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Philosophical transactions. Series A, Mathematical, physical, and engineering sciences logoLink to Philosophical transactions. Series A, Mathematical, physical, and engineering sciences
. 2018 Nov 26;377(2136):20170399. doi: 10.1098/rsta.2017.0399

Thermally activated crack fronts propagating in pinning disorder: simultaneous brittle/creep behaviour depending on scale

A Cochard 1, O Lengliné 1, K J Måløy 2, R Toussaint 1,2,
PMCID: PMC6282409  PMID: 30478211

Abstract

We study theoretically the propagation of a crack front in mode I along an interface in a disordered elastic medium, with a numerical model considering a thermally activated rheology, toughness disorder and long-range elastic interactions. This model reproduces not only the large-scale dynamics of the crack front position in fast or creep loading regimes, but also the small-scale self-affine behaviour of the front. Two different scaling laws are predicted for the front morphology, with a Hurst exponent of 0.5 at small scales and a logarithmic scaling law at large scales, consistently with experiments. The prefactor of these scaling laws is expressed as a function of the temperature, and of the quenched disorder characteristics. The cross-over between these regimes is expressed as a function of the quenched disorder amplitude, and is proportional to the average energy release rate, and to the inverse of temperature. This model captures as well the experimentally observed local velocity fluctuation probability distribution, with a high-velocity tail P(v)∼v−2.6. This feature is shown to arise when the quenched disorder is sufficiently large, whereas smaller toughness fluctuations lead to a lognormal-like velocity distribution. Overall, the system is shown to obey a scaling determined by two distinct mechanisms as a function of scale: namely, the large scales display fluctuations similar to an elastic line in an annealed noise excited as the average front travels through the pinning landscape, while small scales display a balance between thresholds in possible elastic forces and quenched disorder.

This article is part of the theme issue ‘Statistical physics of fracture and earthquakes’.

Keywords: pinning, thermal, scaling

1. Introduction

The propagation of cracks in disordered elastic media is a widely studied physical phenomenon, with applications in engineering, and in mechanical hazards in natural media [1]. This fundamental phenomenon rules the failure of man-made structures, or of natural materials in Earth science (e.g. [2,3]). It involves different physical processes, such as long-range elastic interactions, thermally activated processes and heterogeneous material properties.

Modelling of slow crack front propagation at a finite temperature where long-range elastic interactions are dominant is of crucial importance to fill the gap in knowledge between experiments and models. Experimentally, there have been a number of studies on the advance of crack fronts in mode I, which have been shown to present a morphology following scaling laws different at small and large scales [4], an average dynamics compatible with an Arrhenius Law [5], and a velocity distribution displaying a heavy power-law tail P(v)∼v−2.6 [68], with important consequences for the large-scale behaviour of the crackling activity [9].

These experimental features are still not reproduced together by a unifying theoretical model, although a number of numerical and theoretical models have been proposed (see reviews [1,10]).

Most of the numerical and theoretical models so far have focused on so-called quasi-static models, defined by force equilibrium, corresponding to a temperature T = 0. Some models also consider a rheology with a viscous term linear in velocity [1,11]. Such models give rise to an intermittent local activity characterized by a depinning transition and can be viewed as a critical phenomenon [1]. However, these models fail to reproduce experimental conditions, as no temperature is introduced in the system. They produce crack velocities limited to a bimodal distribution (either the front is pinned or the front advance is instantaneous), and for most of them, front morphology does not display any cross-over length. These two features are in contradiction with the experimental observations [4,5]. Quasi-static fibre bundle models have recently been shown to give rise to a cross-over between two scaling regimes [12]. Elastic line models have also been shown to display two scaling regimes, which can be detected in avalanche distributions or in front morphology, and the cross-over was found to be proportional to the Larkin length [13]. Some elastic line models with small disorder lead to logarithmic scaling for the front roughness growth [14]. However, cracks in both kinds of models are still immobile when under a critical force threshold, unlike experimental ones that show a creep regime. Adding temperature into the system produces a thermal rounding of the depinning transition, allowing movement of the elastic line below the pinning force (e.g. [15]). This slow or creeping regime has been extensively documented from numerous experiments, notably in the context of rock mechanics (e.g. [16]). The mechanism of creep in random environments has also been studied both theoretically and numerically (e.g. [17,18]). Creep models often arise as a generalization, at a finite temperature T, of the models defined in the zero-temperature limit. The thermal rounding of the depinning transition, however, modifies several statistical features compared to extremal models; it notably induces a temperature-dependent correlation length defining scales at which annealed dynamics is dominating [15,19,20]. Little work has, however, been done on elastic line models at finite temperatures with long-range interactions (non-local kernel) in heterogeneous media—modelling has been done on the creep of elastic lines following a Paris Law, which characterizes the mechanics of fatigue [21]. These features of creep of an elastic line at finite temperature are of fundamental importance to render the crack propagation under realistic environmental conditions and are necessary for comparisons with experimental observations. We propose here a model comprising an annealed noise, represented by an Arrhenius Law, quenched disorder, i.e. a random distribution of local toughness, and long-range elastic interactions. Our numerical scheme incorporating these properties differs from those models used to solve similar problems at zero temperature, e.g. the extremal dynamics model [22] or the Bortz–Kalos–Lebowitz (BKL) algorithm [23].

In order to test the validity of our model, we compare its results with features reported in experiments during interfacial crack propagation. This experimental set-up is of particular interest, as it has allowed the direct observation of crack propagation and led to the characterization of numerous robust properties of the crack dynamics. We show that our model is in agreement with all reported properties, namely the distribution of the local speeds, the roughness of the crack front line and the macroscopic evolution of the crack. In addition to this numerical model, we also provide theoretical developments that explain the observed scaling laws, and predict their prefactors and cross-over as a function of the elastic parameters, quenched disorder distribution and temperature.

2. Model and method

We define the modelled interface as a square of dimension Lr × Lr over which a crack front, a(x, t), is propagating as a function of time t, in the direction y perpendicular to x. We denote L0 the distance between the loading point and the bottom edge of the modelled area. The crack front is thus bounded between L0 and L0 + Lr. The crack is lying on the middle of two plates of thickness h and width Lr (figure 1).

Figure 1.

Figure 1.

Geometry of the modelled configuration. The square of dimension Lr × Lr represents the area where we model the crack front propagation. (Online version in colour.)

Fluctuations of the fracture energy, Gc(x, y), over the interface are defined on a set of N discrete sites of size dl = Lr/N, using a Gaussian distribution of mean μGc and standard deviation σGc (figure 2).

Figure 2.

Figure 2.

(a) Example of a generated interface with N = 2048. The colours refer to the local values of Gc and the dark line is the crack front line propagating from bottom to top. The average position of the front along the x-direction is denoted Inline graphic. (b) Distribution of the local values of Gc for the surface shown in (a). In this example, we set μGc = 200 J m−2 and σGc = 50 J m−2. (c) Zoom on part of the interface around the crack front line. The area is represented by a black rectangle in (a). (Online version in colour.)

The crack front is then loaded by a macroscopic energy release rate, Inline graphic, based on the geometry of the experimental set-up [5], assuming a perfectly elastic behaviour of the bulk, and neglecting mode II loading [24]:

2. 2.1

where E is the Young modulus of the plate, h its thickness and u(t) and Inline graphic are the deflection of the beam and the average front position at time t, respectively [25]. The local fluctuations of the energy release rate along the crack front a(x, t) are expanded from the macroscopic values following [26]:

2. 2.2

where γ[a](x, t) is the influence function that reflects the static elastic interactions among sites due to the roughness of the front line:

2. 2.3

where PV denotes the principal value.

