In this paper we analyze the system of equations that models the behaviour of materials with a double porous structure. We introduce dissipation mechanisms in both structures. We show existence, uniqueness and analyticity for the solutions of the system. As consequences, exponential stability and impossibility of localization for the solutions are obtained.
Materials with double porosity have been the aim of study of many recent works. The first contributions about this theory were written at the beginning of the 60’s and are due to Barenblatt et al. [2,3]. Some other authors have also contributed to develop this theory (without trying to be exhaustive, we refer to [1,5,14,15,20,25,27,29,30,32,33]). The now called double porosity model allows a material to have two porous structures: the macro porosity, which is connected with the pores of the body of the material, and the micro porosity, which is connected with the fissures in the skeleton of the material. For this reason, this model is very interesting in different fields as geophysics or mechanics of bones [2,5,8,14]. As Straughan [27] noticed, ‘a good example of this may be seen in [19] where they show a pile of rocks, but the rocks themselves are full of fissures (or cracks), and the macro porosity degrades over a period of ten years leaving a pile of finer material characteristic of the micro porous structure’. The previous contributions are based on the use of Darcy’s law. The usual formulation of the theory involves the displacement, the pressure associated with the pores and the pressure associated with the fissures [27,28,30,33].
Nunziato and Cowin [22] proposed a theory for the behavior of porous solids. They established that the skeletal is elastic and the interstices are void of material. Following these ideas, Iesan and Quintanilla [13] set another theory for elastic materials with double porosity, which is currently being studied [10,28,31]. As our work is also related with the study of the solutions of porous-elastic materials, it is worth recalling several contributions about this topic [4,6,7,9,12,16,18,21,23,24].
In this paper we consider that the skeletal is viscoelastic and, at the same time, we introduce viscosity effects in both porous structures. This new setting gives rise to a dissipative system and it is not based on the law of Darcy. We will prove that the solutions of this system are generated by an analytic semigroup. Therefore, some regularity properties to the solutions arise. For instance, their orbits are analytical functions with respect to the time. That means that we can recover the solutions in terms of the time derivatives of the function in a fixed point (it is important to know the thermomechanical situations where such kind of regularity holds). Exponential stability and impossibility of localization of the solutions are also direct consequences of the analyticity.
We want to highlight the mathematical similarities between the equations for porous-elastic materials and those for microstretch materials. In fact, the equations that we analyze in this paper can also be viewed as equations describing a mixture of microstretch materials when their macroscopic structures coincide.
The plan of the paper is as follows. In Section 2 we recall the basic equations of the theory we are dealing with and the conditions that we assume over the constitutive coefficients. Sections 3, 4 and 5 are devoted, respectively, to prove the uniqueness, existence and analyticity of the solutions of the proposed system of equations. Finally, in Section 6 we state the conclusions.
Basic equations
We consider a body that at time occupies a bounded region B of the Euclidean three-dimensional space. As usual, the configuration of the body at time is taken as the reference configuration, and the motion of the body is referred to the reference configuration from a fixed system of rectangular Cartesian axes. Each particle of the body is identified with its position, which in the reference configuration is given by , for . At time t, the position of the particle will be denoted by
where is a given interval of time.
We denote by φ the volume fraction field corresponding to pores, and by ψ the volume fraction field corresponding to fissures.
Following the ideas proposed by Iesan and Quintanilla [13], we know that, in the absence of supply terms, the evolution equations are given by
In the above equations, is the stress tensor, and are the equilibrated stress vectors, and ξ and ζ are the equilibrated body forces. Constants ρ, and represent, respectively, the mass density and the products of the mass density by the equilibrated inertia.
Notice that, from a mathematical point of view, the kind of materials that we study here can be considered as a sub-case of porous viscoelastic mixtures [11]. Therefore, we can take the equations from there.
The constitutive equations that we consider in this paper are given by
Here, is the strain tensor, , , , , , , , , , , , , and are tensors of different order satisfying the following symmetries:
Substituting the constitutive equations into the evolution equations, we obtain the system that we want to analyze.
The internal energy of the system is given by the function defined by
and the dissipation by
If we work with isotropic and homogeneous materials, then the constitutive equations reduce to
Now λ, μ, b, d, , , α, , , N, γ, M, , , and are real numbers. The internal energy and the dissipation become, respectively,
and
The following inequalities (see [13]) are the necessary and sufficient conditions for the internal energy U to be positive:
The conditions to guarantee the positivity of the dissipation D are (see [13]):
We want to study the problem determined by the evolution equations (2.1) and the constitutive equations (2.2) on the bounded region B. To set a well posed problem, we need to impose boundary and initial conditions.
