首页> 外文期刊>Meccanica: Journal of the Italian Association of Theoretical and Applied Mechanics >Bridge-Pier Caisson foundations subjected to normal and thrust faulting: physical experiments versus numerical analysis
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Bridge-Pier Caisson foundations subjected to normal and thrust faulting: physical experiments versus numerical analysis

机译:承受正断层和推力断层的Bridge-Pier Caisson基础:物理实验与数值分析

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Surface fault ruptures can inflict serious damage to engineering structures built on or near them. In the earthquakes of Kocaeli, Chi-chi, and Wenchuan a number of bridges were crossed by the emerging normal or thrust faults suffering various degrees of damage. While piles have proved incapable of tolerating large displacements, massive embedded caisson foundations can be advantageous thanks to their rigidity. The paper explores the key mechanisms affecting the response of such bridge foundations subjected to dip-slip (normal or thrust) faulting. A series of physical model experiments are conducted in the National Technical University of Athens, to gain a deeper insight in the mechanics of the problem. The position of the caisson relative to the fault rupture is parametrically investigated. High-resolution images of the deformed physical model is PIV-processed to compute caisson displacements and soil deformation. A novel laser scanning technique, applied after each dislocation increment, reveals the surface topography (the relief) of the deformed ground. 3D finite element analyses accounting for soil strain-softening give results in accord with the physical model tests. It is shown that the caisson offers a kinematic constraint, diverting the fault rupture towards one or both of its sides. Depending on the caisson's exact location relative to the rupture, various interesting interaction mechanisms develop, including bifurcation of the rupture path and diffusion of plastic deformation.
机译:表面断层破裂会严重破坏其上或其附近的工程结构。在Kocaeli,Chi-chi和汶川地震中,许多桥梁被正在遭受不同程度破坏的正断层或逆冲断层所穿过。事实证明,桩不能承受大的位移,但大型的沉箱基础由于其刚性而具有优势。本文探讨了影响这种桥梁基础在倾滑(法向或推力)断裂作用下响应的关键机制。在雅典国立技术大学进行了一系列物理模型实验,以更深入地了解问题的机理。通过参数研究沉箱相对于断层破裂的位置。对变形后的物理模型的高分辨率图像进行PIV处理,以计算沉箱位移和土壤变形。在每次位错增量之后应用一种新颖的激光扫描技术,可以揭示变形地面的表面形貌(浮雕)。考虑到土壤应变软化的3D有限元分析得出的结果与物理模型测试一致。结果表明,沉箱提供了运动学上的约束,使断层破裂向其一侧或两侧转向。根据沉箱相对于破裂的确切位置,发展出各种有趣的相互作用机制,包括破裂路径的分叉和塑性变形的扩散。

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