Abstract
The present study approaches the theory of Moore–Gibson–Thompson thermoelasticity in the context of the materials with double porosity structure. The main results of the present study are based on a reciprocity theorem for the thermoelastic materials with double porosity that leads us in determining of the uniqueness theorems for the solution of mixed problems for the materials with double porosity. The reciprocity theorem is a Betti-type result that has the main goal to establish the connection between the external action systems and their thermoelastic states. In order to obtain the uniqueness results, it was introduced a new form of energy equation.
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1 Introduction
In the last years, the Moore–Gibson–Thompson (MGT) equations have drawn the attention of many researchers. Although initially, the MGT equation modeled the physical phenomena from fluid mechanics, [1], in the last years it was approached under the thermoelasticity theory from the MGT perspective, where the heat transfer is governed by an integro-differential equation, [2]. The MGT thermoelasticity with two temperatures is studied in [3]. Many scholars approached this theory from a theoretical point of view [4,5,6,7] and also from a practical point of view [7,8,9,10,11]. The domain of influence under the MGT thermoelasticity theory was studied recently, [16, 17]. Some papers deal with the linear elasticity theory for bodies with a dipolar structure [14, 15]. In the present study, we considered the MGT theory in the context of materials with double porosity. The bodies with double porosity are encountered in many technical domains having applicability in building materials or geology, [18, 19] as well as in medicine, having applications in the study of the bones [20].
The materials with double porosity structure present a high interest, fact that is proved by the numerous papers that deal this type of media, [21,22,23,24,25,26,27,28]. Also, this type of material was approached by us in some previous studies, [29,30,31].
The present paper is structured as follows. In Sect. 2 is defined the mixed problem for MGT thermoelasticity with double porosity structure. Section 3 highlights the main results of the present study that are based on a reciprocity theorem for the anisotropic thermoelastic materials with double porosity that leads us in determining of the uniqueness theorems for the solution of mixed problems for the materials with double porosity. The reciprocity theorem is a Betti-type result that has the main goal to establish the connection between the external action systems and their thermoelastic states. In order to obtain the uniqueness results, it was introduced a new form of energy equation.
2 Basic equations
The motion equations of a double porous material are:
The balance equations are:
In the equations that govern the linear thermoelasticity of the double porous material (1), (2), we have the following notations: \(\rho \) is the density of the body, \(\kappa _1, \kappa _2\) are the equilibrated inertia coefficients, \(\tau _j\) and \(\sigma _j\) are the stress vectors and \(t_{ij}\) is the stress tensor on the surface of the body \(\partial {\varOmega }\). The forces that act on the double porous body are:
-
the direct forces \(F_i\);
-
the forces that act on the pores: p is the intrinsic force and M is the extrinsic force;
-
the forces that act on the cracks: r is the intrinsic force and N is the extrinsic force.
In these equations, we have noted by dot the variation in report with time of the displacement field \(u_i\) and the volume fraction fields \(\phi , \psi \).
The differential Moore–Gibson–Thompson (MGT) equation for thermoelasticity was obtained by Quintanilla (MMS/2019) for the relaxation parameter \(\gamma >0\) in the context of Maxwell and Cattaneo heat conduction:
where \(K_{ij}\) is the conductivity rate tensor, \(\theta \) is the temperature and c is the thermal capacity.
In order to have a mixed-initial boundary value problem, we have the initial conditions:
for all \(x\in {\varOmega }\), where \({\varOmega }\) is the three dimensional domain that is considered smooth enough in order to apply the divergence theorem.
The Dirichlet boundary conditions are:
Further, we consider the following assumptions:
-
(a)
The thermal capacity c(x) is a positive function such as there is a positive constant \(c_0>0: c(x)\ge c_0>0\);
-
(b)
For every vector \(\zeta _i\), there is a positive constant \(k^*\) such as:
$$\begin{aligned} K^*_{ij}\zeta _i\zeta _j\ge k^*\zeta _i\zeta _i; \end{aligned}$$(a.1) -
(c)
For every vector \(\zeta _i\), there is a positive constant \({\tilde{k}}\) such as
$$\begin{aligned} h_{ij}\zeta _i\zeta _j\ge {\tilde{k}}\zeta _i\zeta _i, \end{aligned}$$(a.2)where \(h_{ij}(x)=K_{ij}(x)-\gamma K_{ij}^*(x)\);
-
(d)
For every vector \(\zeta _i\), there is a positive constant \(k^0\) such as:
$$\begin{aligned} K_{ij}\zeta _i\zeta _j\ge k^0\zeta _i\zeta _i. \end{aligned}$$(a.3)
The deformations of the bodies with double porosity are given by the following variables: \(u_i(x,t), \phi (x,t),\psi (x,t), \theta (x,t), (\forall )(x,t)\in {\varOmega }\times [0,\infty )\).
