Numerical simulations examining the relationship between wall-roughness and fluid flow in rock fractures

被引:134
|
作者
Crandall, Dustin [1 ]
Bromhal, Grant [1 ]
Karpyn, Zuleima T. [2 ]
机构
[1] Natl Energy Technol Lab, Geosci Div, Morgantown, WV 26507 USA
[2] Penn State Univ, Dept Energy & Mineral Engn, University Pk, PA 16802 USA
关键词
Fracture roughness; CT scanning; Navier-Stokes; Rock fractures; RELATIVE PERMEABILITY; CAPILLARY-PRESSURE; FRACTAL DIMENSION; MULTIPHASE-FLOW; NAVIER-STOKES; MODEL; DISSOLUTION; TRANSPORT; APERTURE;
D O I
10.1016/j.ijrmms.2010.03.015
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Understanding how fracture wall-roughness affects fluid flow is important when modeling many subsurface transport problems. Computed tomography scanning provides a unique view of rock fractures, allowing the measurement of fracture wall-roughness, without destroying the initial rock sample. For this computational fluid dynamics study, we used several different methods to obtain three-dimensional meshes of a computed tomography scanned fracture in Berea sandstone. These volumetric meshes had different wall-roughnesses, which we characterized using the Joint Roughness Coefficient and the fractal dimension of the fracture profiles. We then related these macroscopic roughness parameters to the effective flow through the fractures, asdetermined from Navier-Stokes numerical models. Thus, we used our fracture meshes to develop relationships between the observed roughness properties of the fracture geometries and flow parameters that are of importance for modeling flow through fractures in field scale models. Fractures with high Joint Roughness Coefficients and fractal dimensions were shown to exhibit tortuous flow paths, be poorly characterized by the mean geometric aperture, and have a fracture transmissivity 35 times smaller than the smoother modeled fracture flows. Published by Elsevier Ltd.
引用
收藏
页码:784 / 796
页数:13
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