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491.
将地基视为多层各向同性弹性体,对Euler-Bernoulli梁进行有限单元离散分析,对地基-梁接触面采用边界积分法求解,根据地基-梁接触面的竖向位移协调和光滑接触条件,应用有限元与边界元耦合的方法推导出各向同性成层弹性地基上的Euler-Bernoulli梁的半数值半解析解。基于文中理论,编制了相应的程序,通过与现有文献对比,验证了文中理论的正确性,对比分析了分层地基与等效均匀地基两种模型上的弹性地基梁。研究结果表明,分层地基与等效均匀地基两种模型上弹性地基梁性状差异较大,实际弹性地基梁计算中应采用分层地基模型。 相似文献
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考虑裂隙非饱和膨胀土边坡入渗模型与数值模拟 总被引:19,自引:0,他引:19
包含裂隙的非饱和膨胀土中的渗流具有随时间变化的特性。采用常规试验测定非饱和膨胀土膨胀时程曲线,定量地描述了膨胀土中裂隙在入渗过程中逐渐愈合的特征, 建立了考虑裂隙的非饱和膨胀土边坡入渗的数学模型;用有限元数值模拟方法分析了边坡地形、裂隙位置、裂隙开展深度及裂隙渗透特性等对边坡降雨入渗的影响。结果表明, 坡上位置的裂隙对边坡入渗影响较大;裂隙对边坡入渗的影响随裂隙深度的增大而增大,且存在一最大的影响程度;裂隙的存在加快了膨胀土的入渗速率;考虑裂隙随入渗而愈合时, 入渗达到平衡的时间有所延长。 相似文献
496.
砂井地基固结的三维有限元模型及应用 总被引:2,自引:0,他引:2
一维和二维的数值方法对刻画砂井地基的固结都不够准确和全面,但砂井密集地基的完全三维耦合模拟难度比较大。在对称性原理和Biot固结理论基础上,对三维渗流-二维变形的有限单元方法(PDSS法)进行了改进,给出了砂井地基经济合理的三维剖分方案,使PDSS模型能够直接刻画正三角形布局的砂井。砂井重新布置到节点上而非处理成单元,原模型计算中砂井附近径向流的偏离也得到修正。改进的PDSS模型还与反求参数的方法相结合,用于真空联合堆载预压下砂井路基固结变形的工程模拟。 相似文献
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《地震研究进展(英文)》2022,2(4):100170
Soils with spatial variability are the product of natural history. The mechanical properties tested by soil samples from boreholes in the same soil layer may be different. Underground structure service in surrounding soils, their seismic response is controlled by the deformation of the surrounding soils. The variability of soil mechanical parameters was not considered in the current research on the seismic response of underground structures. Therefore, a random field model was established to describe the spatial variability of surrounding soils based on the random field theory. Then the seismic response of underground structures in the random field was simulated based on the time-domain explicit global FEM analysis, and the soil mechanical parameters and earthquake intensity influencing the seismic response of surrounding soils and underground structures were studied. Numerical results presented that, the randomness of soil parameters does not change the plastic deformation mode of surrounding soils significantly. The variation coefficients of inter-story deformation of structures and lateral deformation of columns are much smaller than that of mechanical parameters, and the randomness of soil parameters has no obvious effect on the structural deformation response. 相似文献
499.
Combination of FEM and CMA‐ES algorithm for transmissivity identification in aquifer systems
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In this paper, we propose a coupling of a finite element model with a metaheuristic optimization algorithm for solving the inverse problem in groundwater flow (Darcy's equations). This coupling performed in 2 phases is based on the combination of 2 codes: This is the HySubF‐FEM code (hydrodynamic of subsurface flow by finite element method) used for the first phase allowing the calculation of the flow and the CMA‐ES code (covariance matrix adaptation evolution strategy) adopted in the second phase for the optimization process. The combination of these 2 codes was implemented to identify the transmissivity field of groundwater by knowing the hydraulic head in some point of the studied domain. The integrated optimization algorithm HySubF‐FEM/CMA‐ES has been validated successfully on a schematic case offering an analytical solution. As realistic application, the integrated optimization algorithm HySubF‐FEM/CMA‐ES was applied to a complex groundwater in the north of France to identify the transmissivity field. This application does not use zonation techniques but solves an optimization problem at each internal node of the mesh. The obtained results are considered excellent with high accuracy and fully consistent with the hydrogeological characteristics of the studied aquifer.However, the various numerical simulations performed in this paper have shown that the CMA‐ES algorithm is time‐consuming. Finally, the paper concludes that the proposed algorithm can be considered as an efficient tool for solving inverse problems in groundwater flow. 相似文献
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