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. 2022 Apr 20;28(2):592–610. doi: 10.1177/10812865221086547

The energy release rate for non-penetrating crack in poroelastic body by fluid-driven fracture

Victor A Kovtunenko 1,, Nyurgun P Lazarev 2
PMCID: PMC9893035  PMID: 36743389

Abstract

A new class of constrained variational problems, which describe fluid-driven cracks (that are pressurized fractures created by pumping fracturing fluids), is considered within the nonlinear theory of coupled poroelastic models stated in the incremental form. The two-phase medium is constituted by solid particles and fluid-saturated pores; it contains a crack subjected to non-penetration condition between the opposite crack faces. The inequality-constrained optimization is expressed as a saddle-point problem with respect to the unknown solid phase displacement, pore pressure, and contact force. Applying the Lagrange multiplier approach and the Delfour–Zolésio theorem, the shape derivative for the corresponding Lagrangian function is derived using rigorous asymptotic methods. The resulting formula describes the energy release rate under irreversible crack perturbations, which is useful for application of the Griffith criterion of quasi-static fracture.

Keywords: Poroelasticity, hydraulic fracturing, crack, contact, incremental formulation, variational inequality, Lagrangian, asymptotic analysis, shape derivative, energy release rate, path-independent integral

1. Introduction to poroelastic modeling

In the paper, we proceed the development of constrained optimization theory for a new class of variational models arising in poroelasticity and motivated by hydrofracking. A two-phase poroelastic body consisting of solid phase and pores saturated with a Newtonian fluid is considered. We suggest that the body contains a fluid-driven crack (called fractures) since formed by the pressure of a pumped fluid. For physical consistency, the crack is subjected to a non-penetration inequality between opposite faces (the fracture walls). This description allows a compressive pressure at which the crack might close. Here, it would be worthwhile to comment that mutual contact of adjacent crack faces admits the phenomenon of mechanically closed, but hydraulically open cracks (which could arise, e.g., through the presence of debris in an otherwise fluid-conducting crack).

The poroelastic model is described by governing equations stated in incremental form with respect to unknown solid phase displacement, pore pressure, and contact force. The system is endowed with the fluid pressure, which is prescribed inhomogeneous and different on the fracture walls. In the multi-scale formulation, the pressurized fracture equations are coupled with governing equations for the fluid pressure to a single model. Typically, fluid flow in the fracture is governed by the Reynolds lubrication equation, which assumes a local cubic law (see Baykin and Golovin [1]). Modeling of the fluid pressure using a linear diffraction equation was suggested in Mikelić et al. [2]. In our work, we account for the channelized fluid flow as a prescribed boundary condition. In its turn, the boundary data can be achieved by flow modeling as well as directly from geomechanical data.

The nonlinear theory of solids with non-penetrating cracks and their quasi-static propagation was developed in the variational framework by Khludnev and co-authors [3,4]. For dynamic modeling of cracks, we cite the monograph of Bratov et al. [5]. The non-penetration approach was continued for frictional contact phenomena at the crack in Itou et al. [6] and the limiting small strain in the proceeding works [7,8]. We cite the study [9] for Timoshenko plates with cracks, and the study [10] addressing optimal control problems. Also anti-cracks, rigid, and soft inclusions were incorporated in the theory (see Khludnev et al. [11]). For suitable numerical methods, see Hintermüller et al. [12]. Recently, in Kovtunenko [13], we derived non-penetration conditions at the fluid-driven crack in two-phase poroelastic medium.

Alternatively to the sharp-interface approach, in a brittle zone, the crack surface can be approximated by a phase-field function as described in Mikelić et al. [14] which may be beneficial for numerical reasoning. Then, the crack and its propagation are determined based on the energy minimization approach to brittle and quasi-brittle fracture (see Kovtunenko [15]). The readers may find helpful the discrete perturbation of global potentials due to crack extension in the vein of variational eigen-erosion methods from Schmidt et al. [16].

The concept of soil and poromechanics was established well by Biot and Terzaghi [17,18] and further developed by Barenblatt et al. [19] and Meirmanov [20] and others. We cite Fellner and Kovtunenko [21] and Kovtunenko and Zubkova [22] for homogenization of a two-phase medium consisted of solid phase and pores, and Sazhenkov et al. [23] for the related multi-scale analysis. In our modeling, we follow the hydraulic fracturing formulation given by Golovin and Baykin [24] and Skopintsev et al. [25] with co-authors as presented next.

For a linear elastic solid phase, the second-order symmetric tensors of linearized strain ε and Cauchy stress σ are connected by Hooke’s law

σ=Aε+τ0, (1)

with the help of the fourth-order symmetric tensor of elastic coefficients A, which assumed to be elliptic, and subjected to a prestress τ0. The prestress admits mechanical stresses of geological layers in reservoir in their natural state as well by fracking (see the influence of the prestress on the failure zone development in Valov et al. [26]). Accounting for the pore pressure p, the effective stress is introduced as

τ=σαpI, (2)

where α(0,1] is the Biot coefficient, and I is the identity tensor. Omitting inertia terms in equations of motion and keeping the minus sign, the quasi-static equilibrium equation reads

divτ=0. (3)

After substitution into equation (3) of equations (1) and (2) and the symmetric gradient of the displacement vector u

ε(u)=12(u+uT), (4)

where T stands for the transposition; it implies the elliptic equation with respect to unknown u

div(Aε(u)+τ0αpI)=0. (5)

The fluid content in pores is constituted by

ζ=Sp+αtrε, (6)

where S>0 is the storativity, and trε implies dilatation according to equation (4). In the mass balance

ζt=divq, (7)

the flow velocity vector q is assumed given by the Darcy flow

q=κp, (8)

where κ=kr/ηr is determined by the permeability kr>0 and the effective viscosity ηr>0. Inserting equations (6) and (8) into equation (7) results in the parabolic equation with respect to p/t and u/t

t(Sp+αtrε(u))div(κp)=0. (9)

From the mathematical point of view, the fully coupled poroelastic equations (5) and (9) present a degenerate elliptic-parabolic system; thus, standard existence theorems are not applicable here. After differentiation of the elliptic equation (5) with respect to time, the system turns into a pure parabolic problem. Its solvability was established by applying the theory of implicit evolution equations (see Showalter [27]). However, the parabolic problem does not conform to the unilateral conditions. On the other side, the governing equations formally coincide with thermoelastic equations when replacing the pore pressure p for temperature. From the literature on thermoelasticity, existence results utilizing the pseudo-monotonone theory were known (see Khludnev and Kovtunenko [3], section 3.3), however, restricted to small coupling coefficients α. Avoiding these restrictive assumptions, in Kovtunenko [13] we proved the well-posedness based on Rothe’s semi-discretization in time of parabolic equation (9), which reduces it to the elliptic equation with respect to unknown p at fixed time t>δ>0

S(pptδ)+αtrε(uutδ)δdiv(κp)=0, (10)

for given ptδ:=p(tδ) and utδ:=u(tδ), then passing the time step δ to zero.

