Mathematical Problems in Engineering

Volume 2009, Article ID 925187, 5 pages

http://dx.doi.org/10.1155/2009/925187

## Generalized Variational Principle for Long Water-Wave Equation by He's Semi-Inverse Method

^{1}Department of Mathematics, Jiaying University, Meizhou, Guangdong 514015, China^{2}Nonlinear Scientific Research Center, Faculty of Science, Jiangsu University, Zhenjiang, Jiangsu 212013, China

Received 4 February 2009; Accepted 7 March 2009

Academic Editor: Ji Huan He

Copyright © 2009 Weimin Zhang. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

#### Abstract

Variational principles for nonlinear partial differential equations have come to play an important role in mathematics and physics. However, it is well known that not every nonlinear partial differential equation admits a variational formula. In this paper, He's semi-inverse method is used to construct a family of variational principles for the long water-wave problem.

#### 1. Introduction

In this paper we apply He’s semi-inverse method [1–12] to establish a family of variational formulations for the following higher-order long water-wave equations:

When , equations (1.1) and (1.2) were investigated in [13], but the generalized variational approach for the discussed problem has not been dealt with.

#### 2. Variational Formulation

We rewrite (1.1) and (1.2) in conservation forms:

According to (1.1) or (2.1) we can introduce a special function defined as

Similarly from (1.2) or (2.2) we can introduce another special function defined as

Our aim in this paper is to establish some variational formulations whose stationary conditions satisfy (1.1), (2.5), or (1.2), (2.3), and (2.4). To this end, we will apply He’s semi-inverse method to construct a trial functional:

where is a trial Lagrangian defined as

where is an unknown function of , and/or their derivatives. The advantage of the above trial Lagrangian is that the stationary condition with respect to is one of the governing equations (2.2) or (1.2).

Calculating the above functional equation (2.6) stationary with respect to and , we obtain the followimg Euler-Lagrange equations:

where is called He’s variational derivative [14–17] with respect to , which was first sugested by He in [2], defined as

We search for such an so that (2.8) is equivalent to (2.3), and (2.9) is equivalent to (2.4). So in view of (2.3) and (2.4), we set

from (2.11), the unknown can be determined as

Finally we obtain the following needed variational formulation:

*Proof. *Making the above functional equation (2.13) stationary with respect to , , and , we obtain the following Euler-Lagrange equations:
Equation (2.14) is equivalent to (1.2), and (2.15) is equivalent to (2.4); in view of (2.4), (2.16) becomes (2.3).

Similary we can also begin with the following trial Lagrangian:

It is obvious that the stationary condition with respect to is equivalent to (2.1) or (1.1). Now the Euler-Lagrange equations with respect to and are

In view of (2.5), we have

From (2.19), the unknown function can be determined as

Therefore, we obtain another needed variational formulation:

#### 3. Conclusion

We establish a family of variational formulations for the long water-wave problem using He’s semi-inverse method. It is shown that the method is a powerful tool to the search for variational principles for nonlinear physical problems directly from field equations without using Lagrange multiplier. The result obtained in this paper might find some potential applications in future.

#### Acknowledgments

The author is deeply grateful to the referee for the valuable remarks on improving the paper.

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