the (g′/g)-expansion method for the coupled boussinesq equation
TRANSCRIPT
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Procedia Engineering 00 (2011) 000–000
www.elsevier.com/locate/procedia
ICM11
The )(G
G′ -expansion method for the coupled Boussinesq equation
Reza Abazari*
Young Researchers Club, Islamic Azad University, Ardabil Branch, P.O. Box 56169-54184, Ardabil, Iran
Abstract
In this work, the )/'( GG -expansion method with the aid of Maple is applied to construct more general exact solutions of the
coupled Boussinesq equations, where the French scientist Joseph Valentin Boussinesq (1842-1929) described in the 1870’s model equations for the propagation of long waves on the surface of water with a small amplitude. Each of the obtained solutions, namely hyperbolic function solutions, trigonometric function solutions and rational function solutions contain an explicit linear function of the variables in the considered equation. It is shown that the proposed method provides a powerful mathematical tool for solving nonlinear wave equations in mathematical physics and engineering problems.
© 2011 Published by Elsevier Ltd. Selection and peer-review under responsibility of ICM11
Keyword: Boussinesq systems, )/'( GG -expansion method, hyperbolic function solutions, trigonometric function solutions, rational function solutions.
1. Introduction
Partial differential equations (PDEs) describe various nonlinear phenomena in natural and applied sciences such as fluid dynamics, plasma physics, solid state physics, optical fibers, acoustics, mechanics, biology and mathematical finance. Their solution spaces are infinite dimensional and contain diverse solution structures. It is of significant importance to solve nonlinear PDEs from both theoretical and practical points of view. Due to the nonlinearity of differential equations and the high dimension of space variables, it is a difficult job for us to determine whatever exact solutions to nonlinear PDEs. Particularly, various methods have been utilized to explore different kinds of solutions of physical models described by nonlinear PDEs. One of the basic physical problems for those models is to obtain their travelling wave solutions(also known as solitons). In mathematics and physics, a soliton is a self reinforcing solitary wave, a wave packet or pulse, that maintains its shape while it travels at constant speed. Solitons are caused by a cancelation of nonlinear and dispersive effects in the medium. The term "dispersive effects" refers to a property of certain systems where the speed of the waves varies according to frequency. Solitons arise as the solutions of a widespread class of weakly nonlinear dispersive partial differential equations describing physical systems. The soliton phenomenon was first described by John Scott Russell (1808–1882) who observed a solitary wave in the Union Canal in Scotland. He reproduced the phenomenon in a wave tank and named it the
* Corresponding author. Tel.: +98 451 4471544; fax: +98 451 5514701. E-mail address: [email protected], [email protected].
1877–7058 © 2011 Published by Elsevier Ltd.doi:10.1016/j.proeng.2011.04.473
Physics Engineering 10 (2011) 2845–2850
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2846 Reza Abazari / Physics Engineering 10 (2011) 2845–28502 Author name / Procedia Engineering 00 (2011) 000–000
"Wave of Translation" (also known as travelling wave solutions or solitons)[1]. The soliton solutions are typically obtained by means of the inverse scattering transform [2] and owe their stability to the integrability of the field equations.
It has been a successful idea to generate exact solutions of nonlinear wave equations by reducing PDEs into ordinary differential equations (ODEs). Many approaches to exact solutions in the literature follow such an idea, which contain the tanh-function method [3], the sech-function method [4], the homogeneous balance method [5, 6] the extended tanh-function method [7], the sine-cosine method [8], the tanh-coth method [9], the Jacobi elliptic function method [10], the exp-function method [11], the F-expansion method [12], the mapping method [13], and the extended F-expansion method [14]. Given an ODE of differential polynomial type, either constant-coefficient or variable-coefficient, one can always adopt computer algebra systems to search for rational solutions pretty systematically. This is one of the main reasons why those reduction methods work well. But, most of the methods may sometimes fail or can only lead to a kind of special solution and the solution procedures become very complex as the degree of nonlinearity increases.
Recently, the )/'( GG -expansion method, firstly introduced by Wang et al. [15], has become widely used
to search for various exact solutions of NLEEs [15]-[21]. The main idea of this method is that the traveling wave solutions of non--linear equations can be expressed by a polynomial in )/'( GG , where )(= ξGG satisfies the
second order linear ordinary differential equation 0,=)()()( ξµξλξ GGG +′+′′ where tkx ωξ += and ω,kare arbitrary constants. The degree of this polynomial can be determined by considering the homogeneous balance between the highest order derivatives and the non--linear terms appearing in the given non-linear equations.
