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. 2022 Sep 16;12:15562. doi: 10.1038/s41598-022-19656-w

On a two-dimensional model of generalized thermoelasticity with application

Ethar A A Ahmed 1,, A R El-Dhaba 2, M S Abou-Dina 3, A F Ghaleb 3
PMCID: PMC9481564  PMID: 36114264

Abstract

A 2D first order linear system of partial differential equations of plane strain thermoelasticity within the frame of extended thermodynamics is presented and analyzed. The system is composed of the equations of classical thermoelasticity in which displacements are replaced with velocities, complemented with Cattaneo evolution equation for heat flux. For a particular choice of the characteristic quantities and for positive thermal conductivity, it is shown that this system may be cast in a form that is symmetric t-hyperbolic without further recurrence to entropy principle. While hyperbolicity means a finite speed of propagation of heat waves, it is known that symmetric hyperbolic systems have the desirable property of well-posedness of Cauchy problems. A study of the characteristics of this system is carried out, and an energy integral is derived, that can be used to prove uniqueness of solution under some boundary conditions. A numerical application for a finite slab is considered and the numerical results are plotted and discussed. In particular, the wave propagation nature of the solution is put in evidence.

Subject terms: Materials science, Mathematics and computing, Applied mathematics, Computational science, Software

Introduction

The hyperbolic systems of partial differential equations have been a subject of permanent interest, whether in the theory for their unique properties, or for their appicability to the phenomenon of wave propagation in several branches of Science and Technology. Problems of generalized thermoelasticity leading to heat wave propagation have provided great opportunity to investigate solutions of hyperbolic systems of partial differential equations under various initial and boundary conditions. Ruggeri1 presented a survey on the relations between mathematical problems for quasi-linear hyperbolic systems and extended thermodynamics in continuum theories. It was shown that the system of balance laws can be symmetrized by use of an appropriate choice of the field variables. A purely thermal case was treated by Wilmański2, ch. 9] using an undetermined multipliers technique. Müller3 investigated the symmetric hyperbolic systems of partial differential equations in extended thermodynamics. Selivanov and Selivanova4 studied the computability properties of a system of symmetric hyperbolic equations by a difference scheme. Othman et al.5 investigated generalized thermoelastic diffusion in a homogeneous, isotropic elastic half-space based on the Green-Naghdi theory. Abbas and Zenkour6 used finite elements to investigate a two-dimensional problem under Green and Naghdi theory of thermoelasticity for a fiber-reinforcement anisotropic half-space subjected to a thermal boundary shock to assess the effects of initial stress and rotation. Cimmelli et al.7 presented a review of the modern mathematical methods in the generalized thermodynamics of continuous media. He et al.8 studied a two-dimensional generalized thermoelastic diffusion problem for a half-space. Mishra9 solved a 2D-problem of heat transfer in a thin plate based on single-phase-lagging heat conduction by superposition technique and Fourier series expansion. Ghaleb et al.10 presented a model of electro-thermoelasticity within the theory of generalized thermodynamics. Abbas and Marin11 studied a 2D-problem of generalized thermoelasticity for a half-space with surface laser heating. Rogolino et al.12 derived two generalized heat-transport hyperbolic equations and studied thermodynamical compatibility for both. Jou13 considered some fundamental aspects of non-equilibrium thermodynamics with a view on heat transport in nanosystems. Mahmoud et al.14 investigated nonlinear heat wave propagation in rigid thermal conductors. Alzahrani et al.15 studied a two-dimensional problem of a porous medium in extended thermodynamics using spectral method. Ahmed et al.1618 investigated two-dimensional problems of piezo-thermoelasticity within the dual-phase-lag model for layered media and a quarter-space. Solutions were presented based on normal modes technique, as well as numerical solutions by finite differences. Concerning the solution of systems of hyperbolic partial differential equations, Bonet et al.19 proposed a novel computational framework for thermoelasticity based on the use of a system of first order conservation laws. An explicit stabilised Petrov-Galerkin framework was proposed for the numerical solution of thermoelastic problems. Numerical examples were presented.