However, equation (2.3) is not suitable for numerical implementation, due to the inverse square (hyper) singularity. We also want to use periodic boundary conditions along x to avoid edge effects. Equation (2.3) may be reformulated using an integration by parts [26] to the weakly singular and more usual expression

2. 2.4

Its corresponding expression for Lr-periodic boundary conditions, obtained after a similar integration by parts, is (simply writing Inline graphic and assuming a(x, t) is Lr-periodic along x) γ(x, t) = − (1/Lr) Inline graphic. However, the spectral formulation introduced by Perrin et al. [27], consisting of expressing a(x, t) in (2.4) as a Fourier series of period Lr, is a very natural way of modelling periodic boundary conditions. As a test, we compute the energy release rate for simple front shapes, expressed from the real space and from the Fourier space formulations, to known analytical solution. We find that this spectral method provides more accurate results than our implementations of the other mathematically equivalent formulations above, so this is what is used for the numerical results shown in this paper.

Specifically, inserting the Fourier series Inline graphic in (2.4), and noting that Inline graphic, one gets

2. 2.5

(see also [28, §5]). For numerical implementation, the summation is truncated to some large integer, N, and the Fourier coefficients An are computed using the same number of sampled values aj(t) = a(j × dl, t) through the discrete Fourier transform (DFT):

2. 2.6

remembering that, for N even, the (single) Nyquist component of the DFT, at j = N/2, contains information of both the positive and negative Nyquist frequencies: DFT[a(t)]N/2 = AN/2 + AN/2 = 2ℜ(AN/2(t)). In more compact form,

2. 2.7

the DFT being evaluated with the FFTW fast Fourier transform (FFT) algorithm [29], keeping in mind that the discrete frequency n∈[0, N/2] for N even and n∈[0, (N − 1)/2] for N odd.

We then assume that the propagation of the crack at the local scale (i.e. the mesoscopic scale) is controlled by a process which is defined by an activation energy mechanism. As derived from numerous experiments [16] and as verified directly on the considered experimental set-up [5], the advance rate of the crack tip Inline graphic is dependent on the temperature T, on the energy release rate G, and on an activation energy which is here assimilated to the fracture energy Gc:

2. 2.8

with λ = α2/kBT, where α is an atomic length scale associated with the energy barrier of the fracturing process, kB is the Boltzmann constant and v1 is related to the velocity for breaking microscopic bonds.

This law arises from basic thermodynamics (see [25] for kinetic crack growth): for each atomic site undergoing potentially an irreversible breaking transition, there is an activation threshold in free energy ΔFc = Fc − F0, below which the material bond only vibrates without breaking, where F0 is the energy of the non-excited unbroken state of this site. This free energy is site-dependent, according to the material properties of this bond. Writing it as proportional to a surface energy, one gets ΔFc = α2Gc, where α is the separation along the surface of the elementary breaking sites. The probability that an energy level F above the basic energy state is reached is, according to statistical physics, a Boltzmannian distribution of the free energy: it is proportional to eF/kBT. If the density of energetic states is (roughly) constant—as, for example, for a quantized harmonic oscillator—the total probability that the element considered reaches a free energy allowing the breaking transition, above the activation energy ΔFc, is: Inline graphic. If this activation energy is exceeded, the site considered along the front can either break irreversibly, with a transition energy to the next state of basic energy F1, with a probability proportional to e−(F1F)/kBT; or it can alternatively unexcite without breaking, and come back to the unbroken state, towards state of basic energy F0, with a probability proportional to e−(F0F)/kBT. The probability that it transitions to a broken state, if the activation energy is reached, is thus e−(F1F)/kBT/[e−(F0F)/kBT + e−(F1F)/kBT], which approximates to e−(F1F0)/kBT, assuming that the broken state is sufficiently energetically favourable compared to the thermal noise level, i.e. that (F0 − F1)≪kBT. Since the energy difference between the broken and unbroken states is equal to the mechanical energy release over the surface α2 along the plane crack covered by the site, one has (F0 − F1) = α2G.

The state of activating and breaking the site irreversibly is thus

2.

This transition can happen at this basic probability with a characteristic microscopic attempt frequency ν (molecular collisional frequency arising from the characteristics of the phonons in the material, the ‘thermal bath’), and if the bond irreversibly breaks, the front advances locally by the length α. Hence, with v0 = αν, the speed of the front, averaged over a few attempt periods 1/ν, is Inline graphic, which is the Arrhenius Law in equation (2.8).

We also assume that the temperature is homogeneous and remains constant during the whole crack propagation. This approximation should hold if the temperature variations during the process are much smaller than the laboratory absolute temperature, which is around 300 K. For such constant-temperature situations, the choice of Gc and v1 in the rheology, equation (2.8), presents a redundancy: any change of these parameters preserving Inline graphic leads to an identical behaviour. In this paper, the choice made to raise the invariance under such change is to fix the value of Gc around the characteristic value during the fast stages of the considered situation. In other situations where variable temperatures would be considered, more details on the physico-chemistry of the material would be needed to fix independently Gc and the prefactor v1.

Once discretized, equation (2.8) is in the form of a classical system of N coupled ordinary differential equations (ODEs) with time t as the independent variable; it is solved using an eighth-order Dormand–Prince Runge–Kutta method as described in [30]. We introduce a flat initial crack front, a(x, t = 0) = 0, in the system at time t = 0, and a(x, t) is then represented at evenly spaced intervals over Lr along the x-axis. As values of Gc(x, y) are only defined at discrete sites, local values of the fracture energy, for arbitrary positions of a along y, are obtained through cubic spline interpolation along y. We tested that different interpolation functions or even no interpolation do not change significantly all the obtained results. We keep a snapshot of the front position every 1 ms in order to mimic what is obtained during experiments with a high-speed camera [6]. A direct visual comparison between crack dynamics shows at first order a good agreement between simulations and experiments (figure 3). We recover in the simulation a similar heterogeneous pattern of the front speed which varies of the same order of magnitude in simulations and experiments. In order to draw more quantitative comparisons between our model and experiments, we will then examine some well-defined properties of the experimental crack fronts.

Figure 3.

Figure 3.

(a) Simulation of a crack front propagation obeying equation (2.8). The front propagates from bottom to top, and the displayed interface has a dimension of 5.6 mm along x and 1.4 mm along y. The grey scales refer to the local crack front speed. (b) Crack front speed obtained during an experiment from Tallakstad et al. [7]. The dimensions of the interface are identical to (a).

3. Macroscopic crack evolution

We aim at testing the validity of our model by comparing its predictions with several independent experimental behaviours. We first set several a priori parameters of the model in order to match the experimental setting. The Young modulus is set to E = 3.2 GPa. Geometrical parameters are defined as: h = 5 mm, Lr = 2.84 cm, for the plate thickness and width, respectively. We set N = 2048. The average fracture energy is μGc = 200 J m−2 as a representative value of the experiments [5]. We invert for the values of v1 and λ from the macroscopic behaviour of the crack front by comparing the results of simulations with an experiment reported in [24] with two loading phases: phase I at a constant loading speed Inline graphic for 230 s, and phase II for which the deflection of the beam is maintained constant. The initial front position is L0 = 107.7 mm. We checked that higher values of N induce no change in the macroscopic evolution of the crack. Experimental data are well reproduced by the model when setting λ = 0.15 m2 J−1 and v1 = 0.031 m s−1 (figure 4). This suggests that the Arrhenius Law remains valid on a scale larger than the one at which it was set in the model [5]. It should also be noted that the value of λ corresponds to the value inferred experimentally by Lengliné et al. [5], who found λ = 0.15 m2 J−1, averaging over multiple experiments. The average velocity along the front v as a function of the average energy release rate Inline graphic, shown in figure 4b, was computed using the same technique as the experiments, using the velocity derived via the waiting time matrix (WTM) at a similar pixel scale (as in figure 3). This WTM analysis is based on the following: On a discrete regular grid, Wij is defined as the number of times a front is observed to cross this given pixel ij during an experiment. The front velocity while the front was at this position is then obtained as vij = Δx/(ΔtWij), where Δx is the spatial lattice step, and Δt the interval between two subsequent front positions (the frame rate in the experiments or the simulations). Alternatively, using instead directly the instantaneous velocities computed leads to a more disperse average velocity as a function of Inline graphic, with the same average value at a given Inline graphic. This instantaneous front velocity reduces to a similar behaviour as the one obtained via the WTM when this velocity is averaged over time windows of 0.03 s or larger.

