XFVM modelling of fracture aperture induced by shear and tensile opening

被引:2
|
作者
Conti, Giulia [1 ]
Matthaei, Stephan [2 ]
Jenny, Patrick [1 ]
机构
[1] Swiss Fed Inst Technol, Inst Fluid Dynam, Sonneggstr 3, CH-8052 Zurich, Switzerland
[2] Univ Melbourne, Dept Infrastructure Engn, Melbourne, Vic 3010, Australia
关键词
Shear opening; XFVM; Fracture dilation; Fracture mechanics; HYDRAULIC STIMULATIONS; FLOW; STRESS; PERMEABILITY; DEFORMATION; FAILURE;
D O I
10.1007/s10596-023-10214-5
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
In reservoir simulation, it is important to understand the mechanical behaviour of fractured rocks and the effect of shear and tensile displacements of fractures on their aperture. Tensile opening directly enhances the fracture aperture, whereas shear of a preexisting rough-walled fracture creates aperture changes dependent on the local stress state. Since fracture dilatation increases reservoir permeability, both processes must be included in a realistic and consistent manner into the mechanical reservoir simulation model. Here, we use the extended finite volume method (XFVM) to conduct flow and geomechanics simulations. In XFVM, fractures are embedded in a poroelastic matrix and are modelled with discontinuous basis functions. On each fracture segment the tractions and compressive forces are calculated, and one extra degree of freedom is added for both the shear and tensile displacement. In this particular XFVM implementation we assume that linear elasticity and steady state fluid pressure adequately constrain the effective stress. In this paper, shear dilation is not calculated a posteriori, but it enters the equations such that aperture changes directly affect the stress state. This is accomplished by adding shear dilation to the displacement gradients and therefore ascertains a consistent representation in the stress-strain relations and force balances. We illustrate and discuss the influence of this extra term in two simple test cases and in a realistic layer-restricted two-dimensional fracture network subjected to plausible in situ stress and pore pressure conditions.
引用
收藏
页码:227 / 239
页数:13
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