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Revista mexicana de física

versión impresa ISSN 0035-001X

Rev. mex. fis. vol.69 no.2 México mar./abr. 2023  Epub 05-Nov-2024

https://doi.org/10.31349/revmexfis.69.021401 

Other areas in physics

Extended Jacobi elliptic function solutions for general boussinesq systems

Sait San* 

Rabia Altunay* 

* Eskişehir Osmangazi University, Department of Mathematics-Computer, 26480, Eskişehir-Turkey. e-mail: ssan@ogu.edu.tr


Abstract

In this research paper, we have utilized the Jacobi elliptic function expansion method to obtain the exact solutions of (1+1)- dimensional Boussinesq System (GBQS). The most important difference that distinguishes this method from other methods is the parameters included in the auxiliary equation F'(ξ)=PF4(ξ)+QF2(ξ)+R. As far as the authors know, there is no other study in which such a variety of solutions has been given. Depending on P, Q and R, nineteen the solitary wave and periodic wave solutions are obtained at their limit conditions. In addition, 3D and contour plot graphics for the constructed waves are investigated with the computer package program by giving special values to the parameters involved. The validity and reliability of the method is examined by its applications on a class of nonlinear evolution equations of special interest in nonlinear mathematical physics. The results were acquired to verify that the recommended method is applicable and reliable for the analytic treatment of a wide application of nonlinear phenomena.

Keywords: Jacobi elliptic function method; travelling wave solution; boussinesq system

1 Introduction

We consider the following family of Boussinesq type systems of water wave theory, model by Zhang et al. [1] and Chen et al. [2]

ut+uux+vx=c1uxxt,

vt+1+vu,x=c2uxxx, (1)

where v is the elevation of a water wave and u is the surface velocity of water along x-direction and c1=-(1/2)(ϕ2-(1/3)), c2=(1/2)(1-ϕ2) and ϕ is a depth of water (ϕ=0 is at the bottom, ϕ=1 is on the surface), which have the relation c1-c2=1/3. For the case c1=0,  c2=-1/3, (1) is the classical Boussinesq (cB) system is not linearly well posed in the Hadamard sense [3], it is important because it has an integrable Hamiltonian structure [4] and exact solitary-wave solutions [5-7].

This (1) is also known as Nwogu’s Boussinesq (NB) model is useful for coastal and civil engineering to perform the nonlinear water wave model in a harbour and coastal design. Therefore many scientists studied mathematical properties, such as bifurcation and travelling wave solutions, lie symmetry analysis, single and multiple solitary wave solutions and painleve analysis [8-16].

In recent years, many methods have been developed for the exact solutions of nonlinear evolution equations such as the sub-equation method, the modified trial equation method, the simplest equation method, the generalized Kudryashov method, the symmetry analysis method and so on [17-22]. The main objective of this study is to investigate new traveling wave solutions for NB model by the Jacobi elliptic function method. The effectiveness and efficiency of this method are shown in literature with the various Jacobi elliptic function forms [23-27].

The outline of the present paper is as follows. In Sec. 2, we have a brief description of the Jacobi elliptic function method for solving partial differential equations. In Sec. 3, we apply the Jacobi elliptic function method above mentioned equation. Finally, some conclusions are given the latest section.

2 Jacobi’s elliptic function method

In this section, we would like to describe extended Jacobi elliptic function method. Suppose a nonlinear partial differential equation (NPDE) with independent variables x,t and dependent variable u:

N(u,ut,ux,uxx,...)=0. (2)

Considerthe following travelling wave transformation

u(x,t)=u(ξ),ξ=x-ct, (3)

where c is an arbitrary constant to be determined later. By substituting (3) into (2), we have an ordinary differential equation (ODE):

N(u,u',u'',u''',...)=0. (4)

Let us consider the solutions in the form

u(ξ)=i=0naiFi(ξ), (5)

where F satisfies the (2) and   n   is a positive integer which can be evaluated by balancing the highest order partial derivative term and nonlinear term in (2) or (4). F(ξ) satisfies the following auxiliary equation:

F'(ξ)=PF4(ξ)+QF2(ξ)+R, (6)

where P, Q, and R   are constants. The last equation hence holds for F(ξ):