Figure 4.

Figure 4.

(a) Evolution of the crack front position during an experiment (blue line from Lengliné et al. [5]) and from the simulation (red line) using λ = 0.15 m2 J−1 and v1 = 0.031 m s−1. The vertical black line separates phase I at constant loading rate and phase II, the relaxation phase. (b) Evolution of average crack speed Inline graphic as a function of the energy release rate Inline graphic for the experimental data (blue) and for the simulation (red). The dashed line shows a fit of the form of equation (2.8) with λ = 0.15 m2 J−1 and v1′ = 0.013 m s−1; v1′ is slightly lower than v1 (the difference between v1 and v1′ decreases slowly with σGc here taken as σGc = 50 J m−2). (Online version in colour.)

4. Distribution of local speeds

At the local scale, we evaluate the distribution of the crack front speeds in our model. As reported in [57], the distribution of local speeds higher than the average crack front velocity is found to decay as a power law with exponent η =  − 2.55. We selected a period when the average speed of the crack is approximately constant and computed the local speed distribution similarly to the procedure introduced by Måløy et al. [6]. Exploring the parameter space, we observed that the simulated distributions are controlled by the parameter (σGc/μGc)2λ = 1/ρ (as illustrated in figure 5 where several toughness distributions produce the same velocity distribution). Moreover, N does not have a significant influence on the value of η. For ρ≃125 J m−2, we find that the power-law decay of the distribution at high velocities exhibits a slope compatible with the experimental observations, i.e. η =  − 2.55. Given the value of λ = 0.15 m2 J−1 as deduced from the macroscopic evolution of the crack, we then deduce σGc = 50 J m−2 for μGc = 192 J m−2. It is worth mentioning that the standard deviation σGc = 50 J m−2 matches the one observed experimentally [5]. At higher values of ρ, i.e. lower quenched disorder, the logarithm of the probability distribution function is closer to a quadratic function of log(v) around its maximum, i.e. the distribution is close to lognormal—see insert of figure 5, ρ = 500 J m−2. When the quenched disorder is large enough, a power-law tail at high velocities is observed over around two decades for the distribution of velocities, with the observed exponent in the range η between 2.2 and 3 for the probed values of ρ.

Figure 5.

Figure 5.

Probability density functions (PDFs) of the local crack velocity computed from simulations. Local crack velocity is normalized for each simulation by the average crack front velocity 〈v〉. Collapse of four distributions for the same ρ≃125 J m−2 (triangles, λ = 0.13, μGc = 200, σGc = 50; circles, λ = 0.2, μGc = 200, σGc = 40; squares, λ = 0.08, μGc = 200, σGc = 63; stars, λ = 0.13, μGc = 160, σGc = 40). Black dots correspond to experimentally obtained speed distributions taken from Tallakstad et al. [7]. A power law with an exponent η =  − 2.55 (dashed line) is consistent with the PDF tail for v/〈v〉 > 1 as observed experimentally [6]. Inset: PDFs for two other values of ρ: 500 J m−2 and 62.5 J m−2. (Online version in colour.)

5. Front morphology

We also investigated the scaling of the crack front morphology. Previous experimental studies reported that the crack front is self-affine with a roughness exponent ζ≃0.6 (e.g. [31,32]). More recent data extracted from numerous experiments and at various scales show that actually two distinct regimes emerge depending on the scale of investigation: at small scales, the scaling regime is characterized by a roughness exponent ζ≃0.60 while at large scale the exponent is lower and is found around ζ+≃0.35 [4]. From simulations at constant loading velocity, we first investigate the scaling of energy release rate profiles, G(x), before turning to the scaling of a(x). These profiles correspond to the local values of energy release rate for all points on the crack front. We compute the scaling properties of the crack energy release rate profile after averaging 1000 power spectra evenly time-spaced (after a transient regime from an initial condition of a flat front). The crack energy release rate along the front is defined as G(x, t) = G(x, a(x, t)), expressed from equation (2.2) along the modelled fronts of shape a(x, t). We first look at its spatial Fourier power spectrum, PG(k), for a simulation running with parameters deduced from previous tests, namely we use λ = 0.13 m2 J−1, μGc = 200 J m−2 and σGc = 50 J m−2. We see in figure 6 that PG(k) becomes flat in the high-wavenumber domain, reaching the value σ2Gc. This upper limit corresponds to the expected power spectrum of a straight one-dimensional line cut through the Gc(x, y) field. It suggests that, at small scales, fluctuations of energy along the crack front line follow the quenched disorder variations, with a power spectrum insensitive to the deviations between the curved front and a straight line at the average front position. For lower wavenumbers, PG(k) deviates from the constant threshold and becomes a growing function of k (decreasing as k diminishes, as seen in figure 6). We can well render the evolution of PG(k) at these large scales with a relation of the form PG(k)∝k.

Figure 6.

Figure 6.

Power spectra of the energy release rate, PG(k), computed for different simulations. The spectrum in red is computed for a simulation with λ = 0.13 m2 J−1, μGc = 200 J m−2 and σGc = 50 J m−2. For the other spectra: σGc = 10 J m−2 and λ = 0.21 m2 J−1 for the spectrum in green and λ = 0.05 m2 J−1 for the one in blue; for the spectrum in magenta, we keep λ = 0.13 m2 J−1 but change μGc to 100 J m−2. The horizontal dashed lines correspond to σ2Gc while the slanted dashed lines are given by PG(k) = Cλσ2GcμGck. We denote ω+ and ω the prefactor of PG(k) at large scale and the level of PG(k) at small scale, respectively. (Online version in colour.)

We also report in figure 6 several simulations where the parameters λ, μGc and σGc were modified in order to test their influence on the spectrum of the energy profile. For all simulations, we always observe the threshold at high wavenumbers corresponding to σ2Gc and also evidenced PG(k)∝k at low k. We can evaluate from the tested parameters that, at low k, PG(k) = Cλσ2GcμGck, with C a constant—as seen from the consistency of the simulation data and the dashed lines in figure 6. By equating the power spectra in the two spatial frequency domains, we infer the cross-over, kδ, above which the energy of the front line follows the energy profile of the medium. We obtain kδ = 1/(λμGcC), which implies that the cross-over is independent of the amplitude of the quenched disorder fluctuations, σGc, but varies with the temperature and the mean toughness of the interface, μGc.

We can now turn to the scaling of the front position. As indicated from equation (2.6), the scaling of a is related to the scaling of G. Indeed, from equation (2.7) we have

5. 5.1

with K(n) = − 2π|n|/Lr, and the equivalent formulation in the continuous domain, since the wavenumber n is related to the wavevector k as kn = 2πn/Lr, is given by

5. 5.2

where the tilde denotes the Fourier transform defined as Inline graphic.

Expressing in the Fourier space the link between the energy release rate G and the elastic kernel γ, recalling equation (2.2), we get for any non-zero wavevector k,

5. 5.3

since the additive constant term in equation (2.2) only contributes to the k = 0 mode, and the multiplicative prefactor Inline graphic is independent of position.

We thus expect from these last two equalities, for the power spectra Pa(k) and PG(k) of the front shape a(x) and of the energy release rate G(x):

5. 5.4

which, given the observed scaling of PG(k), translates into

5. 5.5

We indeed observe the aforementioned crack front morphology in our numerical simulations (figure 7), i.e. we obtain the two regimes discussed above. At long wavelengths, the observed roughness exponent is ζ+≃0.0 while, at shorter length scales, ζ is 0.5. This is compatible with the experimental observations [4], where at short length scales, ζ≃ 0.5 is determined, while at larger scales, a flattening to lower exponents is observed—which is compatible with local exponent ζ+≃ 0.3 to 0.4, and also compatible with a slow cross-over towards a flattening ζ+≃0 (which corresponds to a subpower scaling law, as a logarithmic behaviour |a(x + Δx) − a(x)|∼log(|Δx|). (This reference mentioned: ‘At large scales, we observe a cross-over to another scaling regime with a smaller roughness exponent ζ = 0.35 ± 0.05. Our data do not rule out a possible slow cross-over to a flat front (no disorder regime), at large scales.’) Indeed, in the simulation a local ζ+≃ 0.35 is compatible with the results over one to two decades of cross-over, as illustrated by the compatibility with the lines in figure 7 around the cross-over scales, and as observed in the experiments [4].

