Abstract
The major finding of this paper is studying the stability of a double diffusive convection using the so-called local thermal non-equilibrium (LTNE) effects. A new combined model that we call it a Brinkmann-Forchheimer model was considered in this inquiry. Using both linear and non-linear stability analysis, a double diffusive convection is used in a saturated rotating porous layer when fluid and solid phases are not in the state of local thermal non-equilibrium. In addition, we discussed several related topics such as the effect of solute Rayleigh number, symmetric properties, Brinkman coefficient, Taylor number, inter-phase heat transfer coefficient on the stability of the system, and porosity modified conductivity ratio. Moreover, two cases were investigated in non-linear theory, the case of the Forchheimer coefficient and the case of the Taylor-Darcy number . For the validation of this work, some numerical experiments were made in the non-linear energy stability and the linear instability theories.
Keywords:
double diffusive convection; porous layer rotation; brinkman model; local thermal non-equilibriummodel; Taylor-Darcy number; Forchheimer model MSC:
35D40; 65C30; 90C55
1. Introduction
Due to their wide range of applications, from the unification of binary mixtures to melting runoff in saturated soil, double diffusive convection problems in fluid and porous media have received a lot of attention in the last few decades, where symmetric properties played an important role in solving these problems. The study of double diffusive-convection in a rotating porous media has been covered and supported theoretically in many studies as well as through practical applications in engineering. The study of double diffusive-convection in a porous medium based on the theory of linear stability for several thermal and solute boundary conditions was first undertaken by [1]. Later, authors in [2] studied the double diffusive-convection in porous media with the existence of double-diffusion effects. An essential study of the effects of rotation on linear and non-linear double diffusive convection in a sparsely packed porous medium can be found in [3]. Important examples and experiments that contain geophysical framework, electrochemistry, and some other applications with an explanation of the non-linear energy stability of double diffusive convection problems, resulting in many future investment, are those in [4,5]. A really deep study and a comprehensive review of the problems associated with these mentioned applications can be found in [6,7]. Moreover, an excellent review of literature on double diffusive natural convection in a porous, fluid-filled medium can be obtained in the book [8]. Other useful review articles on a double diffusive convection in porous media can be found in [9,10,11]. The authors in [12,13,14] studied the non-linear disturbance theory that is used for the observation of the double diffusive convection in a porous horizontal layer. The same study was performed by [15], where the linear stability of thermal convection was analyzed using the Darcy–Brinkman model. Another important category of studies that are related to the problems of double diffusive-convection and the melting of permafrost under the sea can be seen in [16,17,18,19]. The impact of porous medium anisotropy on double diffusive convection was explained in [20]. Further studies with many different applications such as solidify and centrifugal casting of minerals, bio-mechanics, petroleum manufacture, chemical operations and food, rotating machinery, and geophysical problem are found in [21,22,23,24,25,26,27,28,29,30,31,32,33,34,35].
2. Basic Equations
Consider a rotating porous material layer that is located between the two planes and and that has been saturated with fluid as shown in Figure 1 below.
Figure 1.
A rotating fluid saturated porous layer.
The problem can be represented as follows
The equations are:
where is the Laplace operator in 3-dimensions. and denote velocity, pressure, concentration of salt, temperature of the solid and temperature of the fluid, respectively. The terms and denote permeability, dynamic viscosity, gravity, density, porosity, thermal expansion coefficient, solute expansion coefficient, specific heat at constant pressure, inter-phase heat transfer coefficient, thermal conductivity of the fluid expansion coefficient, thermal conductivity of the solid, salt diffusivity, angular velocity of rotation, Forchheimer coefficient and Brinkman coefficient, respectively.
Throughout this paper, we will use both of the standard indicial and Einstein notations, and .
Let us assume that the domain . It is obvious that the equations of (1) hold in , and assume that denote the solution of the initial steady state of the system, such that the fluid flow is vanished, , and assume also that these solutions are in terms of only z, such that:
where , , which is called the steady pressure, and it is given by (2)1 and can be reduced to
To understand how the stability in (2) works, we introduce the perturbation to the steady solutions , such that
Using the equations in (3) and in (4), the system can be introduced as the following
Let us consider now the variables with no dimensions that have the following scales
Here and are the numbers of Rayleigh (dimensionless numbers), and is the Taylor-Darcy number. Therefore, the equations of the system of no-dimension can be given as
where and B are the Forchheimer and Brinkman coefficients, respectively, and the boundary conditions are given by the following
3. Linear Instability
To obtain the threshold for linear instability case, we neglect the nonlinear terms from system (6). Since we have here a linearity, one can find solutions for the form and such that . Thus, we end up having the following system
Now, we consider the so-called “normal mode” of the representation , , and , such that is a plan-form that tiles the plane with .
