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MATHEMATIC-MECHANIC RESEARCH ON THE INFLUENCE OF THE SHUITIANBA FAULT BY THE STRESS FIELD OF THE THREE-GORGE RESERVOIR

机译:三峡库区应力场对疏水界缺失影响的数学 - 机修工研究

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According to the fundamental theory of Hydraulic Stress Field formed by full-storage reservoir, the math-mechanic model is set up. It shows that there is a certain effect on the Fault with the plane range of 5-6 km along the fault zone. Acted by this hydraulic stress field, both walls of the fault are all in condition of compressive stress. The stress increases with depth from zero on the surface. In view of the relationship of the magnitude of stress with expanding depth of the fault, the stress value on its top and foot walls produced by the hydraulic stress field is far higher than that measured in this area, so that is bearable by the fault. The hydraulic stress field brings about a floating support effect to Shuitianba Fault and surrounding rock where the surface displacement is no more than 10 mm and reduced with the increasing depth. Additionally, the top and foot walls of the fault exist clearly a tendency of displacement discontinuity and compressive deformation. After Three-Gorges Reservoir full storage, it is impossible to cause a moderate strong seismicity by a considerable from Shuitianba Fault under a hydraulic stress field condition to give influence to the Three-Gorges Project.
机译:根据全储存储层形成的液压应力场的基本理论,建立了数学机械模型。它表明,沿着断层区域的平面范围为5-6 km的故障存在一定的效果。由该液压应力场作用,故障的两个壁都处于压缩应力的条件下。压力随深度从表面上的深度增加。鉴于膨胀深度的压力幅度的关系,由液压应力场产生的顶部和脚壁上的应力值远远高于该区域中测量的脚壁,因此可以通过故障进行任何可容纳。液压应力场为浮动支撑效果带来了潮汐支撑效果,以及表面位移的围岩岩体不超过10mm,随着深度的增加而减小。另外,故障的顶部和脚壁清楚地存在位移不连续性和压缩变形的趋势。在三峡库尔储存器全储存后,不可能通过在液压应力场条件下从SHINIANBA故障相同地引起适度的强烈地震性,以对三峡工程产生影响。

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