水位循环升降下防渗墙加固红土坝变形特性与机制研究

    • 摘要: 防渗墙加固红土坝随库水位升降呈现不均匀变形和和坝顶裂缝,严重影响其服役性能。本文以江西省乌井水库红土坝为原型,建立物理模型试验系统,监测了八次水位升降下孔隙水压力、土压力和竖向位移变化。研究结果表明:随水位循环升降,孔隙水压力、土压力和竖向位移均呈现周期性变化;土体变形包含了初次蓄水湿化变形,和水位升降下胀缩累积变形。随水位升降次数增加,其中塑性变形分为快速累积、缓慢累积和稳定三个阶段,取决于土体宏观孔隙结构变化,而弹性变形基本不变,归因于微观孔隙结构可逆性;土坝上-下游不均匀变形,受浸润线幅度及其上覆土层荷载共同影响,随浸润线幅度增加,土坝竖向胀缩变形增大,而随上覆土层荷载增大,土体向上膨胀量减小但向下沉降量增加。本研究揭示了水位循环升降下红土坝不均匀变形演化机理,为其服役性能评估提供了理论依据。

       

      Abstract: Due to the effect of water level fluctuations, uneven deformation and crest cracks on the earth dams reinforced by the cut-off walls occurs, affecting its in-service performance. In this study, a physical model was constructed to monitor pore water pressure, earth pressure, and vertical displacement under eight cycles of water-level fluctuation, taking Wujing Reservoir dam as the prototype. The results show that the vertical deformation comprises the initial wetting-induced deformation and cumulative swelling–shrinkage deformation. With increasing cycles, the plastic deformation evolves through three distinct stages—rapid accumulation, slow accumulation, and stabilization, whereas elastic deformation remains unchanged. Uneven deformation between the upstream and downstream side is governed by the phreatic line amplitude and its overlying soil layer load. As the amplitude of the phreatic line increases, the vertical swelling-shrinkage deformation increases; as the load of the overlying soil layer increases, the upward swelling capacity of the soil decreases while the downward settlement increases. This study reveals the mechanism of uneven deformation of lateritic earth dams under water level fluctuations, helpful for its in-service performance evaluation.

       

    /

    返回文章
    返回