Wave Phenomena and Wave Equations
Gerd Leuchs, Mojdeh S. Najafabadi
TL;DR
The paper addresses how to derive the wave equation for different wave phenomena from experimentally determined dispersion relations using a plane-wave form $f(t,\vec{x}) = e^{-i\omega t + i\sum_l k_l x_l}$. It demonstrates a general mapping $g(\omega,k_1,k_2,k_3)=0$ to a differential operator by substituting $i\,\partial_t$ for $\omega$ and $-i\,\partial_{x_l}$ for $k_l$, and illustrates this with light, water waves, and matter waves. For deep-water gravity waves the dispersion $\omega^2 = gk$ leads to a 1D wave equation featuring an imaginary unit and a two-real-component description of surface motion, while for matter waves the dispersion $\omega = \frac{\hbar}{2m}k^2 + C$ yields the Schrödinger equation $i\hbar\partial_t\Psi = -\frac{\hbar^2}{2m}\Delta\Psi + V\Psi$ upon the usual operator substitutions. The discussion emphasizes that the dispersion relation fixes only the mathematical structure of the wave equation and not the physical interpretation of the wave function, highlighting interpretational questions for coherent matter waves and the two-dimensional character seen in water waves.
Abstract
For any kind of wave phenomenon one can find ways to derive the respective dispersion relation from experimental observations and measurements. This dispersion relation determines the structure of the wave equation and thus characterizes the dynamics of the respective wave. Different wave phenomena are thus governed by different differential equations. Here we want to emphasize the experimental approach to matter waves, but before doing so we will discuss and test the procedure for other types of waves, in particular water waves.
