伍法权, 祁生文, 刘彤. 2007: 高地应力条件下边坡岩体卸荷变形的两种表现形式研究室. 工程地质学报, 15(S2): 60-67.
    引用本文: 伍法权, 祁生文, 刘彤. 2007: 高地应力条件下边坡岩体卸荷变形的两种表现形式研究室. 工程地质学报, 15(S2): 60-67.
    WU Faquan, QI Shengwen, LIU Tong. 2007: TWO TYPES OF UNLOADING DEFORMATION OF ROCK SLOPES UNDER HIGH GEOSTRESS CONDITION. JOURNAL OF ENGINEERING GEOLOGY, 15(S2): 60-67.
    Citation: WU Faquan, QI Shengwen, LIU Tong. 2007: TWO TYPES OF UNLOADING DEFORMATION OF ROCK SLOPES UNDER HIGH GEOSTRESS CONDITION. JOURNAL OF ENGINEERING GEOLOGY, 15(S2): 60-67.

    高地应力条件下边坡岩体卸荷变形的两种表现形式研究室

    TWO TYPES OF UNLOADING DEFORMATION OF ROCK SLOPES UNDER HIGH GEOSTRESS CONDITION

    • 摘要: 本文简要介绍了高地应力地区水电高边坡工程中人们十分关注的两个工程地质与岩石力学问题:锦屏一级水电站边坡大范围岩体卸荷松动和小湾导致坝基(肩)岩体开挖快速卸荷问题。作者认为锦屏一级水电站左岸边坡大范围松动变形仍然是自重和构造复合应力场卸荷作用的结果,边坡的规模大、坡度陡,以及高水平构造应力是导致大范围卸荷松动变形的重要因素;小湾电站坝基(肩)岩体开挖过程中出现的坚硬完整岩体板裂、拱裂和葱剥皮等一系列新破裂现象是在高地应力作用下,由于开挖导致垂直坡面应力卸荷,增大边坡表面岩体主应力差和剪应力而引起的快速破裂行为,并通过破裂完成了顺坡面的最大主应力的卸荷,卸荷破裂主要集中在开挖面附近5~6m深度范围内。

       

      Abstract: The paper briefly introduces two types of commonly concerned engineering geological and rock mechani-cal problems of high slopes in hydropower projects under high geostress,1. e.,the baffling large scale relax deform-anon of rock slope at the Jinping No. 1 hydropower station and the fast unloading fractures caused by dam foundation excavation at the Xiaowan hydropower station. The following opinions are presented:①the large scale relax de-formation of the slope at Jinping is actually the result of unloading of the composite stress field of gravity and tecton-is elements,and the large scale,steep slope and strong horizontal tectonic stress are the main factors to enlarge the range of relax deformation.②The phenomena such as thin-tabulate fractures,arciform broken-off andshallot-skin like fractures of fresh hard rock at the excavated surface of dam foundation are caused by unloading of 3 which is almost perpendicular to the slope surface,1. e.,the increase of the difference of principal stresses leads to the rapid failure of rock. As a feature of this kind of rapid unloading relax deformation,the new cracks concentrativelv distributed in the depth of 5~6m near the surface.

       

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