Large-eddy simulations corresponding to the decaying isotropic turbule
nce experiment of Comte-Bellot and Corrsin are performed, using a pseu
do-spectral code that incorporates four models: viscosity and hypervis
cosity types, each implemented for both the subgrid scale stress tenso
r and the subgrid scale force. Two 1/T scalings are also considered fo
r the viscosity amplitude. The dynamic procedure is extended to the fo
ur models and is tested. Results are obtained with and without this pr
ocedure and for both scalings. The main conclusions are: (a) the two v
iscosity models perform equally well; (b) the Kolmogorov scaling perfo
rms as well as the Smagorinsky scaling, yet it is computationally more
efficient; (c) in the dynamic procedure, there is a fairly wide range
of test to grid filter ratios which produces results insensitive to t
his ratio; and (d) the hyperviscosity models lead to energy decay curv
es that follow the experimental data as well as the usual viscosity mo
dels.