In the current contribution, we investigate shape differentiability of the poroelastic problem with non-penetrating crack under irreversible shape perturbations. For this task, we consider the problem in the incremental form (5) and (10), and endow it with a saddle-point formulation. Based on the Lagrange multiplier approach, we apply the formalism of directional differentiability for Lagrangians (see Delfour and Zolésio [28]) and use rigorous asymptotic methods (see González et al. [29]) to derive a shape derivative for the underlying Lagrangian function implying a free energy. The resulting formula describes the energy release rate under irreversible crack perturbations, which is useful for the Griffith criterion of quasi-static crack evolution (see Charlotte et al. [30]). Other shape derivatives were derived in a series of works for non-penetrating cracks and inclusions in linear elastic bodies by Khludnev and his colleagues [3,4] in Khludnev and Shcherbakov [31] within the Euler–Bernoulli beam theory, in Rudoy and Shcherbakov [32] for Kirchhoff–Love plates, in Lazarev [33], Lazarev and Rudoy [34] for Timoshenko plates, and so on.

The structure of the paper is the following one. In section 2, we state the poroelastic problem with non-penetrating crack in the incremental form. In section 3, variational principle is given for a Lagrangian function, and well-posedness of the corresponding saddle-point problem is established. Also, we formulate the Griffith fracture criterion for the crack quasi-static evolution. In section 4, the shape differentiability of the Lagrangian is proven using the asymptotic methods of analysis based on regular perturbations, thus providing us with a semi-analytic formula for the energy release rate. Special cases of the formula are discussed in section 5; its relation to well-known path-independent integrals (called Cherepanov–Rice, or J-integrals) is presented.

2. Formulation of poroelastic problem with non-penetrating crack

We start with a description of geometry as illustrated for 2D in Figure 1.

Figure 1.

Figure 1.

Example geometry of a poroelastic body with evolving crack in 2D.

Let Ω be a reference domain in the Euclidean space of points x=(x1,,xd)TRd, d=2,3. We assume the Lipschitz continuous boundary Ω with outward normal vector n=(n1,,nd)T, and the disjoint union Ω=ΓD·ΓN with ΓDØ. Let an oriented manifold of co-dimension one Σ split Ω into two sub-domains Ω± with Lipschitz continuous boundaries Ω± such that

Ω+Ω=Σ,Ω=Ω+ΩΣ,Ω±ΓDØ. (11)

For a time parameter t(0,T], T>0, we look for a crack evolution along the interface

tΓtΣ, (12)

which is assumed to be C1,1-smooth and irreversible such that

ΓtΓt+ss(0,Tt). (13)

We distinguish the crack faces Γt±Σ± and chose the normal vector nt at Γt outward to Ω, thus inward to Ω+. Physically, Γt represents fractures, whereas the complement

Ωt:=Ω\Γt¯, (14)

implies a reservoir.

For every fixed t(0,T] and xΩt in the time-dependent domain from equations (11) to (14), the poroelastic medium is described by the pore pressure p(t,x) and the solid displacement u=(u1,,ud)T(t,x). The latter is involved in the strain ε(u)={εij(u)}i,j=1d according to equation (4) with the entries ui,j:=ui/xj of the gradient u={ui,j}i,j=1d. The stress σ={σij}i,j=1d(t,x) and the effective stress τ={τij}i,j=1d(t,x) are introduced in equations (1) and (2), respectively, and the prestress is given by the symmetric tensor

τ0={τij0}i,j=1d(x)H1(Ω)symd×d:=H1(Ω;Rsymd×d).

For the reason of analysis, we do not consider here the so-called 2.5D models when physical strain and stress are 3×3-tensors defined over a 2D-domain Ω. The system is governed by equations (5) and (10), where componentwisely (divτ)i:=j=1dτij,j for i=1,,d, and the trace trε(u)=divu:=i=1dui,i. The elastic coefficients in equation (5)

A={Aijkl}i,j,k,l=1d(x)W1,(Ω)symd×d×d×d,

are symmetric: Aijkl=Ajikl=Aklij for i,j,k,l=1,,d, and build a self-adjoint bilinear form

ΩtAε(u):ε(v)dx:=i,j,k,l=1dΩtAijklεkl(u)εij(v)dx, (15)

for all u,vH1(Ωt)d, which is uniformly elliptic and bounded: there exists 0<a¯a¯ such that

a¯uH1(Ωt)2ΩtAε(u):ε(u)dx,|ΩtAε(u):ε(v)dx|a¯uH1(Ωt)vH1(Ωt), (16)

holds for all t[0,T] according to Korn and Poincaré inequalities if u=0 on ΓD. In equation (10), the transport coefficient κW1,(Ω) is assumed uniformly positive and bounded

0<κ¯κ(x)κ¯, (17)

and the time-delayed data in Ωtδ for t(δ,T) are given by functions

utδ=((utδ)1,,(utδ)d)T(t,x)H2(Ωtδ)d,ptδ(t,x)H2(Ωtδ),

such that the irreversibility of crack evolutions (13) provides the inclusion H2(Ωtδ)H2(Ωt) , hence

utδH2(Ωt)d,ptδH2(Ωt)forallt(δ,T). (18)

We decompose the displacement u and the stress τn:=(j=1dτ1jnj,,j=1dτdjnj)T at the boundary into its normal components

nTu:=i=1dniui,nTτn=i,j=1dniτijnj,

implying the vector–vector and matrix–vector multiplications, and tangential components as follows

u=(nTu)n+(u(nTu)n),τn=(nTτn)n+(τn(nTτn)n).

