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Numerical Simulation of Earthquake Induced Soil Liquefaction: Validation against Centrifuge Experimental Results

机译:地震作用下土壤液化的数值模拟:对离心机实验结果的验证

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Two centrifuge tests were performed at the University of Colorado Boulder to fundamentally evaluate site performance and soil-foundation-structure-interaction (SFSI) on uniform, medium-dense, saturated sand undergoing a range of broadband earthquake motions with different characteristics. The test results were also used to evaluate and quantify the capability of a state-of-the-art numerical tool in capturing the key response parameters of interest, such as excess pore pressures, accelerations, and settlements at key locations. In this paper, the experimentally measured and numerically computed excess pore pressures and accelerations within the soil in free-field and under the foundation are compared, showing reasonable agreement (with residuals in spectral accelerations and Arias Intensities ranging from -1.5 to 1). Neither experimental nor numerical results indicated a decrease in foundation accelerations compared to the free-field soil at higher frequencies, which is due to a larger degree of excess pore pressure generation and strength loss in the free-field compared to the soil under the confining pressure of the structure.
机译:在科罗拉多大学博尔德大学进行了两次离心机测试,从根本上评估了均匀,中密集,饱和砂的均匀,中致饱和砂的地点性能和土壤基础结构 - 相互作用(SFSI)进行了一系列宽带地震动作,具有不同的特点。测试结果还用于评估和量化最先进的数值工具在捕获关键响应参数时的能力,例如在关键位置处的过度孔隙压力,加速度和沉降。在本文中,比较了自由场和基础下土壤中的实验测量和数值计算的过度孔隙压力和加速度,显示了合理的一致性(具有差异频谱加速度的残留物,并且arias强度范围为-1.5至1)。与在较高频率下的自由场土壤相比,实验性和数值结果均未表明基础加速度降低,这是由于在限制压力下与土壤相比,自由场的过度孔隙压力和强度损失是由于较大程度的孔隙压力结构。

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