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Several Comments on Influence Zone Depth Progress in Deep Hole Foundations

机译:关于深孔地基影响区深度进展的几点评论

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The paper presents analytical and numerical approaches to the evaluation of the depth of the influence zone; the term influence zone is assigned to the region where the load has substantial influence on the deformation of the soil skeleton. The approach relies on the analytical solution based on the analysis of Westergard subspace assuming elastic material response. The depth of the influence zone must also be taken into account in the back analysis of the soil parameters, e.g. the deformation modulus. The necessity of this is shown by rigid plate field load tests. The standard back analysis based on the Boussinesq half space theory provides unreal data when the load of the plate is not sufficient and the depth of influence zone is small. It is caused by geostatic stress. Due to excavation (e.g. in the deep hole) the soil is significantly over-consolidated and the small surcharge deforms only thin upper layer of the subsoil. Boussinesq formula should be accepted if the depth of influence zone reaches approximately two and half times higher than width of footing.
机译:本文提出了影响区域深度评估的分析和数值方法。 “影响区”一词指的是载荷对土壤骨架变形有实质性影响的区域。该方法基于假设弹性材料响应的基于Westergard子空间分析的解析解决方案。在对土壤参数进行反分析时,例如变形模量。刚性板的现场载荷试验表明了这一点的必要性。当板的载荷不足且影响区域的深度较小时,基于Boussinesq半空间理论的标准反分析将提供不真实的数据。它是由地应力引起的。由于开挖(例如在深孔),土壤明显过度固结,少量的过剩物仅使地下土壤的薄上层变形。如果影响区的深度达到基础宽度的两倍左右,则应采用Boussinesq公式。

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