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One-Dimensional Consolidation Analysis of Saturated Soft Clay Based on Water Content Variation

机译:基于水含量变化的饱和软粘土的一维固结分析

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摘要

The degree of consolidation is an important parameter to evaluate the stability and consolidation effect of soft soil foundation. The degree of consolidation calculated by deformation often overestimates the actual degree of consolidation of soil, resulting in a large post construction settlement. To accurately reflect the actual consolidation degree of soil, based on Terzaghi's consolidation theory, this paper considers that the deformation amount to soil is equal to the volume of water discharged from the soil pores, and theoretically deduces the calculation method of soil consolidation degree with water content. The one-dimensional consolidation test was carried out by improving the test instrument. The results show that the degree of consolidation calculated by water content is smaller than that calculated by deformation in the same time. The pore pressure is calculated by inversion of the consolidation coefficient, which is close to the value of the pore pressure monitored by the test. It is found that there is a linear relationship between pore ratio and pore pressure (u). When the pressure is large, the e-lgu curve is approximately linear, and its slope can be used as an indicator to evaluate the difficulty of pore pressure dissipation.The research results have a certain theoretical value for revealing the consolidation change and development of soft clay.
机译:合并程度是评估软土基础的稳定性和固结效果的重要参数。通过变形计算的整合程度通常高估土壤的实际整合程度,导致大型后施工结算。为了准确反映土壤的实际整合程度,基于Terzaghi的整合理论,本文认为土壤的变形量等于从土壤孔隙排出的水量,并理论上推导了水的土壤固结度计算方法内容。通过改善测试仪进行一维固结试验。结果表明,通过含水量计算的固结程度小于通过同时变形计算的程度。通过固结系数的反转来计算孔隙压力,该固结系数接近通过测试监测的孔隙压力的值。发现孔比和孔隙压力(U)之间存在线性关系。当压力很大时,E-LGU曲线大致线性,其斜率可以用作评估孔隙压力耗散难度的指示。研究结果具有揭示柔软的整合变化和发育的某种理论价值粘土。

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