Propagation regimes, transition times, and approximate universality in 2D hydraulic fracture propagation with fluid lag. (September 2021)

• Record Type: Journal Article
• Authors: Gutiérrez, Julieta; Serebrinsky, Santiago
• Is Part Of: Engineering fracture mechanics. Volume 254(2021)
• Publication Date: 2021-09
• Subjects: Hydraulic fracture -- Fluid lag -- Two dimensional; Fracture mechanics -- Periodicals; Rupture, Mécanique de la -- Périodiques; Fracture mechanics; Periodicals; 620.112605
• DOI: 10.1016/j.engfracmech.2021.107905
• Languages: English
• ISSNs: 0013-7944

Abstract

Abstract: During its lifetime, a hydraulic fracture is known to traverse a trajectory in a region of a parametric space of non-dimensional evolutionary parameters. The topology of this diagram depends upon the phenomena considered. For the specific case of a 2D-plane strain fracture propagating in an elastic solid on a straight path normal to the minimum compressive stress, with a constant rate of injection of an incompressible newtonian fluid, and without leak-off, the diagram is a triangle whose vertices are typically called O, M, and K. The non-dimensional parameters are the toughness K and remote stress T (monotonically increasing with time). At each point in the trajectory P ( t ) = ( K, T ) ( t ), the configuration of the fracture is essentially described by several non-dimensional variables, in this case the opening Ω 0 and pressure Π 0 at the inlet, and the length γ . When fluid lag is considered, as in this case, a fourth variable (e.g., the fluid fraction ξ f ) can be appended to build the descriptive set F 0 = { Ω 0, Π 0, γ, ξ f } . Various propagation regimes are observed across the MKO triangle. As the main results, we: (1) provide specific, K -dependent transition times among the propagation regimes; and (2) found that the transient evolutions of all propagating cracks with moderate values of the non-dimensional toughness ( K ≳ 0 . 3 ), from the OK edge to the MK edge, are contained in a thin bundle about a universal curve in the F 0 -space. This result can be applied, e.g., to readily setup approximate initial conditions for more detailed hydraulic fracture propagation simulations. In addition, we developed a four-parameter family of parametrizations of the MKO triangle suitable for plotting trajectories and other loci on the triangle. Highlights: Transition from early to intermediate time regime is strongly toughness-dependent. Transition from intermediate to late time regime is mildly toughness-dependent. An approximately universal behavior covers a large part of the MKO triangle. Setting of initial conditions for complex simulations can be made easier. A "symmetrized" parametrizationon of the MKO triangle is presented.