Figure 7.

Figure 7.

Inset: Average power spectrum (Pa(k)) computed over 1000 crack fronts during simulations when varying λ = α2/kBT. Units of the parameters in the legend are for Gc, J m−2, for λ, m2 J−1, and for v1, m s−1. Main: Collapse of all power spectra at different temperatures after rescaling the wavenumber k* = k/kc = (k/kref)(Tref/T), and the norm according to the predicted prefactor. The two power laws corresponding to the continuous curve have slopes −1 and −2, i.e. correspond to Hurst exponents ζ+ = 0 at large scales (small k, logarithmic scaling), and ζ+ = 0.5 at small scales (large k). (Online version in colour.)

In order to show the influence of temperature on the variation of kδ, we show the averaged power spectra for different temperatures (i.e. different λ) which can be nicely superimposed by introducing a normalized wavenumber k* = k/kc = (k/kref)(Tref/T) where Tref is a reference temperature and kref a reference wavenumber (figure 7). As will be shown in Section 6, the constant (Tref/kref) depends on the correlation length lc of the quenched disorder, i.e. the critical energy release rate Gc, and its average value μGc, as Tref/kref = α2lcμGc/(2kB).

Interestingly, the cross-over Rc = 1/kδ between the two domains can be estimated for λ = 0.13 m2 J−1 and μGc = 200 J m−2 to be approximately 1 mm, which is comparable to the value reported experimentally [4]. The observed dependence of the cross-over length on temperature has been previously noticed for different models. In the case of short-range elastic interactions, it is found that Rc varies with T with a power-law exponent depending on the percolation properties of the active sites [19]. Other studies proposed that the cross-over length scale might also depend on the difference between the driving force and the depinning threshold (e.g. [17,20]). We also observe that changing the cut-off wavelength of the toughness correlation, lc, influences the cross-over scale Rc, which can be seen as a temperature effect.

6. Theoretical interpretation of the dominant forces at large and small scales

The dynamics of the crack front, at finite temperature, is led by the Arrhenius Law from equation (2.8), with the energy release rate by equation (2.2) as the product of the average value Inline graphic from equation (2.1), and the elastic perturbation γ[a], which depends on the shape of the front a(x) as stated by equation (2.3):

6. 6.1

and

6. 6.2

The quenched disorder associated with the material properties corresponds to a spatial distribution of the critical energy release rate:

6. 6.3

Inserting equations (6.2) and (6.3) into equation (6.1) leads to

6. 6.4

Assuming that the average critical energy release rate along the front during propagation is around the average value of the quenched distribution in the plane, Inline graphic, we can write

6. 6.5

where

6. 6.6

This last equation can be expressed with a one-dimensional Fourier transform as

6. 6.7

The product above can be considered as follows: each of the product terms have a form

6. 6.8

where ℜ(z) and ℑ(z) refer, respectively, to the real and imaginary parts of the complex number z. The second term in the product is the exponential of a pure imaginary number, of norm 1: it does not affect the norm of the product. The first term in the product can be written as

6. 6.9
6. 6.10

where

6. 6.11

For any k, there are positions x≃ − θ[2π]/k where the product above reduces to Inline graphic.

Hence, if the norm ∥z∥ is not significantly smaller than 1, then for certain positions x, the value of the term in the product, Inline graphic, becomes exponentially large, so that the front speed will become locally large, and the unpinned front shuffles very fast, during an avalanche, through new configurations of the quenched disorder—until this term ∥z∥ becomes small again for all k.

Three cases can be considered to obtain the value of Inline graphic: If Inline graphic, this term can be approximated as Inline graphic, and z is given by Inline graphic. The magnitude of this is of order λσGc, which is smaller than 1, allowing one to approximate Inline graphic. When Inline graphic, the order of magnitude of z is also ∥z∥ ≤ λσGc, smaller than 1. Eventually, if Inline graphic, one has Inline graphic. Since λσGc is a finite number (around 0.1 to 1 in the simulation examples, corresponding to the experimental match), this case where ∥z∥≫λσGc also corresponds to ∥z∥≫1, which is discussed in the previous paragraph: this situation is unstable and corresponds to a large velocity, an avalanche during a depinning event.

The product of all these exponential terms, in a configuration where they are stabilized in situations where Inline graphic, will be denoted R(t), and apart from the fast avalanches, it will stay constant, around 1.

Conversely, for other values of k, the perturbation due to the elastic interactions will always be small in front of the quenched disorder, i.e. at all times, we will have

6. 6.12

so that for all positions x, at all times, we will have

6. 6.13

For these modes, with Inline graphic, and ∥ϵk∥≪1, the exponential terms in the sum can be approximated as Inline graphic, and the product, to leading order, as

6. 6.14

For these modes, there will be constantly slow accelerations or decelerations around an average rate of change.

With these considerations over the two types of modes, the sum over non-zero wavenumbers can thus be approximated as follows in equation (6.7): large terms are unstable in this sum, since the velocity depends exponentially on the sum, and the sum blows up quickly when a term grows above the average. When the terms of the sum are small with respect to 1, they modulate the velocity with respect to the average velocity. We conclude that there are two possible cases for the interaction term: either it is small enough so that

6. 6.15

or, after a very short time, the Fourier component jumps to a new value where it is comparable to the average velocity. Apart from the very short unstable times where the velocity jumps far from the average, the Fourier modes take random values within the characteristic value:

6. 6.16

Considering the case where interactions are small, the velocity, from equation (6.7), can thus be expressed as

6. 6.17

where the sum is limited over wavenumbers that produce a stable propagation of the front. R(t) is the fluctuating term taking into account the jumps to bring back the argument of the exponential to the average value by reshuffling the values of Inline graphic that go for short periods beyond the saturation level: it is most of the time around 1, with these short periods of large values above it—intermittent avalanches.

As introduced above, in the other case for the interaction term, we have a saturation so that Inline graphic We first focus on this case, which defines the range where elastic interactions are balancing quenched noise amplitude. The level of saturation is set by the amplitude of the quenched disorder fluctuations with respect to the average. Indeed, the power spectrum, PG(k), is given by equation (6.2), valid for any k≠0:

6. 6.18

Since, in the considered case

6. 6.19

we can write

6. 6.20

and as Inline graphic, for non-correlated quenched noise, the power spectrum PG(k) scales as

6.

This theoretical prediction is satisfied, as shown by the various levels of dashed lines at large wavenumbers in figure 6. This behaviour of saturation of the interaction kernel at large k, i.e. at small scales, is identical to the one expected in a quasi-static model, in which the elastic kernel exactly balances the quenched disorder. Hence, this model at finite temperature predicts, at small scale, front morphologies comparable to those expected in such models [3335].

Hence, at small scale, the amplitude of the Fourier mode of the elastic kernel saturates around a characteristic amplitude. This has a direct consequence on the front morphology: this elastic kernel can also be expressed as a function of the front shape, which in Fourier space reads from equation (5.2) as

6. 6.21

Since, from equation (6.20), Inline graphic, this implies for the Fourier amplitude of the front shape Inline graphic, at these scales, that

6. 6.22

i.e.

6. 6.23

or, for non-correlated quenched noise, since Inline graphic one expects a power spectrum of the front as

6. 6.24

i.e. a self-affine scaling [4] with a Hurst exponent ζ such that −2 = − 1 − 2ζ, i.e. ζ = 0.5.

