无锡地区考虑软土流变特性的水平向基床系数分析
Coefficient of horizontal sub-grade reaction considering rheological properties of soft soils in Wuxi region
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摘要: 无锡地区土层大部为软土,土体流变性较强,在深基坑工程施工过程中土压力及围护结构变形受时间、空间影响显著;基于室内不同应力路径粉质黏土流变试验结果,得出无锡地区粉质黏土的流变特性符合Kelvin三参数流变模型;以Kelvin模型为基础提出考虑软土流变特性的水平向基床系数的三参数修正模型;通过实测地连墙位移值反演水平向基床系数,反演分析表明水平向基床系数随施工工期的增加而变小,随土层埋深的增加而变大,最终趋于稳定值;并根据反演的水平向基床系数,确定三参数修正模型各参数的取值范围,进而得到无锡地区粉质黏土考虑流变特性的水平向基床系数修正公式,为深基坑的设计计算分析提供指导。Abstract: The most soil layers are soft soils and their rheology is stronger, so the earth pressure and deformation of retaining structures are significantly influenced by time and space during the construction process of deep foundation pit. It is derived that rheological properties of silty clay in Wuxi region accord with Kelvin rheological model with three parameters based on the rheological test results of silty clay under different stress paths. A modified model of three parameters for the coefficient of horizontal sub-grade reaction is proposed considering the rheological propertices of silty soils. The coefficient of horizontal sub-grade reaction is back analyzed through the measured displacement of diaphragm wall, and the analysis shows that the coefficient decreases with the increase of the construction period, but it increases with the increase of the buried depth of soil layers and finally tends to a stable value. The ranges of various parameters of the modified model are determined, and then a modified formula for the coefficient of horizontal subgrade reaction of silty clay is obtained considering the rheological properties in Wuxi region. The results may provide guidance for the calculation and analysis of the deep foundation pit.