基于FLAC3D多裂隙模型的层状岩质边坡破坏特征及稳定性
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TU457

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国家自然科学基金(51474008,41472235);安徽省自然科学基金(1508085QE89)


Analysis of failure characteristics and stability of layered rock slope based on multi-fracture model of FLAC3D
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    摘要:

    采用FLAC3D多裂隙本构关系,建立层状岩坡平面破坏特征的各向异性数值分析模型。运用强度折减法,得出边坡安全系数与层间弱面倾角β、坡角α、坡高H以及岩体抗剪强度之间的关系,并采用灰色关联法给出了各因素对安全系数的影响程度。研究结果表明:顺倾向边坡,当β≤15°时,其破坏形式主要是拉裂-剪切-滑移破坏,滑面不沿层间弱面;当15°<β<α时,产生顺层滑移破坏;当β≥α时,坡顶处沿弱面滑移,坡角处弯折破坏。反倾向边坡,当β<50°时主要为压剪破坏,β较大时(β≥50°)为倾倒破坏。随着β的增大,顺倾向边坡的安全系数呈先减、后增、再减的趋势,且水平层状边坡的稳定性要高于直立边坡;反倾向边坡的安全系数变化趋势与顺倾向边坡相反。当β>α时,顺倾向边坡的稳定性要高于同倾角的反倾向边坡。顺倾向边坡,坡高对其稳定性影响最大,其次为弱面黏聚力和坡角,而弱面倾角和弱面摩擦角相对影响较小;反倾向边坡,各因素对其稳定性的影响程度依次为弱面摩擦角、坡角、坡高、弱面黏聚力和弱面倾角。

    Abstract:

    Using the FLAC3D multi-fracture constitutive relation, a numerical model of anisotropic failure characteristics of a layered rock slope was established. With the strength reduction method, the relationships between the slope safety coefficient and the interlayer weak plane dip angle β, slope angle α, slope height H, and shear strength of the rock mass were determined, and the impacts of various factors on the safety coefficient were investigated with the grey correlation method. Results show that for a bedding slope(with the slope direction consistent with the obliquity of the rock layer)at β ≤15°, damage is mainly caused by tensile cracking-shear-slippage failure, and a sliding surface does not occur along the interlayer weak plane; bedding slippage failure appears at 15°<β<α; and the top of the slope slips along the weak plane, and bending failure appears at the slope foot at β≥α. For a reverse slope(with the slope direction opposite to the obliquity of the rock layer), the compression-shear failure is the main failure mode at β<50°, and toppling failure appears when β is larger(β≥50°). With the increase of β, the safety coefficient of the bedding slope shows a tendency to decrease first, then increase, and then decrease again, and the stability of the horizontal layered slope is higher than that of the vertical one. The safety factor change tendency of the reverse slope is opposite to that of the bedding slope. In the case of β>α, the stability of the bedding slope is higher than that of the reverse slope at the same dip angle. For a bedding slope, the slope height has the greatest impact on the stability, followed by the cohesion of the weak plane and slope angle, and the influences of the dip angle and friction angle of the weak plane are relatively small; for a reverse slope, the influence of each factor on its stability is ranked by the friction angle of the weak plane, slope angle, slope height, and cohesion and dip angle of the weak plane.

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鲁海峰,姚多喜,胡友彪,等.基于FLAC3D多裂隙模型的层状岩质边坡破坏特征及稳定性[J].水利水电科技进展,2017,37(4):36-41.(LU Haifeng, YAO Duoxi, HU Youbiao, et al. Analysis of failure characteristics and stability of layered rock slope based on multi-fracture model of FLAC3D[J]. Advances in Science and Technology of Water Resources,2017,37(4):36-41.(in Chinese))

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  • 收稿日期:2016-07-20
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  • 在线发布日期: 2017-07-02
  • 出版日期: 2017-07-10