F''=2PF3+QF,F'''=6PF2+QF',F'''=24P2F5+20PQF3+(12PR+Q2)F (7)

With the help of Maple, substituting (6) into (4) along with (7) and collecting the coefficients of the same power Fi(F')j  (j=0,1,  i=0,1,2,...) and setting each of the attained coefficients to be zero we have a set of over determined algebraic equations. And after we solve this by Maple, we find P, Q, R and c. Substituting the attained results into (6), gives the exponential and periodic solutions. It is well-known that (6) has families of Jacobi elliptic function solutions as follows [28,29]:

In this Table snξ,  cnξ,  dnξ are respectively Jacobian elliptic sine function, Jacobian elliptic cosine function and the Jacobian elliptic function and the other Jacobian functions can be generated by these three kinds of functions, namely

nsξ=1snξ,    ncξ=1cnξ,    ndξ=1dnξ,    scξ=cnξsnξ,csξ=snξcnξ,    dsξ=dnξsnξ,    sdξ=snξdnξ

Case P Q R
F(ξ)
1
m2
-(1+m2)
1
snξ
2
-m2
2m2-1
1-m2
cnξ
3—4 1
-(1+m2)
m2
nsξ
5 1
-(1+m2)
m2
dcξ
6
1-m2
2-m2
1
scξ
7—8 1
2-m2
1-m2
csξ
9—10
14
1-2m22
14
nsξ±csξ
11
(1-m2)4
(1+m2)2
(1-m2)4
ncξ±scξ
12
P>0
Q<0
m2Q2(1+m2)2P
-m2Q(1+m2)Psn-Q1+m2ξ
13
P<0
Q>0
(1-m2)Q2(m2-2)2P
-Q(2-m2)PdnQ2-m2ξ
14 1
m2+2
1-2m2+m4
dnξcnξsnξ
15
-4m
6m-m2-1
-2m3+m4+m2
mcnξdnξmsn2ξ+1
16
4m
-6m-m2-1
2m3+m4+m2
mcnξdnξmsn2ξ-1
17—18
14
(1-2m2)2
14
snξ1±cnξ
19
(1-m2)4
(1+m2)2
(1-m2)4
cnξ1±snξ

Also these functions satisfying the following formulas:

sn2ξ+cn2ξ=1,dn2ξ+m2sn2ξ=1,ns2ξ=1+cs2ξ,ns2ξ=m2+m2ds2ξ,sc2ξ+1=nc2ξ,m2sd2ξ+1=nd2ξ.

And addition derivative properties,

sn'ξ=cnξdnξ,cn'ξ=-snξdnξ,dn'ξ=-m2snξcnξ.

The Jacobian-elliptic functions degenerate into hyperbolic functions when m1 as follows:

snξtanhξ,{cnξ,dnξ}ξ,{scξ,sdξ}sinhξ,{dsξ,csξ}ξ,{ncξ,ndξ}coshξ,nsξcothξ,{cdξ,dcξ}1. (8)

The Jacobian-elliptic functions degenerate into trigonometric functions when m0 as follows:

{snξ,sdξ}sinξ,{cnξ,cdξ}cosξ,scξtanξ,{nsξ,dsξ}cscξ,  {ncξ,dcξ}secξ,csξcotξ,{dnξ,ndξ}1. (9)

3 Generalized Boussinesq System (GBQS)

Suppose that the travelling wave solutions for Eq. (11) are of the forms as follows:

u(x,t)=u(ξ),v(x,t)=v(ξ),ξ=x-ct, (10)

where c is a constant to be determined later and ξ is an arbitrary constant.

ut+uux+vx=c1uxxt,

vt+1+vux=c2uxxx. (11)

By substituting (10) into (11), we have an ordinary differential equation (ODE):

-cu'+uu'+v'+cc1u'''=0,

-cv'+u'+uv'+vu'-c2u'''=0. (12)

where prime denotes differentiation with respect to ξ. Now, balancing the nonlinear terms u''' and u'u, we get m=2. Balancing the nonlinear terms u''' and uv', we get n=2. Hence, from (5), we might constitute

u(ξ)=a0+a1F(ξ)+a2F(ξ)2,

v(ξ)=b0+b1F(ξ)+b2F(ξ)2, (13)

in which a0,a1,a2,b0,b1 and b2 are undetermined constants. Substituting (13) and (6) into (12) and setting the coefficients of Fi(ξ)F'(ξ)j=0,  i=0,1,2,3,  j=0,1 to zero yields the following set of algebraic equations for a0,a1,a2,b0,b1, b2 and c:

