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Self-similar fault slip in response to fluid injection

Published online by Cambridge University Press:  12 October 2021

Robert C. Viesca*
Affiliation:
Department of Civil and Environmental Engineering, Tufts University, Medford, MA 02155, USA
*
†Email address for correspondence: robert.viesca@tufts.edu

Abstract

There is scientific and industrial interest in understanding how geologic faults respond to transient sources of fluid. Natural and artificial sources can elevate pore fluid pressure on the fault frictional interface, which may induce slip. We consider a simple boundary value problem to provide an elementary model of the physical process and to provide a benchmark for numerical solution procedures. We examine the slip of a fault that is an interface of two elastic half-spaces. Injection is modelled as a line source at constant pressure and fluid pressure is assumed to diffuse along the interface. The resulting problem is an integro-differential equation governing fault slip, which has a single dimensionless parameter. The expansion of slip is self-similar and the rupture front propagates at a factor $\lambda$ of the diffusive length scale $\sqrt {\alpha t}$. We identify two asymptotic regimes corresponding to $\lambda$ being small or large and perform a perturbation expansion in each limit. For large $\lambda$, in the regime of a so-called critically stressed fault, a boundary layer emerges on the diffusive length scale, which lags far behind the rupture front. We demonstrate higher-order matched asymptotics for the integro-differential equation, and in doing so, we derive a multipole expansion to capture successive orders of influence on the outer problem for fault slip for a driving force that is small relative to the crack dimensions. Asymptotic expansions are compared with accurate numerical solutions to the full problem, which are tabulated to high precision.

Information

Type
JFM Papers
Copyright
© The Author(s), 2021. Published by Cambridge University Press
Figure 0

Figure 1.Counter-clockwise: (a) Unbounded elastic body containing a fault, loaded remotely with fault-normal and shear stress $\sigma$, $\tau$. The fault is embedded within a thin poroelastic layer, assumed to be much more permeable than the surroundings. Fluid injected at $x=0$ diffuses along the fault as $\sqrt {\alpha t}$, inducing quasi-static slip out to a distance $a(t)$. The fault has constant friction coefficient $f$. (c) Black: relation between rupture growth factor $\lambda$ and a parameter reflecting the initial state of stress and injection pressure, where $\sigma '=\sigma -p_o$ and $p_o$ is pre-injection fault fluid pressure. Dashed: asymptotic behaviours, (3.5) and (3.8). (d) Same as bottom left, with abscissa arranged to occupy a finite interval. (b) Plot of self-similar slip distributions at three instants in time after the start of injection, $t=1$, 5 and 10 min, for the specific choices $\sigma =50\ \text {MPa}$, $\tau =12\ \text {MPa}$, $p_o=20\ \text {MPa}$, $\Delta p = 12\ \text {MPa}$, $f=0.5$, $\alpha _{hy}=0.01\ \text {m}^2\ \text {s}^{-1}$, $\mu =30\ \text {GPa}$, $\nu =1/4$, $\mu '=20\ \text {GPa}$. For these choices, the parameter $(1-\tau /\tau _p)\sigma '/\Delta p=0.5$. The corresponding self-similar slip distribution and factor $\lambda$ are given in table S1 in the supplementary material available at https://doi.org/10.1017/jfm.2021.825.

