Skip to main content
PLOS ONE logoLink to PLOS ONE
. 2014 Jun 20;9(6):e97552. doi: 10.1371/journal.pone.0097552

Thin Film Flow in MHD Third Grade Fluid on a Vertical Belt with Temperature Dependent Viscosity

Taza Gul 1, Saed Islam 1, Rehan Ali Shah 2, Ilyas Khan 4, Sharidan Shafie 3,*
Editor: Victor M Ugaz5
PMCID: PMC4064968  PMID: 24949988

Abstract

In this work, we have carried out the influence of temperature dependent viscosity on thin film flow of a magnetohydrodynamic (MHD) third grade fluid past a vertical belt. The governing coupled non-linear differential equations with appropriate boundary conditions are solved analytically by using Adomian Decomposition Method (ADM). In order to make comparison, the governing problem has also been solved by using Optimal Homotopy Asymptotic Method (OHAM). The physical characteristics of the problem have been well discussed in graphs for several parameter of interest.

Introduction

The subject of non-Newtonian fluids is popular and is an area of active research specially in mathematics, industry and engineering problems. Examples of non-Newtonian fluids include plastic manufacturing, performance of lubricants, food processing, movement of biological fluids, wire and fiber coating, paper production, transpiration cooling, gaseous diffusion, drilling mud, heat pipes etc. These fluids are described by a non-linear relationship between stress and the rate of deformation tensors and therefore several models have been proposed. There are several subclasses of non-Newtonian fluids. Third grade fluid is one of the important fluid in this category and its equation is based on strong theoretical foundations, where relation between stress and strain is not linear. Therefore, in this problem, we have considered third grade fluid. Considerable efforts have been made to study non-Newtonian fluids for various geometrical configurations via analytical techniques. Some developments in this direction are discussed in [1][19]. On the other hand, the physical importance of thin film has been highlighted by scientists and engineers. Amongst them, Khalid and Vafai [20] studied hydrodynomic squeezed flow and heat transfer over a sensor surface. Miladinova et al. [21] investigated thin film flow of a power law liquid falling from an inclined plate where it was observed that saturation of non-linear interaction occur in a permanent finite amplitude wave.

Similarly, Taza Gul et al. [22] investigated effects of slip condition on thin film flow of third grade fluids for lifting and drainage problem under the condition of constant viscosity. The effects of various parameters on the lift and drainage velocity profiles are also studied.

It is crystal clear that the physical problems are frequently modeled, using non-linear differential equations. Recently, several analytical and numerical techniques were used for solution of such non-linear problems. In order to find analytical approximate solutions of non-linear differential equations, researchers usually use approximate techniques such as Homotopy Perturbation Method (HPM) [23], Homotopy Analysis Method (HAM) [24] and Optimal Homotopy Asymptotic Method (OHAM) [25]. OHAM is a powerful mathematical technique and has already been applied to several non-linear problems. Marinca and Herisanu [26] used OHAM for solving non-linear equations arising in heat transfer problems. In another paper, Marinca [27] applied OHAM to study steady flow of a fourth grade fluid past a porous plate. Joneidi et al. [28] analyzed micropolar flow in a porous channel with high mass transfer. Siddiqui et al. [29] examined a thin film flow of non-Newtonian fluid over a moving belt. In another study, Siddiqui et al. [30] discussed the thin film flow of a fourth grade fluid down a vertical cylinder. Costa and Macedonio [31] noticed that increase in velocity may produce additional growth of local temperature. Nadeem and Awais [32] investigated thin film unsteady flow with variable viscosity. They analyzed the effect of variable thermo capillarity on the flow and heat transfer. Ellahi and Riaz [33] discussed analytical solution for MHD flow in a third grade fluid with variable viscosity. Whereas Aksoy et al. [34] found an approximate analytical solution for flow of a third grade fluid through a parallel plate channel filled with a porous medium.