It thus appears from the exposed literature that 2D systems of equations of thermoelasticity in extended thermodynamics have been tackled in few cases with the aim of finding solutions to particular boundary-value problems. Analysis of such systems to explore the behaviour of solutions and well-posedness of Cauchy problems has been done only rarely sofar. The present work is situated in this context. A first order 2D linear system of plane strain thermoelasticity for a transverse isotropic material is presented within the frame of extended thermodynamics. The equations are those of classical thermoelasticity, supplemented by Cattaneo evolution equation for the heat flux. This system, in which velocities replace mechanical displacements, is shown to be reducible to a symmetric t-hyperbolic form for a particular choice of the characteristic quantities and for positive heat conduction coefficient, without further reference to an entropy principle. This result is to be contrasted to that stated by Müller3, according to which the set of quasi-linear first order balance equations of extended thermodynamics may be written in symmetric hyperbolic form by a suitable choice of fields, provided the entropy principle is observed. It is known that symmetric hyperbolic systems behave well, in the sense of well-posedness of the Cauchy problem, i.e existence, uniqueness and stability of solutions with respect to boundary conditions. A study of the characteristics of the system is carried out, and an energy integral is derived, that can be used to prove uniqueness of solution under some convenient boundary conditions. It is thus shown that the proposed system of equations is valid for the description of heat wave propagation. A numerical experiment is considered for the rectangular slab under specified boundary conditions and zero initial conditions using COMSOL Multiphysics software. Numerical results are produced for a particular solution and the obtained quantities of practical interest are represented graphically and discussed.

The linear system of equations

Let ux,uy denote the mechanical displacement components, vx,vy- the corresponding velocity components, σxx,σyy,σxy- the identically non-vanishing stress components in the plane, θ- the temperature measured from a reference temperature θ0 and qx,qy- the heat flux components. The linear equations of plane generalized thermoelasticity for a transverse isotropic material within the theory of extended thermodynamics read:

  1. Equations of motion
    ρvxt-σxxx-σxyy=0, 1
    ρvyt-σxyx-σyyy=0, 2
  2. Heat equation
    θ0γvxx+vyy+ρCeθt+qxx+qyy=0, 3
  3. Cattaneo–Vernotte relations. These evolution laws for the heat flux components replace the classical Fourier law for heat conduction. Divided throughout by thermal relaxation times τ1 and τ2 respectively, these relations read:
    ρθ0qxt+n11qx+m11θx=0, 4
    ρθ0qyt+n22qy+m22θy=0, 5
  4. The generalized Hooke’s law differentiated w.r.t. time, thus allowing to eliminate the mechanical displacement components in favour of the velocities:
    σxxt-λ+2μvxx-λvyy+γθt=0, 6
    σyyt-λvxx-λ+2μvyy+γθt=0, 7
    σxyt-μvxy-μvyx=0. 8

The problem thus reduces to the solution of eight basic partial differential equations of the first order. These equations involve eight unknowns: two velocity components, three identically non vanishing stress components, temperature and two heat flux components. Having resolved this system of equations, one can then find the mechanical displacement components by quadrature from the relations:

uxt-vx=0, 9
uyt-vy=0. 10

Here, ρ is the mass density, λ,μ- Lamé coefficients, γ- the thermoelastic coefficient and m11,m22 are constants related to the coefficients of heat conduction. Young’s modulus will be denoted E and Poisson’s ratio σ.

It is not difficult to anticipate a time damping of the heat wave, due to the terms involving n11 and n22 in the Cattaneo evolution equations. In order to relate the coefficients m11,m22,n11 and n22 in Eqs. (4 and 5) to known physical quantities, it is sufficient to compare these two equations to the well-known standard forms of the evolution equations for the heat flux (C.f.10,21):

τ1qxt+qx+k11θx=0,τ2qyt+qy+k22θy=0,

where τ1, τ2 are the thermal relaxation times for the x- and y-directions respectively, and k11, k22 are the thermal conductivities in these two directions. Direct comparison of these last two equations with (4) and (5) reveals that

m11=ρθ0k11τ1,m22=ρθ0k22τ2,n11=ρθ0τ1,n22=ρθ0τ2.

