Abstract
The dependence on the lateral distance y to the center-plane and on time t of the average of the scalar dissipation rate chi = 2D vertical bar del Z vertical bar(2) conditioned on the scalar Z has been investigated in a temporally-evolving shear layer using a direct numerical simulation. As the inviscid scaling of the unconditional mean dissipation rate is approached, the conditional mean (chi) over barz follows also an approximate self-similar behavior within the time interval considered in the simulations and (chi) over barz shows two strong peaks at a distance of about one vorticity thickness from the center-plane, with dissipation values about 3 times the one in the central region. It is showed that this spatial variation is introduced by the nonturbulent/turbulent transition regions, which are identified by means of gradient trajectories of the scalar field.
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