2a22+24cc1a2P=0,

3a1a2+6cc1a1P=0,

-2ca2+a12+2a0a2+2b2+8cc1a2Q=0,

-ca1+a0a1+b1+cc1a1Q=0,

4b2a2-24c2a2P=0,

3b2a1+3b1a2-6c2a1P=0,

2a2-2cb2+2b2a0+2b1a1+2b0a2-8c2a2Q=0,

-cb1-c2a1Q+a1+b1a0+b0a1=0. (14)

Solving the set of nonlinear algebraic equations by help of Maple program, the following results are attained.

a0=-12-2c2c1+8c2c12Q-c2cc1,

a1=0,a2=-12cc1P,

b0=14-4c2c12+8c2Qc2c12+c22c2c12,

b1=0,b2=6c2P,c=c. (15)

Substituting these results into (13), we have the following solution of Eq. (16):

u(ξ)=-12-2c2c1+8c2c12Q-c2cc1-12cc1PF(ξ)2,

v(ξ)=14-4c2c12+8c2Qc2c12+c22c2c12+6c2PF(ξ)2. (16)

With the means of table and from the above solution (16), one might induce more general united Jacobian-elliptic function solutions of Eq. (12). Hereby, we attain the following exact solutions.

In the limit case when m1, we get the solitary wave solutions of Eq. (12). In the limit case when m0, we acquire the traveling wave solutions of Eq. (12).

Case 1. If we take P:m2,  Q:-(1+m2), then F(ξ)=snξ, thus

u1=-12-2c2c1+8c2c12Q-c2cc1-12cc1Psn2ξ,

v1=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Psn2ξ.

In the limit case when m1, then F(ξ)=tanhξ, and we attain one of the solitary wave solutions of Eq. (12) as

u1(x,t)=-12-2c2c1-16c2c12-c2cc1-12cc1tanh(x-ct)2,

v1(x,t)=14-4c2c12-16c2c2c12+c22c2c12+6c2tanh(x-ct)2.

Case 2. When P:-m2,  Q:(2m2-1) are chosen, then F(ξ)=cnξ, therefore

u2=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pcn2ξ,

v2=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pcn2ξ.

Considering m1, then F(ξ)=sechξ, and one of the solitary wave solutions of Eq. (12) has been obtained as

u2(x,t)=-12-2c2c1+8c2c12-c2cc1+12cc1 sech (x-ct)2,

v2(x,t)=14-4c2c12+8c2c2c12+c22c2c12-6c2 sech (x-ct)2.

Case 3. Choosing P:1,  Q:-(1+m2), it may be denoted from table F(ξ)=nsξ, hence

u3=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pns2ξ,

v3=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pns2ξ.

As m1, then F(ξ)=cothξ, and one of the solitary wave solutions of Eq. (12) can be stated as

u3(x,t)=-12-2c2c1-16c2c12-c2cc1-12cc1coth(x-ct)2,

v3(x,t)=14-16c2c2c12-4c2c12+c22c2c12+6c2coth(x-ct)2.

Case 4. Supposing P:1,  Q:-(1+m2) from table this choices correspond to F(ξ)=nsξ, hence

u3=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pns2ξ,

v3=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pns2ξ.

For m0 from (9), F(ξ)=cscξ, and we acquire one of the periodic solutions of Eq. (12) as

u4(x,t)=-12-2c2c1-8c2c12-c2cc1-12cc1csc(x-ct)2,

v4(x,t)=14-4c2c12-8c2c2c12+c22c2c12+6c2csc(x-ct)2.

Case 5. Considering P:1,  Q:-(1+m2) from (9) F(ξ)=dcξ, hence

u5=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pdc2ξ,

v5=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pdc2ξ.

If m0, then F(ξ)=secξ, and one of the periodic solutions of Eq. (12) has been attained as

u5(x,t)=-12-2c2c1-8c2c12-c2cc1-12cc1sec(x-ct)2,

v5(x,t)=14-8c2c2c12-4c2c12+c22c2c12+6c2sec(x-ct)2.

