Abstract
This article continues the work on dipolar thermoelastic materials, which are a special case of multipolar continuum mechanics. This theory allows a double-porous structure: a macro-porosity related to pores in the material and a microporosity, which shows fissures in the porous skeleton. This paper constructs a mathematical model for dipolar materials, which have a double-porosity structure by considering a fractional order Duhamel–Neumann stress–strain relation. The heat conduction is described by Cattaneo’s equations. The results are the constitutive equations of the linear theory of thermoelasticity with fractional order strain. The equations are valid for anisotropic materials and are called the Duhamel–Neumann equations with fractional order. Finally, the isotropic case is considered under the conditions of plane strain in order to perform some numerical simulations for samples of porous copper.
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Appendix
Appendix
Proof of Lemma 1
Proof
The first equation from (1) is multiplied by \({\dot{u}}_i\) and is integrated over \(\Omega \) to obtain
The second equation from (1) is multiplied by \({\dot{\phi }}_{jk}\). Then, we sum up over j and k and integrate over \(\Omega \) to obtain
The first equation from (2) is multiplied by \(\dot{\varphi }\) and is integrated over \(\Omega \) to obtain
The second equation from (2) is multiplied by \(\dot{\psi }\) and is integrated over \(\Omega \) to obtain
We substitute relations (53), (54), (55) and (56) into the principle of conservation of energy (11) to obtain
By doing integration by parts
and by substituting (58), (59), (60) and (61) into (57), we obtain
which can be rewritten as
or in the pointwise form
We obtain from Eqs. (64) and (14)
\(\square \)
Proof of Theorem 1
Proof
We obtain from the first relation in (15) and the chain rule
By comparing formulae (19) \(\rho _0\dot{\phi }=t_{ij}\dot{\tilde{\varepsilon }}_{ij}+\eta _{ij}\dot{\kappa }_{ij}+\mu _{ijk}\dot{\chi }_{ijk}+ \sigma _i\dot{\varphi }_{,i}-\xi \dot{\varphi }+\tau _i\dot{\psi }_{,i}-\zeta \dot{\psi }+q_{i,i}+\rho _0Q- \rho _0\eta {\dot{T}}-\rho _0 T\dot{\eta }\) and (66), we obtain
and
The proof is complete if we compute the derivatives above by formula (17). \(\square \)
Proof of Theorem 2
Proof
Using the equality for \(\eta \) from (67) and (68), we obtain
By using Eqs. (69) and (17), we obtain the gradient of the heat flux in the form
Let \(T\approx T_0\) for linearity, where \(T_0\) is the constant absolute temperature of the body in its reference state. Therefore, we get
The non-Fourier heat equations give
\(\square \)
Closed-form solution in the isotropic case
We consider the problem of plane strain biaxial deformation of a rectangular specimen as in [37] for isotropic dipolar elasticity with double porosity in the stationary case. We consider that \(\tau =0\), \(\theta =0\) and we assume that \(u_1(x_1)=c_1 x_1\), \(u_2(x_2)=c_2 x_2\), \(\phi _{11}=c_3\), \(\phi _{22}=c_4\), \(\phi _{12}=\phi _{21}=0\), \(\varphi =c_5\) and \(\psi =c_6\), where \(c_i\) are constants. These satisfy the displacement boundary conditions \(u_1(x_1=0)=0\) and \(u_2(x_2=0)=0\). Following [37], we show in the sequel that they also satisfy the governing equations and the remaining boundary conditions, so that they must be the unique solution of the problem.
By substituting the expressions above into the equations from Theorem 4, we are only left with Eqs. (46), (49), (51) and (52), which become
The boundary conditions are \(t_{22}+\eta _{22}=\tilde{t}_2\) at the top and \(t_{11}+\eta _{11}=0\) at the sides. Hence, we obtain by virtue of the expressions for \(t_{ij}\) and \(\eta _{ij}\)
Then, we solve the above linear system of six equations for \(c_i, i=1,6\), and we substitute into the definitions of the functions, which yields
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Chirilă, A., Marin, M. The theory of generalized thermoelasticity with fractional order strain for dipolar materials with double porosity. J Mater Sci 53, 3470–3482 (2018). https://doi.org/10.1007/s10853-017-1785-z
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DOI: https://doi.org/10.1007/s10853-017-1785-z