Abstract
We present an implicit moving mesh algorithm for the study of the propagation of plane-strain hydraulic fracture in an impermeable medium. In particular, the fluid front is allowed to lag behind the fracture tip. The solution, expressed in the proper scaling, evolves, for a given value of a dimensionless toughness, from a zero stress/zero time self-similar solution characterized by a finite lag, to a large stress/large time self-similar solution with zero lag. A numerical solution for the transient problem is presented using two distinct meshes, stretching at different velocities, for the lag and fluid filled part of the crack. The lubrication and elasticity equations are solved in a coupled manner using an implicit scheme. The lag size, also coupled to the preceding equations, is obtained via the fracture propagation condition. The numerical results are discussed and compared with the known zero lag solution for large stress/large time.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 4863-4880 |
| Number of pages | 18 |
| Journal | Computer Methods in Applied Mechanics and Engineering |
| Volume | 196 |
| Issue number | 49-52 |
| DOIs | |
| State | Published - Nov 1 2007 |
Bibliographical note
Funding Information:We thank Dr. D.I. Garagash from Clarkson University for making available his zero-time/zero-stress solution as well as for fruitful discussions during the course of this research. We also gratefully acknowledge support of this research by Schlumberger, CSIRO Petroleum, the Donors of The Petroleum Research Fund administered by the American Chemical Society (Grant No. ACS-PRF 43081-AC8), and the National Science Foundation (Grant No. 0600058). Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.
Keywords
- Fluid-driven crack
- Hydraulic fracture
- Moving boundary
- Tip cavity