The main objective of this research is to study thin film flow of MHD third grade fluid over a vertical belt under the influence of temperature with variable viscosity. More exactly, we are interested in showing the effects of MHD and variable viscosity with heat transfer in a thin film fluid flow such as silicate melts and polymers. In these fluids, viscous friction generates a local increase in temperature near the belt with decrease in resultant viscosity and frequently increases the flow velocity. The governing problem is solved using an analytical technique known as Adomian Decomposition Method (ADM). This technique was introduced by Adomian [35], [36] for finding the approximate solutions for linear and non-linear differential equations. Wazwaz [37], [38] used ADM for reliable treatment of Bratu-type and Rmden-Fowler equations. For comparisons and accuracy of results, the governing problem has also been solved by using OHAM.

Basic Equations

The continuity, momentum and energy equations for incompressible, isothermal and electrically conducting third grade fluid are;

graphic file with name pone.0097552.e006.jpg (1)
graphic file with name pone.0097552.e007.jpg (2)
graphic file with name pone.0097552.e008.jpg (3)

Here, Inline graphic is the constant density, Inline graphic denotes gravitational acceleration, Inline graphic is the velocity vector of the fluid, Inline graphic defines temperature, Inline graphic is the thermal conductivity, Inline graphic is specific heat, Inline graphic Inline graphic denotes material time derivative, Inline graphic is the current density and Inline graphic is the Cauchy stress tensor. Moreover, a uniform magnetic field Inline graphic is applied in a direction, perpendicular to the belt. The Lorentz force per unit volume is given by

graphic file with name pone.0097552.e020.jpg (4)

The Cauchy stress tensor Inline graphic is given by

graphic file with name pone.0097552.e027.jpg (5)

where Inline graphic denotes spherical stress, Inline graphic is the hydrostatic pressure and shear stress tensor Inline graphic, is defined as

graphic file with name pone.0097552.e031.jpg (6)

Here Inline graphic ,Inline graphic are the material constants and A 0, A 1, A 2, A 3 are the kinematical tensors given by

graphic file with name pone.0097552.e034.jpg (7)

Formulation of Lift Problem

Consider, a wide flat belt moves vertically upward at a constant speed U through a large bath of third grade liquid. The belt carries a layer of liquid of constant thickness, δ with itself. For analysis, coordinate system is chosen in which the y-axis is taken parallel to the surface of the belt and x-axis is perpendicular to the belt. Uniform magnetic field is applied transversely to the belt. It is assumed that the flow is steady and laminar after a small distance above the liquid surface layer and the external pressure is atmospheric everywhere.

Velocity and temperature fields are

graphic file with name pone.0097552.e038.jpg (8)

Using the velocity field given in Eq. (8) the continuity Eq. (1) satisfies identically and Eq. (5) gives the following components of stress tensor:

graphic file with name pone.0097552.e039.jpg (9)
graphic file with name pone.0097552.e040.jpg (10)
graphic file with name pone.0097552.e041.jpg (11)
graphic file with name pone.0097552.e042.jpg (12)
graphic file with name pone.0097552.e043.jpg (13)

Incorporating Eqs. (9–13) into the momentum and energy equations (2, 3), we get

graphic file with name pone.0097552.e049.jpg (14)
graphic file with name pone.0097552.e050.jpg (15)

The corresponding boundary conditions are:

graphic file with name pone.0097552.e051.jpg (16)
graphic file with name pone.0097552.e052.jpg (17)

Introducing the following non-dimensional variables

graphic file with name pone.0097552.e053.jpg (18)

where Br is the Brinkman number , M 2 is the magnetic parameter, Inline graphic is the non-Newtonian parameter and St is the Stock’s number.

For Reynold’s model, the dimensionless viscosity

graphic file with name pone.0097552.e055.jpg (19)

Using Taylor series expansion, one may represent viscosity and its derivative as follows:

graphic file with name pone.0097552.e056.jpg (20)

Using the above dimensionless variables into Eqs. (14–17) and dropping out the bar notations, we obtain.

Eq. (14) has been rectified for Eq. (21, 22)

graphic file with name pone.0097552.e057.jpg (21)
graphic file with name pone.0097552.e058.jpg (22)
graphic file with name pone.0097552.e059.jpg (23)
graphic file with name pone.0097552.e060.jpg (24)

Solution of Lifting Problem

The OHAM solution

In order to solve the system of equations (2124), we define the linear, non-linear functions and source terms respectively as follows:

graphic file with name pone.0097552.e061.jpg (25)
graphic file with name pone.0097552.e062.jpg (26)

Now, OHAM is applied to non-linear coupled ordinary differential Eqs. (21, 22) and Eqs. (25, 26) as follows:

graphic file with name pone.0097552.e063.jpg
graphic file with name pone.0097552.e064.jpg (27)

We consider Inline graphic as the following.

graphic file with name pone.0097552.e066.jpg
graphic file with name pone.0097552.e067.jpg (28)

Substituting Inline graphic from Eq. (28) into Eq. (27) and after some simplifications based on power of p-terms, we get the following.