Let the following time-dependent data are prescribed in the reservoir for all t(0,T)

g=(g1,,gd)T(t,x)L2(ΓN)d,pre(t,x)H2(Ωt). (19)

With its help, we state mixed inhomogeneous boundary conditions on the outer boundary

u=0onΓD,τn=gonΓN,p=preonΩ. (20)

The assumed regularity of the data will be used further for asymptotic expansions in sections 4 and 5.

Across the crack Γt, functions defined in Ωt allow discontinuity by the mean of jump

[[u]]:=u|Γt+u|Γt,[[τ]]:=τ|Γt+τ|Γt,[[p]]:=p|Γt+p|Γt.

We suggest no tangential effective stress at the crack faces

τnt(ntTτnt)nt=0onΓt±, (21)

and continuity of the fluid pressure over the fracture walls

p=pre±onΓt±. (22)

The fluid pressure pre± prescribed in equation (19) is different on Γt±, coincide at the crack-tip, respectively, crack-front in 3D, and can be determined from the lubrication equations in fractures (see Golovin and Baykin [24]).

Assuming at Γt± the standard boundary condition in the normal direction

ntTτnt+pre±=0, (23)

would lead to interpenetration between the opposite crack faces under compressive stress. For the physical consistency, non-penetration at the crack is suggested

ntT[[u]]0onΓt, (24)

see Figure 1. The inequality constraint (24) leads to complementary conditions

[[ntTτnt+pre]]=0,ntTτnt+pre0,(ntTτnt+pre)(ntT[[u]])=0onΓt. (25)

Conditions (25) imply that equality (23) holds at those points where the crack is open, i.e., ntT[[u]]>0. Otherwise, the closed crack ntT[[u]]=0 in equation (25) has the compressive stress ntTτnt+pre0.

3. Variational principle for the crack problem

In the domain with crack defined in equation (14), we have the following generalized Green’s formula (see Khludnev and Kovtunenko [3], section 1.4) for the elasticity operator

Ωt(divτ)Tvdx=Ωtτ:ε(v)dxτn,vΓN+τnt,vΓt+τnt,vΓt, (26)

for all τL2(Ωt)symd×d and divτL2(Ωt)d,vH1(Ωt)d with v=0 on ΓD. Here, the boundary stresses τn on ΓN and τnt on Γt± are distributions defined in a generalized sense by duality mappings ·,·ΓN and ·,·Γt±, which turn into usual integrals for functions. For the stationary transport operator, Green’s formula

Ωtdiv(κp)qdx=ΩtκpTqdx, (27)

holds for all functions pH1(Ωt),ΔpL2(Ωt), and qH01(Ωt).

Inserting into equation (26) the equilibrium equation (5), using the Neumann condition τn=g on ΓN from equation (20), and τnt=(ntTτnt)nt at the crack due to the zero tangential stress in equation (21), we obtain

0=Ωtτ:ε(v)dxΓNgTvdSx+ntTτnt,ntTvΓt+ntTτnt,ntTvΓt.

By the virtue of [[ntTτnt+pre]]=0 in equation (25), adding and subtracting pre follows the variational equation with respect to τ

Ωtτ:ε(v)dxΓNgTvdSxΓtntT[[prev]]dSx+ntTτnt+pre,ntT[[v]]Γt=0, (28)

for all test functions vH1(Ωt)d with v=0 on ΓD. The jump at the crack Γt is well defined

ntT[[v]]H001/2(Γt),

in the Lions–Magenes space of functions, which continuation by zero in Σ belongs to H1/2(Σ). Its counter-part in the duality ·,·Γt is determined in the adjoint space of linear continuous functionals

λ:=ntTτnt+preH001/2(Γt). (29)

Then, the complementarity conditions (24) and (25) take the weak form

ntT[[u]]0,λ,ξntT[[u]]Γt0forallξH001/2(Γt)suchthatξ0, (30)

and newly introduced variable λ in equation (29) implies the contact force. Inserting the transport equation (10) into Green’s formula (27) and using equation (18) results in the variational equation with respect to p

Ωt([S(pptδ)+αtrε(uutδ)]q+δκpTq)dx=0, (31)

for all test functions qH01(Ωt).

Gathering the weak variational formulation (28)–(31) and recalling τ=Aε(u)+τ0αpI, for the triple (u,p,λ), we define a Lagrange function L:H1(Ωt)d×H1(Ωt)×H001/2(Γt)R by

L(u,p,λ;Γt):=Ωt{(12Aε(u)+τ0):ε(u)[S(12pptδ)+αtrε(uutδ)]pδ2κ|p|2}dxΓNgTudSxΓtntT[[preu]]dSx+λ,ntT[[u]]Γt, (32)

accounting for the identity αpI:ε(u)=αtrε(u)p and multiplying the quadratic terms by 1/2. With its help existence of a weak solution to the problem is established in the next.

Theorem 1 (solution existence)

There exists a triple (ut,ptpre,λt)K(Ωt) in the feasible set

K(Ωt):={(v,q,μ)H1(Ωt)d×H01(Ωt)×H001/2(Γt)|v=0onΓDandμ0},

solving uniquely the saddle-point problem

L(ut,q,μ;Γt)L(ut,pt,λt;Γt)L(v,pt,λt;Γt), (33)

for all test functions (v,q,μ)K(Ωt). Then, it solves the poroelastic problem with non-penetrating crack stated in the weak form of equations (28)–(31), and vice versa.

Proof

With respect to the primal variable uL(u,p,λ;Γt), the Lagrangian in equation (32) builds a quadratic bilinear form, which is bounded and positive definite due to the estimates (16) of A. With respect to the dual variable, the quadratic bilinear form pL(u,p,λ;Γt) is bounded and negative definite because of estimates (17) of κ. The mapping λL(u,p,λ;Γt) is linear. Therefore, the unique saddle-point in equation (33) exists by the virtue of minimax theorems.

