粤北山区斜坡高填路基强降雨下失稳机制研究

    Study on instability mechanism of high-fill subgrade on slopes in northern Guangdong mountains under heavy rainfall

    • 摘要: 粤北山区某高速公路斜坡高填路基强降雨下发生垮塌事故,本文依托事故现场工况开展强降雨下斜坡高填路基边坡失稳机制研究。采用GMS三维渗流模型,以场区周围天然山脊为模型分水边界,依据地貌、地层条件建立三维渗流场模型,输入域内降雨过程,参照现状测点地下水位时程,通过反演可以复现事故发生前地下水的空间分布及变化特征。山谷路段斜坡高填路基伴存的填平区或洼地强降雨下汇集积水形成高位水头压力,叠加深层岩土体渗流导致斜坡高填路基失稳。强降雨过程地表入渗是地下水渗流场特征的主要控制要素,结合防护措施的造价和施工难度,场区范围的水力防护措施以覆盖层+排水沟方案的性价比为最优。

       

      Abstract: A collapse accident occurred on a high-fill subgrade on slope of an expressway on a slope in the mountainous area of northern Guangdong under heavy rainfall. Based on the working conditions at the accident site, this paper investigates the instability mechanism of the high-fill subgrade on a slope under heavy rainfall. The GMS three-dimensional seepage model is adopted, with natural ridges around the site set as watershed of the model. A three-dimensional seepage field model is established according to geomorphological and stratigraphic conditions. The rainfall process within the computational domain is imported, and by referencing the time histories of groundwater levels at in-situ monitoring points, inversion analysis is carried out to reproduce the spatial distribution and variation characteristics of groundwater prior to the accident. Water accumulates in filled areas and low-lying zones adjacent to the sloped high-fill subgrade in valley sections during heavy rainfall, generating high hydraulic head pressure. Superimposed on the seepage in deep rock and soil mass, this combined effect triggers the instability of the sloped high-fill subgrade. Surface infiltration during heavy rainfall constitutes the dominant controlling factor governing the characteristics of the groundwater seepage field. Considering the construction cost and construction difficulty of protective measures, the scheme combining impermeable covering layer and drainage ditch exhibits the best cost-effectiveness for hydraulic protection within the study area.

       

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