“…Meanwhile, the differential operators are defined as u x � (zu/zx), u t � (zu/zt), u txx � (z 3 u/ zt zx 2 ), u xx � (z 2 u/zx 2 ), and u xxx � (z 3 u/zx 3 ). Particularly, when k � λ � c � 0 and a � 1, equation (1) is the wellknown completely integrable dispersive shallow water wave equation, noted as the Camassa-Holm (C-H) equation [1][2][3][4][5][6], that was firstly reckoned as a bi-Hamiltonian partial differential equation by Fokas and Fuchssteiner [7], which possesses infinitely many conservation laws. When λ � 0, equation (1) is the Dullin-Gottwald-Holm (D-G-H) equation [8,9] derived by asymptotic expansion in the shallow water regime, from the Hamiltonian for Euler's equation and also shown to be bi-Hamiltonian.…”