As boundary conditions we assume that
where , and are prescribed functions.
As initial conditions we assume that
where , , , , and are also prescribed functions.
Uniqueness of solutions
In this section we will see the uniqueness of the solutions supposing only that the dissipation is positive definite (nothing is said about the internal energy). In fact, we will prove that the only solution with null initial conditions and null boundary conditions is the null solution. This fact will prove the uniqueness.
Let us write the null Dirichlet boundary conditions that we assume:
We also suppose in this section that ρ, and are positive and that D is positive definite. This last assertion says that the inequality
holds for an appropriate positive constant C.
The conservation of the energy, when homogeneous Dirichlet boundary conditions and null initial conditions are assumed, gives
The last equality comes from the assumption that the initial conditions vanish.
From the above expression, we introduce the following notation:
and we define the function . Obviously, .
Therefore,
where is a calculable positive constant depending on the constitutive coefficients and the first eigenvalue of the fixed membrane problem (see [26]),
The next step in our analysis uses the Poincaré-type inequality that says that the following estimate
holds for every function such that .
Therefore, in our case, there exists a positive constant such that
To obtain the last inequality we have used also the classical Poicaré inequality: if is a function that vanishes in the boundary of B then there exists such that
From the positivity of the dissipation function, it can be seen that
where is a positive constant that can be calculated in terms of the constitutive coefficients and the first eigenvalue of the fixed membrane problem. From (3.3), it follows that . If we consider , then we find that vanishes in the interval . From the definition of , and taking into account again the positivity of the dissipation D, it follows that for every . Thus, we have proved that the problem has only the null solution in the interval . Repeating this argument in , for , we obtain that the only solution is the null solution.
Let us assume that,,and that D is positive definite. Then the Dirichlet initial boundary value problem has at most one solution.
Existence of solution
In this section we use the results of the semigroup of linear operators theory to obtain an existence theorem. We restrict our attention to the homogeneous version of the Dirichlet boundary conditions (3.1).
In the remaining part of the paper we assume that D is positive definite and that the internal energy U is also positive. That means that there exists a positive constant K such that
We assume again that ρ, and are positive.
We now transform the boundary-initial value problem defined by system (2.3), boundary conditions (3.1) and initial conditions (2.8) into an abstract problem on a suitable Hilbert space.
We denote
where and are the usual Sobolev spaces, which take values in the complex field.
Let us consider the following operators:
Let be the matrix operator defined by
where , , , , and , represent the identity operators in the respective spaces.
The domain of the operator is .
It is clear that the subspace
is contained in the domain and it is a dense subset of .
The initial boundary value problem (2.3), (3.1), (2.8) can be transformed into the following abstract equation in the Hilbert space ,
where
We introduce in the inner product
where and
Here, as usual a bar over a variable denotes its complex conjugate.
We note that (4.5) defines a norm which is given by
where
This norm is equivalent to the usual norm in .
The operatorhas the propertyfor any, where the inner productis defined in (
4.5
).
Let . Using the divergence theorem and the boundary conditions we see that
In view of the assumptions on the tensors we obtain the stated inequality. □
The operatorsatisfies the condition.
Let . We must show that the equation
has a solution . If we write the matrix and we operate, we find the following system:
Substituting the first, third and fifth equations into the others, we obtain the following system with unknowns u, φ and ψ:
Notice that
On the other side,
defines a coercive and bounded bilinear form on . Hence, the Lax–Milgram theorem implies the existence of a solution to the system of equations (4.9). Thus, equation (4.7) has also a solution. It is clear, from the regularity theory of linear elliptic systems, that being a positive constant independent of . □
The operatorgenerates a semigroup of contractions in.
The proof follows from the above lemmas and the Lumer–Phillips corollary to the Hille–Yosida theorem.
Finally, as a consequence, we have the following result.
Assume that. Then, there exists a unique solutionto problem (
4.3
).
Analyticity of solutions
Now we will prove that the semigroup obtained in the previous section is analytic. In order to do so, we use the following result, which can be found in the classical book of Liu and Zheng [17].
Let us considera-semigroup of contractions generated by the operatorin the Hilbert space. Suppose that. Thenis analytic if and only ifholds.
To apply Theorem 5.1 to our situation, we need to consider the resolvent equation
where and . We shall take , with . Therefore, our equation becomes
The imaginary axis is contained in the resolvent of. That is:
Since , following the arguments of Liu and Zheng (see [17], page 25), we assume that the imaginary axis is not contained in the resolvent set. Then there exists a real number with such that the set is contained in and . Therefore, there exist a sequence of real numbers with , , and a sequence of unit norm vectors in the domain of the operator such that
Notice that, if we consider , we obtain a system like the one considered in (5.1) changing δ by and where in , in , in and in .
