KdV Equation - weakly nonlinear weakly disspersive

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In summary, the KdV equation describes small amplitude shallow water waves that are both weakly nonlinear and weakly dispersive. This means that the wave amplitude must be small for the equation to accurately model large solitons. However, it is possible to numerically model these solitons. Solitons are stable, nonlinear pulses that exhibit a balance between nonlinearity and dispersion. The KdV equation can also be derived in 3D, known as the KP equation.
  • #1
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Hi guys,

I have been reading up on the KdV equation and everywhere it states that the waves need to be 'weakly nonlinear and weakly disspersive.' From a physical point of view does this mean that the wave amplitude must be small?

If that is the case how would one model large solitons numerically? Or would that be impossible?

Thanks in advance.
 
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  • #2
The blurb in Arnold's "Mathematical Methods of Classical Mechanics" notes that the equation first arose by considering waves in shallow water, but doesn't state any restrictions on the general solution.

Boyd's "nonlinear optics" has a section on solitions- solitions occur when the self-phase modulation cancels group-velocity dispersion-but again does not require anything to be 'small'.

What's your book?
 
  • #3
The KdV equation equation is derived under the assumption of shallow water and small amplitude.
 
  • #4
The correct term for a wave which is localized and retains its form over a long period of time is: solitary wave. However, a soliton is a solitary wave having the additional property that other solitons can pass through it without changing its shape. But, in the literature it is customary to refer to the solitary wave as a soliton, although this is strictly incorrect. Solitons are stable, nonlinear pulses which exhibit a fine balance between non-linearity and dispersion.

The KdV equation is the most famous solitary wave equation which describes small amplitude shallow water waves in a channel. It is interesting to note that, a KdV solitary wave in water that experiences a change in depth will retain its general shape. However, on encountering shallower water its velocity and height will increase and its width decrease; whereas, on encountering deeper water its velocity and height will decrease and its width increases.
 
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  • #5
It is possible to derive a KdV equation in 3D as well, this is usually called the KP equation.
 

1. What is the KdV equation?

The Korteweg-de Vries (KdV) equation is a partial differential equation that describes the propagation of long, weakly nonlinear, and weakly dispersive waves in a continuous medium. It was first derived in the late 19th century to describe the behavior of shallow water waves, but it has since found applications in various fields such as fluid dynamics, plasma physics, and nonlinear optics.

2. What does "weakly nonlinear" mean in the context of the KdV equation?

"Weakly nonlinear" refers to the assumption that the amplitude of the waves described by the KdV equation is small compared to the characteristic length scale of the system. This allows for the use of perturbation methods to solve the equation and obtain approximate solutions.

3. How is the KdV equation different from other nonlinear wave equations?

The KdV equation is unique in that it allows for the formation and propagation of solitons, which are localized, stable, and non-dispersive wave solutions. This is due to the balance between nonlinear and dispersive effects in the equation, which leads to the formation of solitary waves that can maintain their shape and speed as they travel.

4. What are some applications of the KdV equation?

The KdV equation has been used to model a wide range of physical phenomena, such as shallow water waves, surface waves in fluids, ion-acoustic waves in plasmas, and light pulses in optical fibers. It has also been applied in the study of turbulence and chaos, as well as in the field of mathematical biology to describe the propagation of nerve impulses in neurons.

5. What are the limitations of the KdV equation?

While the KdV equation is a powerful tool for studying weakly nonlinear and weakly dispersive waves, it does have some limitations. For instance, it cannot accurately describe highly nonlinear or highly dispersive waves. Additionally, it assumes a one-dimensional or quasi-one-dimensional system, which may not be applicable in all cases. Researchers have developed extensions and modifications of the KdV equation to overcome some of these limitations and improve its applicability.

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