On the contrary, for the other case, Inline graphic i.e. elastic interactions are well below the quenched noise amplitude. Using this, one can linearize equation (6.17), leading to

6. 6.25

which describes the evolution of the crack front line when interactions are small. It will be shown later that this behaviour is observed at large wavelength, i.e. small wavenumber. For this domain, one has, as shown above, using the average value R(t)∼1 as an approximation for R(t), which is most of the time around such value:

6. 6.26

This ODE can be integrated in time, noting that:

6. 6.27

so that, by the variable constant method,

6. 6.28

and the solution can be expressed as:

6. 6.29

The process is thus similar to an anomalous diffusion with a random term arising from the quenched disorder through which the system goes at average speed, Inline graphic. Such anomalous diffusion systems are common in systems with interactions, e.g. in fluctuating dipolar chains [36,37]. The first term represents the convolution of the random term due to the material variable properties by the response function representing the memory of the system, Inline graphic. The second term represents the memory of the initial conditions. For initially straight fronts, it is equal to zero. For large enough propagation times, one can also write:

6. 6.30

This system presents a generalization of anomalously diffusing systems in thermal baths with fat-tail memory [37,38]. It is interesting to see that an annealed-like noise arises from propagating the front through the quenched noise at a certain speed. Similarly to such anomalously diffusing systems, one can evaluate the amplitude of the Fourier mode after some time. From the auto-correlation function of a Fourier mode, averaging over starting time t2, for a fixed time lag t1 − t2, one gets

6. 6.31

where the star denotes the complex conjugate. We will use the fact that the quenched disorder is uncorrelated above a size lc, to approximate its Fourier transform along the front as the one obtained for a straight line travelling at speed Inline graphic in this landscape:

Along such straight fronts at positions Inline graphic and Inline graphic, the values of Inline graphic and Inline graphic correspond to a white noise of square amplitude σ2Gc that are correlated for spatial distances |x′ − x′′| < lc (where lc is defined as the correlation range of the quenched disorder), and time lags such that Inline graphic. Hence, expressing this condition with a Heaviside function Θ as Inline graphic, the resulting time integration kernel in the equation above can be expressed as

6. 6.32

with δ(t′ − t′′) the Dirac function. In Fourier space, with DFT of steps lc, this corresponds to

6.

with δkk the Kronecker symbol. We checked in the numerical model the validity of this approximation.

This can be used in equation (6.31) to obtain the time correlation of the Fourier modes of the front shape:

6. 6.33

This leads to the auto-correlation function of the front shape after time has led it to saturation:

6. 6.34

The decorrelation time of these Fourier modes is thus scale-dependent, with Inline graphic. The amplitude of the k wave mode of the front shape is given as

6. 6.35

This corresponds to a self-affine behaviour with a Hurst exponent 0, as predicted for elastic lines in annealed noise, as e.g. analysed by [34,39], i.e. a total amplitude for points at separation ΔL along the front scaling logarithmically as WL)∼log(ΔL). For the elastic interactions for these large-scale modes, from equation (6.2), this leads to

6. 6.36

Assuming that the effective average value of G during propagation scales as the average value μGc of the quenched disorder Gc, one gets

6. 6.37

This is indeed the scaling found for small k: the amplitude of the Fourier transform of the energy release rate is proportional to k for large wavelengths, and this theory explains the numerical findings for the prefactor, i.e. that PG(k) = Cλσ2GcμGc|k|.

According to these analytical considerations, for small k, we have Inline graphic and the front propagates similarly to an elastic line in an annealed noise of average μGc, fluctuations of standard deviation σGc, and time correlation Inline graphic (figure 8). For larger k, the argument of the exponential in the Arrhenius Law saturates, so that Inline graphic: the small-scale (large-k) wave modes are pinned on the quenched disorder, and the front propagation is similar to that of a quasi-static elastic line model: this corresponds to a flat spectrum of the energy release rate at a characteristic level PG(k)∼σ2Gc; and the front presents a Hurst exponent of 1/2 (figure 8).

Figure 8.

Figure 8.

Comparisons between the predicted values of the energy release rate power spectrum PG(k) and the observed values in the simulations. Predictions of the values of PG(k) are given at large scale by equation (6.37) and are compared to values extracted from simulation results ω+. At small scale analytical results predicted by equation (6.20) are compared to the values ω corresponding to the plateau PG(k) in simulations.

The system toggles between annealed and quenched behaviour at the scale where the energy spectrum becomes comparable to the large-k saturation value, i.e. at a characteristic scale 2π/kc, so that

6. 6.38

i.e.

6. 6.39

These scalings for the power spectrum of G allow one to predict a collapse for the power spectra of the energy release rate, as PG(k)/σ2Gc as a function of k/kc:

6. 6.40

Indeed, all simulations collapse on the predicted scaling function, as seen in figure 9. For the shape of the front, this scaling predicts the following collapse of the Fourier power spectra of the front shape a(x):

6. 6.41

Indeed, all simulations collapse in this representation, on scaling functions corresponding to these predicted prefactors, as seen in figure 7.

Figure 9.

Figure 9.

Inset: Power spectra of the energy release rate, PG(k), computed for different simulations. Units of the parameters in the legend are for Gc, J m−2, for λ, m2 J−1, and for v1, m s−1. Main: When the spectrum is rescaled by σ2Gc, and the wavenumbers as k/kc with kc = 2/(lcλμGc), the power spectra collapse, according to the theory. The two continuous lines correspond to PG(k)/σ2Gc = 1 and PG(k)/σ2Gc = k/kc. (Online version in colour.)

Recalling that λ = α2/kBT with α a characteristic size between breaking elements projected over the average plane, kB the Boltzmann constant and T the absolute temperature (in kelvin), and that lc is the correlation length of the quenched disorder and μGc its average value, the critical length in the system is

6. 6.42

Above this size, the system is dominated by thermal fluctuations (i.e. it behaves as if the noise were annealed), and below it is essentially pinned by the quenched noise: indeed, we have established above that for scales below Rc (k larger than kc), the self-affine character of the morphology comes from an equilibrium between the elastic interactions and the quenched disorder (Inline graphic), as in a quasi-static model. Conversely, for the scales above Rc (k smaller than kc), the elastic interaction term is small (Inline graphic), the dynamic equation for the Fourier mode of the front ak(t) can be linearized, and the dynamics corresponds to the linear response of an elastic line in an annealed noise—where this pseudo-thermal noise arises from sampling the quenched noise with a homogeneously advancing front.

Around this scale Rc, the front shape deviates from the small-scale self-affine scaling with a Hurst exponent of 0.5, with a progressive flattening of the slope in Fourier mode. This could be the origin of the smoothening observed at large scales, as reported in [4]. For the experimentally determined values λ = α2/kBT∼0.13 m2 J−1, μGc = 200 J m−2, and a correlation size of the quenched disorder lc = 2.8 × 10−2/2048 m≃13.7 μm, this corresponds to a critical value Rc around 1 mm. This corresponds indeed to the cross-over values seen in figures 6 and 7. This also corresponds, in order of magnitude, to the experimental range, where a softening of the front scaling is found [4].

7. Discussion

The results of our numerical simulations show a good agreement with various experimental observations. We first documented at the macroscopic scale the propagation of the crack that well renders an Arrhenius Law behaviour defined by equation (6.1) and observed experimentally. It is noteworthy that, even when the elastic energy at the crack tip is lower than a critical threshold (similar to a Griffith energy criterion), we reproduce the propagation of the crack. This creeping behaviour results from the introduction of a finite temperature in the model compared to quasi-static simulation defined at T = 0. Our results show that the global response of the system is similar to the local response imposed at the mesoscale, provided that the fluctuations of the interface disorder are not too high.

As a second step, we turned to comparisons between simulations and experiments at the local scale. We showed that the shape of the local front velocity distribution is governed by a parameter ρ = μ2Gc/(σ2Gcλ), with λ = α2/kBT. The higher the relative disorder fluctuation term (σGc/μGc) or the lower the temperature T, the broader the distribution of local speed. Extrapolating ρ to a very low value will then produce a very intermittent activity with very fast movements and long repose periods of local velocity. This is expected when the thermal rounding is very sharp and is similar to a pinning regime. On the other hand, for high values of ρ, i.e. for high temperature or low disorder fluctuations, the velocity becomes more homogeneous and local sites along the front are all propagating around the mean crack velocity. For a set of parameters corresponding to those encountered experimentally, we have shown that we are able to reproduce the correct shape of the velocity distribution, notably, we reproduce the correct power-law decay of the PDF tail with exponent η =  − 2.55. It is remarkable to note that such power-law decay is a very robust experimental observation. Indeed, if one interprets this result in light of our simulations, changing significantly the shape of the velocity distribution requires an important change of the experimental conditions (for example, a fourfold decrease of the absolute temperature for the case reported in figure 6).

