ENGINEERING PHYSICS AND MATHEMATICS
An efficient analytical approach for MHD viscous
flow over a stretching sheet via homotopy perturbation
sumudu transform method
Sushila
a,*
, Jagdev Singh
b, Y.S. Shishodia
ca
Department of Physics, Jagan Nath University, Village-Rampura, Tehsil-Chaksu, Jaipur 303 901, Rajasthan, India bDepartment of Mathematics, Jagan Nath University, Village-Rampura, Tehsil-Chaksu, Jaipur 303 901, Rajasthan, India c
Jagan Nath University, Village-Rampura, Tehsil-Chaksu, Jaipur 303 901, Rajasthan, India
Received 28 September 2012; revised 22 November 2012; accepted 8 December 2012 Available online 29 January 2013
KEYWORDS Sumudu transform; Homotopy perturbation method; He’s polynomials; Stretching sheet; MHD viscous flow
Abstract In this paper, we present an efficient analytical approach based on new homotopy per-turbation sumudu transform method (HPSTM) to investigate the magnetohydrodynamics (MHD) viscous flow due to a stretching sheet. The viscous fluid is electrically conducting in the presence of magnetic field and the induced magnetic field is neglected for small magnetic Reynolds number. Finally, some numerical comparisons among the new HPSTM, the homotopy perturbation method and the exact solution have been made. The numerical solutions obtained by the proposed method show that the approach is easy to implement and computationally very attractive.
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1. Introduction
The boundary layer flow of an incompressible viscous fluid over a continuously stretching sheet is often occurs in the sev-eral engineering and industrial processes. It has attracted con-siderable interest during the last few decades. Such flows have important applications in industries, for example in the aero-dynamic extrusion of a polymer sheet from a die, hot rolling,
the cooling of an infinite metallic plate in a cooling bath, the boundary layer along a liquid film in condensation process, glass–fiber production and so on [1–3]. Many metallurgical processes involve the cooling of continuous strips or filaments by drawing them through a quiescent fluid. The mechanical properties of the final product strictly depend on the stretching and cold drawing rates in the process. The pioneering work in this area was conducted by Sakiadis[4,5] and the boundary layer flow on a continuously stretching surface with a constant speed was investigated by several researchers in the field. Spe-cifically Crane[6]found a closed form solution for flow of an incompressible viscous fluid past a stretching plate. Gupta and Gupta [7] added suction or injection on the surface which models condensation or evaporation, a uniform transverse magnetic field, when the fluid is electrically conducting, by Anderson[8]. The joint effect of viscoelasticity and magnetic * Corresponding author. Tel.: +91 9461673365.
E-mail addresses: [email protected] ( Sushila), jagdevsingh [email protected](J. Singh),[email protected](Y.S. Shishodia). Peer review under responsibility of Ain Shams University.
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field on Crane’s problem has been investigated by Ariel [9]. The flow past a stretching sheet need not be necessarily two-dimensional because the stretching of the sheet can take place in a number of ways. It can be three-dimensional when the stretching is radial. The three-dimensional and axisymmetric stretching flat surface was studied by Wang[10]. The flow in-side a stretching channel or tube was conin-sidered by Brady and Acrivos [11] and the flow outside a stretching tube by Wang[12]. The unsteady stretching sheet was investigated by Wang[13]and Usha and Sridharan[14]. A non-iterative solu-tion for the MHD flow has been given by Ariel[15]using the technique of Samuel and Hall[16], Ariel et al. [17]and Ariel
[18]applied HPM and extended HPM to derive the analytical solution to the axisymmetric flow past a stretching sheet.