The above governing equations need to be cast in a convenient form for later work. For this, Eqs. (6 and 7) will be replaced by their symmetrized forms:

ασxx+βσyyt-vxx=0, 11
ασyy+βσxxt-vyy=0, 12

where

σxx=σxx+γθ,σyy=σyy+γθ,α=λ+2μ4μ(λ+μ)=1-ν2E,β=-μ4μ(λ+μ)=-(1+ν)(1-2ν)2E. 13

It may be easily verified that

α2-β2=14μ(λ+μ)=(1+ν)2(1-2ν)E2>0. 14

Excluding Eqs. (9 and 10) which may be considered independently in a later stage as explained above, the system of eight basic equations is written in matrix form as:

AUt+BUx+CUy=F. 15

Matrices A, B and C have dimension (8×8) and are given as:

A=ρ00000000ρ00000000αβ000000βα00000000100000000ρCe00000000ρθ000000000ρθ0,B=00-100γ000000-1000-10000000000000000-μ000000θ0γ000001000000m110000000000,C=0000-1000000-10γ00000000000-1000000-μ00000000θ0γ0000010000000000000m2200,F=000-n11-n22000,U=vxvyσxxσyyσxyθqxqy.

The following definitions are taken from Godunov20, pp. 85-88]:

Definition 1

A surface S with equation ϕx,y,t=0 on which

detϕtA+ϕxB+ϕyC=0, 16

or, equivalently,

detτA+ξB+ηC=0, 17

where τ,ξ,η denotes a vector normal to the surface S , is called a characteristic for the system of Eq. (15).

Definition 2

The system of Eq. (15) is said to be t-hyperbolic if its characteristic equation has exactly 8 real and different roots τ for arbitrary real values of the parameters (ξ,η).

In the case of multiple roots, the system still preserves all the main properties of hyperbolic systems.

Definition 3

The system of Eq. (15) is said to be symmetric, t-hyperbolic if the matrices A, B, C are symmetric and, moreover, matrix A is positive definite.

It is well-known that for symmetric, t-hyperbolic systems one can deduce the so-called energy integral, which represents a powerful tool to prove a theorem on the uniqueness of solution.

Reduction to symmetric t-hyperbolic form

In what follows, we investigate the possibility of diagonalizing the matrix τA+ξB+ηC for all values of (ξ,η) and τ>0, in order to simplify the considered system of equations and reveal its nature. As a first step, the basic equations will now be reformulated in dimensionless form. To this end, introduce the following set of dimensionless variables for length, time, temperature heat flux, velocity and stress:

x~=xL0,y~=yL0,t~=tT0,θ~=θθ0,q~=qQ0,v~=vc,σ~xx=σxxμ,

The characteristic quantities θ0,L0,T0,Q0,c are kept undetermined at this stage, but will be defined later on step by step so as to achieve some properties and simplifications. The two characteristic quantities L0 and T0 are related to each other by:

L0T0=c.

It may be noticed that the characteristic quantities θ0 and Q0 are independent of each other according to the basic assumption of extended thermodynamics adopted in the present model (see10, for example). This fact provides some flexibility in attaining the required final form of the equations.

After removing the tilde, the system of eight basic equations in dimensionless form reads:

vxt-cT2c2σxxx-cT2c2σxyy+γθx=0, 18
vyt-cT2c2σxyx-cT2c2σyyy+γθy=0, 19
θt+γρCevxx+vyy+Q0ρcCeθ0qxx+qyy=0, 20
ασxx+βσyyt-vxx=0, 21
ασyy+βσxxt-vyy=0, 22
σxyt-vxy-vyx=0, 23
qxt+n11Tρθ0qx+m11ρcQ0θx=0, 24
qyt+n22Tρθ0qy+m22ρcQ0θy=0, 25

where

α=αμ,β=βμ,γ=γθ0ρc2.

The matrices of the system now read:

A=100000000100000000αβ000000βα000000001000000001000000001000000001,B=00-cT2c200γ000000-cT2c2000-10000000000000000-1000000γρCe00000Q0ρcCeθ0000000m11ρcQ00000000000,C=0000-cT2c2000000-cT2c20γ00000000000-1000000-100000000γρCe00000Q0ρcCeθ00000000000000m11ρcQ000,F=000-n11Tρθ0-n22Tρθ0000.

Matrices B and C can be made symmetric by suitable choices of some parameters, taking in consideration that some characteristic quantities of the system are still kept arbitrary. First, let us choose the characteristic velocity to be equal to the speed of propagation of the purely elastic transverse wave in the linear approximation:

c=cT=μρ.

Next, assume the material parameters are such that the following relation holds:

γ=γρCe,

which amounts to defining the reference temperature as:

θ0=ρc2ρCe=μρCe.

