The most general form for the rapid pressure-strain rate, within the c
ontext of classical Reynolds-stress transport (RST) closures for homog
eneous flows, is derived, and truncated forms are obtained with the ai
d of rapid distortion theory. By a classical RST-closure we here denot
e a model with transport equations for the Reynolds stress tensor and
the total dissipation rate. It is demonstrated that all earlier models
for the rapid pressure-strain rate within the class of classical Reyn
olds-stress closures can be formulated as subsets of the general form
derived here. Direct numerical simulations were used to show that the
dependence on flow parameters, such as the turbulent Reynolds number,
is small, allowing rapid distortion theory to be used for the determin
ation of model parameters. It was shown that such a nonlinear descript
ion, of fourth order in the Reynolds-stress anisotropy tensor, is quit
e sufficient to very accurately model the rapid pressure-strain in all
cases of irrotational mean flows, but also to get reasonable predicti
ons in, for example, a rapid homogeneous shear flow. Also, the respons
e of a sudden change in the orientation of the principal axes of a pla
ne strain is investigated for the present model and models proposed in
the literature. Inherent restrictions on the predictive capability of
Reynolds-stress closures for rotational effects are identified.