Multiscale tip asymptotics in hydraulic fracture with leak-off

TLDR: In this paper, an analysis of the near-tip region of a fluid-driven fracture propagating in a permeable saturated rock is carried out by considering the stationary problem of a semi-infinite fracture moving at constant speed V. The authors show that the solution is characterized by a multiscale singular behaviour at the tip and that the nature of the dominant singularity depends both on the relative importance of the dissipative processes and on the scale of reference.

Abstract: This paper is concerned with an analysis of the near-tip region of a fluid-driven fracture propagating in a permeable saturated rock. The analysis is carried out by considering the stationary problem of a semi-infinite fracture moving at constant speed V. Two basic dissipative processes are taken into account: fracturing of the rock and viscous flow in the fracture, and two fluid balance mechanisms are considered – leak-off and storage of the fracturing fluid in the fracture. It is shown that the solution is characterized by a multiscale singular behaviour at the tip, and that the nature of the dominant singularity depends both on the relative importance of the dissipative processes and on the scale of reference. This solution provides a framework to understand the interaction of representative physical processes near the fracture tip, as well as to track the changing nature of the dominant tip process(es) with the tip velocity and its impact on the global fracture response. Furthermore, it gives a universal scaling of the near-tip processes on the scale of the entire fracture and sets the foundation for developing efficient numerical algorithms relying on accurate modelling of the tip region.