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几何变异性裂隙注浆设备研制及浆液迁扩机理分析

Development of grouting equipment for fractures with geometric variability and analysis of mechanism of slurry migration and diffusion

  • 摘要: 浆液在岩体裂隙内的迁移扩散行为是决定注浆工程效果的基础性物理过程,裂隙粗糙度与开度作为关键几何参量,直接影响浆液流动阻力、前锋形态与迁移扩散范围。为揭示粗糙度、开度等几何参量对承载浆液迁移扩散进程的细观调控及互馈冲刷剥蚀响应机制,自主研发岩体裂隙注浆模拟试验设备,构建复杂岩体裂隙物理模型开展注浆试验,并结合PFC3D数值模拟进行反演验证。研究表明:自研岩体裂隙注浆模拟试验设备由相似模拟试样制测集控设备和岩体裂隙注浆模拟试验设备构成,可在有限立体空间内对复杂岩体裂隙网络进行重构并开展注浆试验,实现从原材料配制到物理模拟试验的全流程一体化操作;模拟粗糙度的砂体粒径越小,浆液迁移扩散速度越快,有效迁移扩散距离越长,砂体颗粒间互锁作用越强,出口堆积体越小,砂−浆终凝沉积痕迹越显著;增大裂隙开度可扩大过浆面积,驱动浆液远距离迁移扩散,部分抵消粗糙度产生的阻滞效应。PFC3D数值模拟结果反演了浆液在主干裂隙内线性态迁移扩散及分支裂隙内离散态或线性态异化迁移扩散的时空演化特征,主干裂隙内最大迁移扩散距离的物理试验和数值模拟结果相对误差均控制在10.0%以内,验证了自研试验设备在刻画浆液迁移扩散行为方面的科学性和适用性。研究结果可为注浆扩散半径预测及工艺参数优化提供机理层面的参考依据。

     

    Abstract: The effectiveness of grouting engineering is determined by the migration and diffusion behavior of slurry within rock fractures, which is a fundamental physical process. Slurry flow resistance, front morphology, and migration-diffusion range are directly influenced by fracture roughness and aperture, which serve as key geometric parameters. A self-developed rock fracture grouting simulation test device was established to reveal the meso-scale regulation of roughness and aperture on slurry migration and diffusion, as well as the associated coupled scour-erosion response mechanisms. A physical model of complex rock fractures is constructed to conduct grouting tests, and the results are inversely validated using PFC3D numerical simulations. The following findings are obtained: The self-developed device consists of similar material specimen preparation, measurement, and control equipment and a rock fracture grouting simulation test apparatus. Complex rock fracture networks can be reconstructed within a limited three-dimensional space, and grouting tests can be performed, enabling a fully integrated operation from raw material preparation to physical simulation tests. For the sand particles simulating roughness, smaller particle sizes are found to lead to faster slurry migration and diffusion, longer effective migration-diffusion distances, stronger interlocking effects between sand particles, smaller outlet accumulations, and more significant final setting deposition traces of the sand-slurry mixture. The slurry flow area is expanded by increasing the fracture aperture, and long-distance slurry migration and diffusion is driven, while the retarding effect caused by roughness is partially offset. The spatiotemporal evolution characteristics of linear migration and diffusion within the main fracture and discrete or linear heterogeneous migration and diffusion within branch fractures are numerically reproduced by the PFC3D numerical simulation results. The relative errors between the physical tests and numerical simulations for the maximum migration and diffusion distance in the main fracture are all within 10.0%, verifying the scientific validity and applicability of the self-developed test device in characterizing slurry migration and diffusion behavior. Mechanistic reference for predicting grouting diffusion radii and optimizing process parameters can be provided by the research results.

     

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