We study analytically and numerically the corrections to scaling in tu
rbulence which arise due to finite size effects as anisotropic forcing
or boundary conditions at large scales. We find that the deviations d
eltazeta(m) from the classical Kolmogorov scaling zeta(m) = m/3 of the
velocity moments [\u(k)\m] is-proportional-to k(-zeta)m decrease like
deltazeta(m)(Re) = c(m) Re-3/10. If, on the contrary, anomalous scali
ng in the inertial subrange can experimentally be verified in the larg
e Re limit, this will support the suggestion that small scale structur
es should be responsible, originating from viscous effects either in t
he bulk (vortex tubes or sheets) or from the boundary layers (plumes o
r swirls), as both are underestimated in our reduced wave vector set a
pproximation of the Navier-Stokes dynamics.