This talk deals with probability density function (pdf) of longitudina
l velocity differences, namely delta upsilon = upsilon(r)(x + r)-upsil
on(r)(x) where upsilon(r) is the component of the velocity upsilon alo
ng r. These pdfs evolve from a gaussian shape for large scales r, to a
strongly non gaussian one with reinforced tails (intermittency) for r
dose to the dissipative length. Recently some light was put on this e
volution by a theory which takes into account the finite value of the
Reynolds number. In some sense, intermittency could be a finite Reynol
ds effect.