Based on the optimality condition for equation (33), we calculate the Gateaux derivative of the Lagrangian

lims01s(L(ut+sv,pt,λt;Γt)L(ut,pt,λt;Γt))=0,

and get the variational equation (28) for u=ut, the stress τt:=Aε(ut)+τ0αptI, and the contact force ntTτtnt+pre=λt according to equation (29). Conversely, from equation (28), it follows by convexity the minimum in equation (33)

L(ut,pt,λt;Γt)L(v,pt,λt;Γt).

Similarly, computing the limit

lims01s(L(ut,pt+sq,λt;Γt)L(ut,pt,λt;Γt))=0,

results in equation (31) for p=pt and u=ut. The converse assertion that equation (31) implies the maximum

L(ut,q,λt;Γt)L(ut,pt,λt;Γt),

is true by the concavity of pL(u,p,λ;Γt). The maximum in equation (33) with respect to μ taken at q=pt implies the dual complementarity conditions

λt0,μλt,ntT[[ut]]Γt0forallμH001/2(Γt)suchthatμ0, (34)

which are equivalent to equation (30) for λ=λt and u=ut. The proof is complete.

For a perturbation parameter s(0,Tt), we consider an irreversible crack perturbation Γt+s satisfying equation (13) (see illustration in Figure 1) and the perturbed domain with crack

Ωt+s:=Ω\Γt+s¯, (35)

according to equation (14). Let space points y=(y1,,yd)T be related to the perturbed geometry Ωt+s. The perturbed Lagrangian L:H1(Ωt+s)d×H1(Ωt+s)×H001/2(Γt+s)R is defined according to equation (32) as

L(v,q,μ;Γt+s):=Ωt+s{(12Aε(v)+τ0):ε(v)[S(12qptδ)+αtrε(vutδ)]qδ2κ|q|2}dyΓNgTvdSyΓt+snt+sT[[prev]]dSy+μ,nt+sT[[v]]Γt+s. (36)

The perturbed saddle-point problem (33) reads

L(ut+s,q,μ;Γt+s)L(ut+s,pt+s,λt+s;Γt+s)L(v,pt+s,λt+s;Γt+s), (37)

for all test functions (v,q,μ)K(Ωt+s) in the perturbed feasible set

K(Ωt+s)={(v,q,μ)H1(Ωt+s)d×H01(Ωt+s)×H001/2(Γt+s)|v=0onΓDandμ0}.

According to Theorem 1, there exists the unique solution (ut+s,pt+spre|t+s,λt+s)K(Ωt+s) to equation (37). It is also the solution to the perturbed poroelastic problem with non-penetrating crack from equations (28)–(31)

Ωt+sτt+s:ε(v)dyΓNgTvdSyΓt+snt+sT[[prev]]dSy+λt+s,nt+sT[[v]]Γt+s=0, (38)

for all test functions vH1(Ωt+s)d with v=0 on ΓD, where τt+s=Aε(ut+s)+τ0αpt+sI and λt+s=nt+sTτt+snt+s+pre; the perturbed complementarity conditions

nt+sT[[ut+s]]0,λt+s,ξnt+sT[[ut+s]]Γt+s0forallξH001/2(Γt+s)suchthatξ0; (39)

and the perturbed stationary transport equation

Ωt+s([S(pt+sptδ)+αtrε(ut+sutδ)]q+δκpt+sTq)dy=0, (40)

for all test functions qH01(Ωt+s).

With the help of reduced Lagrangian L in equation (32) calculated on the saddle-point from equation (33), and its perturbation in equation (36) calculated on the saddle-point from equation (37), we define a directional derivative (called the shape derivative) as the one-sided limit

tL(ut,pt,λt;Γt):=lims0+1s(L(ut+s,pt+s,λt+s;Γt+s)L(ut,pt,λt;Γt)). (41)

Physically, equation (41) implies the energy release rate by extension of the crack. For a constant surface energy density γ>0, let us denote the increase in surface energy due to creation of the new crack by

Gt:=lims0+1s(2γΓt+sdSy2γΓtdSx)>0. (42)

Based on equations (41) and (42), Griffith’s fracture criterion can be stated as the following condition

|Γt+s||Γt|,(tL(ut,pt,λt;Γt)+Gt)(|Γt+s||Γt|)0. (43)

Together with irreversibility (13), the inequalities in equation (43) imply the two cases:

  • if /tL(ut,pt,λt;Γt)+Gt<0, then Γt+s=Γt and crack does not grow;

  • if /tL(ut,pt,λt;Γt)+Gt0, then |Γt+s|>|Γt| and crack will begin to grow.

For the reason of fracture criterion (43), the main aim of our further consideration will be to provide a formula for calculating the shape derivative L/t in equation (41) (also the limit Gt in equation (42)).

4. Energy release rate by fluid-driven fracture

The crack perturbation can be carried out either in explicit or implicit form. In the explicit case, given a kinematic flow

[(s,x)ϕs=((ϕs)1,,(ϕs)d)T,ϕs1=((ϕs1)1,,(ϕs1)d)T]C1([0,T];W1,(Ω)d), (44)

associates a coordinate transformation y=ϕs(x) and its inverse x=ϕs1(y) such that

[ϕs1°ϕs](x)=x,[ϕs°ϕs1](y)=y.

We suppose that it builds a diffeomorphism of the cracked domains in equations (14) and (35)

ϕs:ΩtΩt+s,xy;ϕs1:Ωt+sΩt,yx. (45)

From equation (44), a time-dependent kinematic velocity is defined as Λ|t+s:=[dϕs/ds]°ϕs1.

In the implicit case, let a vector of kinematic velocity

Λ=(Λ1,,Λd)T(t,x)C([0,T];W1,(Ω)d), (46)

be given such that

Λ=0onΩ,ΛTnt=0onΓt, (47)

preserving the outer boundary and irreversible cracks in equation (13). This determines the flow in equation (45) by means of solutions to the Cauchy problem for non-autonomous and nonlinear ordinary differential equation (ODE) system

ddsϕs=Λ(t+s,ϕs)fors(0,Tt),ϕs=xass=0, (48)

and to the initial problem for a linear transport equation

sϕs1+(yϕs1)Λ|t+s=0for(s,y)(0,Tt)×Ω,ϕs1=yass=0, (49)

where the gradient yϕs1=((ϕs1)i/yj)i,j=1d, and Λ|t+s(y)=Λ(t+s,y). We assume the both equations (44) and (46) hold.