Magnetohydrodynamics (MHD) is the study of the interac-tion of conducting fluid with electromagnetic phenomena. The flow of an electrically conducting fluid in the presence of mag-netic field is important in several areas of science and engineer-ing such as MHD power generation, MHD flow generators, and MHD pumps. Most boundary-layer models can be re-duced to systems of nonlinear ordinary differential equations which are solved by numerical and analytical methods. Analyt-ical methods have significant advantages over numerAnalyt-ical meth-ods in providing analytic, verifiable, rapidly convergent approximation. There exists a wide class of literature dealing with the problems of approximate solutions to nonlinear dif-ferential equations with various different methodologies, called perturbation methods. The perturbation methods have some limitations, e.g., the approximate solution involves series of small parameters which poses difficulty since majority of non-linear problems have no small parameters at all. Although appropriate choices of small parameters some time leads to ideal solution but in most of the cases unsuitable choices lead to serious effects in the solutions. Therefore, an analytical method is welcome which does not require a small parameter in the equation modeling the phenomenon. The homotopy per-turbation method (HPM) was first introduced by He[19]and was further developed by him[20–26]. The HPM is in fact, a coupling of the traditional perturbation method and homoto-py in topology [27]. This method was applied to helmhotz equation and fifth-order KdV equation [28], nonlinear equa-tion arising in heat transfer[29], determining frequency–ampli-tude relation of a nonlinear oscillator with discontinuity[30], gas dynamics equation [31] and fractional nonlinear Schro¨-dinger equation[32]. Very recently, Singh et al.[33]have pro-posed a new approach named homotopy perturbation sumudu transform method (HPSTM) to solve the nonlinear partial dif-ferential equations. The homotopy perturbation sumudu transform method (HPSTM) is a combination of sumudu transform method, HPM and He’s polynomials and is mainly due to Ghorbani[34,35].
The objective of this paper is to present a simple recursive algorithm based on the new HPSTM which produces the series solution of MHD boundary-layer equations for stretching sheet problem. The advantage of this technique is its capability of combining two powerful methods for obtaining exact and approximate analytical solutions for nonlinear equations. The fact that HPSTM solves linear and nonlinear problems without using Adomian’s polynomials can be considered as a clear advantage of this technique over this decomposition method. It is worth mentioning that the proposed method is capable of reducing the volume of the computational work
as compared to the classical methods while still maintaining the high accuracy of the numerical result; the size reduction amounts to an improvement of the performance of the approach.
2. Sumudu transform
In early 90s, Watugala [36] introduced a new integral trans-form, named the sumudu transform and applied it to the solu-tion of ordinary differential equasolu-tion in control engineering problems. The sumudu transform is defined over the set of functions
A¼ ffðtÞj9M;s1;s2>0;jfðtÞj<Mejtj=sj;ift2 ð1Þ
j
½0;1Þg by the following formula
fðuÞ ¼S½fðtÞ ¼ Z 1
0
fðutÞet dt; u2 ðs1;s2Þ: ð1Þ For further detail and properties of this transform, see
[37–39].
3. Basic idea of HPSTM
In order to elucidate the solution procedure of the new HPSTM, we consider the following general form of 3rd order non-homogenous nonlinear ordinary differential equation with the initial conditions is given by
f000þb
1ðxÞf00þb2ðxÞf0þb3ðxÞf¼gðfÞ; ð2Þ fð0Þ ¼a; f0ð0Þ ¼b; f00ð0Þ ¼c: ð3Þ Taking the sumudu transform on both sides of Eq.(2), we get
S½f000 þS½b
1ðxÞf00þb2ðxÞf0þb3ðxÞf ¼S½gðfÞ: ð4Þ Using the differentiation property of the sumudu trans-form, we have
S½f ¼aþbuþcu2þu3S½gðfÞ u3S½b
1ðxÞf00þb2ðxÞf0
þb3ðxÞf: ð5Þ
Operating with the sumudu inverse on both sides of Eq.(5)
gives
f¼GðxÞ þS1½u3S½gðfÞ S1½u3S½b
1ðxÞf00þb2ðxÞf0
þb3ðxÞf; ð6Þ
where G(x) represents the term arising from the source term and the prescribed initial conditions. Now we apply the HPM
f¼X 1
m¼0 pmf
m; ð7Þ
and the nonlinear term can be decomposed as
gðfÞ ¼X 1
m¼0
pmHm; ð8Þ
for some He’s polynomialsHm[35,40]that are given by
Hm¼ 1 m! @m @pm g X1 i¼0 pif i ! " # p¼0 ; m¼0;1;2;3;. . . ð9Þ Substituting Eqs. (7) and (8) in Eq.(6), we get
X1 m¼0 pmf m¼GðxÞ þp S1 u3S X1 m¼0 pmH m " # " #! p S1 u3 S b1ðxÞ X1 m¼0 pm f00 mþb2ðxÞ X1 m¼0 pm f0 mþb3ðxÞ X1 m¼0 pm fm " # " #! ; ð10Þ which is the coupling of the sumudu transform and the HPM using He’s polynomials. Comparing the coefficients of like powers of p, the following approximations are obtained.
