董雪, 刘文连, 徐则民. 2013: 缓倾坡内层状岩质高边坡稳定性分析以黄桷湾危岩高边坡的主斜坡为例. 工程地质学报, 21(4): 619-625.
    引用本文: 董雪, 刘文连, 徐则民. 2013: 缓倾坡内层状岩质高边坡稳定性分析以黄桷湾危岩高边坡的主斜坡为例. 工程地质学报, 21(4): 619-625.
    DONG Xue, LIU Wenlian, XU Zemin. 2013: STABILITY ANALYSIS OF HIGH ROCK SLOPE WITH GENTLE BEDDING DIP AT HUANG JUEWAN. JOURNAL OF ENGINEERING GEOLOGY, 21(4): 619-625.
    Citation: DONG Xue, LIU Wenlian, XU Zemin. 2013: STABILITY ANALYSIS OF HIGH ROCK SLOPE WITH GENTLE BEDDING DIP AT HUANG JUEWAN. JOURNAL OF ENGINEERING GEOLOGY, 21(4): 619-625.

    缓倾坡内层状岩质高边坡稳定性分析以黄桷湾危岩高边坡的主斜坡为例

    STABILITY ANALYSIS OF HIGH ROCK SLOPE WITH GENTLE BEDDING DIP AT HUANG JUEWAN

    • 摘要: 黄桷湾危岩高边坡是泥岩和砂岩呈类似夹心饼干状软硬互层结构、缓倾坡内的岩质高切坡。危岩高边坡除坡顶的陡崖处厚层砂岩发生崩塌失稳外,主斜坡体下部还存在局部的切层失稳。为确保高边坡下部的工程建设的顺利开展和居民的安全,采用数值模拟的方法对高边坡的主斜坡进行稳定性评价,选取天然自重和地震动荷载两种工况进行分析。计算结果表明:(1)主斜坡岩体在两种工况下仍处于稳定状态,但在地震动荷载作用下稳定系数下降显著; (2)陡崖和主斜坡接触带附近及主斜坡坡脚处应力集中现象明显,发生破坏的可能性更大; (3)主斜坡潜在滑移面位于坡内中深部,剪出口位置可能位于主斜坡的坡脚处。

       

      Abstract: Huang Juewan high-steep rock slope is composed by mudstone and sandstone. The rock beddings are similar to the cookies.They have soft and hard layers with gentle dip layered structure. The high-steep slope in addition to the top of the steep cliff in thick sandstone occurred collapses. Outside the instability main slope body bottom, there are local cutting layer instability. To ensure a smooth start of the lower part of high slope and the safety of the residents, this paper uses the method of numerical simulation on the high slope of the stability evaluation. The paper selects the natural dignity and seismicity load as the two conditions for slope stability analysis. The results show that:(1)Main slope rock mass in the two kinds of working conditions is still in the stable state; but seismic loads slope stability reduced significantly influence; (2)Steep cliff and main slope near the contact zone and the ramp slope foot place obvious stress concentration phenomenon more likely to damage; (3)the potential sliding surface of slope is located in the central slope. The cut points may be located at the slope toe.

       

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