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Penetration Model for Installation of Skirted Foundations in Layered Soils

机译:层状土壤中裙式基础安装的渗透模型

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During installation of a skirted foundation, resistance to penetration is a combination of side and tip resistances. When penetrating a permeable soil unit, tip resistance in particular can be high but if seepage water flow from the outside to the inside of the skirted foundation exists, the pore water gradient will reduce the effective stresses and therefore also penetration resistance. Recent installation data from the field and laboratory suggest that this effect can also occur during installation in layered profiles. This paper presents a model that accounts for seepage flow in unlimited permeable layers that are overlain by one or several impermeable layers. The model assumes that seepage flow in the underlying sand layer is induced by an incremental lift of the internal soil plug, which enables the transfer of some of the differential pressure applied under the foundation lid to the bottom of the lifted soil plug. A single equation is proposed to calculate the critical suction number for layered soil conditions that can be used with an empirical model to calculate the reduction in penetration resistance. A calibration of the proposed equation for the critical suction number is carried out using an axis symmetrical finite-element model that uses a linear elastic soil model and assumes steady-state flow conditions. The calibration of the proposed equation for calculating the critical suction number was first carried out for a homogenous permeable soil. This was done to benchmark the model against previously published data. In a second step, the calibration was done for a layered profile and different flow boundary conditions. The proposed penetration model is demonstrated by back-calculating full-scale installations. The paper closes with a discussion of the main assumption of plug lift, and a simple model to evaluate the degree of plug lift is proposed.
机译:在安装裙式地基时,抗穿透性是侧部和顶部阻力的组合。当渗透到可渗透的土壤单元中时,尤其是尖端阻力可能很高,但是如果存在从裙状基础的外部向内部流动的渗水,则孔隙水梯度会降低有效应力,从而降低渗透阻力。来自野外和实验室的最新安装数据表明,在分层配置文件中安装期间也可能发生这种影响。本文提出了一个模型,该模型解释了一层或几层不可渗透层覆盖的无限渗透层中的渗流情况。该模型假设下面的砂层中的渗流是由内部土壤塞的增量提升引起的,这使得能够将施加在基础盖下的一些压差转移到提升的土壤塞的底部。提出了一个方程来计算分层土壤条件的临界吸力值,该方程可与经验模型一起使用,以计算抗渗透性的降低。使用轴对称有限元模型对建议的临界吸力数方程进行校准,该模型使用线性弹性土壤模型并假定为稳态流动条件。首先对均质的可渗透土壤进行了用于计算临界吸力值的拟议方程的校准。这样做是为了对照先前发布的数据对模型进行基准测试。第二步,针对分层轮廓和不同的流动边界条件进行校准。反向计算的完整安装量证明了建议的渗透模型。最后,本文讨论了柱塞举升的主要假设,并提出了一个简单的模型来评估柱塞举升的程度。

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