p0: f0¼GðxÞ; p1 : f1¼S1½u3S ½H 0 S1½u3S ½b1ðxÞf000þb2ðxÞf00 þb3ðxÞf0; p2 : f2¼S1½u3S½H 1 S1½u3S ½b1ðxÞf001þb2ðxÞf01 þb3ðxÞf1; .. . ð11Þ 4. Mathematical model
The MHD boundary layer flow over a flat plate is governed by the continuity and the Navier–Stokes equations for an incom-pressible viscous fluid. The fluid is electrically conducting un-der the influence of an applied magnetic fieldB(x) normal to the stretching sheet. The induced magnetic field is neglected. The resulting boundary-layer equations are:
@U @xþ @V @y¼0; ð12Þ U@U @xþV @U @y ¼v @2U @y2 r B2ðxÞ q U; ð13Þ
where U andV are the velocity components in thex andy
directions, respectively. Alsov,qandrare the kinematic vis-cosity, density and electrical conductivity of the fluid. TheB(x) is taken as[41]BðxÞ ¼ B0xn1=2.
The boundary conditions applicable to the present flow are
Uðx;0Þ ¼cxn; Vðx;0Þ ¼0; and Uðx;1Þ ¼0: ð14Þ
To solve the problem, momentum and energy equations are firstly nondimensionalized by introducing the following dimen-sionless variables: g¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi cðnþ1Þ 2v r xn21y; ð15Þ U¼cxnf0ðgÞ; ð16Þ V¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi cvðnþ1Þ 2 r xn21 fðgÞ þn1 nþ1gf 0ðgÞ : ð17Þ
Using Eqs. (15)–(17), the governing equations can be re-duced to nonlinear differential equation of the form:
f000þff00bðf0Þ2Mf0¼0; fð0Þ ¼0; f0ð0Þ ¼1 and f0ð1Þ ¼00; ð18Þ where b¼ 2n nþ1 M¼ 2rb20 qcð1þnÞ: ð19Þ
5. HPSTM solution and discussion
In this section, we apply the new HPSTM to obtain an approx-imate analytical solution of (18), (19). By applying the sumudu transform on the both sides of Eq.(18), we have
S½fðgÞ ¼uþau2þu3S½bðf0Þ2
ff00þMf0; ð20Þ wheref00ð0Þ ¼a.
The inverse sumudu transform implies that
fðgÞ ¼gþag 2 2 þS 1½ u3S½bðf0Þ2 ff00þMf0: ð21Þ Now applying the HPM, we get
X1 m¼0 pmf mðgÞ ¼gþ ag2 2 þp S 1 u3S b X 1 m¼0 pmH mðgÞ ! " " X 1 m¼0 pmH0 mðgÞ ! þM X 1 m¼0 pmf0 mðgÞ !##! ; ð22Þ
whereHm(g) andH0mðgÞare He’s polynomials[35,40]that
rep-resents the nonlinear terms. So, He’s polynomials are given by X1 m¼0 pmH mðgÞ ¼ ðf0Þ 2 ðgÞ: ð23Þ
The first few components of He’s polynomials, are given by
H0ðgÞ ¼ ðf00Þ 2ð gÞ; H1ðgÞ ¼2f00ðgÞf01ðgÞ; H2ðgÞ ¼ ðf01Þ 2ð gÞ þ2f00ðgÞf02ðgÞ; .. . ð24Þ
Table 1 Comparison of the values off00ð0Þobtained by HPM
[42], HPSTM and the exact solution.