Figure 1

Figure 2.(a) Self-similar distributions of slip $\delta$ with distance from injection point $x$, which is scaled by the crack half-length $a(t)=\lambda \sqrt {\alpha t}$. Solid red and black curves are numerical solutions to the full problem. Dashed curves are leading-order asymptotic solutions. Each curve corresponds to one value of $\lambda$ in the range $\lambda =10^{-3},10^{-2},\ldots ,10^3$. Black curves correspond to $\lambda =10^{-3},10^{-2},10^{-1},10^0$ from top to bottom, with the first three indistinguishable on this scale; red curves correspond to $\lambda =10^1,10^2,10^3$ from top to bottom. Cyan-dashed: solution for small $\lambda$, (3.6). Blue-dashed: ‘outer’ solutions for large $\lambda$, (3.9). To facilitate comparisons, two vertical scales are used: one for black and cyan-dashed curves, and another for red and blue-dashed curves. (b) For large values of $\lambda$, the distribution of slip is plotted over distances scaled by $\sqrt {\alpha t}$, which is much smaller than the crack length $a(t)$. This ‘inner’ behaviour is described by (3.10), a single numerical solution shown here as black-dashed curves. Curves correspond to $\lambda =10^1,10^2,10^3$ from bottom to top.

Figure 2

Figure 3.The maximum slip, which occurs at $x=0$, as it relates to the factor $\lambda$ shown as (a) semi-log and (b) log–log plots. Red-dashed: end-member scalings at small $\lambda$, (3.7), and at large $\lambda$, (3.13). Blue-dashed: approximation of $\delta (0)$ for all $\lambda$, (3.16).

Figure 3

Figure 4.The peak slip as it relates to the problem parameter $(1-\tau /\tau _p)\,\sigma '/\Delta p$. Red-dashed: scalings as the parameter approaches its bounds, derived from (3.7) and (3.13) and the asymptotic relations between the parameter and $\lambda$, (3.5) and (3.8).

Figure 4

Figure 5.Self-similar distribution of slip $\delta$, less the first-order term, (5.6), in the asymptotic expansion for slip (5.4) in the marginally pressurized limit (small $\lambda$). From top to bottom, black curves correspond to the difference for $\lambda =2,1,{1}/{2},{1}/{4},{1}/{8}$. The cyan-dashed curve is the second-order term of the expansion, (5.7).

Figure 5

Table 1.Select solutions $h(x)$ to the problem $g(x)=({1}/{{\rm \pi} })\int _{-1}^1({h'(s)}/({x-s}))\,\textrm {d}s$, with $h(\pm 1)=0$.

Figure 6

Figure 6.Spatio-temporal component, $f(x/\sqrt {\alpha t})$, of ‘inner’ solution for slip $\delta$ in the critically stressed limit, (3.10). Shown in black on linear (a), log–linear (b) and logarithmic (c) axes. Red- and blue-dashed curves: outer and inner asymptotic behaviour of $f$, (3.12) and (3.15).

Figure 7

Figure 7.Self-similar distribution of slip in the critically stressed limit (large $\lambda$). In this limit the rupture extent $a(t)$ outpaces the diffusive distance $\sqrt {\alpha t}$. (a,b) Black curves from right to left correspond to full solutions for the self-similar slip profiles for $\lambda =10,100,1000$. (a) Red-dashed and blue-dashed lines correspond to outer and inner solution expansion to first order. (b) Red-dashed and blue-dashed lines correspond to outer and inner solution expansion to second order. Outer solution is given by (6.9)–(6.12). Inner solution given by (7.9).

Figure 8

Figure 8.Comparison of approximations to the full solution of peak fault slip (black curve) in the vicinity of $\lambda =1$. First- and second-order approximations in the marginally pressurized and critically stressed limits, given respectively by (5.9) and (8.1), are shown as red-dashed and red-dot–dashed curves. Blue-dashed curve: approximation provided for all values of $\lambda$, (3.16).

Figure 9

Figure 9.Solution for self-similar slip profile in black for $\lambda =5$. (a,b) Superimposed blue- and red-dashed curves, respectively, showing inner and outer solutions to (a) leading and (b) next order. (c) Superposition of leading and next-order composite solutions as blue- and red-dashed curves. (d) The difference between the self-similar solution and the composite solutions at leading and next order are respectively the blue and red-dashed curves. (e,f) Semi-logarithmic plots comparing the leading- and next-order composite solutions, in blue- and red-dashed curves, to the self-similar solution, in black.

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