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首页> 外文期刊>Advances in Water Resources >Effects of fracture surface roughness and shear displacement on geometrical and hydraulic properties of three-dimensional crossed rock fracture models
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Effects of fracture surface roughness and shear displacement on geometrical and hydraulic properties of three-dimensional crossed rock fracture models

机译:裂缝表面粗糙度和剪切位移对三维交叉岩石裂缝模型几何和水力特性的影响

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摘要

While shear-flow behavior through fractured media has been so far studied at single fracture scale, a numerical analysis of the shear effect on the hydraulic response of 3D crossed fracture model is presented. The analysis was based on a series of crossed fracture models, in which the effects of fracture surface roughness and shear displacement were considered. The rough fracture surfaces were generated using the modified successive random additions (SRA) algorithm. The shear displacement was applied on one fracture, and at the same time another fracture shifted along with the upper and lower surfaces of the sheared fracture. The simulation results reveal the development and variation of preferential flow paths through the model during the shear, accompanied by the change of the flow rate ratios between two flow planes at the outlet boundary. The average contact area accounts for approximately 5-27% of the fracture planes during shear, but the actual calculated flow area is about 38-55% of the fracture planes, which is much smaller than the noncontact area. The equivalent permeability will either increase or decrease as shear displacement increases from 0 to 4 mm, depending on the aperture distribution of intersection part between two fractures. When the shear displacement continuously increases by up to 20 mm, the equivalent permeability increases sharply first, and then keeps increasing with a lower gradient. The equivalent permeability of rough fractured model is about 26-80% of that calculated from the parallel plate model, and the equivalent permeability in the direction perpendicular to shear direction is approximately 1.31-3.67 times larger than that in the direction parallel to shear direction. These results can provide a fundamental understanding of fluid flow through crossed fracture model under shear.
机译:到目前为止,虽然已经在单个裂缝尺度上研究了通过裂缝介质的剪切流行为,但对3D交叉裂缝模型水力响应的剪切效应进行了数值分析。该分析基于一系列交叉断裂模型,其中考虑了断裂表面粗糙度和剪切位移的影响。使用改进的连续随机加法(SRA)算法生成粗糙的裂缝表面。剪切位移施加在一个裂缝上,同时另一个裂缝随剪切裂缝的上下表面移动。仿真结果揭示了剪切过程中通过模型的优先流动路径的发展和变化,伴随着出口边界处两个流动平面之间的流速比的变化。在剪切过程中,平均接触面积约占断裂面的5-27%,但实际计算出的流动面积约为断裂面的38-55%,远小于非接触面。当剪切位移从0 mm增加到4 mm时,等效渗透率将增加或减小,这取决于两个裂缝之间的相交部分的孔径分布。当剪切位移连续增加到20 mm时,等效渗透率先急剧增加,然后以较低的斜率继续增加。粗糙裂缝模型的等效渗透率约为平行板模型计算的等效渗透率的26-80%,垂直于剪切方向的等效渗透率约为平行于剪切方向的等效渗透率的1.31-3.67倍。这些结果可以提供对在剪切作用下穿过交叉裂缝模型的流体流动的基本了解。

著录项

  • 来源
    《Advances in Water Resources》 |2018年第3期|30-41|共12页
  • 作者单位

    Shandong Univ Sci & Technol, State Key Lab Min Disaster Prevent & Control Cofo, Qingdao 266510, Peoples R China;

    China Univ Min & Technol, State Key Lab Geomech & Deep Underground Engn, Xuzhou 221116, Peoples R China;

    Shandong Univ Sci & Technol, State Key Lab Min Disaster Prevent & Control Cofo, Qingdao 266510, Peoples R China;

    Shaoxing Univ, Ctr Rock Mech & Geohazards, Shaoxing 312000, Peoples R China;

    China Univ Min & Technol, State Key Lab Geomech & Deep Underground Engn, Xuzhou 221116, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Crossed fracture model; Roughness; Shear; Permeability;

    机译:交叉断裂模型粗糙度剪切渗透率;

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