Case 6. If we get P:1-m2,  Q:2-m2, then F(ξ)=scξ, therefore

u6=-12-2c2c1+8c2c12Q-c2cc1-12cc1Psc2ξ,

v6=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Psc2ξ.

As long as m0,F(ξ)=tanξ, and we obtain one of the traveling wave solutions of Eq. (12) as

u6(x,t)=-12-2c2c1+16c2c12-c2cc1-12cc1tan(x-ct)2,

v6(x,t)=14-4c2c12+16c2c2c12+c22c2c12+6c2tan(x-ct)2.

Case 7. For choices P:1,Q:(2-m2) from table, F is obtained as F(ξ)=csξ, in this way the solution may be expressed as

u7=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pcs2ξ,

v7=14-4c2c12+8c2c2c12+c22c2c12+6c2Pcs2ξ.

Moreover, for m1 from(8), F(ξ)=cschξ, and one of the solitary wave solutions of Eq. (12) can be found as

u7(x,t)=-12-2c2c1+8c2c12-c2cc1-12cc1csch(x-ct)2,

v7(x,t)=14-4c2c12+8c2c2c12+c22c2c12+6c2csch(x-ct)2.

Case 8. Setting P:1,Q:(2-m2), then F(ξ)=csξ, due to this settings,

u8=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pcs2ξ,

v8=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pcs2ξ.

Furthermore, for m0 by using from (9) ,F(ξ)=cotξ, and we attain one of the traveling wave solutions of Eq. (12) as

u8(x,t)=-12-2c2c1+16c2c12-c2cc1-12cc1cot(x-ct)2,

v8(x,t)=14-4c2c12+16c2c2c12+c22c2c12+6c2cot(x-ct)2.

Case 9. If we take P=(1/4),Q=(1-2m2/2) it may be deducted from table, F(ξ)=nsξ±csξ, therefore

u9=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pnsξ±csξ2,

v9=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pnsξ±csξ2.

In this case for m1,F(ξ)=cothξ±cschξ, and one of the solitary wave solutions of Eq. (12) can be shown as

u9(x,t)=-12-2c2c1-4c2c12-c2cc1-3cc1(coth(x-ct)±csch(x-ct))2,

v9(x,t)=14-4c2c12-4c2c2c12+c22c2c12+32c2(coth(x-ct)±csch(x-ct))2.

Case 10. Regarding P=1/4, Q=1-2m2/2, then F(ξ)=nsξ±csξ, so

u10=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pnsξ±csξ2,

v10=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pnsξ±csξ2.

In addition, for m0,F(ξ)=cscξ±cotξ, and the periodic solution of Eq. (12) can be obtained as

u10(x,t)=-12-2c2c1+4c2c12-c2cc1-3cc1(csc(x-ct)±cot(x-ct))2,

v10(x,t)=14-4c2c12+4c2c2c12+c22c2c12+32c2(csc(x-ct)±cot(x-ct))2.

Case 11. Assigning P=(1-m2)/4,Q=(1+m2)/2, then F(ξ)=ncξ±scξ, hence

u11=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pnsξ±csξ2,

v11=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pnsξ±csξ2.

In the limit case when m0,F(ξ)=secξ±tanξ, and the periodic solution of Eq. (12) can be written as

u11(x,t)=-12-2c2c1+4c2c12-c2cc1-3cc1sec((x-ct)±tan(x-ct))2,

v11(x,t)=14-4c2c12+4c2c2c12+c22c2c12+32c2sec((x-ct)±tan(x-ct))2.

Case 12. If we choose P>0, Q<0 from table, F(ξ)=-m2Q/(1+m2)Psn-Q/(1+m2)ξ, so

u12=-12-2c2c1+8c2c12Q-c2cc1-12cc1-m2Q(1+m2)sn2-Q1+m2ξ,

v12=14-4c2c12+8c2Qc2c12+c22c2c12+6c2-m2Q(1+m2)sn2-Q1+m2ξ.

In the limit case when m1,F(ξ)=(-m2Q)/([1+m2]P)tanh-Q/(1+m2)ξ, and the solitary wave solution of Eq. (12) can be stated as

u12(x,t)=-12-2c2c1+8c2c12Q-c2cc1+6cc1Qtanh12-2Q(x-ct)2,

v12(x,t)=14-4c2c12+8c2c2Qc12+c22c2c12-3c2Qtanh12-2Q(x-ct)2.