The following Traits 1–4 are needed to prove the shape differentiability of the Lagrangian.

Trait 1 (bijection of feasible sets)

The function composition with ϕs forms is a bijective map between the feasible sets

(v,q,μ)(v~,q~,μ~):=(v°ϕs,q°ϕs,μ°ϕs):K(Ωt+s)K(Ωt). (50)

Indeed, equation (50) follows straightforwardly from the diffeomorphism in equation (45). Trait 1 allows us to transform one-to-one the perturbed Lagrangian L from equation (36) to the reference geometry by setting

L~(s,v~,q~,μ~;Γt):=L(v,q,μ;Γt+s),L~(0,v~,q~,μ~;Γt)=L(v~,q~,μ~;Γt), (51)

for all (v,q,μ)K(Ωt+s). Applying equation (51) to the perturbed saddle-point problem (37), we have

L~(s,u~t+s,q~,μ~;Γt)L~(s,u~t+s,p~t+s,λ~t+s;Γt)L~(s,v~,p~t+s,λ~t+s;Γt), (52)

for all test functions (v~,q~,μ~)K(Ωt), and (u~t+s,p~t+spre,λ~t+s)K(Ωt) is the unique solution to equation (52). Thus, the next trait holds.

Trait 2 (existence of saddle point)

The set of saddle-points (u~t+s,p~t+spre,λ~t+s) in equation (52) is a singleton for every s[0,Tt].

We write the s-dependent Lagrangian L~ defined in equation (51) in the explicit form following from equation (36)

L~(s,v~,q~,μ~;Γt)=Ωt{(12A~E(ϕ~sT,v~)+τ~0):E(ϕ~sT,v~)[S(12q~p~tδ)+αtrE(ϕ~sT,v~u~tδ)]q~δ2κ~|ϕ~sTq~|2}JsdxΓNgTv~dSxΓtn~t+sT[[p~rev~]]ωsdSx+μ~,n~t+sT[[v~]]ωsΓt. (53)

Here, we have used the chain rule yv=ϕ~sTv~, the notation of d-by- d symmetric tensor

E(M,v~):=12(Mv~+v~TMT)forMRd×d, (54)

such that E(I,v~)=ε(v~) according to equation (4), the Jacobian determinant

Js:=det(ϕs)inΩt,ωs:=|ϕ~sTnt|JsatΓt, (55)

and the fact that ϕs is the identity transformation at ΓN.

Trait 3 (asymptotic expansion)

The asymptotic expansion of L~ from equation (53) as s0+ holds

L~(s,v~,q~,μ~;Γt)=L(v~,q~,μ~;Γt)+ssL~(0,v~,q~,μ~;Γt)+o(s). (56)

The partial derivative L~/s in equation (56) is a continuous function of the first argument given by the explicit representation for τ[0,Tt)

sL~(τ,v~,q~,μ~;Γt):=Ωt{divΛ|t+τ(12Aε(v~)+τ0αq~I):ε(v~)+Λ|t+τT(12Aε(v~)+τ0):ε(v~)(Aε(v~)+τ0αq~I):E(Λ|t+τT,v~)divΛ|t+τ[S(12q~ptδ)αtrε(utδ)]q~+Λ|t+τT(Sptδ+αtrε(utδ))q~δ[κ(12divΛ|t+τ|q~|2q~TΛ|t+τq~)+12Λ|t+τTκ|q~|2]}dxΓt((divΓtΛ|t+τntT+Λ|t+τTntT)[[prev~]]+Λ|t+τT[[prev~T]]nt)dSx+μ~,(divΓtΛ|t+τntT+Λ|t+τTntT)[[v~]]Γt, (57)

where the tangential divergence divΓtΛ:=divΛntTΛnt at Γt.

Proof

As s0, the following asymptotic expansion of the terms entering equations (53)–(55) takes place (see, e.g., Sokolowski and Zolesio [35], Chapter 2)

A~=A+sΛTA+o(s),τ~0=τ0+sΛTτ0+o(s),n~t+s=nt+sntΛ+o(s),κ~=κ+sΛTκ+o(s),p~re=pre+sΛTpre+o(s),p~tδ=ptδ+sΛTptδ+o(s),Js=1+sdivΛ+o(s),ωs=1+sdivΓtΛ+o(s),ϕ~sT=IsΛT+o(s),E(ϕ~sT,v~)=ε(v~)sE(ΛT,v~)+o(s),u~tδ=utδ+sutδΛ+o(s),trE(ϕ~sT,u~tδ)=trε(utδ)+sΛT[trε(utδ)]+o(s). (58)

Inserting representations (58) into the Lagrangian L~ given by equation (53), we derive its expansions (56) in the first argument. Since Λ|t+τ is a continuous function of the argument t+τ, then the partial derivative τL~/s(τ,·) in equation (57) is continuous and implies Λ|t+τ=Λ at τ=0. This finishes the proof.

The last trait is rather involved and proven in Appendix 1.

Trait 4 (strong convergence)

There exists a subsequence of saddle–points (u~t+sk,p~t+skpre,λ~t+sk) in equation (52) converging for sk0 as k to the saddle-point (ut,ptpre,λt) in equation (33)

(u~t+sk,p~t+sk,λ~t+sk)(ut,pt,λt)stronglyinH1(Ωt)d×H1(Ωt)×H001/2(Γt). (59)

Traits 1–4 satisfy all assumptions in Delfour and Zolésio [28] (Chapter 10, Theorem 5.1), thus provide the following theorem (see the detailed proof in González et al. [29]).

Theorem 2 (shape differentiability of Lagrangian)

The shape derivative from equation (41) exists expressed by

tL(ut,pt,λt;Γt)=limsk0+1sk(L~(sk,u~t+sk,p~t+sk,λ~t+sk;Γt)L(ut,pt,λt;Γt))=sL~(0,ut,pt,λt;Γt), (60)

where (ut,pt,λt) is the solution to the poroelastic problem with non-penetrating crack (28)–(31), and formula for the partial derivative /sL~ is given in equation (57).

In the following, we specify our main result stated in Theorem 2 with respect to the so-called J-integrals well-known in brittle fracture for linear elastic bodies with cracks.

