Dispersive media split wave speed into phase and group velocity

Evidence

Equation 1.11 is significantly different from that for quasi-longitudinal and transverse shear waves. In particular, the velocity is now frequency dependent and increases with frequency. This results in dispersive propagation of waves with different frequencies traveling at different velocities. Therefore waveshape is not preserved in bending wave propagation. One can hear the effect of this if one listens to the “chirp” sound emitted by ice covering a pond when hit by a thrown rock. The dispersion and the fourth root arise because, unlike quasi-longitudinal and transverse shear waves, the spatial derivatives in the wave equation are fourth order instead of second order because the bending wave is an amalgam of longitudinal and transverse waves. — David M. Howard, Jamie Angus, Acoustics and Psychoacoustics, 128 (#expands, via linked claim)

Categorization

Category: Causal Relationships

Broader Connections