马昊,黄达,石林. 2020.基于断距-层厚特征统计的反倾边坡S型破坏演化数值模拟[J].工程地质学报,28(6):1160-1171. doi:10.13544/j.cnki.jeg.2019-042. DOI: 10.13544/j.cnki.jeg.2019-042
    引用本文: 马昊,黄达,石林. 2020.基于断距-层厚特征统计的反倾边坡S型破坏演化数值模拟[J].工程地质学报,28(6):1160-1171. doi:10.13544/j.cnki.jeg.2019-042. DOI: 10.13544/j.cnki.jeg.2019-042
    Ma Hao, Huang Da, Shi Lin. 2020. Numerical simulation of S-shaped failure evolution of anti-dip slope based on statistics of broken length and layer thickness[J]. Journal of Engineering Geology, 28(6): 1160-1171. doi: 10.13544/j.cnki.jeg.2019-042.
    Citation: Ma Hao, Huang Da, Shi Lin. 2020. Numerical simulation of S-shaped failure evolution of anti-dip slope based on statistics of broken length and layer thickness[J]. Journal of Engineering Geology, 28(6): 1160-1171. doi: 10.13544/j.cnki.jeg.2019-042.

    基于断距-层厚特征统计的反倾边坡S型破坏演化数值模拟

    NUMERICAL SIMULATION OF S-SHAPED FAILURE EVOLUTION OF ANTI-DIP SLOPE BASED ON STATISTICS OF BROKEN LENGTH AND LAYER THICKNESS

    • 摘要: 三峡库区巫峡龚家坊至独龙一带存在大量反倾不稳定边坡,多具有薄厚互层和软硬相间的岩体结构,边坡高度普遍在500 m以上。现场调查表明独龙7#边坡(D7)具有明显的“S”型柔性变形现象。为探明反倾边坡“S”型变形破坏机制,以独龙段反倾边坡为依托,从边坡的岩体结构调查、破坏模式概化、监测资料分析、变形破坏模拟等角度对软硬互层反倾高边坡的破坏机制进行研究。通过现场调查与无人机倾斜摄影,建立了边坡的三维模型,进而提取航拍数据,获得了岩层厚度、断距等的统计规律;基于断距-层厚统计规律,通过离散元软件UDEC对库水软化作用下D7边坡“S”型变形机理进行了模拟分析。研究表明:(1)独龙段边坡普遍具有陡倾内逆向层状结构,发育3组结构面,岩体被切割成块;(2)根据软岩占比,可将独龙段边坡分为2类:A类边坡软岩层占约20%,断距/层厚值分布于0.7~2.8区间,并集中于1.2~1.8;B类边坡软岩层占比约10%,断距/层厚值分布于0.5~3.3区间,并集中于0.6~1.5;A类边坡岩体长细比更大;(3)长期监测表明,边坡在库水位低值时位移量大,D7边坡位移持续增大,潜在整体失稳;(4)离散元模拟表明,边坡破裂面自坡脚延伸,中部硬岩区起到支撑并抑制上部变形的作用,边坡硬岩区与软岩区的差异变形以及变形体不同部位惯性的差异是导致岩层“S”型变形的主因,最终分别过“S”形岩层两个反弯点形成两条剪切带,形成自下而上的柔性弯曲-滑移型破坏。(5)断距-层厚比(S/T)可影响边坡破坏模式,比值越大,反折变形区与坡脚垮塌区越小,当S/T≥2时,S型变形不再发育。

       

      Abstract: There are many unstable anti-dip slopes in the Gongjiafang-Dulong section of the Three Gorges Reservoir area. These slopes are generally over 500 m high, and usually possess thin-thick interbedded and soft-hard interbedded structures. Field investigation show that D7 slope has obvious S-shaped flexible deformation. In order to further explore the mechanism of S-type toppling, this paper adopts the methods combining investigation, statistics, GPS monitoring and DEM simulation. Through field investigation and UAV tilt photography, a three-dimensional model of Dulong slope is established. And then through extracting the aerial data, the statistical laws of broken length and layer thickness are obtained. Based on the statistical laws, the S-type toppling mechanism of D7 slope under the action of reservoir water softening is simulated by the discrete element software of UDEC. The results show that:(1)Dulong slope has a steep anti-dipped layered structure, and three sets of structural planes cut the rock mass into blocks. (2)According to the proportion of soft rock, the Dulong slope can be divided into two types. The soft layer number of A-type slope account for about 20%, larger than that of B-type slopes with a proportion of 10%. The ratio of broken thickness and layer thickness(S/T) of A-type slopes is situated between 0.7 and 2.8 and concentrates on 1.2~1.8. The ratio of B-type slopes situates between 0.5 and 3.3 and concentrates on 0.6~1.5. (3)Long-term monitoring shows that the slope moving is larger when the reservoir water level dropping, and the continuously increasing displacement of the D7 slope makes it possible to lose integral stability. (4)The DEM simulation shows that the fracture surface extends from the slope toe, and the hard rock layers in the middle slope restrain the deformation of the upper part. The differential deformation between hard and soft rock layers and the inertia difference in different parts of deformable body are the main causes of S-type toppling. Two shear belts form across the two inversion points of S-shaped layers respectively, and the slope finally form flexible bending-slip failure. (5)The ratio of S/T can affect the slope failure mode. The larger the ratio is, the smaller the reverse deformation area and the toe collapse area are. When the S/T≥2, the slope failure mode turns to flexural toppling without S-shaped deformation.

       

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