考虑流固耦合的拱坝动力分析

Tecnia Pub Date : 2022-08-08 DOI:10.21754/tecnia.v32i2.1376
Yoshi Raul Vela Calderón, Hugo Victor Luis Scaletti Farina
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引用次数: 0

摘要

拱坝失效的社会、经济和环境后果使得评估其动态响应以降低灾害风险至关重要。由于这些大坝的细长性和灵活性往往会增加地震期间的流体-结构相互作用,因此本工作比较了秘鲁北部Marañón河假设拱坝在满库和空库条件下的动力响应。使用三种公式来估计流体动力学压力:韦斯特加德的附加质量、欧拉和拉格朗日。这些比较是针对不同发震源的地震进行的,这些地震以前与重现期为10000年的统一危险谱相匹配。在COMSOL Multiphysics软件中,使用有限元方法推导了大坝-水库-地基系统的地震需求,在假设大坝和地基域的线弹性行为的情况下,采用无质量地基方法进行时程分析,忽略了波浪在地基中传播的影响,但考虑了其刚度。结果表明,拉格朗日公式和欧拉公式产生了相似的地震需求,而韦斯特加德的附加质量公式是保守的。满储层条件通常会增加地震需求,但结果将取决于为流体假设的边界条件和地震特征等因素。与相同的统一危险谱相匹配的地震不一定会产生相同的动力响应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dynamic analysis of arch dams considering fluid-structure interaction
The social, economic, and environmental consequences of the failure of an arch dam make it essential to evaluate its dynamic response to mitigate the risk of a disaster. Since the slenderness and flexibility of these dams tend to increase the fluid-structure interaction during an earthquake, this work compares the dynamic response of a hypothetical arch dam in the Marañón river, in northern Perú, for both full and empty-reservoir conditions. Three formulations were used to estimate the hydrodynamic pressures: Westergaard’s added mass, Eulerian and Lagrangian. The comparisons were performed for earthquakes of distinct seismogenic sources, previously matched to a uniform hazard spectrum with a return period of 10000 years. The finite element method was used to derive the seismic demands of the dam-reservoir-foundation system in COMSOL Multiphysics software, carrying out time-history analyses assuming linear elastic behavior of the dam and foundation domains and a massless foundation approach, ignoring the effect of waves propagation in the foundation but considering its stiffness. The results show that the Lagrangian and Eulerian formulations produce similar seismic demands, while Westergaard’s added mass formulation is conservative. The full-reservoir condition generally increases the seismic demands, but the results will depend on the boundary conditions assumed for the fluid and the characteristics of the earthquake, among other factors. Earthquakes matched to the same uniform hazard spectrum do not necessarily produce equal dynamic responses.
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