Bretherton equation

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In mathematics, the Bretherton equation is a nonlinear partial differential equation introduced by Francis Bretherton in 1964:[1]

utt+uxx+uxxxx+u=up,

with p integer and p2. While ut,ux and uxx denote partial derivatives of the scalar field u(x,t).

The original equation studied by Bretherton has quadratic nonlinearity, p=2. Nayfeh treats the case p=3 with two different methods: Whitham's averaged Lagrangian method and the method of multiple scales.[2]

The Bretherton equation is a model equation for studying weakly-nonlinear wave dispersion. It has been used to study the interaction of harmonics by nonlinear resonance.[3][4] Bretherton obtained analytic solutions in terms of Jacobi elliptic functions.[1][5]

Variational formulations

The Bretherton equation derives from the Lagrangian density:[6]

=12(ut)2+12(ux)212(uxx)212u2+1p+1up+1

through the Euler–Lagrange equation:

t(ut)+x(ux)2x2(uxx)u=0.

The equation can also be formulated as a Hamiltonian system:[7]

utδHδv=0,vt+δHδu=0,

in terms of functional derivatives involving the Hamiltonian H:

H(u,v)=(u,v;x,t)dx   and   (u,v;x,t)=12v212(ux)2+12(uxx)2+12u21p+1up+1

with the Hamiltonian density – consequently v=ut. The Hamiltonian H is the total energy of the system, and is conserved over time.[7][8]

Notes

  1. 1.0 1.1 (Bretherton 1964)
  2. (Nayfeh 2004)
  3. (Drazin Reid)
  4. Hammack, J.L.; Henderson, D.M. (1993), "Resonant interactions among surface water waves", Annual Review of Fluid Mechanics 25: 55–97, doi:10.1146/annurev.fl.25.010193.000415, Bibcode1993AnRFM..25...55H 
  5. (Kudryashov 1991)
  6. (Nayfeh 2004)
  7. 7.0 7.1 Levandosky, S.P. (1998), "Decay estimates for fourth order wave equations", Journal of Differential Equations 143 (2): 360–413, doi:10.1006/jdeq.1997.3369, Bibcode1998JDE...143..360L 
  8. Esfahani, A. (2011), "Traveling wave solutions for generalized Bretherton equation", Communications in Theoretical Physics 55 (3): 381–386, doi:10.1088/0253-6102/55/3/01, Bibcode2011CoTPh..55..381A 

References