We made a final comparison between our simulations and experimental data concerning the morphology of the crack front line. We showed that our simulations display a crack front morphology with a cross-over length separating two regimes: a regime with a Hurst exponent ζ+ = 0.0 at large scale and a regime with a higher Hurst exponent ζ = 0.5 at a smaller scale. This cross-over between two regimes has also been reported experimentally, with the transition to a higher Hurst exponent at small scale [4]. We note that there still exists a difference between exponents obtained in our simulations and those observed in experiments. Distinguishing if this discrepancy arises from a limited resolution on the experimental data or if other phenomena may have been neglected in our model is difficult to assess. We nevertheless obtained estimates of the roughness exponents quite close to the experimentally observed ones. Furthermore, the cross-over length scale reported in our simulations is of the correct order of magnitude compared to the one described in experiments. Results of our simulations concerning roughness exponents of the crack front are also validated by theoretical derivations from the Arrhenius model. This theoretical analysis also leads us to determine the physical mechanism operating above or below the cross-over length Rc. In a first regime, at large scale, elastic interactions are well below the quenched noise amplitude and the front propagates similarly to an elastic line in an annealed noise. At smaller scale, below Rc, elastic interactions are balancing quenched noise amplitude and the front propagation is similar to that of a quasi-static elastic line model. We note that the quasi-static elastic line model gives a Hurst exponent H = 0.35–0.39, somewhat lower than the value obtained here at small scale (e.g. [22]). However, in this model and in the regime of small fluctuations of the crack front line, the Hurst exponent takes a higher value H = 0.5, similar to the one found here [33]. It suggests that in the small-scale regime, our model is similar to the elastic line model in the presence of small fluctuations. A speculative explanation for this observation is related to the different dynamics between our model and the quasi-static elastic line model. In our model, all points along the crack front line are moving at each time step, maintaining the crack front line in an equilibrium position at each time step. In the quasi-static elastic line model, only one point is advanced at a time and reaches its new equilibrium position. The dynamics of the crack front line introduced in our model could thus be an explanation for the H = 0.5 exponent rather than the value H = 0.35–0.39.

Recent studies have suggested that the use of the elastic kernel as proposed in [26] should be taken cautiously as it is limited to the approximation of an infinite medium [40]. Finiteness of the medium is suspected to have an influence on the reported scaling. However, the shape of the elastic kernel computed in [40] is the same as in the infinite case for a range of interactions smaller than the plate thickness. Since the experimental data available and compared to the current model are essentially in a scale range equal to or smaller than the thickness, this justifies that the modifications of the kernel due to finite thickness can be neglected. Preliminary simulations incorporating the elastic kernel computed in [40] that accounts for the finiteness of the elastic medium, i.e. for the limited thickness of the polymethyl methacrylate (PMMA) plate, confirm the validity of this approximation (but analysing what happens at large scales, above the thickness, is beyond the scope of the current paper).

A limitation of our study is that it is restricted to cracks propagating at low velocities. This choice of restricting our simulation to slow speeds is motivated by the main purpose of this article, which aims at comparing the results of the model with experimental cracks propagating in the same velocity range. Although no influence of the velocity was observed on the reported scaling during our simulations, it is possible that such effects might appear at higher speeds. It is also readily possible that other effects may manifest at higher speeds when approaching the rupture velocity of the material. In particular, at the local scale, dynamic rupture might take place, as observed experimentally by the recording of acoustic emissions [41], and might influence the crack propagation by redistributing elastic stress [42]. In our simulations, we did not consider any dynamic effect and implicitly hypothesized that these dynamic effects have a limited influence on the tested crack front features. Limiting the complexity of our model also allows us to track more easily any individual effect induced by each of its parameters. We also show that, despite its simplicity, our model is able to reproduce all reported robust experimental features.

A second approximation made in our model is the hypothesis of a homogeneous and constant temperature field. It is indeed quite likely that the fracturation process in experiments releases some heat at the crack tip as observed in PMMA [43]. Local increases of temperature have the ability to change the local crack propagation speed in our model as defined by equation (2.8). However, we hypothesized that at the scale of investigation this effect can be ignored in our model. Temperature increase of a few degrees around crack tips was observed or modelled in the case of fatigue in steel [44], or locally tenth of degrees or more in the case of fracture in paper [45]. This choice of negligible temperature increase at the crack tip in the current model was done for simplicity as a first approximation, and is shown to produce some agreement with the experimental observations. Incorporating the impacts of crack tip temperature elevation is the subject of ongoing further research.

It is also likely that other processes, not taken into account in our model, play some role in the propagation of cracks in heterogeneous media and may also offer alternative explanations for some of the observed features. For example, it is noteworthy that other groups [8,46] were able to capture some of the experimental features exposed here, such as the velocity distribution, while not considering the effect of temperature in the crack propagation. The model of Laurson et al. [13] could also capture two scaling laws in the front morphology. The cross-over length found there, proportional to the Larkin length, differed from the one identified in the model presented here. Interestingly, a recent model of interfacial crack propagation was also able to capture much of the experimental data tested here (velocity distribution and roughness exponent) [12]. In this model, the cross-over of the roughness exponent is related to the transition from a percolation regime at small scale (giving H = 2/3) to an elastic line model at larger scale (H = 0.39). It thus remains to distinguish at which scale each of these mechanisms is governing the scaling of the front morphology. This investigation is left for further study.

The results of this model can also be analysed in the light of the classification between strong pinning regime and weak pinning regime, reported for elastic lines propagating with a Paris Law creep rheology [21]. For these models, smooth values of quenched disorder map lead to a dynamics where G = Gc (or equivalently, K = Kc, with K the stress intensity factor) all along the front: this is termed the weak pinning regime. By contrast, for quasi-static models (as e.g. in [22]), a behaviour where G ≤ Gc (or K ≤ Kc) is observed, which is termed the strong pinning regime, and attributed to sharp transitions in quenched disorder [21]. With respect to this classification, the model presented in the current paper is neither in the weak nor in the strong pinning regime, but rather in one or the other depending on the scales considered: as shown above, the front at small scales follows a weak pinning regime behaviour, with a scaling dictated by Inline graphic for k > kc. By contrast, at large scales, for k < kc, the scaling is dictated by the thermal noise rather than the quenched disorder, and one has Inline graphic, which, in the terminology of [21], corresponds to a strong pinning behaviour. The exact scaling at these large scales, as shown in the previous sections, can be computed from the diffusion of an elastic line in a thermal noise.

Our model has been intentionally limited to a one-dimensional line model in order to test the results of our simulations with experimental observations of in situ crack propagation. It is appealing to generalize the results of our model to higher-dimension systems and in particular to fault systems. Discussing our results in terms of fault mechanics provides an insight into the notion of seismic coupling. The seismic coupling coefficient is defined as the ratio of seismic to aseismic deformation on a fault plane in a bounded geographical area. In our configuration, if one accepts to extrapolate the computed velocity distribution to dynamic rupture speed, then the ratio of seismic to aseismic deformation would be given by the level of the distribution tail in the range of dynamic speed. As we have shown, this level is governed by the parameter ρ. Linking our geometrical configuration to a simple one-dimensional fault model as proposed in [47,48] we can thus interpret our results in terms of slip on faults. In particular, our results give a possible interpretation for this notion of seismic coupling with the introduction of the coefficient ρ. This coefficient is shown to vary with temperature, which exhibits large-scale variations within the Earth. It is also proposed to vary with the amplitude of the toughness heterogeneities on the fault plane, due for example to the presence of asperities on the interface. Such conclusions are in agreement with the conceptual model proposed in [49].

