Modified governing equation and numerical simulation of seepage flow in a single fracture with three-dimensional roughness

被引:26
作者
He, Guanhong [1 ,2 ]
Wang, Enzhi [1 ]
Liu, Xiaoli [1 ]
机构
[1] Tsinghua Univ, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
[2] Guangzhou Metro Design & Res Inst Co Ltd, Guangzhou 510100, Guangdong, Peoples R China
基金
中国国家自然科学基金;
关键词
Groundwater; Seepage; Flow in fracture; Rough angle; Three-dimension; FLUID-FLOW; SURFACE-ROUGHNESS; HYDRAULIC CONDUCTIVITY; FRICTION FACTOR; ROCK JOINTS; PERMEABILITY; TORTUOSITY; PARAMETER;
D O I
10.1007/s12517-015-2036-8
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Roughness and tortuosity influence groundwater flow through a fracture. Steady flow through a single fracture can be described primitively by the well-known Cubic Law and Reynolds equation with the assumption that the fracture is made of smooth parallel plates. However, ignoring the roughness and tortuosity of the fracture will lead to inaccurate estimations of the flow rate. To obtain a more accurate flow rate through a rough fracture, this paper has derived a modified governing equation, taking into account the three-dimensional effect of the roughness. The equation modifies the Reynolds equation by adding correction coefficients to the terms of the flow rates, which are relative to the roughness angles in both the longitudinal and transverse directions. Experiments of steady seepage flow through sawtooth fractures were conducted. The accuracy of the modified equation has been verified by comparing the experimental data and the theoretical computational data. Furthermore, three-dimensional numerical models were established to simulate the steady flow in rough fractures with the triangular, sinusoidal surfaces and the typical joint roughness coefficient (JRC) profiles. The simulation results were compared with the calculation results of the modified equation and the current equations. The comparison indicates that the flow rate calculated by the modified equation is the closest to the numerical result.
引用
收藏
页码:1 / 20
页数:20
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