5. Representation of the energy release rate as J-integral

For the kinematic velocity Λ from equations (46) and (47), let there exists a d-dimensional set OΩ with the C1,1-smooth boundary O and outward normal n such that outside it the solution to equations (28)–(31) is regular

(ut,pt,λt)H2(Ωt\O)d×H2(Ωt\O)×L2(Γt\O). (61)

Typically, O surrounds crack-tip, crack-front, kinks, and other singular points, where singular solutions are locally admissible. Inside O, we assume the velocity constant, e.g., equal to one, such that

Λ0inO. (62)

We denote for short Ot:=O\Γt¯. Based on properties (61) and (62), in the following, we will integrate by parts the expression in equation (57).

Theorem 3 (J-integral)

Under assumptions (61) and (62), the shape derivative in equation (60) for the solution of the poroelastic problem with non-penetrating crack (28)–(31) admits equivalent representation by the following sum

sL~(0,ut,pt,λt;Γt)=JOt+JO\Γt+JΓtO+JΓt\O+JOΓt, (63)

where the integrals are

JOt:=Ot{ΛT(12Aε(ut)+τ0):ε(ut)+ΛT(Sptδ+αtrε(utδ))ptδ2ΛTκ|pt|2}dx, (64)
JO\Γt:=O\Γt{(ΛTn)[(12Aε(ut)+τ0αptI):ε(ut)(S(12ptptδ)αtrε(utδ))pt]ΛTutTτtnδκ(12(ΛTn)|pt|2(ΛTpt)(nTpt))}dSx, (65)
JΓtO:=λt,ΛTntT[[ut]]ΓtOΓtOΛT(ntT[[preut]]+[[preutT]]nt)dSx,usingthenotationλt,ΛTntT[[ut]]ΓtO:=λt,ΛTntT[[ut]]ΓtΓt\OλtΛTntT[[ut]]dSx, (66)
JΓt\O:=δΓt\OΛTκ[[ptptT]]ntdSx, (67)
JOΓt:={(ΛTtt)ntT[[preut]]OΓtin2D,OΓt(ΛTbt)ntT[[preut]]dLxin3D, (68)

and the effective stress τt=Aε(ut)+τ0αptI. In equation (68) tt is a tangential vector at Γt positive oriented to nt in 2D, and bt=tt×nt is a binomial vector within the moving frame at Γt in 3D.

Proof

We rearrange the terms in formula (57) on the solution (ut,pt,λt) in the sum

sL~(0,ut,pt,λt;Γt)=k=06Ik. (69)

The terms not including Λ are gathered in

I1:=Ωt{ΛT(12Aε(ut)+τ0):ε(ut)+ΛT(Sptδ+αtrε(utδ))ptδ2ΛTκ|pt|2}dxΓtΛT(ntT[[preut]]+[[preutT]]nt)dSx+λt,ΛTntT[[ut]]Γt.

Since the assumptions of regularity (61) and (62), the complementarity conditions in equation (25) hold pointwise at Γt\O, therefore

I0:=λt,divΓtΛntT[[ut]]Γt=Γt\O(divΓtΛ)λtntT[[ut]]dSx=0.

In I2,,I6, we integrating by parts with respect to Λ. Using τt=Aε(ut)+τ0αptI, we calculate

I2:=Ωt\OdivΛ(12Aε(ut)+τ0αptI):ε(ut)dx=O\Γt{(ΛTn)(12Aε(ut)+τ0αptI):ε(ut)}dSx+Ωt\O{ΛT(12Aε(ut)+τ0):ε(ut)+αΛTpttrε(ut)ΛTε(ut):τt}dx,

where the last term ΛTε(ut):τt will be shortened when adding

I3:=Ωt\Oτt:E(ΛT,ut)dx=Ωt\O{i=1dΛT(ut)i(divτt)i+ΛTε(ut):τt}dxO\ΓtΛTutTτtndSx+Γt\OΛT[[utTτt]]ntdSx,

and divτt=0 due to the equilibrium equation (3), then

I4:=Ωt\OdivΛ(S(12ptptδ)αtrε(utδ))ptdx=Ωt\O{ΛTpt(S(ptptδ)αtrε(utδ))ΛT(Sptδ+αtrε(utδ))pt}dxO\Γt(ΛTn)(S(12ptptδ)αtrε(utδ))ptdSx,

which due to equation (10) constitutes the zeroth term

ΛTpt[S(ptptδ)+αtrε(ututδ)δdiv(κpt)]=0,

together with I2 and

I5:=Ωt\Oδκ(12divΛ|pt|2ptTΛpt)dx=Ωt\Oδ(12ΛTκ|pt|2ΛTptdiv(κpt))dxO\Γtδκ(12(ΛTn)|pt|2(ΛTpt)(nTpt))dSxΓt\OδκΛT[[ptptT]]ntdSx.

For I6, differentiating along the crack gets

I6:=Γt\OdivΓtΛntT[[preut]]dSx=Γt\OΛT([[preutT]]nt+ntT[[preut]]+[[utTpre]]nt)dSx(ΛTtt)ntT[[preut]]OΓtin2D,orOΓt(ΛTbt)ntT[[preut]]dLxin3D,

where in 2D a tangential vector tt at Γt is positive oriented to nt, and in 3D a binomial vector bt=tt×nt builds the moving frame at Γt.

The integrals from I3 and I6 over Γt\O, where the stress is determined pointwisely, can be combined using the boundary conditions (21), (23), definition of λt in equation (29), and the following calculation

Γt\OΛT(λtntT[[ut]]+[[utTτt]]nt+[[utTpre]]nt)dSx=Γt\OΛT(λtntT[[ut]]+[[utT]]λtnt)dSx=Γt\OΛTλt(ntT[[ut]])dSx=Γt\OΛTλtΓt(ntT[[ut]])dSx=0, (70)

by decomposing the vectors into normal and tangential components and using ΛTnt=0 at the crack Γt. The pointwise product in equation (70) is zero due to the complementarity conditions (25) after application of the tangential differentiation Γt:=nt(ntT) to ntT[[ut]]=0. Finally, collecting the integral terms I1 I6 in equation (69) together with equation (70) provides the expressions (63)–(68).

