压缩以及从第二主压缩到蠕变和最后蠕变的过渡。本文试图确定这些阶段的定量起点和特征。根据Terzaghi的一维固结理论得出的所有固结后的土壤的数学特征。它被称为主要合并的常数。它用于研究次级合并的开始及其对初级合并的影响。得出了土壤蠕变和完全没有一次压缩的另一特性。建议使用方法来确定主要和次要固结系数以及压缩指数。

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