Zero components:

graphic file with name pone.0097552.e069.jpg (29)

First components:

graphic file with name pone.0097552.e070.jpg (30)

Solving Eqs. (29, 30) along with boundary conditions (23, 24), we get the term solutions as fallows.

Zero term solution:

graphic file with name pone.0097552.e071.jpg (31)

First term solution:

graphic file with name pone.0097552.e072.jpg (32)

The second term solution for velocity and temperature are too bulky, therefore, only graphical representations up to second order are given.

The series solutions of velocity profile and temperature distribution are

graphic file with name pone.0097552.e073.jpg (33)

The arbitrary constants Inline graphic are found out by using the residual

graphic file with name pone.0097552.e075.jpg (34)

For velocity profile and temperature distribution the arbitrary constants are mentioned in graphs.

The constants Inline graphic can also be obtained from Collocation and Ritz methods.

The ADM solution

The inverse operator Inline graphic of the ADM on the second order coupled Eqs. (21,22) is used:

graphic file with name pone.0097552.e078.jpg (35)
graphic file with name pone.0097552.e079.jpg (36)

The series solutions of Eqs. (35, 36):

graphic file with name pone.0097552.e080.jpg (37)
graphic file with name pone.0097552.e081.jpg (38)

The Adomian polynomials Inline graphic and Inline graphic for Eqs. (37, 38) are defined as

graphic file with name pone.0097552.e084.jpg (39)
graphic file with name pone.0097552.e085.jpg (40)
graphic file with name pone.0097552.e086.jpg (41)
graphic file with name pone.0097552.e087.jpg (42)
graphic file with name pone.0097552.e088.jpg (43)
graphic file with name pone.0097552.e089.jpg (44)

The components of Adomian polynomials are derived from Eqs. (39–44) as:

graphic file with name pone.0097552.e090.jpg (45)
graphic file with name pone.0097552.e091.jpg (46)

The series solutions of Eqs. (37, 38) are derived as:

graphic file with name pone.0097552.e092.jpg (47)
graphic file with name pone.0097552.e093.jpg (48)

The velocity and temperature components are obtained by comparing both sides of Eqs. (47, 48):

Components of the lift problem up to second order are:

graphic file with name pone.0097552.e094.jpg (49)
graphic file with name pone.0097552.e095.jpg (50)
graphic file with name pone.0097552.e096.jpg (51)
graphic file with name pone.0097552.e097.jpg (52)
graphic file with name pone.0097552.e098.jpg (53)
graphic file with name pone.0097552.e099.jpg (54)

subject to the boundary conditions

graphic file with name pone.0097552.e100.jpg (55)
graphic file with name pone.0097552.e101.jpg (56)

Using boundary conditions from Eqs. (55, 56) into Eqs. (49–54), we obtain

graphic file with name pone.0097552.e102.jpg (57)
graphic file with name pone.0097552.e103.jpg (58)
graphic file with name pone.0097552.e104.jpg (59)
graphic file with name pone.0097552.e105.jpg (60)

Due to lengthy calculations, the analytical results have been given up to first order but they have been shown graphically up to second order.

Formulation of Drainage Problem

Under the same assumptions as in the previous problem, we consider a film of non-Newtonian liquid draining down the vertical belt. The belt is stationary and the fluid drains down the belt due to gravity. The gravity in this case is opposite to the previous case. The coordinate system is selected same as in the previous case. Assuming that the flow is steady and laminar, external pressure is neglected whereas the fluid shear forces keep gravity balanced and the thickness of the film remains constant.

Boundary conditions for the drainage problem are

graphic file with name pone.0097552.e106.jpg (61)

Using non-dimensional variables, the boundary conditions for drainage problem become

graphic file with name pone.0097552.e107.jpg (62)

For temperature distribution, the boundary conditions are same as given in Eq. (56).