b M HPM[42] HPSTM Exact solution 1 0 1 1 1 1 1.41421 1.41421 1.41421 5 2.44948 2.44948 2.44948 10 3.31662 3.31662 3.31662 50 7.14142 7.14142 7.14142 100 10.0499 10.0499 10.04987 500 22.383 22.383 22.38302 1000 31.6386 31.6386 31.63858
Table 2 Variation inf00ð0Þat the different values ofbandM
obtained by HPM[42]and HPSTM. b M HPM[42] HPSTM 1.5 0 1.1486 1.1547 1 1.5252 1.5252 5 2.5161 2.5161 10 3.3663 3.3663 50 7.1647 7.1647 100 10.0664 10.0776 500 22.3901 22.3904 1000 31.6432 31.6438
Figure 1 The results offobtained by HPSTM, HPM[42]and exact solutions forb= 1, when (a)M= 0, (b)M= 1, (c)M= 50, and (d)M= 50.
And forH0 mðgÞwe find that X1 m¼0 pmH0 mðgÞ ¼fðgÞf00ðgÞ; ð25Þ H0 0ðgÞ ¼f0ðgÞf000ðgÞ; H0 1ðgÞ ¼f0ðgÞf001ðgÞ þf1ðgÞf000ðgÞ; H02ðgÞ ¼f0ðgÞf002ðgÞ þf1ðgÞf001ðgÞ þf2ðgÞf000ðgÞ; .. . ð26Þ
Comparing the coefficients of like powers ofp, we have
p0:f 0¼gþ ag2 2 ; ð27Þ p1:f1¼ ð2b1Þ 120 a 2 g5þðM1þ2bÞ 24 ag 4þðMþbÞ 6 g 3 ; ð28Þ p2:f 2¼ ð20b232bþ11Þ 40320 a 3g8 þð11þ10Mbþ20b 2 8M32bÞ 5040 a 2g7 þð312b8Mþ10b 2 þ10MbþM2Þ 720 ag 6 þðM 2þ2b2 2b2Mþ3MbÞ 120 g 5 ; ð29Þ p3 :f3¼ð 600b3 1596b2 þ1398b375Þ 39916800 a 4 g11 þð375546bMþ300Mb 2þ 600b3 1596b2þ 1398bþ243MÞ 3628800 a 3 g10 þð129þ42bM 2 þ300b3 39M2 þ548b710b2 þ243M546bMþ300Mb2 Þ 362880 a 2 g9 þð15þ120Mb 2þ M3þ 80b3 166b2þ 103bþ80M39M2þ 42bM2 196bMÞ 40320 ag 8 þðM 3 10M2þ 11bM2þ 20b2 M26bMþ8Mþ8b16b2þ 10b3Þ 5040 g 7 ;... ð30Þ and so on. In this way, the remaining terms of the HPSTM ser-ies can be calculated.