Case 13. For choices P<0, Q>0, then F(ξ)=-Q/(2-m2)PdnQ/(2-m2)ξ, hence

u13=-12-2c2c1+8c2c12Q-c2cc1-12cc1-Q(2-m2)dn2Q2-m2ξ,

v13=14-4c2c12+8c2Qc2c12+c22c2c12+6c2-Q(2-m2)dn2Q2-m2ξ.

In the limit case when m1, F(ξ)=-Q/([2-m2]P)Q/(2-m2)ξ, and we get one of the solitary wave solutions of Eq. (12) as

u13(x,t)=-12-2c2c1+8c2c12Q-c2cc1+12cc1Qsech(Q(x-ct))2,

v13(x,t)=14-4c2c12+8c2c2Qc12+c22c2c12-6c2Qsech(Q(x-ct))2.

Case 14. While P=1, Q=m2+2, then F(ξ)=dnξcnξ/snξ, therefore

u14=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pdn2ξcn2ξsn2ξ,

v14=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pdn2ξcn2ξsn2ξ.

In the limit case when m0,F(ξ)=cosξ/sinξ, and one of the traveling wave solutions of Eq. (12) can be evaluated as

u14(x,t)=-12-2c2c1+16c2c12-c2cc1+12cc1cos2(x-ct)sin2(x-ct),

v14(x,t)=14-4c2c12+16c2c2c12+c22c2c12+6c2cos2(x-ct)sin2(x-ct).

Case 15. When P=-4/m, Q=6m-m2-1, then F(ξ)=mdnξcnξ/(msn2ξ+1), hence

u15=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pm2dn2ξcn2ξm2(sn2ξ+1)2,

v15=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pm2dn2ξcn2ξm2(sn2ξ+1)2.

As long as m1,F(ξ)=msechξsechξ/(mtanhξ tanhξ+1), and we get one of the solitary wave solutions of Eq. (12) as

u15(x,t)=-12-2c2c1+32c2c12-c2cc1+48cc1sech4(x-ct)(tanh2(x-ct)+1)2,

v15(x,t)=14-4c2c12+32c2c2c12+c22c2c12-24c2sech4(x-ct)(tanh2(x-ct)+1)2.

Case 16. Setting P=4/m, Q:-6m-m2-1, then F(ξ)=mdnξcnξ/(msn2ξ-1), so

u16=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pm2dn2ξcn2ξm2(sn2ξ-1)2,

v16=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pm2dn2ξcn2ξm2(sn2ξ-1)2.

When m1, F(ξ)=msechξsechξ/(mtanhξtanhξ-1), and we obtain one of the solitary wave solutions of Eq. (12) as

u16(x,t)=-12-2c2c1-64c2c12-c2cc1-48cc1sech4(x-ct)(tanh2(x-ct)-1)2,

v16(x,t)=14-4c2c12-64c2c2c12+c22c2c12+24c2sech4(x-ct)(tanh2(x-ct)-1)2.

Case 17. If we get P=1/4, Q=(1-2m2)/2, then F(ξ)=snξ/(1±cnξ), hence

u17=-12-2c2c1+8c2c12Q-c2cc1-12cc1Psn2ξ(1±cnξ)2,

v17=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Psn2ξ(1±cnξ)2.

If m1, F(ξ)=tanhξ/(1±sechξ), and one of the solitary wave solutions of Eq. (12) can be stated as

u17(x,t)=-12-2c2c1-4c2c12-c2cc1-3cc1tanh2(x-ct)(1±sech(x-ct))2,

v17(x,t)=14-4c2c12-4c2c2c12+c22c2c12+3c2tanh2(x-ct)2(1±sech(x-ct))2.

Case 18. Supposing P=1/4,Q=(1-2m2)/2, then F(ξ)=snξ/(1±cnξ), therefore

u18=-12-2c2c1+8c2c12Q-c2cc1-12cc1Psn2ξ(1±cnξ)2,

v18=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Psn2ξ(1±cnξ)2.

