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Article

Unsteady Magnetohydrodynamic Convective Fluid Flow of Oldroyd-B Model Considering Ramped Wall Temperature and Ramped Wall Velocity

1
Department of Mathematics, Government Postgraduate Gordon College, Rawalpindi 46000, Pakistan
2
Department of Mathematical Sciences, Federal Urdu University of Arts, Science & Technology, Near Zero Point, G-7/1, Islamabad 44000, Pakistan
3
Department of General Studies, Jubail Industrial College, Al Jubail 35718, Saudi Arabia
4
Department of Mathematics & Statistics, International Islamic University, Islamabad 44000, Pakistan
5
Department of Mathematics, COMSATS University Islamabad, Park Road Chak Shahzad, Islamabad 44000, Pakistan
*
Author to whom correspondence should be addressed.
Mathematics 2019, 7(8), 676; https://doi.org/10.3390/math7080676
Submission received: 18 June 2019 / Revised: 16 July 2019 / Accepted: 20 July 2019 / Published: 29 July 2019

Abstract

:
This paper examines unsteady magnetohydrodynamic (MHD) convective fluid flow described by the Oldroyd-B model using ramped wall temperature and velocity simultaneously. The fluid flow is closed to an infinite vertical flat plate immersed through a porous medium. Laplace transformation is used to find solutions of momentum and energy equations. Afterwards, the Nusselt number and skin friction coefficient are obtained. A parametric study is performed to investigate the effects of ramped velocity and temperature (at wall) on the considered fluid flow model.
MSC:
76D03; 76S05; 76W05; 76M25

1. Introduction

Non-Newtonian fluids gained a wide deal of attention due to their practical utility in modern technologies. Examples of non-Newtonian fluids are blood, paints, oils, greases and polymer solutions and so forth [1,2,3]. Mixed convective flows of non-Newtonian fluids under the action of magnetohydrodynamic (MHD) force, are of great importance in MHD pumps and power generators, accelerators, energy generators, aerodynamic heating, polymer fabrication and purification of mineral oil and so forth. Convective flows through a porous medium play an imperative role in locating gas and oil reservoirs in the earth [4]. In agriculture, convective flows are used to locate the sub-ground water reservoirs [5]. In metallurgy, the flow of liquid metal under the strong magnetic field in a porous medium takes place during a solidification process [6].
The above mentioned practical applications are the main motivations behind this work. Many complex fluids exhibit a combination of elastic and viscous behavior for example, polymer solutions and melts, oil, toothpaste and clay. The Oldroyd-B model is one of the simplest models that includes the history of the flow and capable of describing viscoelastic fluids. In this study, we investigated the MHD convective fluid flow of the Oldroyd-B model subject to ramped velocity and ramped temperature (at wall), through a porous medium. The literature reveals that the simultaneous implementation of above mentioned conditions, ramped