Conditional averages of the velocity field, subgrid-scale (SGS) stress
es and SGS dissipation are calculated using the velocity fields obtain
ed from the DNS of plane channel flow. The detection criteria isolate
the coherent turbulent structures that contribute most strongly to the
energy transfer between the large, resolved scales and the subgrid, u
nresolved, ones. Separate averages are computed for forward and backwa
rd scatter. The interscale energy transfer is found to be strongly cor
related with the presence of the turbulent structures typical of wall-
bounded flows: quasi-streamwise and hairpin vortices, sweeps and eject
ions. In the buffer layer, strong SGS dissipation is observed near lif
ted shear layers; the forward scatter is associated with ejections, th
e backscatter with sweeps. Both backward and forward scatter occur in
close proximity to longitudinal vortices that form a very shallow angl
e to the wall. Further away from the solid boundary, in the logarithmi
c region and beyond, both forward and backward energy transfer are ass
ociated prevalently with ejections. Eddy viscosity models do not predi
ct the three-dimensional structure of these events adequately, while s
cale-similar models reproduce the correlation between the large-scale
coherent structures and the SGS events more accurately. (C) 1996 Ameri
can Institute of Physics.