For m0,F(ξ)=sinξ/(1±cosξ), and the travelling wave solution of Eq. (12) can be obtained as

u18(x,t)=-12-2c2c1+4c2c12-c2cc1-3cc1sin2(x-ct)(1±cos(x-ct))2,

v18(x,t)=14-4c2c12+4c2c2c12+c22c2c12+3c2sin2(x-ct)2(1±cos(x-ct))2.

Case 19. If we get P=(1-m2)/4, Q=(1+m2)/2, then F(ξ)=cnξ/(1±snξ), hence

u19=-12-2c2c1+8c2c12Q-c2cc1-12cc1Pcn2ξ(1±snξ)2,

v19=14-4c2c12+8c2Qc2c12+c22c2c12+6c2Pcn2ξ(1±snξ)2.

In the limit case when m0, F(ξ)=cosξ/(1±sinξ), and the travelling wave solutions of Eq.(12) can be attained as

u19x,t=-12-2c2c1+4c2c12-c2cc1-3cc1cos2x-ct(1±sin(x-ct))2,

v19(x,t)=14-4c2c12+4c2c2c12+c22c2c12+3c2cos2(x-ct)2(1±sin(x-ct))2.

4 Discussions

The dynamical behaviour of constructed solutions shows the different soliton type solutions. We obtained some important soliton solutions and profiles of the solutions is as follows: Figure 1, shows the physical structure of single soliton with parameters, c=c1=c2=1. Figure 2, exhibits the physical structure of shock wave soliton with parameters, c=c1=c2=1. Figure 3, represents the physical structure of periodic wave solution with parameters, c=c1=c2=1. Figure 4, shows the physical structure of shock wave solution with parameters, c=c1=c2=1. Figure 5, shows the physical structure of periodic wave solution with parameters, c=c1=c2=1. Comparing with the results in [1,2], we obtained more comprehensive solutions. As our knowledge, the results have not been previously reported. We expect that the results will be used future studies. In future work, conservation laws, which have a very important role in physics, can be obtained by group invariant analysis method. Also complexton and interactive solutions can be considered by various methods.

Figure 1 The figures represent the single solitonsolutions u1(x,t) and v1(x,t) with respectively 3-dimensional plots and contour plots when c=c1=c2=1 and x,t=-5,5×[-2,2].  

Figure 2. The figures represent the shock wave soliton solutions u3(x,t) and v3(x,t) with respectively 3-dimensional plots and contour plots, when c=c1=c2=1 and x,t=-5,5×[-2,2].  

Figure 3. The figures represent the periodic wave solutions u4(x,t) and v4(x,t) with respectively 3-dimensional plots and contour plots, when c=c1=c2=1 and x,t=-5,5×[-2,2].  

Figure 4. The figures represent the shock wave soliton solutions u9(x,t) and v9(x,t) with respectively 3-dimensional plots and contour plots, c=c1=c2=1 and x,t=-5,5×[-2,2].  

Figure 5. The figures represent the periodic wave solutions u10(x,t) and v10(x,t) with respectively 3-dimensional plots and contour plots, when c=c1=c2=1 and x,t=-5,5×[-2,2].  

5 Conclusion

In this article we considered the (1+1)-dimensional Boussinesq System which were encountered in real world application problems such as coastal and civil engineering, harbour and coastal design. Jacobi elliptic function method were applied to investigate the traveling wave solutions of the governing system. By means of this method we have constructed exact solutions for nineteen cases. These solutions including trigonometric and hyperbolic functions and original to our knowledge. The hyperbolic solutions (including solitary wave solution) and trigonometric-function solutions of Eq. (12) can be attained in the limited case when the modulus m1 and m0 respectively. All solutions were verified Maple package program by putting them back into the original equation. Taking the parameters with special values, we presented 3-D and contour graphs of the Jacobi elliptic function solutions of the underlying equation. (Figs.1-5) The algorithm is very applicative and influential to investigate many solutions, therefore it might be also applied to many other nonlinear differential equations in mathematical physics.

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How to Cite. S. SAN, “Extended Jacobi elliptic function solutions for general boussinesq systems”, Rev. Mex. Fís., vol. 69, no. 2 Mar-Apr, pp. 021401 1-, Mar. 2023.

Received: November 25, 2021; Accepted: June 27, 2022

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