8. Conclusion

In conclusion, we presented a model of crack propagation in heterogeneous media governed by an Arrhenius Law. Despite its simple expression, we showed that our model is in full agreement with all reported features of interfacial crack front propagation in the presence of disorder (morphology, speed distribution and macroscopic dynamics): the speed distribution is found to present a non-Gaussian power-law tail p(v)∼v−2.6. The front morphology is found to obey a self-affine scaling with a Hurst exponent around H∼0.5 at small scales, and a cross-over to H∼0 at large scales. These features are different from purely quasi-static models, where only quenched noise is included, without the thermal part: indeed, in such models, the power-law distribution of the local speeds has not been obtained, no large-scale flattening is observed. By contrast with quasi-static models, our model also predicts the creep behaviour, i.e. the correct non-zero large-scale velocity at fixed loading.

The parameters inferred in our model which best reproduce the experimental observations correspond to realistic values encountered during experiments. Our numerical results are supported by an analytical analysis explaining why thermal noise plays a role at large scales and why quenched disorder plays a role at small scales. This theoretical development also predicts both scaling regimes of the crack shape, and how the cross-over scale depends on the characteristics of the disorder, on the size of the breaking elements, and on temperature. We also showed that the existence of a parameter, ρ = μ2GckBT/(σ2Gcα2), governs the shape of the local speed distribution. This parameter is defined from the temperature of the system T, a size connected to the individual breaking of molecular bonds α, and the relative fluctuations of the quenched disorder σGc with respect to the characteristic energy release rate μGc. We finally emphasize that our results explain why, even in the presence of disorder, macroscopic observations of slow crack growth are well modelled by an Arrhenius relation, and highlight the importance of thermal fluctuations in governing the propagation of a crack which yields characteristic properties not only at a global scale but also at a small scale. It also opens some possibility of inverting physical parameters related to the crack environment from the observation of its dynamical and morphological features.

Acknowledgements

The authors thank S. Santucci, T. Vincent-Dospital, E.G. Flekkøy, K.T. Tallakstad, A. Hansen and L. Ponson for insightful discussions.

Data accessibility

The numerical code is accessible upon request to the authors.

Authors' contributions

R.T., A.C., O.L. and K.J.M. stated the basis of the model. A.C. and O.L. wrote the numerical model. A.C. and O.L. ran the model and generated the figures. R.T. together with K.J.M. performed the analytical developments. R.T., O.L., A.C. and K.J.M. wrote the text. All authors read and approved the manuscript.

Competing interests

We declare we have no competing interests.

Funding

The authors acknowledge the support of the LIA France–Norway D-FFRACT, the Universities of Strasbourg and Oslo, the CNRS-INSU, the ITN FLOWTRANS and the ANR LANDQUAKE. This work was partly supported by the Research Council of Norway through its Centres of Excellence funding scheme, project no. 262644.