If we multiply by and take its real part we obtain that
It then follows that
These two facts contradict the assumption that has unit norm and the proof is complete. □
There exists a positive constant C such that for anywhere
If we multiply the first equation of (5.1) by , the second one by , the third one by , the fourth one by , the fifth by , the last one by , and we add all the results we obtain at the left-hand side the following expression:
Notice that the first line of (5.2) is an imaginary number. The second and third lines are also imaginary because they are the sum of three differences of conjugate complex numbers. Finally, recalling the definition of the operators , , , and , from the fourth line we obtain the dissipation, which is positive.
Moreover, the norm of the right-hand side is bounded by , for a positive constant . □
There exists a positive constant C such that for anywhereUis the solution to problem (
5.1
).
Now we multiply the first equation of (5.1) by , the second one by , the third one by , the fourth one by , the fifth by , the last one by , and we add all the results. Notice that if , then . That means that now the real part of the sum of the left-hand side is just the imaginary part of (5.2).
Notice that
and, hence, it is real.
Taking into account the first line of (5.2), now we obtain another real part, which is .
Therefore, a positive constant can be found such that
and, hence,
As a consequence, we obtain
From this inequality we get that
where and δ is sufficiently greater. □
The semigroup generated by the operatoris analytic.
Since is the infinitesimal generator of a strongly continuous semigroup, and as , we have . From Lemma 5.4 we have
Then,
□
One important consequence of the analyticity of the semigroup is the stability of the solutions.
System (
2.3
) is exponentially stable. That is, there exist two positive constants M and ω such that.
Another consequence of the analyticity of the solutions is the impossibility of localization. That means that the only solution that can be identically zero after a finite period of time is the null solution.
Letbe a solution to system (
2.3
) with boundary conditions (
2.7
) and initial conditions (
2.8
) such thatafter a finite time. Then,for every.
Conclusions
In this paper we have investigated several qualitative properties for the system of equations that models the behaviour of viscoelastic materials with double porosity when we assume viscous dissipation on each porous structure. First we have proved the uniqueness of solutions whenever the dissipation is strictly positive. Later we have shown their analyticity when the internal energy and the dissipation are both positive. Exponential stability and impossibility of localization of the solutions are consequences of the analitycity.
Footnotes
Acknowledgements
The work of N. Bazarra and J.R. Fernández was supported by the Ministerio de Economía and Competitividad under the research project MTM2015-66640-P (with the participation of FEDER).
The work of M.C. Leseduarte, A. Magaña and R. Quintanilla is supported by project “Análisis Matemático de Problemas de la Termomecánica”, MTM2016-74934-P, (AEI/FEDER, UE) of the Spanish Ministry of Economy and Competitiveness.
The authors want to thank an anonymous reviewer for his comments.
References
1.
A.Ainouz, Homogenized double porosity models for poro-elastic media with interfacial ow barrier, Mathematica Bohemica136 (2011), 357–365.
2.
G.I.Barenblatt and I.P.Zheltov, On the basic equations of seepage of homogeneous liquids in fissured rock, Akad. Nauk SSSR132 (1960), 545–548(English Translation).
3.
G.I.Barenblatt, I.P.Zheltov and I.N.Kockina, Basic concepts in the theory of seepage of homogeneous liquids in fissured rocks (strata), Prikl. Mat. Mekh.24 (1960), 1286–1303(English Translation).
4.
A.Bedford and D.S.Drumheller, Recent advances: Theories of immiscible and structured mixtures, Int. J. Eng. Sci.21 (1983), 863–960. doi:10.1016/0020-7225(83)90071-X.
5.
J.G.Berryman and H.F.Wang, Elastic wave propagation and attenuation in a double-porosity dual-permeability medium, Int. J. Rock Mechanics and Mining Sciences37 (2000), 63–78. doi:10.1016/S1365-1609(99)00092-1.
6.
M.Ciarletta and B.Straughan, Thermo-poroacoustic acceleration waves in elastic materials with voids, J. Math. Anal. Appl.333 (2007), 142–150. doi:10.1016/j.jmaa.2006.09.014.
7.
S.C.Cowin and J.W.Nunziato, Linear elastic materials with voids, J. Elasticity13 (1983), 125–147. doi:10.1007/BF00041230.
S.C.Cowin and P.Puri, The classical pressure vessel problems for linear elastic materials with voids, J. Elasticity13 (1983), 157–163. doi:10.1007/BF00041232.
10.
