Size effect on the hydraulic behavior of fluid flow through a single rough -walled fracture

被引:13
作者
Zhong, Zhen [1 ,2 ]
Wang, Lei [1 ]
Song, Leibo [1 ,2 ]
Gao, Chao [1 ]
Hu, Yunjin [1 ,2 ]
Gao, Huicai [1 ,2 ]
Song, Fei [3 ]
Rodriguez-Dono, Alfonso [3 ,4 ]
Lou, Rong [5 ]
机构
[1] Shaoxing Univ, Sch Civil Engn, Shaoxing, Peoples R China
[2] Shaoxing Univ, Key Lab Rock Mech & Geohazards Zhejiang Prov, Shaoxing, Peoples R China
[3] Tech Univ Catalonia UPC, Dept Civil & Environm Engn, Barcelona, Spain
[4] CSIC, Inst Environm Assessment & Water Res IDAEA, Barcelona, Spain
[5] Huahui Engn Design Grp Corp Ltd, Shaoxing, Peoples R China
基金
中国国家自然科学基金;
关键词
Size effect; Fluid flow; Reynolds equation; A rough-walled fracture; Representative size; REYNOLDS-EQUATION; SURFACE-ROUGHNESS; TRANSPORT; APERTURE; CONDUCTIVITY; PERMEABILITY; DEPENDENCE;
D O I
10.1016/j.soildyn.2021.106615
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
This study provides a numerical approach to evaluate the effect of sample sizes on fluid flow through a single rough-walled fracture. The rough-walled fracture was generated by using mathematical statistics. Its aperture follows a normal distribution along a large-size plane of dimensions 20 m ? 20 m, and from this large-size fracture plane, a series of fractures with different sizes were extracted. Then, a two-dimensional (2D) Rey-nolds equation was solved to simulate fluid flow through these rough-walled fractures with different mean fracture apertures and roughness. The impact of normal stress on the hydraulic properties was introduced by using a hyperbolic function. The simulated results show a positive correlation between hydraulic conductivity and fracture sizes. In fact, hydraulic conductivity of the fluid flow through a single rough-walled fracture in-creases with the increment of the fracture size until a given size from which it stays constant. The hydraulic conductivity for this given size can then be considered as a representative of that in larger sample sizes. This given size resulted to range from 12 m to 16 m, due to the variations in mean fracture apertures, roughness and normal stress. In addition, it was also found that this representative size tends to decrease with an increase in the mean fracture apertures, while tends to increase as the fracture roughness or the normal stress increases, since those variables affect the fracture topology and contact areas, which play an important role in controlling the tortuosity and connectivity of fluid flow through a rough fracture.
引用
收藏
页数:10
相关论文
共 51 条
[1]   FUNDAMENTALS OF ROCK JOINT DEFORMATION [J].
BANDIS, SC ;
LUMSDEN, AC ;
BARTON, NR .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 1983, 20 (06) :249-268
[2]   REVIEW OF A NEW SHEAR-STRENGTH CRITERION FOR ROCK JOINTS [J].
BARTON, N .
ENGINEERING GEOLOGY, 1973, 7 (04) :287-332
[3]  
Barton N., 1977, Rock Mechanics, V10, P1, DOI 10.1007/BF01261801
[4]  
Batchelor CK, 2000, INTRO FLUID DYNAMICS, P147
[5]   Trapping zones: The effect of fracture roughness on the directional anisotropy of fluid flow and colloid transport in a single fracture [J].
Boutt, David F. ;
Grasselli, Giovanni ;
Fredrich, Joanne T. ;
Cook, Benjamin K. ;
Williams, John R. .
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (21)
[6]  
Briggs S.A., 2014, IMPACT SINGLE FRACTU
[7]   FLUID-FLOW THROUGH ROCK JOINTS - THE EFFECT OF SURFACE-ROUGHNESS [J].
BROWN, SR .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1987, 92 (B2) :1337-1347
[8]   APPLICABILITY OF THE REYNOLDS-EQUATION FOR MODELING FLUID-FLOW BETWEEN ROUGH SURFACES [J].
BROWN, SR ;
STOCKMAN, HW ;
REEVES, SJ .
GEOPHYSICAL RESEARCH LETTERS, 1995, 22 (18) :2537-2540
[9]   TRANSPORT OF FLUID AND ELECTRIC-CURRENT THROUGH A SINGLE FRACTURE [J].
BROWN, SR .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1989, 94 (B7) :9429-9438
[10]   Fluid flow in synthetic rough-walled fractures: Navier-Stokes, Stokes, and local cubic law simulations [J].
Brush, DJ ;
Thomson, NR .
WATER RESOURCES RESEARCH, 2003, 39 (04) :SBH51-SBH515