烧变岩渗流特征及注浆减渗规律实验研究

An experimental study on seepage characteristics and grouting-induced permeability reduction of burnt rocks

  • 摘要:
    背景 烧变岩区是煤层自燃形成的特殊地质体,其内部发育的孔洞裂隙系统为地下水赋存与运移提供了优势空间,但对邻近煤层安全开采构成严重水害威胁。
    方法 针对这一工程难题,采用三维重构技术系统解析烧变岩内部空隙结构特征,并通过室内渗流实验与注浆实验,揭示典型烧变岩的渗流规律与注浆减渗机制。
    结果和结论 (1)烧变岩试样内部孔洞裂隙高度发育,空隙结构呈现复杂多变的空间展布特征,贯通大孔裂隙占总空隙的56.72%,主要孔裂隙网络间连通性一般。(2)渗流实验表明,烧变岩渗流水力梯度与流速呈现显著非线性特征,其渗流动力学行为符合Forchheimer方程表征规律,不同渗流方向的渗透性差异显著,渗透系数相差约50%。(3)黏土水泥浆在烧变岩孔裂隙系统中具有良好的可注性,其有效扩散距离主要受孔裂隙喉道的几何约束效应控制,随着与注浆口的距离增大,浆液对孔裂隙的充填比例逐渐降低。(4)烧变岩注浆后减渗效果显著,被注体的渗流水力梯度与流速仍呈现非线性特征,且注浆后 14 d内减渗率随时间延长逐渐增长并最终趋于稳定。研究成果为烧变岩区煤层开采水害防治提供了的理论依据与技术参考。

     

    Abstract:
    Background Burnt rocks represent special geobodies formed by the spontaneous combustion of coal seams. Their pore and fracture systems provide preferential spaces for groundwater occurrence and migration while also posing severe water hazard threats to the safe mining of adjacent coal seams.
    Methods To address this engineering challenge, this study systematically analyzed the void structures within burnt rocks using three-dimensional reconstruction technology. Through laboratory seepage and grouting experiments, this study revealed the seepage patterns and grouting-induced permeability mechanisms of typical burnt rock specimens.
    Results and Conclusions The burnt rock specimens contained highly developed pores and fractures, with the void structures showing complex and various spatial distributions. The interconnected large pores and fractures accounted for 56.72% of the total volume of voids, suggesting moderate connectivity in primary pore and fracture networks. Seepage experiments indicate that the burnt rocks exhibited a significant nonlinear relationship between the hydraulic gradient and flow velocity of seepage, with their seepage dynamics behavior consistent with the patterns characterized by the Forchheimer equation. The permeability varied significantly along different seepage directions, with differences in permeability coefficients of about 50%. Clay-cement grout exhibited high injectability within pore-fracture systems in the burnt rocks. The effective diffusion distance of the grout was predominately governed by the geometrical confinement effect of the pore-fracture throats. The proportion of pores and fractures filled by grout gradually decreased with an increase in the distance from the grouting port. The burnt rocks exhibited significant permeability reduction after grouting. The hydraulic gradient and flow velocity maintained a nonlinear relationship after grouting. Within 14 days after grouting, the permeability reduction rate increased with time, eventually stabilizing. These findings provide a theoretical basis and technical reference for water hazard prevention and control during coal seam mining in burnt rock areas.

     

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