We present several concluding remarks as follows:

  • With the help of tangential gradient and ΛTnt=0 at Γt, formula (66) can be expressed equivalently

JΓtO=λt,ΛTΓtntT[[ut]]ΓtOΓtOΛT(ΓtntT[[preut]]+[[ΓtpreutT]]nt)dSx.
  • Applying the coordinate transformation ϕs, using expansion of ωs in equation (58), and differentiating along the crack, we calculate the limit in equation (42)

Gt=2γlims0+1sΓt(ωs1)dSx=2γ{ΛTtt|Γtin2D,ΓtΛTbtdLxin3D.
  • It is worth noting that JO\Γt from equation (66) is related to J-integrals known for linear elastic bodies. We clarify the relation in the following corollary.

Corollary 1 (non-penetrating crack in linear elastic body under fluid-driven fracture)

If the factors S=α=κ=0, then the Lagrangian L in equation (32) implies the strain energy

L(u,p,λ;Γt)=Ωt(12Aε(u)+τ0):ε(u)dxΓNgTudSxΓtntT[[preu]]dSx+λ,ntT[[u]]Γt. (71)

The strain energy release rate is given according to equation (57) by

sL~(0,ut,pt,λt;Γt)=Ωt{divΛ(12Aε(ut)+τ0):ε(ut)+ΛT(12Aε(ut)+τ0):ε(ut)(Aε(ut)+τ0):E(ΛT,ut)}dxΓt((divΓtΛntT+ΛTntT)[[preut]]+ΛT[[preutT]]nt)dSx+λt,(divΓtΛntT+ΛTntT)[[ut]]Γt.

Let the elasticity coefficients A and prestress τ0 be constant. Then, under assumptions (61) and (62), the shape derivative is expressed equivalently by the integrals from equations (63)–(68)

sL~(0,ut,pt,λt;Γt)=O\Γt{(ΛTn)(12Aε(ut)+τ0):ε(ut)ΛTutTτtn}dSx+JΓtO+JOΓt. (72)

If pre is constant and the crack Γt is plane in O, then pre=nt=0 at ΓtO such that JΓtO=0, and the strain energy release rate in equation (72) implies the path-independent sum

sL~(0,ut,pt,λt;Γt)=O\Γt{(ΛTn)(12Aε(ut)+τ0):ε(ut)ΛTutTτtn}dSx+JOΓt. (73)
  • We finish the paper by emphasizing that formulas of the shape derivative obtained in the paper are of practical use to predict when fluid-driven fractures will begin to grow.

Appendix 1

Proof of the strong convergence in Trait 4

We split the proof in five subsequent steps.

Uniform estimate of (u~t+s,p~t+s)

Applying Theorem 1 to the s-dependent problem (52), its saddle-point (u~t+s,p~t+spre,λ~t+s)K(Ωt) satisfies the necessary and sufficient optimality conditions like (38)–(40)

Ωt(A~E(ϕsT,u~t+s)+τ~0αp~t+sI):E(ϕsT,v~)JsdxΓNgTv~dSxΓtn~t+sT[[p~rv~]]ωsdSx+μ~,n~t+sT[[v~]]ωsΓt=0, (74)
Ωt([S(p~t+sp~tδ)+αtrE(ϕ~sT,u~t+su~tδ)]q~+δκ~p~t+sTϕ~s1ϕ~sTq~)Jsdx=0, (75)
n~t+sT[[u~t+s]]0,λ~t+s,ξn~t+sT[[u~t+s]]ωsΓt0forallξH001/2(Γt)suchthatξ0, (76)

for all test functions (v~,q~)H1(Ωt)d×H01(Ωt) such that v~=0 on ΓD. With the help of asymptotic expansion (56) and (57) in Trait 3 and applying Taylor’s theorem, we can decompose equations (74)–(76) as s0+ akin to the reference problem (28)–(31)

Ωt(Aε(u~t+s)+τ0αp~t+sI):ε(v~)dxΓNgTv~dSxΓtntT[[prev~]]dSx+λ~t+s,n~t+sT[[v~]]ωsΓt=sBu(s,(u~t+s,p~t+s),v~), (77)
Ωt([S(p~t+sptδ)+αtrε(u~t+sutδ)]q~+δκp~t+sTq~)dx=sBp(s,(u~t+s,p~t+s),q~), (78)
λ~t+s,n~t+sT[[v~]]ωsΓt=λ~t+s,ntT[[v~]]Γt+sBλ(s,λ~t+s,v~), (79)

where the remainders in the form of Lagrange build the bilinear forms

Bu(s,(u~t+s,p~t+s),v~):=Ωt{Λ|t+sθuT(Aε(u~t+s)+τ0):ε(v~)+(Aε(u~t+s)+τ0αp~t+sI):(divΛ|t+sθuε(v~)E(Λ|t+sθuT,v~))}dx+Γt((divΓtΛ|t+sθuntT+Λ|t+sθuTntT)[[prev~]]+Λ|t+sθuT[[prev~T]]nt)dSx, (80)
Bp(s,(u~t+s,p~t+s),q~):=Ωt{divΛ|t+sθp[S(p~t+sptδ)+αtrε(u~t+sutδ)]q~+Λ|t+sθpT[Sptδ+αtrε(utδ)]q~δp~t+sT(κdivΛ|t+sθpI(κIκT)Λ|t+sθp)q~}dx, (81)
Bλ(s,λ~t+s,v~):=λ~t+s,(divΓtΛ|t+sθλntT+Λ|t+sθλTntT)[[v~]]Γt, (82)

which are bounded for the parameters θu,θp,θλ[0,1].