The energy function has the following quadratic form in the context of the linear thermoelasticity for materials with double porosity structure:
The constitutive equations for the bodies with double porosity in the context of linear thermoelasticity are:
The relations (7) are obtained based on the quadratic form of internal energy (6), i.e.,
The energy equation is:
where \(\delta \) is the heat supply, \(q_i\) is the heat flux, \(\eta \) is the entropy and \(T_0\) is the absolute temperature that is considered constant in the reference configuration. Taking into account the constitutive equation regarding the entropy (7)\(_6\) and the flux equation (7)\(_7\), the energy equation will have the following form:
In the context of MGT theory of thermoelasticity for materials with double porosity structure, it is necessary to insert the initial conditions for \(t=0\):
The mixed problem for the MGT theory has the boundary conditions:
where \(u_i^*, t_i^*, \phi ^*, \psi ^*, m^*, \theta ^*, \nu ^*\) are prescribed functions for a specific moment of time \(t^*\) that can be finite or infinite.
The boundary of the domain \({\varOmega }\) is divided in four surfaces \(\partial {\varOmega }_1\), \(\partial {\varOmega }_2\), \(\partial {\varOmega }_3\), \(\partial {\varOmega }_4\). The complement of the considered surface is noted by superscript index “c” such that: \(\partial {\varOmega }_i\cap \partial {\varOmega }_i^c=\emptyset \) and \(\partial {\varOmega }_i\cup \partial {\varOmega }_i^c=\partial {\varOmega }\), \(\forall i=\overline{1,4}\).
The components of the surface force traction, surface couple and flux are expressed by:
In the context of MGT theory of thermoelasticity for materials with double porosity structure, the mixed problem is formed from Eqs. (1), (2), (7) and (8) with initial conditions (10) and the boundary conditions (11).
The solution of the considered problem is the ordered array \((u_i,\phi ,\psi ,\theta )\) and it is represented by the effect of the external actions \((E_A)\) on the system that are defined by the ordered array:
The thermoelastic state \((T_S)\) generated by the external forces is defined by:
Further, we will consider that on the double porous material act two different loading systems:
and for each loading system, we have two thermoelastic states:
3 Reciprocity and uniqueness theorems
In this section, we will enunciate some reciprocity theorems that are of Betti’s type. These theorems are useful in order to determine a reciprocity relation between the external action systems and their corresponding thermoelastic states. Further, we consider the convolution product \(*\).
Theorem 1
Let us consider the external action systems \(E_A^{(i)}\) for two different types of loadings and their thermoelastic states \(T_S^{(i)}\), respectively. The following reciprocity relation takes place:
Proof
In order to obtain the reciprocity relation of Betti type, we will apply the Laplace transform to Eqs. (1) and (2). Let us consider that the image through the Laplace transform of the original function f(x, t) will be \({{\overline{f}}}(x,t)\). Therefore, the governing equations for the double porous materials will have the following form:
The energy equation (9) through the Laplace transform will be:
The constitutive equations through the Laplace transform will have the following form:
The boundary conditions (11) through the Laplace transform become:
Writing Eq. (14)\(_1\) for each loading and multiplying with \({{\overline{u}}}_i^{(2)}\) and \({{\overline{u}}}_i^{(1)}\), respectively, and after that subtract and integrate on the considered domain, we obtain:
In the first integral from the right side of (18), we apply the divergence theorem, and in the second integral from the right side of (18), we will take into account the constitutive Eq. (16). Therefore, Eq. (18) will have the following form:
Next, we write Eq. (14)\(_2\) for the both loading systems and compute the subtraction after each equation is multiplied by \({\overline{\phi }}^{(2)},{\overline{\phi }}^{(1)}\), respectively. Integrating on \({\varOmega }\), we obtain:
In the first integral from the right side, we apply the divergence theorem, and for both integrals, we take into account the constitutive equations. Therefore, the relation (20) will have the following form:
At last, we multiply the equations from (14)\(_3\) with \({\overline{\psi }}^{(2)}\) and \({\overline{\psi }}^{(1)}\) written for each load of the system, making the subtraction and integrate on the considered domain. Now we have:
