
We calculate the term of the variant equation estab-
lished as the following
U(
ξ
) = a0+a1f(
ξ
) + b1g(
ξ
),
a0is arbitrary. Using
G(
ξ
) = A1sinh
ξ
+A2cosh
ξ
−
µ
,
and
f(
ξ
) = G′
G,g(
ξ
) = 1
G.
We have the exact solution
u22 =a0+a1
A1cosh(Vt −x) + A2sinh(V t −x)
A1sinh(Vt −x) + A2cosh(Vt −x)
−c11
−A1sinh(Vt −x) + A2cosh(Vt −x),
where
a1=3V2−1
2V,c1=±3A2
1−A2
2+
µ
2V2−1
2V.
where V,A1,A2are arbitrary constants. The solution
u22, Traveling wave solution, is illustrated in Figure
5 (Appendix).
All the analytic solutions attained corresponding to
Eq. (1.1), and Eq. (1.2) have been exactly substituted
for checking satisfaction.
5 Conclusion
By utilizing the prevalent (G’/G,1/G)-method, the hy-
perbolic function solutions of the Benney-Luke equa-
tion, and the extended Benney-Luke equation have
been found and illustrated in both two and three di-
mensions. The (G’/G,1/G)-method has supported the
variety of solutions of the Benney-Luke equation that
are meaningful in studying the propagation of the wa-
ter wave surface. Compared to previous studies, the
present method has attained a new form of kink-type
solutions, and traveling wave solutions that play a sig-
nificant role in studying the water surface tensions.
Acknowledgment:
The authors acknowledge the anonymous reviewer’s
comments, which improve the manuscript’s quality,
and kindly provide advice and valuable discussions.
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WSEAS TRANSACTIONS on MATHEMATICS
DOI: 10.37394/23206.2024.23.29
Nguyen Minh Tuan, Sanoe Koonprasert,
Sekson Sirisubtawee, Phayung Meesad, Nattawut Khansai