汶川地震对江口电站进水口边坡稳定性影响分析
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
汶川地震发生后,江口电站进水口边坡监测结果显示边坡表面位移较小,深层位移较大,但测斜仪位移分布曲线较光滑,且震后边坡位移变化较小,说明进水口边坡基本稳定。测斜仪位移分布曲线是否出现Z形突变,以及位移—时间过程线有无明显增长,可作为边坡稳定的依据。
The monitoring results of water-intake slope of Jiangkou Hydropower Station after Wenchuan Earthquake show that the surface displacement is small and the deep one is large,however,the displacement curve is smooth,and the variation of displacement is small,indicating that the water-intake slope is basically steady. Whether or not there occur Z-type mutation of displacement distribution curves and obvious increase of displacement-time curves can be used as the criterion for the slope stability.
引文
[1]何秀凤,贾东振,乐洋.基于卡尔曼滤波方法的高边坡变形分析与预测.水电自动化与大坝监测,2009,33(2):48-50.
    [2]郭永刚,苏克忠.从汶川大地震论水利工程强震安全监测.水电自动化与大坝监测,2009,33(3):56-59.
    [3]刘康.锦屏一级水电站左岸高边坡变形监测设计及成果初步分析.水电自动化与大坝监测,2008,32(3):64-67.
    [4]方大勇.边坡长期监测中测斜仪测量数据的修正.水电自动化与大坝监测,2006,30(4):56-58.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心