Finally, define the characteristic heat flux so that:

Q0ρcCeθ0=mρcQ0=M,sayQ0=mCeθ0,m=m11=m22.

The characteristic time T0 will be determined depending on the thermal relaxation time in the numerical example treated below.

The final form of the basic system of eight equations is:

vxt-σxxx-σxyy+γθx=0, 26
vyt-σxyx-σyyy+γθy=0, 27
θt+γvxx+vyy+Mqxx+qyy=0, 28
ασxx+βσyyt-vxx=0, 29
ασyy+βσxxt-vyy=0, 30
σxyt-vxy-vyx=0, 31
qxt+nqx+Mθx=0, 32
qyt+nqy+Mθy=0, 33

where

n=n11T0ρθ0=n22T0ρθ0

for the transversely isotropic case under consideration.

By elimination, one easily deduces from the above equations the following expression for the dimensionless speed of the heat wave:

M=mρcQ0=mρμCeθ0=kτμCe. 34

Characteristics

In order to find the characteristics of the system of partial differential equations under consideration, note that the symmetric matrices A, B and C are now given by:

A=100000000100000000αβ000000βα000000001000000001000000001000000001,B=00-100γ000000-1000-10000000000000000-1000000γ00000M000000M0000000000,C=0000-1000000-10γ00000000000-1000000-100000000γ00000M0000000000000M00,F=000-12n-12n000,U=vxvyσxxσyyσxyθqxqy

and

detA=α2-β2>0.

Matrix A is positive definite as can be directly verified, with eigenvalues: 1,α+β,α-β, the first eigenvalue being repeated six times. The corresponding normalized eigenvectors are shown below together with their corresponding eigenvalues:

10000000,010000001,0012120000α+β,00-12120000α-β,00001000,00000100,00000010,000000011.

Introduce the matrix T whose columns are the eigenvectors of matrix A, arranged as shown above:

T=10000000010000000012-120000001212000000001000000001000000001000000001

The similarity transformation with matrix T: X=TTXT applied to matrices A, B and C yields the following:

A=100000000100000000α+β00000000α-β000000001000000001000000001000000001,B=00-12120γ000000-1000-1200000001200000000-1000000γ00000M000000M0000000000,C=0000-100000-12-120γ000-120000000-12000000-100000000γ00000M0000000000000M00,F=00-12n-12n-12nρ000,U=vxvy12σyy+σxx12σyy-σxxσxyθqxqy.

The new matrices are all symmetric. Moreover, A is positive definite. Thus, the transformed system of equations is symmetric, t-hyperbolic.

Further, consider the symmetric matrix W=A-1/2ξB+ηCA-1/2:

W=00-12ξα+β12ξα-β-ηγξ0000-12ηα+β-12ηα-β-ξγη00-12ξα+β-12ηα+β00000012ξα-β-12ηα-β000000-η-ξ000000γξγη0000MξMη00000Mξ0000000Mη00.

This matrix is diagonalized by means of a matrix O, say:

OTA-1/2ξB+ηCA-1/2O=D.

Then the two symmetric matrices A and ξB+ηC are simultaneously diagonalizable by means of the transformation S=A-1/2O for all real values of (ξ,η). Moreover, the diagonal form of the first matrix is the unit matrix:

STAS=OTA-1/2AA-1/2O=OTO=I,STξB+ηCS=OTA-1/2ξB+ηCA-1/2O=OTWO=D.

The diagonal matrix D may be obtained from the eigenvalues of matrix W. The characteristic equation of this matrix is:

λ2λ6-α1λ4+α2λ2-α3=0. 35

The expressions for the coefficients are as follows:

α1=ξ2+η21+γ2+M2+αα2-β2,α2=121α-β+M21+αα2-β2ξ2+η22+121α+β+γ2ξ2-η22+1+α+βα2-β2ξ2η2,α3=M2α2-β2αξ6+η6+ξ2ξ2+η21+α+2β,

from which it is seen that they are all positive. For sufficiently small absolute values of ξ and η, the value of α1 is much larger than the values of the other two coefficients α2 and α3.