Solution of Drainage Problem

The OHAM solution

From Eqs. (21, 22), the linear, non-linear functions and source term (in drainage case), it is opposite due to gravity) are respectively defined as

graphic file with name pone.0097552.e108.jpg (63)
graphic file with name pone.0097552.e109.jpg (64)

OHAM is applied to non-linear coupled ordinary differential Eqs. (63, 64) as

graphic file with name pone.0097552.e110.jpg
graphic file with name pone.0097552.e111.jpg (65)

We consider Inline graphic as the following

graphic file with name pone.0097552.e113.jpg (66)

Substituting Inline graphic and Inline graphic from Eq. (66) into Eq. (65) we have the following components of velocity and temperature.

Zero components:

graphic file with name pone.0097552.e116.jpg (67)

First components:

graphic file with name pone.0097552.e117.jpg (68)

Solving Eqs. (67, 68) with boundary conditions (61, 62), we get

graphic file with name pone.0097552.e118.jpg (69)
graphic file with name pone.0097552.e119.jpg (70)

Like previous problem, results up to first order terms haven been obtained.

ADM solution

Using ADM on Eqs. (21, 22), the Adomian polynomials in equations (45, 46) for both problems are same whereas the different velocity components are obtained as:

Components of the Problem

The boundary conditions of first and second components for drainage velocity profile are same as given in Eq. (56). Also, the boundary conditions for temperature distribution are same as given in Eq. (57) but solution of these components is different, depends on the different velocity profile of drainage and lift problems. Due to lengthy analytical calculation, solutions up to first order terms are included whereas the graphical representations up to second order terms are given. Using boundary conditions (62) and (56) into Eqs. (49–54), the components, solution are obtained as:

graphic file with name pone.0097552.e120.jpg (71)
graphic file with name pone.0097552.e121.jpg (72)
graphic file with name pone.0097552.e122.jpg (73)
graphic file with name pone.0097552.e123.jpg (74)

Results and Discussion

The effect of Stock number Inline graphic magnetic parameter Inline graphic, Brinkman number Inline graphic non-Newtonian parameter Inline graphic and viscosity parameter Inline graphic in lifting and drainage problems together with the physical interpretation of the problem have been discussed in Figs. 120. Fig. 1 shows the geometry of lift and drainage problems. A comparison of the ADM and OHAM solutions is shown in Figs. 25 for various values of physical parameters. It is found from these figures that ADM and OHAM solutions are in good agreement. Figs. 6 and 7 provide variation of velocity and temperature distribution for different values of Brinkman number. It has been found that velocity decreases whereas temperature inside the fluid increases by increasing Inline graphic while keeping the other parameters fixed. In Fig. 8, we observed that velocity decreases with an increase in the Stock number Inline graphic. Physically, it is true as increasing Stock number causes the fluids thickness and reduces its flow. The effect of Stock number Inline graphic on temperature distribution has been illustrated in Fig. 9. It is observed that temperature Θ increases monotonically for large values of Stock number Inline graphic. The effect of viscosity parameter Inline graphic on lift velocity u is shown in Fig. 10. It is observed that the speed of flow decreases by increasing Inline graphic. The speed of flow is actually caused by shears thickening and thinning effects due to increase and decrease in viscosity parameter. A similar situation is observed in Fig. 11 where an increase in viscosity parameter Inline graphic decreases temperature distribution. Here, the velocity profiles are parabolic in nature and their amplitudes depend on the magnitude of the viscosity parameter Inline graphic. Variations of the magnetic parameter Inline graphic on lift velocity have been studied in Fig. 12. Here, it is clear that the boundary layer thickness is reciprocal to the transverse magnetic field and velocity decreases as flow progresses towards the surface of the fluid. On the other hand, temperature profile as shown in Fig. 13 indicates that fluid temperature increases with magnetic parameter. Fig. 14 shows that velocity increases in drainage flow when Stock number Inline graphic increases. Physically, it is due to friction which seems smaller near the belt and higher at the surface of the fluid. Further, it is found from Fig. 15 that temperature profile also increases when Inline graphic is increased. Fig. 16 illustrates the effect of variable viscosity parameter Inline graphic on the drain flow. It is observed that at higher values of viscosity parameter Inline graphic, velocity of the fluid increases gradually towards the surface of the fluid. However, it is found from Fig.17, that an increase in viscosity parameter Inline graphic causes gradual decrease in temperature field. The effects of non-Newtonian parameter Inline graphic on drain velocity have been studied in Fig. 18. We observed that an increase in Inline graphic raises drain velocity profile and decreases temperature profile as shown in Fig. 19. Finally for the accuracy purpose the present results are compared with published work in [22] in Fig. 20 and in table 1. An excellent agreement is found.

