首页|期刊导航|煤田地质与勘探|基于FBM的部分充填裂隙渗流特性仿真研究

基于FBM的部分充填裂隙渗流特性仿真研究OA

Investigating seepage in rough porous media fractures using fractional Brownian motion simulation

中文摘要英文摘要

[背景]天然岩体裂隙在长期地质与水力作用下,常被泥沙、矿物等渗透性材料部分充填,形成包含未充填空隙的复杂结构,其渗流特性对油气开采、矿山防治水及地下工程稳定性具有重要影响.[方法]为揭示其渗流机理,基于分形布朗运动生成具有不同分形维数的未充填空隙粗糙轮廓,并推导部分充填裂隙整体渗透率表达式,建立自由流-多孔介质渗流耦合数值模型,系统研究裂隙压降、残余开度及充填基质渗透率对部分充填裂隙渗流行为与整体渗透率的影响规律.[结果和结论](1)部分充填裂隙整体渗透率在低压降下保持稳定,在高压降下因惯性效应而衰减;粗糙壁面引发的涡流可导致渗透率降低,最大约25.9%.(2)残余开度对裂隙渗透率及有效水力开度起主导控制作用,其影响显著强于粗糙度分形维数.随残余开度从0.1 mm增至5.0 mm,整体渗透率呈非线性增长,跨越6个数量级(10-12~10-6m2).(3)充填基质渗透率对整体渗透率的影响可分为3个阶段:低渗透率阶段(k<10-10 m2),流动由未充填空隙主导,整体渗透率稳定;中渗透率阶段(10-10 m2<k<10-5m2),整体渗透率随基质渗透率增长,流量分配向几何比例趋近;高渗透率阶段(k>10-5m2),渗透率增长趋缓并逐渐稳定,且残余开度越大,基质渗透率的影响越弱.(4)在低充填基质渗透率阶段(k<10-10 m2),部分充填裂隙整体渗透率理论预测值在不同分形维数与残余开度下均与数值仿真吻合良好,可有效表征此类裂隙的渗流机制.

[Background]Natural rock fractures are often partially filled with permeable materials such as silt and miner-als under long-term geological and hydraulic actions,forming complex structures containing unfilled voids.The seepage characteristics of such fractures significantly influence petroleum extraction,mine water prevention,and the stability of underground engineering projects.[Methods]To reveal the underlying seepage mechanisms,this study generated rough profiles of unfilled voids with different fractal dimensions based on Fractional Brownian Motion.A theoretical expres-sion for the overall permeability of partially filled fractures was derived,and a coupled free flow-porous medium flow numerical model was established.This framework was used to systematically investigate the effects of fracture pressure drop,residual aperture,and filling matrix permeability on the seepage behavior and overall permeability of partially filled fractures.[Results and Conclusions]The results indicate that:(1)The overall permeability of partially filled frac-tures remains stable under low pressure drops but decays under high pressure drops due to inertial effects;vortex in-duced by rough walls can reduce permeability by up to approximately 25.9%.(2)The residual aperture plays a dominant role in controlling fracture permeability and the effective hydraulic aperture,with its influence significantly stronger than that of the fractal dimension of roughness.As the residual aperture increases from 0.1 mm to 5 mm,the overall permeab-ility exhibits nonlinear growth,spanning six orders of magnitude(from 10-12 m2 to 10-6 m2).(3)The influence of filling matrix permeability can be divided into three stages:in the low-permeability stage(k<10-10m2),flow is dominated by the unfilled void,and the overall permeability remains stable;in the intermediate stage(10-10<k<10-5m2),the overall per-meability increases with matrix permeability,and the flow distribution approaches the geometric proportion;in the high-permeability stage(k>10-5m2),the permeability growth slows and gradually stabilizes,with the influence of matrix per-meability weakening as the residual aperture increases.(4)In the low filling matrix permeability stage(k<10-10m2),the theoretical predictions of the overall permeability of partially filled fractures show good agreement with numerical simu-lations across varying fractal dimensions and residual apertures,demonstrating the model's effectiveness in representing the seepage behavior of such fractures.

刘伟韬;孔德斌;毛庆福;赵吉园;顾玉龙;张逍

山东科技大学安全与环境工程学院,山东青岛 266590||山东科技大学能源与矿业工程学院,山东青岛 266590山东科技大学能源与矿业工程学院,山东青岛 266590||北京科技大学资源与安全工程学院,北京 100083汶上义桥煤矿有限责任公司,山东济宁 272155山东科技大学安全与环境工程学院,山东青岛 266590山东科技大学安全与环境工程学院,山东青岛 266590山东科技大学能源与矿业工程学院,山东青岛 266590||新疆喀拉通克矿业有限责任公司,新疆阿勒泰 836106

矿业与冶金

部分充填裂隙分形布朗运动分形维数渗透率

partially filled fracturefractional Brownian motionfractal dimensionpermeability

《煤田地质与勘探》 2026 (8)

141-153,13

山东省自然科学基金项目(ZR2023ME002)国家自然科学基金项目(52304238,42472324)

10.12363/issn.1001-1986.26.01.0044

评论