Consider the related cubic equation:

(f(z)=)z3-α1z2+α2z-α3=0. 36

One easily verifies that

f(0)=α2>0,f(0)=-2α1<0. 37

The local extrema of function f are located at:

z1=α1-α12-3α2,z2=α1+α12-3α2. 38

The discriminant for this cubic equation is:

Δ=18(α1)(α2)(α3)-4(α1)3(α3)+(α1)2(α2)2-4(α2)3-27(α3)2 39

It is easy to see that sufficient conditions to get a curve shape for the cubic polynomial as in fig.1, i.e. for the eigenvalues to be real, are:

α12-3α20,z13-α1z12+α2z1-α3z23-α1z22+α2z2-α30. 40

For the used values of the material parameters, these two conditions are likely to be satisfied for all values of ξ and η. The fulfillment of the two conditions was achieved numerically as illustrated in Figs. 2 and 3. At the particular point (ξ=0,η=0), all eigenvalues are coincident and equal to zero. Thus the Eq. (35) has eight real roots: A double root equal to zero, three positive roots, and three negative roots, the roots being symmetrically positioned with respect to the origin. One is finally led to the following:

Figure 1.

Figure 1

Cubic polynomial.

Figure 2.

Figure 2

Satisfaction of the first condition for -0.5ξ,η0.5.

Figure 3.

Figure 3

Satisfaction of the second condition for -0.5ξ,η0.5.

Theorem

For all real values of the parameters ξ,η, the characteristic Eq. (17) of the considered linear system of equations has eight real roots symmetrically positioned w.r.t. origin of the real line: there are three positive roots, three negative roots and a zero root of multiplicity 2.

The energy integral

It is well-known (c.f.20) that an energy integral can be derived for symmetric t-hyperbolic systems of partial differential equations. If V denotes a region of the t,x,y-space included in the domain of definition of the solution, bounded by a surface S, then the energy integral for the transformed system reads20, p. 123]:

SτA+ξB+ηC,Uds=VDU,U+2F,Udv, 41

where operator D is defined as:

D=tA+xB+yC

and f,g denotes the scalar product of the included functions. For the case under consideration, lengthy manipulations lead to the following form of the r.h.s. of (41):

SτA+ξB+ηC,Uds=Sτ|v|2+|q|2+θ2+α-βσxx2+α+βσyy2+σxy2ds+2SGθv.n+Mθq.n-σv.nds, 42

where n=ξ,η and we have introduced σ with components:

σxx=12σyy+σxx,σyy=12σyy-σxx,σxy=σxy.

It is known that the characteristic surfaces for the wave equation are parts of conuses with axis parallel to the t-axis, so that τ>0. The boundary conditions are taken in the form:

v.n=q.n=σv.n=0, 43

yielding

VDU,U+2F,Udv0. 44

It is well-known that this last inequality leads to uniqueness of solution. The first two boundary conditions in (43) mean impermeability and thermal insulation of the boundary. The third one englobes many cases, among which complete fixing of the boundaries.

Numerical application

As a confirmation of the existence of solutions to the investigated system of equations, we have considered a Cauchy problem for rectangular slab under specified boundary conditions. The solution includes the propagation of three types of waves, the heat wave, the transversal and the longitudinal thermomechanical coupled waves. Setting τ=τ1=τ2 the thermal relaxation time and k=k11=k22 the coefficient of heat conduction, one has to make assumptions concerning the orders of magnitude of constants appearing in (4) and (5):

n11,n22ρθ0τ,m11,m22kρθ0τ.

Thus the dimensionless parameters M and n appearing in the dimensionless Cattaneo Eqs. (32 and 33) satisfy the rules

MkμCeτ,nT0τ.

For the example treated below, one has M1 and n1, hence

τkμCe,T0τ.

With this in mind, let us consider the case of a transversely isotropic material having tentative values of the different geometrical and material parameters shown in Table 1. Consultation of the available tables of material coefficients for metals and alloys reveals that the used values of mass density and specific heat capacity as displayed in Table 1 are within the normal range, while the thermal conductivity lies in the higher range.

Table 1.

Values of the material parameters.

a=0.4m b=0.4m τ=0.444×10-10s
θ0=300K ρ=0.333×104kg/m3 ν=0.435
E=0.861×1010kg/m.s2 λ=2.000×1010kg/m.s2 μ=0.300×1010kg/m.s2
γ=0.230×10-41/K Ce=0.300×104J/kg.K k=400W/m.K

Corresponding to these values:

L010-8m,T010-11s,c103m/s.

