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Dispersion Relation

Frequency domain analysis is extremely revealing in the case of the wave equation in particular. Considering the case of a string defined over the spatial domain $ {\mathcal D}={\mathbb{R}}$, a Fourier transform (in space) and a two-sided Laplace transform (in time) may be used. See Chapter 5 for more details. As a short-cut, one may analyze the behaviour of the test solution

$\displaystyle u(x,y) = e^{st+j\beta x}$ (6.6)

where $ s$ is interpreted as a complex frequency variable, $ s = \sigma + j\omega$, and $ \beta$ is a real wavenumber. It is easy to see that if $ \sigma = 0$, such a test solution is, in fact a traveling wave of temporal frequency $ f = \omega/2\pi$, and wavelength $ \lambda = 2\pi/\beta$. Substituting such a solution into (6.2) gives

$\displaystyle (s^2+\gamma^2\beta^2)u = 0$ (6.7)

Clearly the test solution $ u$ is non-zero everywhere, leading the characteristic equation

$\displaystyle s^2+\gamma^2\beta^2 = 0$ (6.8)

which has roots

$\displaystyle s = \pm j\gamma\beta\qquad \Longrightarrow\qquad \omega = \pm \gamma\beta$ (6.9)

This is known as the dispersion relation for the system (6.2); the frequency and wavenumber of a plane-wave solution are not independent. The fact that there are two solutions results from the fact that the wave equation is second order in time--the solutions correspond to left-going and right-going wave solutions.


next up previous contents index
Next: Phase and Group Velocity Up: Definition Previous: Initial Conditions   Contents   Index
Stefan Bilbao 2006-11-15