Using velocity fields obtained in direct numerical simulations of turb
ulent convection and of turbulent channel flow, the energy transfer pr
ocess among lateral scales of motion in these low Reynolds number flow
s is analyzed. In all cases the energy is transferred most effectively
between scales of similar size. As a result, the subgrid-scale energy
transfer is caused almost exclusively by interactions between resolve
d scales and subgrid scales characterized by wave numbers not greater
than twice the cutoff wave number. The scale dependence of forward and
inverse energy transfers contributing to the total subgrid-scale eddy
viscosity is discussed. The local energy transfer between small scale
s is strongly affected by the nonlocal interactions characterized by a
scale separation greater than a factor of 2 in wave number. However,
the direct energy transfer between scales satisfying this condition is
one order of magnitude less than the local energy transfer between sc
ales of similar size.