velocity and ramped temperature (at wall), have attracted a little attention of the researchers examining such flows. The simultaneous use of ramped wall temperature and velocity conditions are physically important, but mathematically difficult to handle. Ergometers or treadmill testing (TT) is an application of ramped velocity which is currently applied to diagnose cardiovascular diseases. Furthermore, there are many applications of Ramped velocity in making diagnoses, determining prognosis, establishing treatments and examining the functioning of heart and blood vessels system [7]. Bruce [8], Astrand and Rodahl [9] and Myers and Bellin [10] are contributed on TT.
Hayday [11], Schetz [12] and Malhotra et al. [13] presented their work on ramped wall temperature conditions. An efficient and effective way to estimate the increase in temperature due to adiabatic conditions can be controlled with the help of ramped heating. Another important application of controlled temperature boundary conditions (BCs) is reported by Kundu [14]. Kundu [14] affirmed that the thermal therapy is helpful in treating cancerous cells as the therapy has insignificant side effects. Kundu [14] further suggested five types of temperature BCs for better treatment of cancerous cells depending upon Fourier and non-Fourier heating. Seth et al. presented their work on the heat and mass transfer considering ramped temperature (at wall) with the impulsive and moving vertical plate [15,16,17,18,19]. Recently, Chandran et al. [20] used the ramped wall temperature condition with convective viscous fluid flow. Some researches taking into account the ramped temperature conditions can be found in the recent literature [21,22,23,24,25,26].
The conditions of ramped velocity and temperature at wall have significant importance in human health and in many daily life related procedures. The Oldroyd-B fluid model considers the memory effects and elasticity and memory effects. The model also retains rheological effects even for unidirectional flows. The Oldroyd B model gives good approximations of viscoelastic fluids in shear flow and has an unphysical singularity in extensional flow. The model contains Maxwell and viscous fluid as its special cases. If the solvent viscosity is zero, the Oldroyd-B becomes the Upper Convected Maxwell model. Therefore Oldroyd-B model can be regarded as an extension of the Upper Convected Maxwell model which is named after its creator James G. Oldroyd. The focus of the present work is to use the velocity and temperature conditions on ramped wall simultaneously for the convective flow of Oldroyd-B fluid model. Laplace transformation is implemented to solve the Oldroyd-B fluid model subject to ramped velocity and temperature at wall.
The remaining article is presented in five sections: Section 2 comprises model formulation, Section 3 contains analytical solution of the considered model problem, Section 4 comprises the limiting cases, Section 5 presents the numerical results and conclusion is discussed in Section 6.