Using the divergence theorem and the constitutive equations and taking into account the boundary conditions (11), the relation (22) will have the form:
Next, we write the energy equation (15) for both loadings and we multiply them by \({\overline{\theta }}^{(2)}\) and \({\overline{\theta }}^{(1)}\), respectively, and after that subtracting the relations and integrating on the domain \({\varOmega }\), we have:
Using the divergence theorem and taking into account the boundary conditions, the relation (24) becomes:
We may observe that in Eq. (25) appear the terms from (19), (21) and (23); therefore, the relation (25) will take the following form:
In the relation (26), we apply the inverse Laplace transform \({\mathcal {L}}\) and the convolution product noted by \(*\) is obtained. Thus, we use:
The result from Theorem 1 is obtained. \(\square \)
Based on the theory of Green and Lindsay, let us introduce the scalar function:
The energy function of Moore–Gibson–Thompson thermoelasticity will have the expression:
where according to Biot, the generalized free energy function \({\mathcal {E}}\) is given by:
where \(E_i\) is the internal energy. Taking into account the initial conditions of the MGT thermoelasticity from (10), the energy function \({\mathbb {E}}\) will have the following quadratic expression:
where \(A=\frac{3}{2}c, \; B=\frac{3}{2}c\gamma +b{\mathcal {M}}, C=\frac{3}{2}c\gamma ^2+\frac{d}{2}{\mathcal {M}} \) and \({\mathcal {M}}=\beta _{ij}u_{i,j}+a_1\phi +a_2\psi .\) The kinetic energy per mass unit is given by:
Based on the relation of function of energy (30) and kinetic energy (31), we can enunciate the following theorem:
Theorem 2
The variation of energy in the MGT thermoelasticity for double porous materials is expressed by:
Proof
The variation of the kinetic energy in report with time is:
The terms from (34) are obtained from the governing equations for the double porous bodies (1), (2), multiplied by \(\dot{u}_i, {\dot{\phi }}\) and \({\dot{\psi }}\), respectively. Therefore, by integration on the \({\varOmega }\) domain, using the divergence theorem and taking into account the constitutive Eq. (7), Eq. (34) takes the following form:
Integrating on the domain \({\varOmega }\) the variation of the function of energy (30) in report with time, we have:
Taking into account the energy equation given in (9), we have:
Summing the relations (34) and (35) on the domain \({\varOmega }\), we obtain the variation of the energy in the context of the MGT thermoelasticity for double porous materials. Therefore, the result of Theorem 2 is obtained. \(\square \)
Theorem 3
If the energy function \({\mathbb {E}}\) from (30) is positive defined, then the considered mixed problem for double porous materials in the MGT thermoelasticity contexts admits only one solution.
Proof
In order to prove the uniqueness of the solution of the mixed problem for double porous materials in the context of MGT thermoelasticity, we assume that the considered problem admits two solutions: \((u_{i1},\phi _1,\psi _1, \theta _1)\) and \((u_{i2},\phi _2,\psi _2, \theta _2)\).
For null loadings \(F_i, M\) and N and for zero boundary conditions: \(u_i^*=0, \phi ^*=0, \psi ^*=0, t_i^*=0, \lambda ^*=0, m^*=0,\nu ^*=0,\) the difference between these solutions \((u_{i1}-u_{i2},\phi _1-\phi _2,\psi _1-\psi _2, \theta _1-\theta _2)\) is also a solution of the mixed problem for double porous materials in the MGT thermoelasticity context.
Therefore, the energy equation (35) will have the following expression:
Taking into account the null initial conditions for \(t=0\) from (10), we observe that the kinetic energy from (31) and the energy function from (30) are zero: \(E_{{\mathbb {K}}}=0;\; {\mathbb {E}}=0\). Hence, their sum is also zero. Based on the above inequality, on the fact that the energy and the kinetic energy are positive defined, we may draw the conclusion that the difference between the considered solution is null. Therefore, the mixed problem with initial and boundary conditions for the double porous materials in the MGT thermoelasticity context is unique. \(\square \)
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Florea, O.A., Bobe, A. Moore–Gibson–Thompson thermoelasticity in the context of double porous materials. Continuum Mech. Thermodyn. 33, 2243–2252 (2021). https://doi.org/10.1007/s00161-021-01025-z
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DOI: https://doi.org/10.1007/s00161-021-01025-z