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The effect of a non-zero Lagrangian time scale on bounded shear dispersion
Published online by Cambridge University Press: 13 December 2011
Abstract
Previous studies of shear dispersion in bounded velocity fields have assumed random velocities with zero Lagrangian time scale (i.e. velocities are -function correlated in time). However, many turbulent (geophysical and engineering) flows with mean velocity shear exist where the Lagrangian time scale is non-zero. Here, the longitudinal (along-flow) shear-induced diffusivity in a two-dimensional bounded velocity field is derived for random velocities with non-zero Lagrangian time scale
. A non-zero
results in two-time transverse (across-flow) displacements that are correlated even for large (relative to the diffusive time scale
) times. The longitudinal (along-flow) shear-induced diffusivity
is derived, accurate for all
, using a Lagrangian method where the velocity field is periodically extended to infinity so that unbounded transverse particle spreading statistics can be used to determine
. The non-dimensionalized
depends on time and two parameters: the ratio of Lagrangian to diffusive time scales
and the release location. Using a parabolic velocity profile, these dependencies are explored numerically and through asymptotic analysis. The large-time
is enhanced relative to the classic Taylor diffusivity, and this enhancement increases with
. At moderate
this enhancement is approximately a factor of 3. For classic shear dispersion with
, the diffusive time scale
determines the time dependence and large-time limit of the shear-induced diffusivity. In contrast, for sufficiently large
, a shear time scale
, anticipated by a simple analysis of the particle’s domain-crossing time, determines both the
time dependence and the large-time limit. In addition, the scalings for turbulent shear dispersion are recovered from the large-time
using properties of wall-bounded turbulence.
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- Copyright © Cambridge University Press 2011 The online version of this article is published within an Open Access environment subject to the conditions of the Creative Commons Attribution-NonCommercial-ShareAlike licence <http://creativecommons.org/licenses/by-nc-sa/2.5/>. The written permission of Cambridge University Press must be obtained for commercial re-use.
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