2. Model Formulation

The unsteady, incompressible and MHD flow of Oldroyd-B fluid over an infinite vertical plate under the Boussinesq’s approximations can be described by the subsequent equations [27,28]. The Boussinesq’s approximations is used to find the buoyancy force [29].
· V = 0 ,
ρ V t + V . V = J × B + div T + r + ρ g β T T ,
where
T = p I + S ,
and S satisfies the following relation:
1 + λ D D t S = μ 1 + λ r D D t A 1 ,
where V accounts for the unidirectional and unidimensional velocity profile as given below:
V = u y , t , 0 , 0 ,
D D t · is defined as follows:
D S D t = S t + u S x + v S y + w S z ,
p I refers to the indeterminate stress tensor, T denotes the Cauchy stress tensor of Oldroyd-B fluid, S is the extra stress tensor, ρ represents the fluid density, μ is defined as the fluid viscosity, D D t is the material time derivative. Moreover, λ , λ r and r represent the relaxation and retardation times and Darcy’s resistance, respectively. The Rivlin-Ericksen tensor A 1 is as follows:
A 1 = V + V T = 0 u y u y 0 .
The modified version of Darcy’s law for the Oldroyd-B fluid flow is given below:
( 1 + λ t ) r = μ ϕ k 1 + λ r t V .
The Maxwell’s equations are defined as below:
curl E = B t , curl B = μ m J , div B = 0 ,
and
J × B = σ B 0 2 u , 0 , 0
where E , B , J , and μ m represent electric field, total magnetic field, current density and magnetic permeability, respectively.
The aggregate magnetic field is B = b 0 + B 0 . Here, b 0 and B 0 represent the induced magnetic field and the applied magnetic field, respectively. In the light of Equations (3)–(8), Equation (2) takes the following form:
ρ u t = S x y y + J × B x + r x + ρ g β T T .
Multiplying Equation (11) by ( 1 + λ t ) and using Equations (8)–(10) we get the form as given below:
ρ ( 1 + λ t ) u t = 1 + λ t S x y y σ B 0 2 1 + λ t u μ ϕ k 1 + λ t u + ρ g β 1 + λ t T T .
Using Equations (4)–(7) in Equation (11), we get the following form of Equation (12)
( 1 + λ t ) u t = μ ρ 1 + λ r t 2 u y 2 σ B 0 2 ρ 1 + λ t u + ρ g β 1 + λ t T T μ ϕ k 1 + λ r t u .
Geometry of the considered flow model is presented in Figure 1.
Using small magnetic Reynolds number and Boussinesq’s approximation, the equation of motion and the energy equation for Oldroyd-B fluid are as under:
1 + λ t u t = ν 1 + λ r t 2 u y 2 σ B 0 2 ρ 1 + λ t u μ ϕ ρ k 1 + λ r t u + g β ( T T ) ,
ρ C p T t = κ 2 T y 2 ,
with initial conditions (ICs) as given below:
u y , 0 = 0 , T y , 0 = 0 , u t y , 0 = 0 , u y y , 0 = 0 , for y 0
and corresponding (BCs) as follows:
u 0 , t = U 0 t t 0 0 < t t 0 U 0 t t 0 ,
T 0 , t = T + T W T t t 0 0 < t t 0 T W t t 0 ,
and
u y , t 0 , and T y , t T W , when y for t > 0
Dimensionless quantities are defined as:
u = u U 0 , y = y U 0 ν , t = t U 0 2 ν , t 0 = ν U 0 2 , θ = T T T W T , Pr = μ C p κ , Gr = ν g β T W T U 0 3 , λ 1 = λ t 0 , λ 2 = λ r t 0 , M = σ B 0 2 t 0 ρ , 1 K = ϕ t 0 k ,
After applying Equation (20) in Equations (14)–(19), the obtained coupled PDEs system is presented as follows:
a u t + λ 1 2 u t 2 = 1 + λ 2 t 2 u y 2 b u + Gr θ ,
where
a = 1 + M λ 1 + λ 2 K and b = M + 1 K ,
and the energy equation:
Pr θ t = 2 θ y 2 ,
where Pr and Gr are the Prandtl’s and Grashof’s numbers respectively. The corresponding ICs and BCs can be rewritten as:
θ y , 0 = 0 , u y , 0 = 0 , u t y , 0 = 0 , u y y , 0 = 0 , for y 0 ,
θ 0 , t = u 0 , t = t 0 < t 1 1 t > 1 ,
and
u y , t and θ y , t 0 , when y for t > 0 .

