Research Progress on the Instability Mechanisms and Stability Evaluation Method of Buckling Landslides
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摘要:
溃屈型滑坡作为常见的山地灾害，其动力演化过程较为复杂，涉及主动区顺层滑移和被动区弯曲隆起的变形协同，以及主动区和被动区范围的动态变化；开展相关研究通常需要对上述复杂过程进行简化处理，导致现有的溃屈型滑坡研究方法种类繁多但普适性有限。基于文献计量分析方法，本文对溃屈型滑坡相关文献的数量、期刊和关键词进行梳理，系统分析溃屈型滑坡领域的研究现状及发展趋势。在此基础上，首先分类探讨了理论解析、模型试验和数值模拟等溃屈型滑坡失稳机制及稳定性分析方法；随后，系统探讨了溃屈型滑坡稳定性的影响因素，包括岩层倾角、岩层厚度、岩性、滑移面黏聚力和内摩擦角等内在因素，以及水和地震等触发因素。最后，本文对溃屈型滑坡领域未来的研究和实践方向进行了展望。
Abstract:As the common mountainous hazard, the buckling landslide is characterized by complicated dynamic evolution process, which involves the synergistic deformation of the sliding of active zone and the bending-bulging of passive zone, and the dynamic alteration of the ranges of active and passive zones. The simplification of aforementioned evolution process is usually necessary for relevant research on buckling landslides, resulting in a variety of research methods with limited applicability. By using the bibliometric analysis, this paper summarizes the numbers, journals and key words of related literature on the buckling landslides, and systematically reviews the situation and development trend of this research topic. On that basis, the mainstream methods for the bucking mechanism and stability analysis, including the analytical solution, model experiment and numerical simulation, are summarized and discussed; Then, the summary on the influencing factors, including the intrinsic factors such as the dip and thickness of rock layer, the lithology, the cohesion and internal friction angle of basal sliding surface, and the triggering factors such as the water and the earthquake, is performed. Finally, some prospects for the future study and practice in the research field of buckling landslides are provided.
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Key words:
- buckling landslide /
- bibliometric analysis /
- analysis method /
- influencing factor
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表 1 溃屈破坏典型事件及其相关信息
Table 1. Buckling failure events and associated information
事件名称 坡长（m） 坡高（m） 岩层倾角（°） 岩层厚度 岩性组合 文献来源 Malvern Hills边坡溃屈 22.5 15 45 薄层 互层泥岩、板岩 Seale, 2007 Quinette矿山溃屈 173 120 44~50 薄−中层 互层砂岩、页岩 Wang B et al., 2004 Westfield矿山溃屈 160 95 34~40 薄层 互层泥岩 Scoble, 1981 Lavini di Marco斜坡溃屈 454 200 25~29 薄−中层 石灰岩、泥岩 Tommasi et al., 2009 新磨滑坡 1170 400 43~53 中厚层 石英砂岩、千枚岩 Zhao S Y et al., 2018 大奔流滑坡 1462 265 25~40 薄−中层 大理岩、泥岩 丁戈媛和胡新丽, 2020 藕塘滑坡 1800 610 24~29 中厚层 砂岩粉砂岩互层 肖捷夫, 2021 木鱼包滑坡 1500 420 27 中−厚层 砂岩、炭质页岩 Zhou C et al., 2020 
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