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Site Response in a Layered Liquefiable Deposit: Evaluation of Different Numerical Tools and Methodologies with Centrifuge Experimental Results

机译:分层可液化矿床中的场地响应:带有离心机实验结果的不同数值工具和方法的评估

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Results of a centrifuge experiment simulating seismic site response in a layered level liquefiable soil profile are used to evaluate and systematically compare the predictive capabilities of two common numerical platforms and two classes of advanced soil constitutive models (multiyield and bounding surface) used by three different teams. The pressure-dependent multiyield (PDMY02) and simple anisotropic SAND (SANISAND) constitutive models, implemented in open source and commercially available software, were independently calibrated by three teams using the same set of monotonic and cyclic triaxial test results. Class C predictions of the elastoplastic soil response in centrifuge following verification and initial calibration showed excessive dilative tendencies in all constitutive models to different degrees. These tendencies led to a notable overestimation of acceleration spikes at higher frequencies and an underestimation of net excess pore pressures in dense sand. The second calibration phase focused primarily on reducing soil's dilative tendencies to match centrifuge tests, even at the cost of slightly sacrificing aspects of the response at an element level or abandoning the number of cycles to liquefaction. Despite differences in calibration methodologies and priorities among three modelers, the results show that small element tests and centrifuge experiments do not always lead to the same calibrated soil parameters. Further, although current numerical platforms and advanced constitutive models were capable of reproducing many aspects of seismic site response observed in the centrifuge, they still need fundamental improvements to capture volumetric settlements. This is an old problem that needs attention in future numerical and physical model studies.
机译:在分层液化土壤剖面中模拟地震现场响应的离心实验结果用于评估和系统比较三个不同团队使用的两个常用数值平台和两类高级土壤本构模型(多屈服和边界面)的预测能力。由开源和可商购软件实现的压力相关多产(PDMY02)和简单各向异性SAND(SANISAND)本构模型由三支团队使用同一组单调和循环三轴测试结果进行了独立校准。验证和初始校准后,离心机中弹塑性土壤响应的C类预测表明,所有本构模型在不同程度上都有过度的膨胀趋势。这些趋势导致在较高频率下明显地高估了加速度峰值,并低估了稠密沙子中净超额孔隙压力。第二个校准阶段主要集中在降低土壤的膨胀趋势以匹配离心测试,甚至以稍微牺牲元素水平响应方面或放弃液化循环数为代价。尽管三个建模者在校准方法和优先级上存在差异,但结果表明,小元素测试和离心实验并不总是导致相同的校准土壤参数。此外,尽管当前的数值平台和先进的本构模型能够重现离心机中观察到的地震现场响应的许多方面,但它们仍需要进行根本的改进以捕获体积沉降。这是一个老问题,需要在以后的数值和物理模型研究中加以注意。

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