The aim of this paper is to apply the )/'( GG -expansion method to find new hyperbolic and trigonometric
solutions of the following coupled Boussinesq equation
−−++
+++
0,=2
1
0,=6
1)(
xxtxxxxxt
xxtxxt
uuuu
uu
τηη
ηηη(1)
Here, the independent variable, x , is proportional to distance in the direction of propagation while t is proportional to elapsed time. The dependent variables η and u have the following physical interpretation. The
quantity 0),( ηη +tx corresponds to the total depth of the liquid at the point x at time t , where 0η is the height
of the undisturbed water depth. The variable ),( txu represents the horizontal velocity at the point
),(=),( 0θηxyx ( y is the vertical coordinate, with 0,=y corresponding to the channel bottom or sea bed) at
time t . Also, the quantity ),/(= 20ηρτ gΓ is the Bond number where Γ is the surface tension coefficient, ρ is
the density of water and g is the acceleration due to gravity. Thus u is the horizontal velocity field at the height
0θη , where θ is a fixed constant in the interval [0,1] .
With the aid of Maple, new explicit and exact travelling wave and solitary solutions for the Boussinesq systems (1) are obtained by using the )/'( GG -expansion method.
2. Application of the )/'( GG -expansion method for the equation (1)
In this section, we apply the proposed method to obtain new and more general exact solutions of Eq. (1), which arises in several physical applications including the propagation of long waves on the surface of water with a small amplitude. Let us assume the traveling wave solution of Eq. (1) in the form
),(=),(),(=),( ξξη UtxuVtx (2)
where ,= tkx ωξ + and ω,k are constants. Substituting Eq. (2) into Eq. (1) and integrating once with respect to
ξ and setting the integration constants as zero, we obtain the following nonlinear ordinary differential system
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Reza Abazari / Physics Engineering 10 (2011) 2845–2850 2847Author name / Procedia Engineering 00 (2011) 000–000 3
′′−′′−++
′′+++
0,=2
1
2
1
0,=61
232
2
UkVkkUkVU
VkkUVkUV
ωτω
ωω (3)
Suppose that the solution of the nonlinear ordinary differential system (3) can be expressed by a polynomial in )/'( GG as follows:
.)(=)(
,)(=)(
01=
01=
ββξ
ααξ
+′
+′
i
i
n
i
ii
m
i
G
GV
G
GU
(4)
where 00, ≠≠ nm βα and nm, are called the balance number, )0,1,...,=(, miiα and )0,1,...,=(, njjβare constants to be determined later, )(ξG satisfies a second order linear ordinary differential equation (LODE):
0,=)()()( ξµξλξ GGG +′+′′ (5)
where λ and µ are arbitrary constants. By considering the homogeneous balance between the highest order
derivatives and nonlinear terms appearing in nonlinear ordinary differential system (3) we get 2.== nmSubstituting Eqs. (4) along with Eq. (5) into Eq. (3) and collecting all the terms with the same power of )/'( GGtogether, equating each coefficient to zero, yields a set of simultaneous algebraic equations for
0,1,2)=(,,,,, ik iαµλω , and 0,1,2)=(, jjβ , as follows:
( ) ( ) 0,=126
1000
221 βωβαωµβλβµ ++++ kk (6)
( ) 0,=)2
1()
2
1(2 0
200
21
22
321 αωαβωλµαµαµβλβµτ −+−+++ kkk (7)
( ) 0,=)6
1
3
1( 101101
22121 βωβαβααωλβµλβµβ ++++++ kk (8)
0,=)())2(2
1(3)6(2 1101
2212
32121 ωαβααωµλαλµαλβλµβµβτ −+−+++++ kkk (9)
( )( ) 0,=1)3
4
3
2
2
1( 2112020
22
221 βωβαβααβωµβλβλβ +++++++ kk (10)
0,=)2
1()
2
3)4((2)84(3 2
21022
212
232
221 αωαααβωλααµλµβλβλβτ −++−+++++ kkk (11)
( ) 0,=)3
5
3
1( 2112
221 kk βαβαωλββ +++ (12)
( ) ( ) 0,=552 122
213
12 ααωλααβλβτ kkk −+++ (13)
0,=2222 βαβω kk + (14)
0,=2
136 2
222
23 ααωβτ kkk −+ (15)
Solving (6)-(15) by use of Maple, we get the following results:
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2848 Reza Abazari / Physics Engineering 10 (2011) 2845–28504 Author name / Procedia Engineering 00 (2011) 000–000
.}6
=,7
2
2
7=,
772
48
1=,
7
26=
,
72
772
168
1=,
7
26=,
726
1=,
772
288
1={
1
2
211
11
21
210
2
02
12
2
11
1210
2
012
1
124
1210
2
θτβα
θβ
τθθατθβτ
θα
τθ
θ
θατθαθ
τωτ
θ
αλτ
θατθµ
k
k
kk
k
kk
kk
k
±+±
+±±+
(16)
where ,67=7,12= 10 τθτθ −− and 0≠k and 1α are free constant parameters. Therefore, substitute the case
(16) in (4), we get
.772
48
1)(
7
2
2
7)(
6=)(
,
7
2
772
168
1)()(
7
26=)(
12
1210
2
11
2
1
2
2
11
1210
2
122
1
τθθατθα
θθτξ
τθ
θ
θατθατθ
ξ
k
k
G
G
G
GkV
k
k
G
G
G
GkU
++′
±′
+±′
+′
±
(17)
Substituting the general solutions of ordinary differential equation (5) into Eq. (19), we obtain three types of
traveling wave solutions of Eq. (1) in view of the positive, negative or zero of µλ 42 − .
