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We use a numerical model to further explore the interactions between the fractures and surrounding matrix.
The fluid transfer between the fractures and the matrix is defined based on the specific transfer functions.
Open image in new window Fig. 5 Relationship between the fractures width and the amplitude of the acoustic wave.
The interactions between the fractures and the heterogeneous reservoir rock, however, are quite complex, and often multiple fractures are created in a single well.
The main objective of this study is to determine when the osmotic transport plays an important role on the mass exchange between the fractures and the rock matrix.
The interactions between the fractures and the heterogeneous reservoir rock, however, are quite complex, which makes it quite difficult to model production from hydraulically fractured systems.
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While re-forming, the bone must be protected from weight bearing and movement between the fracture ends.
The guiding principle in treatment of fractures is restoration of normal length and alignment when necessary and avoidance of motion between the fracture fragments.
Fibrous tissue between the fracture ends was seen.
The fracture closure zone is between the fracture initiation and development zone and the fracture stable development zone.
There were no contact spots between the fracture faces at the beginning of the simulation.
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