3. Analytical Solution of the Problem

Laplace and Inverse Laplace Transforms

We use the Laplace transform tool [30] to tackle the problem because the other analytical method like Homotopy analysis method, perturbation techniques, Adomian decomposition, and method of separation of variables and so forth, do not work because of non-uniform boundary conditions. In order to solve the problem specified through Equations (21)–(26), we define the Laplace transform pair of an almost piecewise continuous function F ( t ) (of exponential order), as an integral of the form:
L F t = 0 F t e s t d t = F ¯ s ,
which is convergent for R e ( s ) > α 0 , where s = ψ + j χ , j = 1 and α 0 is some real number. The inverse Laplace transform of F ¯ s can be evaluated as:
L 1 F ¯ s = 1 2 π j B R F ¯ s e s t d s ,
where B R denotes the Bromwich type contour integral over the contour s = ψ j R to s = ψ + j R , while R approaches ∞ and also the Gaver-Stehfest method is required when there are multivalued functions involved (as in the velocity u ¯ y , s ) as:
F t = lim N 1 t i = 1 L i F α i t ,
where L i and α i are the constants to be determined [31,32,33]. Now using definitions given in Equations (27)–(29), we define Laplace and inverse Laplace transforms of θ y , t and u y , t as:
L θ y , · t = 0 θ y , t e s t d t = θ ¯ y , s ,
L 1 θ ¯ y , · s = 1 2 π i γ i γ + i θ ¯ y , s e s t d s = θ y , t .
The solution of model Equation (23) in the transformed domain s after implementing ICs and BCs, we get the following result:
θ ¯ y , s = 1 exp s s 2 exp Pr s y = G ¯ y , s exp s G ¯ y , s ,
Afterwards, implementing inverse Laplace transform with the help of Equation (28), results in the form of subsequent equation:
θ y , t = G y , t G y , t 1 F t 1 ,
with
G y , t = L 1 exp Pr s y s 2 = t + y 2 Pr 2 erf c y Pr 2 t y Pr t π e y 2 Pr 4 t ,
where Heaviside function is denoted by F.
Applying Laplace transform technique on Equation (21), we obtain the results as follows:
1 + λ 2 s d 2 u ¯ d y 2 b u ¯ + Gr θ ¯ = a s + s 2 λ 1 u ¯ ,
or
d 2 u ¯ d y 2 = a s + s 2 λ 1 + b 1 + λ 2 s u ¯ Gr 1 + λ 2 s θ ¯ .
Now, putting the value of θ ¯ y , s (c.f. Equation (32)) into Equation (36) leads us to the subsequent equation:
d 2 u ¯ y , s d y 2 c u ¯ = Gr 1 e s s 2 e Pr s y 1 + λ 2 s ,
where
c = b + a s + s 2 λ 1 1 + λ 2 s .
The solution of Equation (37), is calculated as below:
u ¯ y , s = 1 e s s 2 H ¯ y , s = H ¯ y , s s 2 e s H ¯ y , s s 2 ,
where
H ¯ y , s = e b + a s + s 2 λ 1 1 + λ 2 s y + Gr e b + a s + s 2 λ 1 1 + λ 2 s y λ 2 Pr λ 1 s m 1 2 m 2 2 Gr e Pr s y λ 2 Pr λ 1 s m 1 2 m 2 2 ,
and
m 1 = a Pr 2 λ 2 Pr λ 1 and m 2 = 1 2 a Pr λ 2 Pr λ 1 2 b λ 2 Pr λ 1 .
As the velocity field contains the multivalued functions in terms of constants m 1 and m 2 , therefore we apply the Gaver-Stehfest method described in [31,32,33] to evaluate the inverse Laplace transform of u ¯ y , s which results in a series solution of the form:
u t , n = ln 2 t k = 1 n V k u ¯ k ln 2 t .
The shear stress on the wall τ w and local Nusselt number N u is derived and presented as follows:
τ w = μ 1 + λ 1 t 1 + λ 2 t u y y = 0 ,
N u = θ / y at y = 0 ,
where
u y y = 0 = H y , t y y = 0 + H y , t 1 F t 1 y y = 0 ,
and N u is given below:
N u = 2 Pr π t t 1 F t 1 .
In this study, one dimensional unsteady flow problem was taken into account for which the advection term becomes zero. The advection term can be considered in the two dimensional problem, which makes the problem nonlinear and the Laplace method cannot be applied.

4. Limiting Models

This section contains two limiting cases:

4.1. Case 1

The velocity and temperature profiles of Oldroyd-B fluid for constant wall velocity and constant wall temperature (isothermal) are as follows:
θ y , t = erf c y Pr 2 t ,
u ( y , t ) = L 1 { u ¯ y , s } = L 1 1 exp s s H ¯ y , s ,
where
H ¯ y , s = e b + a s + s 2 λ 1 1 + λ 2 s y + Gr e b + a s + s 2 λ 1 1 + λ 2 s y λ 2 Pr λ 1 s m 1 2 m 2 2 Gr e Pr s y λ 2 Pr λ 1 s m 1 2 m 2 2 .

4.2. Case 2

The results of Maxwell model can be deduced when λ 2 0 and the viscous fluid flow with ramped wall temperature can be obtained when λ 1 , λ 2 0 [34,35].

