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Numerical investigation of the influence of non-uniform factors on the monotonic/cyclic behaviour of coarse-grained soil

机译:非均匀因素对粗粒土单调/循环行为影响的数值研究

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Coarse-grained soil (CGS) has been extensively used in engineering practices because of their advantages of relatively high strength, easy compaction and small deformation. In engineering design, CGS is usually regarded as a non-liquefiable soil. However, many post-earthquake surveys have shown that CGS, such as sandy gravel, can be seriously liquefied, meaning that under certain seismic loads, CGS with loose to moderate densities might have the potential to be liquefied. In this study, soil-water coupling finite difference-finite element (FD-FE) deformation analyses, based on the cyclic mobility (CM) model, were conducted to investigate the monotonic and cyclic characteristics of CGS. The model can accurately describe the complicated mechanical behaviour of CGS, considering the influences of the stress-induced anisotropy, the density and the naturally deposited structure of soils in a unified way. The material parameters of CGS were calibrated by large-scale triaxial tests. Particularly, the influences of non-uniform factors on the element behaviour of CGS subjected to monotonic/cyclic loading were systematically studied, such as the gravitational stress field (GSF) of the specimens, the friction between the loading plate and specimen (FLPS), the confining pressure, the cyclic shear stress ratio (CSR), and the loading frequency, etc. It is found that the CM model can reproduce the stress-strain-dilatancy relation of CGS in the (CU) over bar and CD tests well and that the GSF and FLPS have a certain impact on the element behaviour of CGS. However the average value results from the numerical simulations can quantitatively and qualitatively describe the monotonic/cyclic mechanical behaviour. In addition, under lower confining pressure or higher CSR, the non-uniform distribution of volumetric and axial strain inside the specimen will be prominent, and the specimen enters the cyclic-mobility stage more easily. High loading frequency and CSR will cause a large distortion of the specimen, at which point the element test, strictly speaking, is no longer an element test.
机译:粗粒土(CGS)具有相对较高的强度,易于压实和较小变形的优点,因此已广泛用于工程实践中。在工程设计中,CGS通常被认为是不可液化的土壤。但是,许多地震后的调查表明,沙砾等CGS可以被严重液化,这意味着在一定地震荷载下,松散到中等密度的CGS可能被液化。在这项研究中,基于循环迁移率(CM)模型,进行了水-水耦合有限差分-有限元(FD-FE)变形分析,以研究CGS的单调和循环特性。该模型可以综合考虑应力引起的各向异性,土壤的密度和自然沉积结构的影响,准确地描述CGS的复杂力学行为。 CGS的材料参数通过大规模三轴测试进行了校准。特别是,系统地研究了非均匀因素对单调/循环荷载作用下CGS元素行为的影响,例如试样的重力应力场(GSF),荷载板与试样之间的摩擦力(FLPS),围压,循环剪应力比(CSR)和加载频率等。发现CM模型可以很好地再现C和CGS在钢筋和CD试验中的应力-应变-剪胀关系,并且GSF和FLPS对CGS的元素行为有一定影响。但是,数值模拟的平均值结果可以定量和定性地描述单调/循环机械行为。此外,在较低的围压下或较高的CSR下,样品内部的体积和轴向应变的不均匀分布会很明显,并且样品更容易进入循环运动阶段。高加载频率和CSR会导致样品变形大,从严格意义上讲,此时元素测试不再是元素测试。

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