When 0,>=42
02
kτθµλ −− using the general solutions of ordinary differential equation (5), we obtain
hyperbolic function solution ),( txuH and ),( txHη of coupled Boussinesq equation (1) as follows:
,
))21
(cosh)21
(sinh(
)(1
14
3=),(
22
012
02
22
210
1
ξτθξ
τθ
θθ
kC
kC
CC
txu
−+−
−±H (18)
,
))21
(cosh)21
(sinh(
)(
2
3=),(
22
012
02
22
21
1
0
ξτθξ
τθθθ
η
kC
kC
CC
tx
−+−
−
H (19)
where ),7
26(=,67=7,12=
110 txk
θτξτθτθ −− and 0≠k and ,, 21 CC are arbitrary constants. It is
easy to see that the hyperbolic solutions (18)-(19) can be rewritten at ,> 22
21 CC as follows
1),))4249
26(
712
2(tanh(
67
17)(6
712
14
3=),( 2
2 −−−
−−−
−−
−±HH ρτ
τττ
ττ
τtx
k
ktxu (20)
1),))4249
26(
712
2(tanh(
76
712
2
3=),( 2
2 −−−
−−−−−
HH ρτττ
τττη tx
k
ktx (21)
while at ,< 22
21 CC one can obtain
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Reza Abazari / Physics Engineering 10 (2011) 2845–2850 2849Author name / Procedia Engineering 00 (2011) 000–000 5
1),))4249
26(
712
2(coth(
67
17)(6
712
14
3=),( 2
2 −−−
−−−
−−
−±HH ρτ
τττ
ττ
τtx
k
ktxu (22)
1),))4249
26(
712
2(coth(
76
712
2
3=),( 2
2 −−−
−−−−−
HH ρτττ
τττη tx
k
ktx (23)
where ),(tanh=2
11
C
C−H
ρ and k are arbitrary constants. Now, when 0,<22
=422
22
kp
q−− ωµλ we obtain
trigonometric function solution ),( txuT and ),( txTη of coupled Boussinesq equation (1) as follows:
,
))21
(cos)21
(sin(
)(1
14
3=),(
22
012
02
12
220
1
ξτθξ
τθ
θθ
kC
kC
CC
txu
−+−
−±T (24)
,
))21
(cos)21
(sin(
)(
2
3=),(
22
012
02
21
22
1
0
ξτθξ
τθθθ
η
kC
kC
CC
tx
−+−
−
T (25)
where ),7
26(=,67=7,12=
110 txk
θτξτθτθ −− and 0≠k and ,, 21 CC are arbitrary constants.
Similarity, the trigonometric solutions (24)-(25) can be rewritten at ,> 22
21 CC and ,< 2
22
1 CC as follows
1),))4249
26(
712
2(tan(
67
17)(6
712
14
3=),( 2
2 +−−
−−−
−−
−TT ρτ
τττ
ττ
τtx
k
ktxu (26)
1),))4249
26(
712
2(tan(
76
712
2
3=),( 2
2 +−−
−−−−−−
TT ρτττ
τττη tx
k
ktx (27)
and
1),))4249
26(
712
2(cot(
67
17)(6
712
14
3=),( 2
2 +−−
−−−
−−
−TT ρτ
τττ
ττ
τtx
k
ktxu (28)
1),))4249
26(
712
2(cot(
76
712
2
3=),( 2
2 +−−
−−−−−−
TT ρτττ
τττη tx
k
ktx (29)
respectively, where ),(tan=2
11
C
C−T
ρ and k are arbitrary constants. Finally, when 0,=42 µλ − then, the
rational function solutions to Eq. (1), obtained as follow:
,))((
=),(2
12
22
2
CtxC
Cktxurat
+± (30)
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2850 Reza Abazari / Physics Engineering 10 (2011) 2845–28506 Author name / Procedia Engineering 00 (2011) 000–000
,))((
=),(2
12
22
2
CtxC
Cktxrat
+η (31)
where ,, 21 CC and k are arbitrary constants.
3. Conclusions
This study shows that the )/'( GG -expansion method is quite efficient and practically well suited for use in
finding exact solutions for the coupled Boussinesq equation. Our solutions are in more general forms, and many known solutions to these equations are only special cases of them. With the aid of Maple, we have assured the correctness of the obtained solutions by putting them back into the original equation. We hope that they will be useful for further studies in applied sciences.
4. Acknowledgment
This work is partially supported by Grant-in-Aid from the Islamic Azad University, Young Researchers Club, Ardabil Branch, Iran.
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