Figure 1. Geometry of the problem (a) Lift problem and (b) Drainage problem.

Figure 1

Figure 20. Comparison of the present results with published work [22] when Inline graphic.

Figure 20

Figure 2. Comparison of ADM and OHAM methods for lift velocity profile. Inline graphic.

Figure 2

Figure 5. Comparison of ADM and OHAM methods for drainage temperature distribution.Inline graphic.

Figure 5

Figure 6. Influence of the Brinkman number on the lift velocity profile when Inline graphic .

Figure 6

Figure 7. Influence of the Brinkman number on the lift temperature distribution when Inline graphic .

Figure 7

Figure 8. Effect of Stock number on the lift velocity profile. when Inline graphic .

Figure 8

Figure 9. Effect of Stock number on the lift temperature distribution when Inline graphic .

Figure 9

Figure 10. Effect of viscosity parameter on the lift velocity profile. when Inline graphic .

Figure 10

Figure 11. Effect of viscosity parameter on the lift temperature distribution when Inline graphic .

Figure 11

Figure 12. The effect of magnetic force on lift velocity profile when Inline graphic .

Figure 12

Figure 13. The effect of magnetic force on lift temperature distribution when Inline graphic .

Figure 13

Figure 14. The effect of Stock number on velocity for drainage problem when Inline graphic .

Figure 14

Figure 15. The effect of Stock number on temperature for drainage problem when Inline graphic .

Figure 15

Figure 16. Drain velocity for various values of viscosity parameter when Inline graphic .

Figure 16

Figure 17. Drain temperature distribution for various values of viscosity parameter when Inline graphic .

Figure 17

Figure 18. The influence of non-Newtonian parameter Inline graphic on velocity for drainage problem when Inline graphic .

Figure 18

Figure 19. The influence of non-Newtonian parameter Inline graphic on temperature for drainage problem when Inline graphic .

Figure 19

Table 1. Numerical results show the comparison of present results with published work [22] when Inline graphic.

x Present work Published work[22] Absolute error
0 1 1 0
0.1 0.95336886435638888 0.95336886432889 1.11022×10−16
0.2 0.91163368 0.91163368 1.11023×10−16
0.3 0.8742813014374999 0.8742813014375 0
0.4 0.84116332088888 0.84116332088888 0
0.5 0.8123818359375 0.8123818359375 0
0.6 0.788190612 0.788190612 0
0.7 0.76891138782638 0.76891138782638 0
0.8 0.754865408 0.754865408 0
0.9 0.74632017043749 0.7463201704375 0
1.0 0.7434513888888 0.7434513888888 0

Figure 3. Comparison of ADM and OHAM methods for lift temperature distribution.Inline graphic.

Figure 3

Figure 4. Comparison of ADM and OHAM methods for drainage velocity profile.Inline graphic.

Figure 4

Future Work

We intend to carry out researches in future on third grade fluid on vertical belt regarding the following discussions:

  1. Time dependent third grade fluid on vertical belt.

  2. Vogel Model third grade fluid on vertical belt with slip boundary conditions.

  3. Third grade fluid on vertical belt wit surface topography.

  4. Third grade fluid on vertical rotating disc with surface topography.

Conclusion

In this work, we have investigated the thin film flow non-Newtonian third grade fluid due to vertical belt and the fluid was subjected to lifting and drainage. Analytical solutions of the lifting and drainage problems have been obtained using ADM and OHAM. It has been shown graphically that these solutions are identical. The results for velocity and temperature have been plotted graphically and discussed in detail. It has been observed that these solutions are valid not only for small but also for large values of the emerging parameters. It has been observed that in both cases of lift problem velocity decreases while temperature increases with increasing Brinkman number Inline graphic. However, in drainage problem both velocity and temperature increases.

