ConceptComplete

The Wave Equation - Examples and Constructions

Explicit solutions to the wave equation provide insight into wave behavior and serve as building blocks for more complex solutions through superposition.

ExampleD'Alembert's Solution (1D)

The general solution to the one-dimensional wave equation utt=c2uxxu_{tt} = c^2 u_{xx} is: u(x,t)=F(x−ct)+G(x+ct)u(x,t) = F(x - ct) + G(x + ct) where FF and GG are arbitrary twice-differentiable functions representing right-moving and left-moving waves, respectively.

Given initial conditions u(x,0)=f(x)u(x,0) = f(x) and ut(x,0)=g(x)u_t(x,0) = g(x), the solution is: u(x,t)=12[f(x−ct)+f(x+ct)]+12câˆĢx−ctx+ctg(s) dsu(x,t) = \frac{1}{2}[f(x-ct) + f(x+ct)] + \frac{1}{2c}\int_{x-ct}^{x+ct} g(s)\,ds

This is D'Alembert's formula, showing how initial displacement and velocity evolve into traveling waves.

ExampleStanding Waves

For a string fixed at both ends (x=0x = 0 and x=Lx = L), separation of variables u(x,t)=X(x)T(t)u(x,t) = X(x)T(t) yields: un(x,t)=sin⁥(nĪ€xL)[Ancos⁥(nĪ€ctL)+Bnsin⁥(nĪ€ctL)]u_n(x,t) = \sin\left(\frac{n\pi x}{L}\right)\left[A_n\cos\left(\frac{n\pi ct}{L}\right) + B_n\sin\left(\frac{n\pi ct}{L}\right)\right]

These are normal modes with frequencies Ήn=nĪ€cL\omega_n = \frac{n\pi c}{L}. The general solution is a superposition: u(x,t)=∑n=1∞un(x,t)u(x,t) = \sum_{n=1}^\infty u_n(x,t)

ExampleSpherical Waves (3D)

In three dimensions with spherical symmetry, setting v=ruv = ru transforms the wave equation to: vtt=c2vrrv_{tt} = c^2 v_{rr}

D'Alembert's solution gives: u(r,t)=F(r−ct)r+G(r+ct)ru(r,t) = \frac{F(r - ct)}{r} + \frac{G(r + ct)}{r}

The first term represents an outgoing spherical wave, the second an incoming wave. The 1/r1/r decay reflects energy spreading over expanding spherical surfaces.

Remark

The method of images extends these solutions to domains with boundaries. For a semi-infinite domain x>0x > 0:

  • Dirichlet boundary condition u(0,t)=0u(0,t) = 0: Use odd extension of initial data
  • Neumann boundary condition ux(0,t)=0u_x(0,t) = 0: Use even extension of initial data
ExamplePlane Wave Solutions

The plane wave u(x,t)=Acos⁥(k⋅xâˆ’Ī‰t+Ī•)u(x,t) = A\cos(\mathbf{k} \cdot \mathbf{x} - \omega t + \phi) is a solution if the dispersion relation Ή=câˆŖkâˆŖ\omega = c|\mathbf{k}| holds, where k\mathbf{k} is the wave vector. These solutions are fundamental in Fourier analysis of wave phenomena.

These explicit solutions demonstrate key wave phenomena: traveling waves, standing waves, dispersion, and the superposition principle. They form the foundation for understanding more complex wave behavior in realistic systems.