Let , assumed finite. The displacement is . By stationarity, its two-time covariance is , with even for a real scalar process. Integrating over the two triangles of the square gives the Taylor turbulent dispersion identity
A sufficient condition for ordinary long-time variance growth is with . The dominated convergence theorem then gives
More generally the necessary asymptotic condition for a finite positive variance-based diffusion coefficient is convergence of to that coefficient. Absolute integrability is sufficient, not necessary. A zero integral does not give nondegenerate ordinary diffusion. Moreover a second-moment calculation alone does not establish a normal distribution or an entire diffusive scaling limit; those require additional probabilistic assumptions.
For the specified positive autocorrelation, direct integration gives, when ,
Thus the power-law velocity-correlation dispersion has the following regimes. If , the Lagrangian integral time is and ordinary variance growth holds, with . At the exact expression is . If ,
For ,
The last two regimes spread faster than ordinary diffusion and have no finite long-time diffusion coefficient. Their slowly decaying velocity memory is responsible. At short times all these correlations instead give the ballistic law .
Take and initially . Write , and set , . The advection-diffusion equation is . Integration by parts in the unbounded coordinate gives the longitudinal moment hierarchy for shear transport
All three moments obey Neumann boundary conditions at the walls. The initial values are , , . These manipulations require finite moments and vanishing boundary terms at ; diffusion of the compact initial distribution supplies the required decay for positive time.
The zeroth moment remains exactly . Since is a Neumann eigenfunction, put . Then and , giving
For the second moment, . Thus , with
The equation for has positive damping and bounded forcing, so remains bounded. In the equation for , the decaying term in contributes only a bounded accumulated transient. Over a complete nonzero-frequency cycle, and . Consequently
This proves oscillating shear dispersion in an insulating channel, including the local-in- leading term, not just a cross-channel average. The instantaneous derivative retains bounded periodic oscillations; its cycle-averaged slope is . Thus is the leading second moment, rather than a literal rate proportional to .
The asymptotic statement holds for fixed positive diffusivity and fixed nonzero frequency, after times long compared with and the oscillation period. If , transverse diffusion adjusts rapidly to the changing shear flow, and
This is the cycle average of the instantaneous steady-shear enhancement . At exactly , there is no cycle average: and . Hence the zero-frequency and long-time limits do not commute. In the intermediate range , the shear is approximately steady at its initial amplitude and that latter enhancement is appropriate.

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