奥灰岩渗透特性与断层注浆扩散规律实验研究

    Experimental study on permeability characteristics and fault grouting diffusion law of limestone

    • 摘要: 传统断层注浆技术中将断层构造简化为单一裂隙模型,导致理论结果与现场施工数据存在较大差异性。针对此问题,以奥灰岩层为背景,采用UDEC软件分析了不同裂隙宽度、水灰比、注浆压力条件下的浆液渗透特性。比较了单一裂隙模型、单一裂隙与断层正交模型的注浆扩散规律,并根据现场注浆压力数据进行阐释验证。结果表明:裂隙宽度与水灰比的增加对于浆液扩散范围的影响分别呈现出指数型与对数型增长的特征。浆液的扩散规律在不同的断层条件下存在3种类型,当断层为单一窄裂隙结构时,表现为急剧增压型;当断层为大尺寸裂隙结构时,表现为缓慢增压型;当断层为连通性较差的多个裂隙的组合结构时,表现为波动增压型。

       

      Abstract: The traditional fault grouting technology simplifies the fault structure into a single fracture model, which leads to a large difference between the theoretical results and the field construction data. To solve this problem, the grout permeability characteristics under different crack widths, water-cement ratio and grouting pressure were analyzed by using UDEC software. The grouting diffusion rules of single crack model, single crack model and fault orthogonal model are compared, and the field grouting pressure data are used to explain and verify. The results show that the effects of increasing crack width and water-cement ratio on the grout diffusion range are exponential and logarithmic, respectively. There are three types of grout diffusion under different fault conditions. When the fault is a single narrow fissure structure, it shows a sharp pressurization type. When the fault is a large size fracture structure, it shows a slow pressurization type. When the fault is a combination of several fractures with poor connectivity, it is a wave booster type.

       

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