Hence, letting
Now, multiplying Equation (11)1 by and , yields
With , (13) is reduced to
Since the boundary condition is represented on , one can rewrite W as series of the sin function, such that , where . Next, with , and a is the number of waves in the series in (15), one can obtain
Then, minimizing with respect to , we obtain
where
As finding the zeros of Equation (17) analytically is almost impossible, we use some iterative methods for solving nonlinear equations such as Newton Raphson (NR), Bisection, and many other methods that can be seen in [36]. In fact, we use here the Newton–Raphson iterative method (NR) to solve the equation in (17) as we already tried with many different methods, but the results of NR method are more accurate and method converges to the solutions faster than the methods with fewer iterations. The following steps show how we use NR method. First, let
Next, we can create a sequence of initial solutions by using the following formula:
where we select . In fact, the tolerance here is and by repeating the iterations we can keep creating the solutions until we satisfy the condition below:
Moreover, we can use another method such as the fixed-point method (FP), where can write the previous mentioned equation as below:
Then, with , one may use the formula below:
One may also use here the tolerance and by repeating the iterations we can keep creating the solutions until we satisfy the condition below:
4. Nonlinear Energy Stability Theory
4.1. Nonlinear Stability Analysis with Forchheimer Coefficient
Before developing the nonlinear energy stability analysis, we can start by taking the third component of Equation (6)1 in the system (6), which will lead to
substituting (22)1 into (22)2, we obtain
Let us suppose that V represents the period cell, represents the norm on , and represents the inner product on . Niow, multiplying (23) by w, (6) by , (6) by and (6)5 by and integrating over V, yield
If , then with substituting as the constant in poincarés inequality, we can see that
where , from integrating (26) with , we have
From Equation (6)1 (), with substituting as the constant in the poincarés inequality, one could show that
by using Youngs inequality, we obtain
hence,
Therefore, also ensures the exponential decay One can show that is equivalent to , where is the value of R for which . This value of is the nonlinear stability threshold.
To solve the maximum problem (27), we study the Euler Lagrange equations which can be found from
Thus, the equations of Euler Lagrange appear from variational problem (28), are
Now, eliminating the Lagrange multiplier , and representing the normal mode and notation as described in Section 3, system (29), yields
Now, one may evaluate the critical Rayleigh number (CRN) by using the following
4.2. Nonlinear Stability Analysis with Taylor-Darcy Number
Multiply, (6)1 by , (6)3 by , (6)4 by and (6)5 by and integrating over V, we obtain
where denotes the . Let us assume now that both of and are positive parameters. Therefore, by multiplying (31)1 by , (31)4 by and adding these two equations with (31)2 and (31)3, we obtain
where and are given by
With some mathematical simplifications, we obtain
where
such that is the space of admissible functions.
In fact, if then substituting as the constant in poincarés inequality, one can obtain
where . Now integrating (33) with , yields
Then, the decay of is clearly obtained.
Since the global stability has been already established, we can study the maximum problem (34) keeping in mind its condition as . In fact, we could solve this maximization problem by studying the equations of Euler Lagrange which can be obtained from the following
Now, by using the above equation and the values of both and , one can obtain the following equations
The above equations in (35) are called the Euler Lagrange equations, where represents the Lagrange multiplier. Now, by taking the third component in (35)1, one can remove the Lagrange multiplier. Thus, we obtain
Introducing the normal mode representations, then, system (36) becomes
Now, one my evaluate the critical Rayleigh number (CRN) by using the following
5. Discussion of Results
For the validation of the proposed work, we present in this section some experimental examples and focus on the numerical solutions of the instability of the linear case and the stability of the nonlinear case. The numerical solutions of the systems in (11) (the linear instability), with respect to the stationary and oscillatory convection cases. The results are reported when and . Furthermore, we discuss the different values of and in Figure 2, Figure 3, Figure 4 and Figure 5. Chebyshev collocation method has been used for solving the systems of eigenproblems (11), (30) and (37). More information about these types of systems can be seen in [21,22,23,24,37,38,39]. The solutions are then presented in Table 1, Table 2 and Table 3, which comprise and which are called the critical thermal Rayleigh numbers (CTRN) for both of the linear instability theory and the non-linear stability theory, respectively. In fact, these values have been evaluated from (11), (30) and (37) in order to compute the various values of and , respectively, with . We can see in the results that the values of and B are increasing in the stability case, while the stability curve fall away from the instability curve for the large values of . However, in Table 2 and Table 3, the values of which have been evaluated from (30) for the nonlinear stability theory are oscillating with different values of and ; thus, from Table 1, we can see that the linear instability theory is more accurate than the nonlinear stability theory. Consequently, we can observe that these effects in the physical sense are overlapping in somehow in a competition with each other. In addition, we can see that the CTRN values do not change and stay the same in the two cases (the linear and nonlinear cases) without any critical unstable senses.
Figure 2.
(the number of Rayleigh) versus with respect to the values of .
Figure 3.
(the number of Rayleigh) versus with respect to the values of M.
Figure 4.
(the number of Rayleigh) versus with respect to the values of B.
Figure 5.
(the number of Rayleigh) versus with respect to the values of .
Table 1.
Critical thermal Rayleigh number against and , with .
Table 2.
Critical thermal Rayleigh number against and , with .
Table 3.
Critical thermal Rayleigh number against and , with .
6. Conclusions and Future Direction
The stability of a double diffusive convection problem using the local thermal non-equilibrium (LTNE) effects has been considered in this recent work. In addition, a new model has been used along with a new approach by using two numerical methods to analyze the linear and non-linear stability of the mentioned problem. From the results of the critical thermal Rayleigh numbers (CTRN), we were able to compute the various values of and , respectively, with that we used to analyze the linear and non-linear stability. For future work, one might use different models than Brinkmann-Forchheimer and a different numerical method than the one we used to solve the equation in (17).
Author Contributions
Formal analysis, G.A.M., O.B. and K.S.A.-G.; Data curation, G.A.M., J.A. and O.B.; Funding acquisition, J.A.; Methodology, G.A.M.; Project administration, J.A.; Resources, A.H.A. and O.B.; Software, A.H.A.; Supervision, J.A. and O.B.; Validation, K.S.A.-G. and O.B.; Visualization, A.H.A.; Writing—review and editing, A.H.A. and K.S.A.-G. All authors read and agreed to the published version of the manuscript.
Funding
This research received no external funding.
Institutional Review Board Statement
Not applicable.
Informed Consent Statement
Not applicable.
Data Availability Statement
Not applicable.
Conflicts of Interest
The authors declare no conflict of interest.
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