5. Results and Discussion

The present section comprises of solution profiles considering different parameter values, such as, Prandtl number (Pr), Grashof number (Gr), magnetic parameter (M), porosity (K), relaxation time ( λ 1 ) , and dimensionless time (t). The numerical results are divided into two main categories: (1) Oldroyd-B fluid model with ramped wall temperature and ramped wall velocity and (2) Oldroyd-B fluid model with constant temperature at wall and ramped wall velocity. In the numerical results, the solid line is used for Oldroyd-B model considering ramped temperature profiles and velocity conditions, while the dashed lines are used for Oldroyd-B model with constant temperature and ramped velocity conditions. Figure 2, Figure 3, Figure 4, Figure 5, Figure 6, Figure 7, Figure 8, Figure 9 and Figure 10 are produced by using the software “Wolfram Mathematica 9.0” (Wolfram Research, Champaign, IL, USA).
The impact of time λ 1 on velocity distribution is shown in Figure 2. It is found that by increasing relaxation time λ 1 , velocity profile decreases as relaxation time causes the thickness of momentum boundary layer. Moreover, the velocity becomes slower for non-isothermal plate than the isothermal one.
The effect of M on the velocity for isothermal plate and ramped temperature is illustrated in Figure 3. Figure 3 depicts that the velocity reduces as the value of M increases because of the Lorentz force which occurs due to imposed magnetic field on an electrically conducting fluid. Consequently, a drag force is produced and fluid motion is retarded and Lorentz force along with other forces becomes weaker therefore the fluid gradually calmed.
The variation in K is shown in Figure 4. The change in parameter K brings acceleration in the velocity field for both the conditions, ramped temperature and isothermal one. It is found that the drag force reduces when permeability of mushy (porous) medium increases, thus, velocity is accelerated in both cases. Moreover, the velocity is higher for the isothermal case as compared to ramped temperature condition.
The effects of Gr for both thermal and isothermal conditions are illustrated in Figure 5. Physically, Gr accounts for the weight of thermal buoyancy force to viscous force. The buoyancy forces increase near the plate and decrease far from the plate with an increase in Gr. Thus, the buoyancy forces with allied forces get weaker and fluid, far from the plate, on free stream surface achieves zero velocity.
Figure 6 shows the results of retardation time on the velocity for both thermal and isothermal conditions. It is found that the flow is accelerated due to the retardation time for both cases. Figure 6 illustrate that the velocity is increased when time is increased for both the cases.
Figure 7 presents the effects of time t (dimensionless) considering both isothermal conditions and ramped temperature on the solution u ( y , t ) .
Figure 8 shows the relationship between shear stress on the wall τ w and Gr under the influence of relaxation time λ 1 . The increase in λ 1 brings decrease in magnitude of the τ w . Internal friction is significantly decreased owing to small viscosity. Figure 9 illustrates that retardation time causes the shear stress on the wall to increase. Figure 10 shows the effects of Prandtl numbers Pr on the temperature profile. It is observed that the temperature profile decreases as Pr increases because the moving fluid gets less heat transfer from the solid plate as Pr increases from 0.7 to 7.

6. Conclusions

The MHD convective fluid flow of Oldroyd-B model is solved analytically subject to ramped velocity and temperature (at wall) simultaneously. The results of the considered model subject to ramped temperature are compared with the isothermal model in a porous medium. It is worthwhile mentioning that the simultaneous use of both the conditions (ramped velocity and ramped temperature), which was the main focus of this study, is limited in the literature though both the conditions are physically important. The solution of the Oldroyd-B fluid model, considering ramped velocity and ramped temperature at the same time, is mathematically difficult. We used Laplace transformation and the Gaver-Stehfest method to solve the model problem. The parametric study is performed and presented graphically and discussed.
Important findings are as follows:
  • An increase in the magnetic parameter (M) on velocity causes decrease in the thickness of the momentum boundary layer.
    Momentum boundary layer increases as parameters values such as, λ 1 , λ 2 , K, Gr and t < 1 increase.
  • An increase in relaxation time λ 1 results in a decrease in velocity (related to skin friction) on the plate.
  • Rate of heat transfer (related to Nusselt numbers Nu) increases when thermal diffusivity related to Pr number increases. For lower Prandtl numbers Pr, the fluid has higher thermal conductivity whereas higher Pr numbers cause resistance in the transfer of heat into the fluid (see [36,37,38]).