The series solution is given by
f¼f0þf1þf2þf3þ ;
p!1: ð31Þ
Substituting Eqs. (27)–(30) into Eq.(31), we obtain the follow-ing series solution
fðgÞ ¼gþag 2 2 þ ð2b1Þ 120 a 2g5þðM1þ2bÞ 24 ag 4 þðMþbÞ 6 g 3þð20b232bþ11Þ 40320 a 3g8 þð11þ10Mbþ20b 28M32bÞ 5040 a 2g7 þð312b8Mþ10b 2þ10MbþM2Þ 720 ag 6 þðM 2þ2b22b2Mþ3MbÞ 120 g 5 þð600b 31596b2þ1398b375Þ 39916800 a 4g11 þð375546bMþ300Mb 2þ600b31596b2þ1398bþ243MÞ 3628800 a 3g10 þð129þ42bM 2þ300b339M2þ548b710b2þ243M546bMþ300Mb2Þ 362880 a 2g9 þð15þ120Mb 2þM3þ80b3166b2þ103bþ80M39M2þ42bM2196bMÞ 40320 ag 8 þðM 310M2þ11bM2þ20b2M26bMþ8Mþ8b16b2þ10b3Þ 5040 g 7þ ð32Þ To selectf00ð0Þ ¼a and g
1, we begin with some initial guess ofaand draw f0. The solution process is repeated with another values ofauntilf0receive to zero. Also,g
1is obtained from highest value ofginf0.
Tables 1 and 2clearly indicate that present solution of new HPSTM shows excellent agreement with the HPM[42]and the exact solution and more convergent than the HPM[42]. This analysis shows that the new HPSTM is valid for MHD viscous flow problems.
6. Results and discussion
Eq.(18)is solved analytically using the new HPSTM. The ana-lytical and the exact solutions offfor different values ofMand bare depicted inFigs. 1 and 2. Furthermore, the comparison between the new HPSTM and the exact solutions off0 is per-formed inFig. 3. The effects of the magnetic parameter M
are shown inFig. 3. It is observed fromFig. 3that whenM, increases, the velocity profile is more and more far away from the wall, and the boundary layer thickness is more and more thicker. Therefore, it is concluded fromFig. 3thatf0decreases whenMincreases. A very good agreement is achieved between the results obtained by the new HPSTM, the HPM[42]and the exact solutions for all values ofg. The results of new HPSTM are better than HPM[42]in large amount ofM.
7. Conclusion
In this paper, a simple algorithm based on new HPSTM has been successfully applied for solving the magnetohydrodynam-ics (MHD) viscous flow due to stretching sheet. An excellent agreement is achieved by comparing the present solution very well with the HPM[42]and exact solution. The method is ap-plied here in direct manner without the use of linearization, transformation, discretization, perturbation, or restrictive assumptions. The approach gives more realistic series solutions that converge very rapidly in physical problems. The proposed method’s ability to solve nonlinear problems without the use of
Figure 3 Comparison of the solution (f0) obtained by HPSTM
Adomian polynomials is evidence of its clear advantage over the decomposition method. In conclusion, the HPSTM could be a promising tool for solving more complex boundary equa-tions that the one studied in this paper.
Acknowledgements
The authors are extending their heartfelt thanks to the review-ers for their valuable suggestions for the improvement of the article. The authors are also thankful to Shri Manish Gupta, Chancellor and Shri Deepak Gupta, Vice-Chairman, Jagan Nath University, Jaipur for providing support and facilities for the research work
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Sushila is an Assistant Professor in the Department of Physics, Jagan Nath Univer-sity, Jaipur-303901, Rajasthan, India. Her fields of research include nuclear physics, solid state physics, plasma physics, fluid mechanics, fractional calculus, homotopy methods, Laplace transform method and sumudu transform method.
Jagdev Singhis an Assistant Professor in the Department of Mathematics, Jagan Nath University, Jaipur-303901, Rajasthan, India. His fields of research include special functions, fractional calculus, fluid mechanics, homoto-py methods, Adomian decomposition method, Laplace transform method and sumudu transform method.
Y.S. Shishodia,Pro-Vice-Chancellor in Jagan Nath University, Jaipur-303901, Rajasthan, India. His area of interest is nuclear physics, solid state physics, positron spectroscopy, laser and plasma technology, solar cells, fluid mechanics, homotopy methods, Laplace transform method and sumudu transform method.