References

  • 1.Bonamy D, Bouchaud E. 2011. Failure of heterogeneous materials: a dynamic phase transition? Phys. Rep. 498, 1–44. ( 10.1016/j.physrep.2010.07.006) [DOI] [Google Scholar]
  • 2.Anderson TL. 1995. Fracture mechanics—Fundamentals and applications, 2nd edn Boca Raton, FL: CRC Press. [Google Scholar]
  • 3.Scholz CH. 2002. The mechanics of earthquakes and faulting. Cambridge, UK: Cambridge University Press. [DOI] [PubMed] [Google Scholar]
  • 4.Santucci S, Grob M, Toussaint R, Schmittbuhl J, Hansen A, Maløy KJ. 2010. Fracture roughness scaling: a case study on planar cracks. Europhys. Lett. 92, 44001 ( 10.1209/0295-5075/92/44001) [DOI] [Google Scholar]
  • 5.Lengliné O, Toussaint R, Schmittbuhl J, Elkhoury J, Ampuero J, Tallakstad K, Santucci S, Måløy K. 2011. Average crack-front velocity during subcritical fracture propagation in a heterogeneous medium. Phys. Rev. E 84, 036104 ( 10.1103/PhysRevE.84.036104) [DOI] [PubMed] [Google Scholar]
  • 6.Måløy KJ, Santucci S, Schmittbuhl J, Toussaint R. 2006. Local waiting time fluctuations along a randomly pinned crack front. Phys. Rev. Lett. 96, 045501 ( 10.1103/physrevlett.96.045501) [DOI] [PubMed] [Google Scholar]
  • 7.Tallakstad KT, Toussaint R, Santucci S, Schmittbuhl J, Måløy KJ. 2011. Local dynamics of a randomly pinned crack front during creep and forced propagation: an experimental study. Phys. Rev. E 83, 046108 ( 10.1103/PhysRevE.83.046108) [DOI] [PubMed] [Google Scholar]
  • 8.Santucci S, Tallakstad KT, Angheluta L, Laurson L, Toussaint R, Måløy KJ. 2018. Avalanches and extreme value statistics in interfacial crackling dynamics. Phil. Trans. R. Soc. A 377, 20170394 ( 10.1098/rsta.2017.0394) [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 9.Tallakstad K, Toussaint R, Santucci S, Måløy KJ. 2013. Non-Gaussian nature of fracture and the survival of fat-tail exponents. Phys. Rev. Lett. 110, 145501 ( 10.1103/PhysRevLett.110.145501) [DOI] [PubMed] [Google Scholar]
  • 10.Bouchaud E. 1997. Scaling properties of cracks. J. Phys. Condens. Matter 9, 4319–4344. ( 10.1088/0953-8984/9/21/002) [DOI] [Google Scholar]
  • 11.Patinet S, Vandembroucq D, Roux S. 2013. Quantitative prediction of effective toughness at random heterogeneous interfaces. Phys. Rev. Lett. 110, 165507 ( 10.1103/PhysRevLett.110.165507) [DOI] [PubMed] [Google Scholar]
  • 12.Gjerden K, Stormo A, Hansen A. 2013. Universality classes in constrained crack growth. Phys. Rev. Lett. 111, 135502 ( 10.1103/PhysRevLett.111.135502) [DOI] [PubMed] [Google Scholar]
  • 13.Laurson L, Santucci S, Zapperi S. 2010. Avalanches and clusters in planar crack front propagation. Phys. Rev. E 81, 046116 ( 10.1103/PhysRevE.81.046116) [DOI] [PubMed] [Google Scholar]
  • 14.Ben-Zion Y, Morrissey J. 1995. A simple re-derivation of logarithmic disordering of a dynamic planar crack due to small random heterogeneities. J. Mech. Phys. Solids 43(9), 1363–1368. ( 10.1016/0022-5096(95)00042-H) [DOI] [Google Scholar]
  • 15.Bustingorry S, Kolton A, Giamarchi T. 2008. Thermal rounding of the depinning transition. Europhys. Lett. 812, 26005 ( 10.1209/0295-5075/81/26005) [DOI] [PubMed] [Google Scholar]
  • 16.Atkinson K. 1987. Fracture mechanics of rocks. London, UK: Academic Press. [Google Scholar]
  • 17.Chauve P, Giamarchi T, Le Doussal P. 2000. Creep and depinning in disordered media. Phys. Rev. B 62, 6241–6267. ( 10.1103/PhysRevB.62.6241) [DOI] [Google Scholar]
  • 18.Chen L-W, Marchetti MC. 1995. Interface motion in random media at finite temperature. Phys. Rev. B 51, 6296–6308. ( 10.1103/PhysRevB.51.6296) [DOI] [PubMed] [Google Scholar]
  • 19.Vandembroucq D, Skoe R, Roux S. 2004. Universal depinning force fluctuations of an elastic line: application to finite temperature behavior. Phys. Rev. E 70, 051101 ( 10.1103/PhysRevE.70.051101) [DOI] [PubMed] [Google Scholar]
  • 20.Kolton AB, Rosso A, Giamarchi T, Krauth W. 2009. Creep dynamics of elastic manifolds via exact transition pathways. Phys. Rev. B 79, 184207 ( 10.1103/PhysRevB.79.184207) [DOI] [Google Scholar]
  • 21.Lazarus V. 2011. Perturbation approaches of a planar crack in linear elastic fracture mechanics: a review. J. Mech. Phys. Solids 59, 121–144. ( 10.1016/j.jmps.2010.12.006) [DOI] [Google Scholar]
  • 22.Schmittbuhl J, Roux S, Vilotte J-P, Måløy KJ. 1995. Interfacial crack pinning: effect of nonlocal interactions. Phys. Rev. Lett. 74, 1787–1790. ( 10.1103/PhysRevLett.74.1787) [DOI] [PubMed] [Google Scholar]
  • 23.Rosso A, Krauth W. 2002. Roughness at the depinning threshold for a long-range elastic string. Phys. Rev. E 65, 025101 ( 10.1103/PhysRevE.65.025101) [DOI] [PubMed] [Google Scholar]
  • 24.Lengliné O, Schmittbuhl J, Elkhoury J, Ampuero J-P, Toussaint R, Måløy K. 2011. Downscaling of fracture energy during brittle creep experiments. J. Geophys. Res. B Solid Earth 116, B08215 ( 10.1029/2010jb008059) [DOI] [Google Scholar]
  • 25.Lawn B. 1993. Fracture of brittle solids, 2nd edn Cambridge, UK: Cambridge University Press. [Google Scholar]
  • 26.Gao H, Rice JR. 1989. A first-order perturbation analysis of crack trapping by arrays of obstacles. J. Appl. Mech. 56, 828–836. ( 10.1115/1.3176178) [DOI] [Google Scholar]
  • 27.Perrin G, Rice JR, Zheng G. 1995. Self-healing slip pulse on a frictional surface. J. Mech. Phys. Solids 43, 1461–1495. ( 10.1016/0022-5096(95)00036-I) [DOI] [Google Scholar]
  • 28.Cochard A, Rice JR. 1997. A spectral method for numerical elastodynamic fracture analysis without spatial replication of the rupture event. J. Mech. Phys. Solids 45, 1393–1418. ( 10.1016/S0022-5096(97)00004-5) [DOI] [Google Scholar]
  • 29.Frigo M, Johnson S. 2005. The design and implementation of FFTW3. Proc. IEEE 93, 216–231. ( 10.1109/jproc.2004.840301) [DOI] [Google Scholar]
  • 30.Hairer E, Nørsett S, Wanner G. 1993. Solving ordinary differential equations I. Nonstiff problems. Berlin, Germany: Springer. [Google Scholar]
  • 31.Schmittbuhl J, Måløy KJ. 1997. Direct observation of a self-affine crack propagation. Phys. Rev. Lett. 78, 3888–3891. ( 10.1103/PhysRevLett.78.3888) [DOI] [Google Scholar]
  • 32.Delaplace A, Schmittbuhl J, Måløy KJ. 1999. High resolution description of a crack front in a heterogeneous plexiglas block. Phys. Rev. E 60, 1337–1343. ( 10.1103/PhysRevE.60.1337) [DOI] [PubMed] [Google Scholar]
  • 33.Schmittbuhl J, Vilotte J-P. 1999. Interfacial crack front wandering: influence of quenched noise correlations. Physica A 270, 42–56. ( 10.1016/S0378-4371(99)00155-7) [DOI] [Google Scholar]
  • 34.Favier E, Lazarus V, Leblond J-B. 2006. Statistics of the deformation of the front of a tunnel-crack propagating in some inhomogeneous medium. J. Mech. Phys. Solids 54, 1449–1478. ( 10.1016/j.jmps.2006.01.004) [DOI] [Google Scholar]
  • 35.Pindra N, Lazarus V, Leblond J, Schmittbuhl J, Toussaint R. 2009. Deformation of the crack front during propagation in some disordered medium: theoretical and experimental studies. In 12th Int. Conf. on Fracture 2009, ICF-12, Ottawa, Canada, 12–17 July, vol. 8, pp. 6356–6364. Red Hook, NY: Curran Associates. [Google Scholar]
  • 36.Toussaint R, Helgesen G, Flekkøy E. 2004. Dynamic roughening and fluctuations of dipolar chains. Phys. Rev. Lett. 93, 108304 ( 10.1103/PhysRevLett.93.108304) [DOI] [PubMed] [Google Scholar]
  • 37.Toussaint R, Flekkøy E, Helgesen G. 2006. Memory of fluctuating Brownian dipolar chains. Phys. Rev. E 74, 051405 ( 10.1103/PhysRevE.74.051405) [DOI] [PubMed] [Google Scholar]
  • 38.Morgado R, Oliveira F, Batrouni GG, Hansen A. 2002. Relation between anomalous and normal diffusion in systems with memory. Phys. Rev. Lett. 89, 100601 ( 10.1103/PhysRevLett.89.100601) [DOI] [PubMed] [Google Scholar]
  • 39.Perrin G, Rice J. 1994. Disordering of a dynamic planar crack front in a model elastic medium of randomly variable toughness. J. Mech. Phys. Solids 42, 1047–1064. ( 10.1016/0022-5096(94)90083-3) [DOI] [Google Scholar]
  • 40.Legrand L, Patinet S, Leblond J-B, Frelat J, Lazarus V, Vandembroucq D. 2011. Coplanar perturbation of a crack lying on the mid-plane of a plate. Int. J. Fract. 170, 67–82. ( 10.1007/s10704-011-9603-0) [DOI] [Google Scholar]
  • 41.Lengliné O, Elkhoury J, Daniel G, Schmittbuhl J, Toussaint R, Ampuero J-P, Bouchon M. 2012. Interplay of seismic and aseismic deformations during earthquake swarms: an experimental approach. Earth Planet. Sci. Lett. 331–332, 215–223. ( 10.1016/j.epsl.2012.03.022) [DOI] [Google Scholar]
  • 42.Ramanathan S, Fisher D. 1998. Onset of propagation of planar cracks in heterogeneous media. Phys. Rev. B 58, 6026–6046. ( 10.1103/PhysRevB.58.6026) [DOI] [Google Scholar]
  • 43.Fuller K, Fox P, Field JE. 1975. The temperature rise at the tip of fast-moving cracks in glassy polymers. Proc. R. Soc. Lond. A 341, 537–557. ( 10.1098/rspa.1975.0007) [DOI] [Google Scholar]
  • 44.Ranc N, Palin-Luc T, Paris PC, Saintier N. 2014. About the effect of plastic dissipation in heat at the crack tip on the stress intensity factor under cyclic loading. Int. J. Fatigue 58, 56–65. ( 10.1016/j.ijfatigue.2013.04.012) [DOI] [Google Scholar]
  • 45.Toussaint R, Lengliné O, Santucci S, Vincent-Dospital T, Naert-Guillot M, Måløy KJ. 2016. How cracks are hot and cool: a burning issue for paper. Soft Matter 12, 5563–5571. ( 10.1039/c6sm00615a) [DOI] [PubMed] [Google Scholar]
  • 46.Bonamy D, Santucci S, Ponson L. 2008. Crackling dynamics in material failure as the signature of a self-organized dynamic phase transition. Phys. Rev. Lett. 101, 045501 ( 10.1103/PhysRevLett.101.045501) [DOI] [PubMed] [Google Scholar]
  • 47.Perfettini H, Schmittbuhl J, Cochard A. 2003. Shear and normal load perturbations on a two-dimensional continuous fault: 1. Static triggering. J. Geophys. Res. B Solid Earth 108, B9, 2408 ( 10.1029/2002JB001804) [DOI] [Google Scholar]
  • 48.Schmittbuhl J, Delaplace A, Måløy KJ, Perfettini H, Vilotte JP. 2003. Slow crack propagation and slip correlations. Pure Appl. Geophys. 160, 961–976. ( 10.1007/PL00012575) [DOI] [Google Scholar]
  • 49.Bourouis S, Bernard P. 2007. Evidence for coupled seismic and aseismic fault slip during water injection in the geothermal site of Soultz (France), and implications for seismogenic transients. Geophys. J. Int. 169, 723–732. ( 10.1111/j.1365-246x.2006.03325.x) [DOI] [Google Scholar]

Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Data Availability Statement

The numerical code is accessible upon request to the authors.


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