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Influence of the water pressure distribution along crack faces on seismic fracture modeling of a dam-reservoir-foundation system

机译:裂缝面水压分布对大坝-水库-基础系统地震裂缝模拟的影响

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摘要

Hydraulic fracturing of concrete dams subjected to strong earthquakes can be a great hazard, yet the water pressure inside cracks lacks prior investigation. A numerical model based on the polygon scaled boundary finite element method (SBFEM) is proposed to investigate the influence of the water pressure distribution along crack faces on the crack propagation process in a gravity dam during earthquakes. A transient water pressure model that considers the effects of the reservoir head, crack mouth opening displacement, opening/closing velocity of the crack, and relative roughness of the crack faces is utilized. Additionally, contact elements are introduced to avoid possible overlapping of crack faces. The dam-reservoir-foundation dynamic interaction is simulated using a formulation based on the SBFEM, which effectively considers water compressibility, absorption of the reservoir sediments and radiation damping of the unbounded foundation. The numerical results show that the distributions of water pressure along crack faces in the dam under seismic loading are significantly different from those in the static case and can be much higher or lower than the static water pressure, depending on the opening or closing mode of the crack. Further, this difference in turn significantly increases the seismic response of the dam, which leads to longer cracks in the dam.
机译:遭受强烈地震的混凝土坝的水力压裂可能是一个巨大的危险,但裂缝内部的水压尚待事先调查。提出了一种基于多边形比例边界有限元法(SBFEM)的数值模型,研究了地震作用下重力面沿裂缝面的水压分布对裂缝扩展过程的影响。利用了一个瞬态水压模型,该模型考虑了油藏头,裂缝口张开位移,裂缝的开/关速度以及裂缝面的相对粗糙度的影响。另外,引入接触元件以避免裂纹面可能重叠。利用基于SBFEM的公式模拟了大坝-水库-基础动力相互作用,该公式有效地考虑了水的可压缩性,水库沉积物的吸收和无边界地基的辐射衰减。数值结果表明,地震荷载作用下大坝沿裂缝面的水压分布与静态情况有很大的不同,取决于水坝的开启或关闭方式,水压可以高于或低于静态水压。裂纹。此外,这种差异反过来会显着增加大坝的地震响应,从而导致大坝中的裂缝更长。

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