We test the variational equation (77) with v~=u~t+s and use λ~t+s,n~t+sT[[u~t+s]]ωsΓt=0 from equation (76)

Ωt(Aε(u~t+s)+τ0αp~t+sI):ε(u~t+s)dx=ΓNgTu~t+sdSx+ΓtntT[[preu~t+s]]dSx+sBu(s,(u~t+s,p~t+s),u~t+s), (83)

then insert q~=p~t+spre into equation (78) such that

Ωt([S(p~t+sptδ)+αtrε(u~t+sutδ)]p~t+s+δκ|p~t+s|2)dx=Ωt(S(p~t+sptδ)+αtrε(u~t+sutδ)pre+δκp~t+sTpre)dx+sBp(s,(u~t+s,p~t+s),p~t+spre). (84)

After summation of equations (83) and (84), the term αp~t+sI:ε(u~t+s)=αtrε(u~t+s)p~t+s is shortened and

Ωt(Aε(u~t+s):ε(u~t+s)+Sp~t+s2+δκ|p~t+s|2)dx=Ωt(τ0:ε(u~t+s)+[Sptδ+αtrε(utδ)]p~t+s+[S(p~t+sptδ)+αtrε(u~t+sutδ)]pre+δκp~t+sTpre)dx+ΓNgTu~t+sdSx+ΓtntT[[preu~t+s]]dSx+sBu(s,(u~t+s,p~t+s),u~t+s)+sBp(s,(u~t+s,p~t+s),p~t+spre). (85)

Applying Young’s inequality, for elliptic A from equation (16) and positive κ from equation (17), the uniform estimate holds

u~t+sH1(Ωt)2+p~t+sH1(Ωt)2C1,C1>0, (86)

for ss0 with sufficiently small s0>0.

Uniform estimate of λ~t+s

From equations (77) and (79), we express the duality

λ~t+s,ntT[[v~]]Γt=Ωt(Aε(u~t+s)+τ0αp~t+sI):ε(v~)dx+ΓNgTv~dSx+ΓtntT[[prev~]]dSx+sBu(s,(u~t+s,p~t+s),v~)sBλ(s,λ~t+s,v~). (87)

Dividing the equality (87) by the norm of ntT[[v~]], taking supremum over v~, using the Cauchy–Schwartz inequality and the bound (86), by the surjectivity of the trace operator we estimate the dual norm

λ~t+sH001/2(Γt)=supv~H1(Ωt)d|λ~t+s,ntT[[v~]]Γt|ntT[[v~]]H001/2(Γt)C2,C2>0. (88)

for ss0 and sufficiently small s0>0.

Weak convergence

By the virtue of uniform estimates (86) and (88), there exists a subsequence sk0+ as k and an accumulation point such that (ut,ptpre,λt)K(Ωt) and

(u~t+sk,p~t+sk,λ~t+sk)(ut,pt,λt)weaklyinH1(Ωt)d×H1(Ωt)×H001/2(Γt). (89)

By the compactness of embedding of the boundary traces, it follows that

u~t+skutstronglyinL2(ΓNΓt+Γt)assk0. (90)

Taking the limit in the sk-dependent problem (74)–(76) as sk0 due to the expansions (77)–(79) and the convergences (89) and (90), the limit (ut,pt,λt) solves the reference variational problem (28)–(31).

Strong convergence of (u~t+sk,p~t+sk)

Testing the reference equations (28) with v=ut, where λt,ntT[[ut]]Γt=0, and inserting q=ptpre into equation (31), after summation the term αptI:ε(ut)=αtrε(ut)pt is shortened, and similarly to equation (85), we obtain

Ωt(Aε(ut):ε(ut)+Spt2+δκ|pt|2)dx=Ωt(τ0:ε(ut)+[Sptδ+αtrε(utδ)]pt+[S(ptptδ)+αtrε(ututδ)]pre+δκptTpre)dx+ΓNgTutdSx+ΓtntT[[preut]]dSx. (91)

We subtract equation (91) from equation (85) and rearrange the terms as follows

Ωt(Aε(u~t+sut):ε(u~t+sut)+S(p~t+spt)2+δκ|(p~t+spt)|2)dx=ΓNgT(u~t+sut)dSx+ΓtntT[[pre(u~t+sut)]]dSx+sBu(s,(u~t+s,p~t+s),u~t+s)+sBp(s,(u~t+s,p~t+s),p~t+spre)+Ωt([Sptδ+αtrε(utδ)](p~t+spt)+[S(p~t+spt)+αtrε(u~t+sut)]pre+δκ(p~t+spt)Tpreτ0:ε(u~t+sut)2[Aε(ut):ε(u~t+sut)+Spt(p~t+spt)+δκptT(p~t+spt)])dx. (92)

On taking the limit as sk0+ in equation (92) due to the boundedness (86) and convergences (89) and (90), it follows

(u~t+sk,p~t+sk)(ut,pt)stronglyinH1(Ωt)d×H1(Ωt), (93)

for elliptic A from equation (16) and positive κ from equation (17).

Strong convergence of λ~t+sk

Subtracting the reference equation (28) from equation (87) such that

λ~t+sλt,ntT[[v~]]Γt=Ωt(Aε(u~t+sut)α(p~t+spt)I):ε(v~)dx+sBu(s,(u~t+s,p~t+s),v~)sBλ(s,λ~t+s,v~), (94)

dividing it by the norm of ntT[[v~]], and taking supremum over v~, applying the Cauchy–Schwartz inequality by the virtue of the boundedness (86) and (88) and the convergence (93), from equation (94) we conclude that

λ~t+skλtstronglyinH001/2(Γt).

Together with equation (93), this finishes the proof of the strong convergence (59) in Trait 4.

Footnotes

Funding: The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: V.A.K. (the first author) is supported by the Austrian Science Fund (FWF) project P26147-N26: PION and the European Research Council (ERC) under the European Union’s Horizon 2020 Research and Innovation Programme (advanced grant no. 668998 OCLOC); he also thanks the Russian Foundation for Basic Research (RFBR) project 18-29-10007 for partial support. The results of appendix were obtained by V.A.K. and L.N.P. (the second author) with the support of the Ministry of Science and Higher Education of the Russian Federation, supplementary agreement no. 075-02-2022-881, 02 February 2022.

ORCID iDs: Victor A Kovtunenko Inline graphic https://orcid.org/0000-0001-5664-2625

Nyurgun P Lazarev Inline graphic https://orcid.org/0000-0002-7726-6742

Contributor Information

Victor A Kovtunenko, Institute for Mathematics and Scientific Computing, University of Graz, Graz, Austria; Lavrentyev Institute of Hydrodynamics, Siberian Division of the Russian Academy of Sciences, Novosibirsk, Russia.

Nyurgun P Lazarev, Regional Scientific and Educational Mathematical Center “Far Eastern Center of Mathematical Research,” North-Eastern Federal University, Yakutsk, Russia.

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