Kortewege de Vries equation

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In summary, the Kortewege de Vries equation is a significant equation used to study wave-like solutions. It is often compared to the Navier-Stokes equation, but the physical interpretation of its terms is still debated. The Sine-Gordon equation also exhibits wave-like solutions, with theta representing the amplitude of swinging pendulums connected by springs. The terms in the KdV equation may have a similar origin, but this remains a subject of further research.
  • #1
kurious
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In the Kortewege de Vries equation what is the physical origin of the
linear and non-linear terms? I'm thinking of the explanation of a water wave here.What properties of the water molecules cause the profile and stability of the wave?
 
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  • #2
Not familiar with that equation, but I am guessing that the molecule's dipole has something to do with this.

Edit : A quick search showed how important it was. It seems soliton solutions were actually discovered with it. Is water is the only material substance capable of this? (not counting solitons in light propagation)
 
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  • #3
The KdV equation is very important indeed, and one can find many references on it. Unfortunately, I don't know any which provides an actual physical interpretation for the several terms. At least not in a satisfactory manner. I also think that the exact same story goes for the Navier-Stockes equation. Everybody agree : it is a very important equation. But nobody agree on the interpretation of the several terms.

This is a very interesting question though. I wish someone will soon pop-up with a good answer.
 
  • #4
Another eqn which admits stable (no dispersion) wave-like solutions is the Sine-Gordon-Eq:

D'Alembert(theta) + Sin(theta) = 0
(using suitable units)
[theta = theta(space,time), of cours]

This theta can be visualized as follows:

Consider a chain of pendulums, each being elastically connected on the top to its neighbours by springs. Theta measures the amplitude of "swinging"
of each pendulum (therefore function of space and time).
They swing in the usual way in the normal gravitational field: therefore the potential term Sin(theta).
The other term in the Sine-Gordon-EQN, namley the differential operator, comes from the continuum-limit of the elastic force modeled here by springs between the pendulums, as in the usual Klein-Gordon-EQN, or in every other harmonic oszilator.

Maybe the terms in the KdV-eqn have a similar origin.
 

1. What is the Kortewege de Vries equation?

The Kortewege de Vries equation is a mathematical model used to describe the behavior of long, one-dimensional waves in certain physical systems, such as water waves or nerve impulses in the brain. It was first proposed by Dutch mathematicians Diederik Korteweg and Gustav de Vries in 1895.

2. What are the key features of the Kortewege de Vries equation?

The Kortewege de Vries equation is a nonlinear partial differential equation that describes the evolution of a wave's amplitude and shape over time. It takes into account both dispersive and nonlinear effects, and can model both solitary waves (solitons) and periodic waves.

3. What are some real-world applications of the Kortewege de Vries equation?

The Kortewege de Vries equation has been used to study a variety of physical phenomena, including water waves, ion-acoustic waves in plasmas, and electromagnetic waves in optical fibers. It has also been used in the fields of neuroscience, biology, and fluid dynamics.

4. How is the Kortewege de Vries equation solved?

The Kortewege de Vries equation can be solved using a variety of mathematical techniques, including the inverse scattering transform, the Hirota bilinear method, and numerical methods such as finite difference or spectral methods. The choice of method depends on the specific problem and the desired level of accuracy.

5. What are the limitations of the Kortewege de Vries equation?

The Kortewege de Vries equation is a simplified model that does not take into account certain physical effects, such as dissipation and external forces. It is also limited to one-dimensional systems and cannot accurately model waves in more complex geometries. Additionally, the equation may not accurately describe highly nonlinear or dispersive waves.

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