Funding Statement

The authors would like to acknowledge the research Management center – UTM and MOE (Ministry of Education) for the financial support through vote 4F109 & 04H27 for this research. Prof. S. Islam gratefully acknowledges the financial support of his visit provided by UTM. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

References

  • 1. Fetecau C, Fetecau C (2005) Starting solutions for some unsteady unidirectional flows of a second grade fluid. Int J Eng Sci 43: 781–789. [Google Scholar]
  • 2. Fetecau C, Fetecau C (2006) Starting solutions for the motion of a second grade fluid due to longitudinal and torsional oscillations of a circular cylinder. Int J Eng Sci 44: 788–796. [Google Scholar]
  • 3. Tan WC, Masuoka T (2007) Stability analysis of a Maxwell fluid in a porous medium heated from below. Phys Lett A 360: 454–460. [Google Scholar]
  • 4. Fakhar K, Zenli Xu, Cheng Yi (2008) Exact solution of a third grade fluid on a porous plate. Appl Math Comput 202: 376–382. [Google Scholar]
  • 5. Yao Y, Liu Y (2010) Some unsteady flows of a second grade fluid over a plane wall. Non-linear Anal Real World Appl 11: 4442–4450. [Google Scholar]
  • 6. Nazar M, Fetecau C, Vieru D (2010) New exact solutions corresponding to the second problem of stokes for second grade fluids. Non-linear Anal Real World Appl 11: 584–591. [Google Scholar]
  • 7. Ali F, Norzieha M, Sharidan S, Khan I, Hayat T (2012) New exact solution of Stokes' second for an MHD second fluid in a porous space. Int J Non-linear Mech 47: 521–525. [Google Scholar]
  • 8. Qasim M (2013) Heat and mass transfer in a Jeffrey fluid over a stretching sheet with heat source. Alex Eng J 52: 571–575. [Google Scholar]
  • 9. Qasim M, Hayat T, Obaidat S (2012) Radiation effect on the mixed convection flow of a viscoelastic fluid along an inclined stretching sheet. Z Naturforsch 67: 195–202. [Google Scholar]
  • 10. Hayat T, Shehzad SA, Qasim M, Asghar S, Alsaedi A (2014) Thermally stratified radiative flow of third grade fluid over a stretching surface. J Thermophysics and Heat Transfer 28: 155–161. [Google Scholar]
  • 11. Qasim M, Noreen S (2014) Heat transfer in the boundary layer flow of a Casson fluid over a permeable shrinking sheet with viscous dissipation. The Europ Physical J Plus 129: 1–8. [Google Scholar]
  • 12. Turkyilmazoglu M (2011) Numerical and analytical solutions for the flow and heat transfer near the equator of an MHD boundary layer over a porous rotating sphere. Int J of Thermal Sc 50: 831–842. [Google Scholar]
  • 13. Turkyilmazoglu M (2010) A note on the homotopy analysis method. Appl Math Lett 23: 1226–1230. [Google Scholar]
  • 14. Turkyilmazoglu M (2010) Analytic approximate solutions of rotating disk boundary layer flow subject to a uniform suction or injection. Int J Mechanical Sc 52: 1735–1744. [Google Scholar]
  • 15. Turkyilmazoglu M (2010) Purely analytic solutions of magnetohydrodynamic swirling boundary layer flow over a porous rotating disk. Computers and Fluids 39: 793–799. [Google Scholar]
  • 16. Fetecau C, Vieru D, Corina Fetecau, Akhter S (2013) General solutions for magnetohydrodynamic natural convection flow with radiative heat transfer and slip condition over a moving plate, Z. Naturforsch. 68a, 659–667 (2013) [Google Scholar]
  • 17. Fetecau C, Corina Fetecau, Mehwish Rana (2013) General solutions for the unsteady flow of second-grade fluids over an infinite plate that applies arbitrary shear to the fluid, Z. Naturforsch. 66a, 753–759. [Google Scholar]
