Investigating the Effect of Depth and Impedance of Foundation Rock in Seismic Analysis of Gravity Dams

IF 0.5 Q4 ENGINEERING, GEOLOGICAL International Journal of Geotechnical Earthquake Engineering Pub Date : 2014-07-01 DOI:10.4018/IJGEE.2014070101
S. G. Joshi, I. Gupta, L. R. Pattanur, P. Murnal
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引用次数: 1

Abstract

The inhomogenieties of the foundation can be modeled explicitly in standard FEM procedure, however, the results vary significantly with the extent of foundation block modeled and mechanism of applying the input earthquake excitation. The substructure approach provides mathematically exact solution but assumes average properties for the entire foundation as viscoelastic half space. This paper has carried out detailed investigations with varying impedance contrasts and different size of foundation block to show that the results, with suitably deconvoluted free-field ground acceleration time-history applied at the base of foundation block in the FEM approach, are in good agreement with the substructure approach. However, the other variants of the FEM approach may lead to erroneous and overestimated stresses in the dam body. As the foundation of gravity dams can generally be approximated as an equivalent homogeneous half-space, the more accurate and efficient substructure approach can be used to model the dam-foundation rock interaction (SSI) effects in most practical situations.
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重力坝地震分析中基岩深度和阻抗的影响研究
基础的非均质性在标准有限元程序中可以得到明确的模拟,但其结果与模拟的基础块的大小和输入地震激励的作用机制有很大的不同。子结构方法提供了精确的数学解,但假定整个基础的平均性能为粘弹性半空间。本文对不同阻抗对比和不同尺寸的基础块体进行了详细的研究,结果表明,有限元方法中对基础块体底部的自由场地加速度时程进行了适当的反卷积,结果与子结构方法吻合较好。然而,FEM方法的其他变体可能导致错误和高估坝体的应力。由于重力坝的基础通常可以近似为一个等效的均匀半空间,因此在大多数实际情况下,可以使用更精确和有效的子结构方法来模拟大坝-基岩相互作用(SSI)效应。
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来源期刊
CiteScore
1.90
自引率
25.00%
发文量
11
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