考虑复杂波场影响的重力坝随机地震响应分析

RANDOM SEISMIC RESPONSE ANALYSIS OF GRAVITY DAM CONSIDERING INFLUENCE OF COMPLEX WAVEFIELD

  • 摘要: 针对重力坝随机地震响应分析尚未有效考虑复杂波场影响的问题,该文提出场址波场的随机模拟方法并对重力坝的随机地震响应开展研究。为确保入射波对场地的代表性,以场地谱为目标完成复杂入射波场的生成和调整。采用非一致波动输入模型实现考虑地基辐射阻尼的复杂波场输入,并以向家坝工程左岸非溢流坝段为例给出复杂波场影响下的重力坝随机地震响应分析成果。结果显示,波场随机模拟方法可提供适合重力坝随机地震响应分析需要的波场信息。在设计峰值地震动对应的随机波场影响下,向家坝非溢流坝段的坝踵第一主应力峰值均值为1.93 MPa,均方差为0.594 MPa,变异系数0.307;下游坝面的第一主应力峰值均值为1.37 MPa,均方差为0.336 MPa,变异系数0.257。算例中坝踵第一主应力峰值的变化范围为1.02 MPa~2.95 MPa,依据正态分布得到坝踵单元受拉破坏的概率为0.281%。

     

    Abstract: Complex wavefields are not effectively considered in the random seismic response analysis of high-gravity dams. The random wavefield method generating the incident waves at the project site is proposed and the random seismic response analysis of the gravity dam is performed in this paper. To ensure the representativeness of the wavefield to site conditions, the wave information is generated and adjusted by comparing the response spectrum of the corresponding horizontal acceleration’s response spectrum at the reference point and the target spectrum. The non-uniform wave input method is utilized to realize the input of complex wavefields and the radiation damping of the foundation. A non-overflow dam section in Xiangjiaba gravity dam is chosen as an example to perform investigations considering the complex wavefield. The results show that the random wavefield method can provide incident waves fit for random seismic response analysis of gravity dams. Under the influence of complex wavefield corresponding to the design ground acceleration, the mean peak of major principal stress at the dam heel is 1.93 MPa, with the MSE 0.594 MPa and the variation coefficient 0.307. The mean peak of major principal stress at the downstream slopeface is 1.37 MPa, with the MSE 0.336 MPa and the variation coefficient 0.257. In these cases, the peaks of major principal stress at the dam heel are from 1.02 MPa to 2.95 MPa, which indicates that the failure probability of the dam heel element is 0.281%, according to the normal distribution of peak response.

     

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