  • 18. Rubbab Q, Vieru D, Fetecau C, Fetecau C (2013) Natural convection flow near a vertical plate that applies a shear stress to a viscous fluid, PLoSONE. 8(11): e78352 doi:10.1371/journal.pone.0078352 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 19. Khan A, Khan I, Ali F, ulhaq S, Shafie S (2014) Effects of wall shear stress on unsteady MHD conjugate flow in a porous medium with ramped wall temperature. PLoS ONE 9(3): e90280 doi:10.1371/journal.pone.0090280 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 20. Khaled ARA, Vafai K (2004) Hydrodynomic squeezed flow and heat transfer over a sensor surface, Int J Eng Sci. 42: 509–519. [Google Scholar]
  • 21. Miladinova S, Lebon G, Toshev E (2004) Thin film flow of a power law liquid falling down an inclined plate. J Non-Newtonian fluid Mech 122: 69–70. [Google Scholar]
  • 22.Gul T, Shah RA, Islam S, Arif M (2013) MHD thin film flows of a third grade fluid on a vertical belt with slip boundary conditions. J Appl Math: Article ID 707286 14.
  • 23. Siddiqui AM, Mahmood R, Ghori QK (2008) Homotopy perturbation method for thin film flow of a third grade fluid down an inclined plane. Chaos Sol Fract 35: 140–147. [Google Scholar]
  • 24.Liao S J (2003) Beyond Perturbation: Introduction to Homotopy Analysis Method. Chapman & Hall/CRC Press Boca Raton.
  • 25. Marinca V, Herisanu N, Nemes I (2008) Optimal homotopy asymptotic method with application to thin film flow. Cent. Eur J Phys 6: 648–653. [Google Scholar]
  • 26. Marinca V, Herisanu N (2008) Application of Optimal homotopy asymptotic method for solving non-linear equations arising in heat transfer. Int Commun Heat Mass Transfer 35: 710–715. [Google Scholar]
  • 27. Marinca V, Herisanu V, Bota C, Marinca B (2009) An Optimal homotopy asymptotic method applied to the steady flow of a fourth grade fluid past a porous plate. Appl Math Lett 22: 245–251. [Google Scholar]
  • 28. Joneidi AA, Ganji DD (2009) Babaelahi (2009) Micro polar flow in a porous channel with high mass transfer. Int Commun Heat Mass Transfer 36: 1082–1088. [Google Scholar]
  • 29. Siddiqui AM, Ahmed M, Ghori QK (2007) Thin film flow of non-Newtonian fluid on a moving belt. Chaos Sol Fract 33: 1006–1016. [Google Scholar]
  • 30. Siddiqui AM, Mahmood R, Ghori QK (2006) Homotopy perturbation method for thin film flow of a fourth grade fluid down a vertical cylinder. Phys Lett A 352: 404–410. [Google Scholar]
  • 31. Costa A, Macedonio G (2003) Viscous heating in fluids with temperature-dependent viscosity implications for magma flows. Nonlinear Proc Geophys 10: 545–555. [Google Scholar]
  • 32. Nadeem S, Awais M (2008) Thin film flow of an unsteady shrinking sheet through porous medium with variable viscosity. Phy Let A 372: 4965–4972. [Google Scholar]
  • 33. Ellahi R, Riaz A (2010) Analytical solution for MHD flow in a third grade fluid with variable viscosity. Math Comput Mod 52: 1783–1793. [Google Scholar]
  • 34. Aksoy Y, Pakdemirly M (210) Approximate analytical solution for flow of a third grade fluid through a parallel-plate channel filled with a porous medium. Springer 83: 375–395. [Google Scholar]
  • 35.Adomian G (1994) Solving frontier problems of physics: the decomposition method. Kluwer Academic Publishers.
  • 36. Adomian G (1992) A review of the decomposition method and some recent results for non-linear equations. Math Comput Model 13: 287–299. [Google Scholar]
  • 37. Wazwaz AM (2005) Adomian decomposition method for a reliable treatment of the Bratu-type equations, Appl Math Comput. 166: 652–663. [Google Scholar]
  • 38. Wazwaz AM (2005) Adomian decomposition method for a reliable treatment of the Emden–Fowler equation. Appl Math Comput 161: 543–560. [Google Scholar]

Articles from PLoS ONE are provided here courtesy of PLOS

RESOURCES