Author Contributions

Conceptualization, M.H.T., A.B.M. and K.M.; methodology, M.H.T., A.B.M., K.M. and S.J.; software, K.M. and S.J; validation, M.R., K.M.; formal analysis, A.B.M. and K.M.; resources, M.R., S.R. and M.S.K.; writing—original draft preparation, K.M., S.J.; writing—review and editing, M.R., S.J., S.R. and M.S.K.; project administration, S.J.

Funding

This research received no external funding.

Conflicts of Interest

The authors declare no conflict of interest.

Nomenclature

BTotal magnetic field
JCurrent density
EElectric field
TCauchy Stress Tensor
rDarcy resistance vector
SExtra Stress tensor
A1Rivlin-Erickson tensor
u , v , w Velocity components
x , y , z Space variables
TTemperature
pPressure
gAcceleration due to gravity
ρ Fluid density
μ m Magnetic permeability
σ Electrical conductivity of the fluid
ϕ Porosity parameter
μ Viscosity of the fluid
λ , λ r Relaxation, retardation times
u Non-dimensional velocity
t Non-dimensional time
T Non-dimensional temperature
MHartmann Number
KNon-dimensional porosity parameter
λ 1 , λ 2 Non-dimensional relaxation & retardation times
GrGrashof’s number
PrPrandtl’s Number
L Laplace transform operator
sLaplace transform parameter

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Figure 1. Geometry of the considered flow model.
Figure 1. Geometry of the considered flow model.
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Figure 2. Influence of relaxation time λ 1 on velocity profile u.
Figure 2. Influence of relaxation time λ 1 on velocity profile u.
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Figure 3. Influence of magnetic parameter M on velocity profile u.
Figure 3. Influence of magnetic parameter M on velocity profile u.
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Figure 4. Influence of porosity K on velocity u.
Figure 4. Influence of porosity K on velocity u.
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Figure 5. Influence of Grashof number Gr on velocity u.
Figure 5. Influence of Grashof number Gr on velocity u.
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Figure 6. Influence of retardation time λ 2 on velocity u.
Figure 6. Influence of retardation time λ 2 on velocity u.
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Figure 7. Influence of time t on velocity u.
Figure 7. Influence of time t on velocity u.
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Figure 8. The graphs of shear stress on the wall Gr for different values of the λ 1 .
Figure 8. The graphs of shear stress on the wall Gr for different values of the λ 1 .
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Figure 9. The graphs of shear stress on the wall Gr for various values of the λ 2 .
Figure 9. The graphs of shear stress on the wall Gr for various values of the λ 2 .
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Figure 10. Influence of Pr on temperature profile.
Figure 10. Influence of Pr on temperature profile.
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Tiwana, M.H.; Mann, A.B.; Rizwan, M.; Maqbool, K.; Javeed, S.; Raza, S.; Khan, M.S. Unsteady Magnetohydrodynamic Convective Fluid Flow of Oldroyd-B Model Considering Ramped Wall Temperature and Ramped Wall Velocity. Mathematics 2019, 7, 676. https://doi.org/10.3390/math7080676

AMA Style

Tiwana MH, Mann AB, Rizwan M, Maqbool K, Javeed S, Raza S, Khan MS. Unsteady Magnetohydrodynamic Convective Fluid Flow of Oldroyd-B Model Considering Ramped Wall Temperature and Ramped Wall Velocity. Mathematics. 2019; 7(8):676. https://doi.org/10.3390/math7080676

Chicago/Turabian Style

Tiwana, Mazhar Hussain, Amer Bilal Mann, Muhammad Rizwan, Khadija Maqbool, Shumaila Javeed, Saqlain Raza, and Mansoor Shaukat Khan. 2019. "Unsteady Magnetohydrodynamic Convective Fluid Flow of Oldroyd-B Model Considering Ramped Wall Temperature and Ramped Wall Velocity" Mathematics 7, no. 8: 676. https://doi.org/10.3390/math7080676

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