Motion is induced by a thermal boundary regime. For this, consider a rectangular domain occupied by a thermoelastic material, with dimensions a and b and sides labeled S1, S2, S3 and S4 as shown in Fig. 4. The origin of the plane Cartesian coordinate system is chosen at the left lower corner of the rectangle, with x-axis along the side S4.

Figure 4.

Figure 4

Schematic representation of the problem.

Initially, the medium is at rest at zero temperature (measured from an initial ambient temperature θ0) and heat flux, and in a stress-free state. The chosen boundary conditions are of mixed type. Mechanically, sides S1, S2 and S4 are traction-free, side S3 is completely fixed so that to suppress rigid body motion of the slab. As concerns the thermal conditions, the normal heat flux is taken to vanish on boundaries S2,S3 and S4, together with Robin thermal condition. Side S1 has a prescribed heating regime that generates the motion. It should be remembered that temperature and heat flux are independent thermodynamical quantities. For definiteness:

(1) At the side S1(x=0,0yb):

σxxS10,y,t=σxyS10,y,t=0 45

and

θS10,y,t=200yb-ytexp-0.1t,0t5×10-30,t>5×10-3,0yb 46

The graphical representation of this function for b=0.4 is illustrated in Fig. 5.

Figure 5.

Figure 5

The applied thermal boundary condition.

(2) At the side S2(y=b,0xa):

σyyS2x,b,t=σxyS2x,b,t=qyS2x,b,t=0, 47

together with Robin thermal condition

θS2yx,b,t+BiθS2=0, 48

(3) At the side S3(x=a,0yb):

σxxS3a,y,t=σxyS3a,y,t=qxS3a,y,t=uxa,y,t=uya,y,t=0 49

and Robin thermal condition

θS3xa,y,t+BiθS3=0, 50

(4) At the side S4(y=0,0xa):

σyyS4x,0,t=σxyS4x,0,t=qyS4x,0,t=0 51

and Robin thermal condition

-θS4yx,0,t+BiθS4=0. 52

Here, Bi is a dimensionless Biot number, with value taken as Bi=0.0144. All the remaining functions not specified in the above boundary conditions are set to zero on the boundaries.

Following similar guidelines as in22,23, COMSOL Multiphysics is used to solve the considered boundary-value problem for Eqs. (2633) under the boundary conditions (4652) and zero initial conditions. For definiteness, we mainly consider the case with M=3.0,n=1.0. The value of M, however, was varied to take on other values in some plots. The produced particular solution has been obtained by the method of finite elements embedded in the above-mentioned software. The mesh could be refined and adjusted for best results.

From symmetry of the considered problem about the median line y=b/2, it follows that the quantities uy,vy,qy,σxy must vanish everywhere in the slab. The numerical computations have confirmed this fact . It thus follows that the displacements, velocities and heat flux take place along the direction perpendicular to the heated face of the slab (the x-direction), and that shear stress vanishes inside the slab.

Figures 6, 7, 8, 9 , 10 and 11 represent topviews of the 3-D distributions at three consecutive time moments of the main physical quantities induced inside the material due to applied boundary conditions.

Figure 6.

Figure 6

Top view of the temperature distribution in the slab at three consecutive time moments.

Figure 7.

Figure 7

Top view of the distribution of qx in the slab at three consecutive time moments.

Figure 8.

Figure 8

Top view of the distribution of ux in the slab at three consecutive time moments.

Figure 9.

Figure 9

Top view of the distribution of vx in the slab at three consecutive time moments.

Figure 10.

Figure 10

Top view of the distribution of σxx in the slab at three consecutive time moments.

Figure 11.

Figure 11

Top view of the distribution of σyy in the slab at three consecutive time moments.

The calculations are performed for a dimensionless heat wave speed M=3. This wave thus travels three times faster than the transversal coupled thermoelastic wave whose dimensionless speed is c=1.0. For the chosen values of the material constants, the longitudinal coupled thermoelastic wave travels at speed 2.944. In all these figures, wave propagation phenomenon is clearly illustrated for both the mechanical and the thermal variables, with oscillations between positive and negative values near the heated side of the slab, and amplitudes monotonically decreasing to zero with distance. For the considered time values, the wave fronts are clearly noticed and the propagating disturbances have not yet reached the far end of the slab and therefore no reflected waves are expected. Larger time values could not be considered due to lack of stability of the computational scheme.

