富水砂质地层基坑注浆止水堵漏扩散效果研究

Investigation on Grouting Diffusion for Seepage Control in Water-rich Sandy Strata of Deep Excavations

  • 摘要: 针对富水砂质地层基坑渗漏注浆问题,建立可视化的基坑注浆模型试验装置和浆液扩散离散元数值模型,通过对比研究,探明注浆材料、注浆压力和地下水位等关键因素对浆液扩散规律的影响,阐明富水砂质地层渗漏条件下不同注浆材料的止水堵漏效果。研究结果表明:在相同渗漏条件下,三种注浆材料的扩散范围依次为双液浆>亲水性聚氨酯>环氧树脂,其扩散效果与浆液的黏度和流动性呈正相关;注浆压力是影响浆液扩散进深的主要因素,而地下水位与浆液扩散效果呈负相关关系。随着注浆压力的增大,浆液扩散半径呈减速式增长趋势,在注浆压力超过0.3 MPa后增长幅度显著减缓;砂土压密率同步增大,并沿径向明显减弱。

     

    Abstract: To address grouting performance in water-rich sandy strata, a visualized grouting model test system and a discrete element numerical model for slurry diffusion were established. Comparative investigations were conducted to clarify the influence of grouting materials, grouting pressure, and groundwater level on the diffusion behavior of slurry, and to evaluate the water-blocking effectiveness of various grouting materials under seepage conditions. The results show that, under identical seepage conditions, the diffusion extent of the three grouting materials ranks as: two-component slurry > hydrophilic polyurethane > epoxy resin. The diffusion performance is positively correlated with slurry viscosity and fluidity. Grouting pressure is the primary controlling factor for slurry penetration depth, while groundwater level exhibits a negative correlation with grouting diffusion effectiveness. With increasing grouting pressure, the slurry diffusion radius exhibits a decelerating growth trend, with a significant reduction in growth rate when the pressure exceeds 0.3 MPa. Meanwhile, sand compaction increases concurrently, but weakens significantly along the radial direction.

     

/

返回文章
返回