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Model for the simulation of swelling-pressure measurements on expansive soils

机译:膨胀土上的膨胀压力测量模拟模型

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Numerous laboratory swelling tests have been reported for the measurement of swelling pressure and the amount of swell of an expansive soil. These test methods generally involve the use of a conventional one-dimensional oedometer apparatus. Few attempts, however, have been made to formulate a theoretical framework to simulate the testing procedures or to visualize the different stress paths followed when using the various methods. The simulation of the oedometer tests on expansive soils is required to fully understand the prediction of heave. The correct measurement of swelling pressure is required for an accurate prediction of heave. It is further anticipated that some information on unsaturated soils property functions may be approximated from the back-analysis of the data. A theoretical model is proposed to describe the pore-water pressures with time and depth in a specimen as well as the volume changes during various oedometer swell tests. The model is formulated based on equilibrium considerations, constitutive equations for an unsaturated soil, and the continuity requirement for the pore fluid phases. The transient water flow process is coupled with the soil volume change process. The model can be used to describe the volume-change behaviour, pore-water pressure, and vertical total stress development in an unsaturated soil during an oedometer test performed by any one of several test procedures. The model has been put into a finite element formulation using the Galerkin technique. All the parameters required to run the model can be obtained by performing independent, common laboratory tests. The proposed model was used to simulate the results from free-swell, constant-volume, constant water content, and loaded-swell oedometer tests. Computed values of volume change, vertical total stress, and pore-water pressure are in good agreement with measured values. [References: 29]
机译:已经报道了许多用于测量膨胀压力和膨胀土壤膨胀量的实验室膨胀试验。这些测试方法通常涉及使用常规的一维里程表设备。但是,很少有人尝试建立一个理论框架来模拟测试程序或可视化使用各种方法时遵循的不同应力路径。为了充分了解升沉的预测,需要对膨胀土上的里程表测试进行模拟。正确预测膨胀压力需要正确测量膨胀压力。还可以预料到,有关不饱和土壤特性函数的一些信息可以从数据的反分析中近似得出。提出了一个理论模型来描述样品中孔隙水压力随时间和深度的变化,以及在各种里程表溶胀试验期间的体积变化。该模型是基于平衡考虑,非饱和土的本构方程以及孔隙流体相的连续性要求而制定的。瞬态水流过程与土壤体积变化过程结合在一起。该模型可用于描述在通过多种测试程序中的任何一种进行的里程表测试期间,非饱和土壤中的体积变化行为,孔隙水压力和垂直总应力的发展。使用Galerkin技术将模型放入有限元公式中。运行模型所需的所有参数都可以通过执行独立的通用实验室测试来获得。所提出的模型用于模拟自由膨胀,恒定体积,恒定水含量和加载膨胀测压计测试的结果。体积变化,垂直总应力和孔隙水压力的计算值与测量值非常吻合。 [参考:29]

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