The first remark concerns the distribution of temperature in the slab. Although the motion was initiated by heating of the left boundary for a finite lapse of time, it is noticed in Fig. 6 that temperature assumes negative values near this boundary for the considered values of time. This seemingly paradoxical situation may be explained by the fact that part of the thermal energy supplied to the medium at the boundary is spent to generate mechanical wave propagation and, therefore, cooling may take place in some parts of the medium. Again, as shown by Ahmed et al.24 for the case of a rigid thermal conductor, negative temperatures can result from unphysical values assigned to the thermal relaxation time.

As noted above, heat flux and temperature are independent thermodynamical variables. Heat flux is initially generated by the thermal boundary condition. In subsequent time moments, it propagates as a wave, with speed M, independently of temperature as shown in Fig. 7.

Still at the heated end, the displacement and the velocity components ux and vx in Figs. 8 and  9 take on negative values in the initial phase of the motion, as the medium expands under heating. Both quantities are seen to tend to zero as the corner points are approached.

The stress components σxx and σyy are illustrated in Figs. 10 and  11. These two components take on negative values near the heated end of the slab, while σyy assumes zero value at the ends y=0,b in conformity with the applied boundary conditions. In order to confirm the satisfaction of the boundary condition for the first stress components, we have produced 2D-Fig. 12 for the distributions of the functions θ,ux and σxx on the median line y=b/2 for time value t=3.2×10-3 and for three values of parameter M, from which it is seen that the stress component σxx in fact satisfies the boundary condition on S1. These figures clearly show the effect of increase of parameter M on the amplitudes of the functions.

Figure 12.

Figure 12

Distributions of T,ux and σxx on the median line y=b/2 for t=3.2×10-3 and three values of M.

Conclusions

We have investigated a two-dimensional system of first-order, partial differential equations of classical thermoelasticity, supplemented with Cattaneo-type evolution equation for the heat flux to replace Fourier law for heat conduction. The model includes only one thermal relaxation time for each component of the heat flux vector. It differs from other well-known models of extended thermodynamics, e.g. Lord and Shulman, Green and Naghdi, two-temperature model, dual-phase-lag model, which all start with different assumptions and yield heat wave propagation (C.f.25). Under the assumption that thermal conductivity must be positive, it turns out that the present system is reducible to symmetric t-hyperbolic form by special choices of some characteristic quantities. This result is to be contrasted with that expressed by Müller3, stating that the set of quasi-linear first order balance equations of extended thermodynamics may be written in symmetric hyperbolic form by a suitable choice of fields, provided constitutive functions are subject to the requirements of the entropy principle. The characteristics of the system were studied and an energy integral was obtained which leads to uniqueness of solution under proper boundary conditions. Thus the present system of equations behaves well in the sense of well-posedness of Cauchy problems, and is therefore valid for the description of heat wave propagation. To confirm the existence of solutions, a numerical experiment for a finite slab was carried out using a finite element scheme built in COMSOL Multiphysics and with tentative values of the different material parameters to produce a particular solution to the problem under specified boundary conditions and zero initial conditions. The numerical results could be obtained only for sufficiently small time values due to difficulties related to the stability of the numerical scheme. The presented three-dimensional plots clearly show the phenomenon of thermal and thermomechanical wave propagation. It was noticed that temperature attains negative values at certain locations inside the slab, although the left boundary is subjected to heating for a certain lapse of time. This is due to the fact that part of the supplied thermal energy is spent on generating the motion. Such phenomenon should not appear in rigid thermal conductors once the value of the thermal relaxation time has been properly assigned (C.f.24). The presented figures show the wave front and the damping of the solution as disturbances progress along the slab. Verification of the satisfaction of the boundary conditions was carried out.

Author contributions

A.F.G. and M.S.A.-D. suggested the model E.A.A.A. worked on the uniqueness theorem A.R.E.-D. fulfilled the numerical part.

Funding

Open access funding provided by The Science, Technology & Innovation Funding Authority (STDF) in cooperation with The Egyptian Knowledge Bank (EKB).

Data availability

All data generated or analyzed during this study are included in this published article

Competing interest

The authors declare no competing interests.

Footnotes

Publisher's note

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Data Availability Statement

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