D.Ieşan, Thermoelastic Models of Continua, Kluwer Academic, Dordrecht, 2004.
11.
D.Ieşan and R.Quintanilla, A theory of porous thermoviscoelastic mixtures, Journal of Thermal Stresses30 (2007), 693–714. doi:10.1080/01495730701212880.
12.
D.Ieşan and R.Quintanilla, On thermoelastic bodies with inner structure and microtemperatures, J. Math. Anal. Appl.354 (2009), 12–23. doi:10.1016/j.jmaa.2008.12.017.
13.
D.Ieşan and R.Quintanilla, On a theory of thermoelastic materials with a double porosity structure, Journal of Thermal Stresses37 (2014), 1017–1036. doi:10.1080/01495739.2014.914776.
14.
N.Khalili and A.P.S.Selvadurai, A fully coupled constitutive model for thermohydro-mechanical analysis in elastic media with double porosity, Geophys. Res. Lett.30 (2003), Art. No. 2268.
15.
N.Khalili and S.Valliappan, Unified theory of flow and deformation in double porous media, Eur. J. Mech. A, Solids15 (1996), 321–336.
16.
M.C.Leseduarte, A.Magaña and R.Quintanilla, On the time decay of solutions in porous-thermo-elasticity of type II, Disc. Cont. Dyn. Syst. Series B13 (2010), 375–391. doi:10.3934/dcdsb.2010.13.375.
17.
Z.Liu and S.Zheng, Semigroups Associated to Dissipative Systems, Research Notes in Mathematics, Vol. 398, Chapman & Hall/CRC, Boca Raton, FL, 1999.
18.
A.Magaña and R.Quintanilla, On the decay of in porous-elasticity with quasistatic microvoids, J. Math. Anal. Appl.331 (2007), 617–630. doi:10.1016/j.jmaa.2006.08.086.
19.
D.Masin, V.Herbstova and J.Bohac, Properties of double porosity clayfills and suitable constitutive models, 2012, http://web.natur.cuni.cz/uhigug/masin/download/mhb_16ICSMGE_Osaka.pdf.
J.E.Muñoz-Rivera and R.Quintanilla, On the time polynomial decay in elastic solids with voids, J Math. Anal. Appl.338 (2008), 1296–1309. doi:10.1016/j.jmaa.2007.06.005.
22.
J.W.Nunziato and S.C.Cowin, A nonlinear theory of elastic materials with voids, Arch. Rat. Mech. Anal.72 (1979), 175–201. doi:10.1007/BF00249363.
23.
P.X.Pamplona, J.E.Muñoz-Rivera and R.Quintanilla, Stabilization in elastic solids with voids, J. Math. Anal. Appl.350 (2009), 37–49. doi:10.1016/j.jmaa.2008.09.026.
24.
P.X.Pamplona, J.E.Muñoz-Rivera and R.Quintanilla, Analyticity in porousthermoelasticity with microtemperatures, J. Math. Anal. Appl.394 (2012), 645–655. doi:10.1016/j.jmaa.2012.04.024.
25.
S.R.Pride and J.G.Berryman, Linear dynamics of double-porosity dual-permeability materials – I, Phys. Rev. E68 (2003), 036603. doi:10.1103/PhysRevE.68.036603.
26.
V.G.Sigillito, Explicit a Priori Inequalities with Applications to Boundary Value Problems, Pitman Publishing, London, 1977.
27.
B.Straughan, Stability and uniqueness in double porosity elasticity, Int. J. Eng. Sci.65 (2013), 1–8. doi:10.1016/j.ijengsci.2013.01.001.
28.
B.Straughan, Mathematical Aspects of Multi-Porosity Continua, Springer, 2017.
29.
M.Svanadze, Dynamical problems of the theory of elasticity for solids with double porosity, Proceedings in Applied Mathematics and Mechanics10 (2010), 309–310. doi:10.1002/pamm.201010147.
30.
M.Svanadze, Plane waves and boundary value problems in the theory of elasticity for solids with double porosity, Acta Applicandae Mathematicae122 (2012), 461–471.
31.
M.Svanadze, Boundary value problems of steady vibrations in the theory of thermoelasticity for materials with a double porosity structure, Archives of Mechanics69 (2017), 347–370.
32.
R.Wilson and E.Aifantis, On the theory of consolidation with double porosity, Int. J. Eng. Sci.20 (1982), 1009–1035. doi:10.1016/0020-7225(82)90036-2.
33.
Y.Zhao and M.Chen, Fully coupled dual-porosity model for anisotropic formations, Int. J. Rock Mech. Min. Sci.43 (2006), 1128–1133. doi:10.1016/j.ijrmms.2006.03.001.