For the established time-periodic response, take a complex separated solution and set . The diffusion equation gives . For , define the penetration depth ; the spatial roots are . Decay at infinity selectsIts real part is the solution of Stokes' second problem:The velocity amplitude decays exponentially, while the phase lags by . Direct substitution verifies the diffusion equation, and the two boundary conditions follow immediately.
These data select a unique periodic response, but do not specify an arbitrary initial transient. With no initial velocity supplied, one may add any suitable solution of the homogeneous-boundary diffusion problem. The displayed solution is the usual established oscillatory flow after transients have decayed.
Separate variables as . The zero values at both plates give the Fourier sine basisExpand the initial profile using orthogonality. With , its coefficients areConsequentlyOnly odd modes occur because the initial profile is symmetric about the midpoint. The coefficients are absolutely summable, so dominated convergence gives uniformly as . The slowest decay rate is , associated with .
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