丁树云, 毕庆涛. 2012: 地震强度对堆石坝变形的影响. 工程地质学报, 20(1): 30-36.
    引用本文: 丁树云, 毕庆涛. 2012: 地震强度对堆石坝变形的影响. 工程地质学报, 20(1): 30-36.
    DING Shuyun, BI Qingtao. 2012: IMPACT OF EARTHQUAKE INTENSITY ON DEFORMATION OF ROCK-FILL DAM. JOURNAL OF ENGINEERING GEOLOGY, 20(1): 30-36.
    Citation: DING Shuyun, BI Qingtao. 2012: IMPACT OF EARTHQUAKE INTENSITY ON DEFORMATION OF ROCK-FILL DAM. JOURNAL OF ENGINEERING GEOLOGY, 20(1): 30-36.

    地震强度对堆石坝变形的影响

    IMPACT OF EARTHQUAKE INTENSITY ON DEFORMATION OF ROCK-FILL DAM

    • 摘要: 采用基于状态相关的剪胀理论的临界状态砂土模型,以SUMDES2D为有限元平台,对直接建造在基岩上的心墙堆石坝进行了1组抗震性能计算,分析了坝体在不同的地震强度下的动力响应,以研究地震强度对土石坝变形机理的影响。计算结果表明,地震强度越大,地震所引发永久变形和局部变形就越大; 文中除了给出土石坝的总体位移及变形状况外,还提供了堆石坝在某些局部位置的应力路径和应力应变关系,探讨了不同地震强度下坝体破坏的内在机理。局部土单元的动力响应,揭示位于坝体上游坝坡马道附近单元由于密实度小,在应力不大的情况下就达到材料的临界状态,随着地震强度的增加,该部位由稳定逐步过渡到临界状态,而后沿着临界状态线发展,土单元由稳定逐步过渡到流动变形。

       

      Abstract: The anti-seismic performance of a rock-fill dam is not only determined by its geometry and composition,but also by the intensity of an earthquake to which the dam is subjected.Through critical state sand model cooperating with the concept of state-dependent dilatancy,a group of fully coupled finite element analyses of the response of a central core rock-fill Dam are presented for the study of the seismic performance.The numerical analysis is on the SUMDES2D platform.The dam was built directly on bedrock to earthquakes of different intensities.The dynamic response of the dam under earthquake intensity was analyzed.The calculation results show that,the bigger the earthquake intensity is,the larger the permanent deformation and local deformation would occur in the dam.The analysis provides not only the overall displacement and deformation of the dam,but also the stress path and stress-strain relationship of local soil unit.The inner destructive mechanism of the dam under different seismic intensities is also further discussed.The dynamic response of local soil unit illustrates whether the critical state of the dam is reached based on the site of the unit and its stress state.The soil units near the berm of upstream slope gradually achieve their critical state of the material as the earthquake intensity increases,and have a flow deformation.

       

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