Waves Bundle Comparison Access

For an ideal flexible string, ( \omega = v|k| ) (linear, nondispersive).

wave packet, dispersion, group velocity, Schrödinger equation, electromagnetic pulse, mechanical wave 1. Introduction A wave bundle (or wave packet) is a superposition of multiple sinusoidal waves with slightly different frequencies and wavenumbers, resulting in a spatially and temporally localized disturbance. From a stone dropped in water to a femtosecond laser pulse and an electron’s probability density, wave bundles are ubiquitous.

[ \psi(x,t) = \frac1\sqrt2\pi \int_-\infty^\infty A(k) , e^i(kx - \omega(k)t) , dk ] waves bundle comparison

[ \omega = c|k| \quad \text(linear, nondispersive) ]

However, real mechanical systems (e.g., deep-water waves) do exhibit dispersion (( \omega \propto \sqrtk )), making them analogous to quantum systems in spreading behavior. Similarly, EM pulses in dispersive media spread. Thus, the key distinction is not mechanical vs. quantum but . For an ideal flexible string, ( \omega =

If ( \omega(k) ) is linear in ( k ), the bundle propagates without distortion. If nonlinear, the envelope spreads over time. Governing equation: 1D wave equation [ \frac\partial^2 y\partial t^2 = v^2 \frac\partial^2 y\partial x^2, \quad v = \sqrtT/\mu ] where ( T ) = tension, ( \mu ) = linear density.

Starting from Gaussian wave packet at ( t=0 ): [ \psi(x,0) = \left( \frac12\pi\sigma_0^2 \right)^1/4 e^-x^2/(4\sigma_0^2) e^ik_0x ] Fourier transform gives ( A(k) \propto e^-\sigma_0^2 (k-k_0)^2 ). Using ( \omega = \hbar k^2/(2m) ), integrate to get [ |\psi(x,t)|^2 = \frac1\sqrt2\pi , \sigma(t) e^-(x - v_g t)^2/(2\sigma(t)^2), \quad \sigma(t) = \sigma_0 \sqrt1 + \left( \frac\hbar t2m\sigma_0^2 \right)^2 ] Hence width grows unbounded as ( t \to \infty ). ∎ From a stone dropped in water to a

[ \omega(k) = \frac\hbar k^22m \quad \text(quadratic, dispersive) ]