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Research on Consolidation of Saturated Hard Clay

机译:饱和硬粘土巩固研究

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The study has carried out on the variation of pore graduation and compression volume (s) of hard clay with time (t) based on the Terzaghi Theory, We classified the pores in hard clay and the porewater in them into three types. The compression volume (s) shows periodicity with the time of consolidation. The boundary of the periods is a critical point. The consolidation rate is high at the beginning of each period, but getting slower with time, which we call it a consolidation cycle. The compress volume (s) shows correlatively with time by the form of Tcrzaghi Theory. But the s-t curve obtained by omitting the cycles does not fit with Terzaghi's theoretical curve well. The practical observation data of subsidence show that the consolidation parameters obtained by consolidation cycles are more approximate to actual conditions, with 10-20 times precision than that got from traditional soil tests. By the analysis of hard clay structure and evolution environment, we found that the occurrence of pores which results from the difference of evolution or environment.
机译:该研究已经基于Terzaghi理论的时间(T)的硬粘土的孔隙梯度和压缩体积的变化进行了研究,我们将硬粘土中的毛孔分为三种类型。压缩体积显示与整合时间的周期性。周期的边界是一个关键点。整个期间的整合率高,但随着时间的推移,我们越来越慢,我们称之为整合周期。压缩体积通过TCRZAGHI理论的形式与时间相关。但通过省略周期获得的S-T曲线不适合Terzaghi的理论曲线。沉降的实际观察数据表明,通过整合循环获得的整合参数更近似于实际条件,精度超过传统土壤测试的精度10-20倍。通过对硬粘土结构和演化环境的分析,我们发现孔隙的发生,从进化或环境的差异导致。

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