M. Ulitsky et Lr. Collins, On constructing realizable, conservative mixed scalar equations using the eddy-damped quasi-normal Markovian theory, J FLUID MEC, 412, 2000, pp. 303-329
The eddy-damped quasi-normal Markovian (EDQNM) turbulence theory has been a
pplied to the covariance spectrum of two passive isotropic scalers with dif
ferent diffusivities in stationary isotropic turbulence A rigorous applicat
ion of EDQNM, which introduces no new modelling assumptions or constants, i
s shown to yield a covariance spectrum that violates the Cauchy-Schwartz in
equality over some of the wavenumbers. One approach to this problem is to d
erive a model based on a stochastic differential equation, as its presence
guarantees realizability. For an isotropic scalar, it is possible to constr
uct a Langevin equation for the Fourier transform of the scalar concentrati
ons that is consistent with each EDQNM scalar autocorrelation spectrum. The
Langevin equations can then be used to construct a model for the covarianc
e spectrum that is realizable. However, the resulting covariance transfer t
erm does not properly conserve the scalar covariance, and so the model is s
till not satisfactory. The problem can be traced to the Markovianization st
ep, which leads to the presence of the scalar diffusivities in the transfer
functions in an unphysical fashion. A simple fix is described which reconc
iles the two approaches and gives conservative, realizable results for all
time.
Next, we apply the EDQNM theory to a more general system involving the mixi
ng of anisotropic scalars. Anisotropy in this case results from a uniform m
ean gradient of the two scalar concentrations in one direction. As with the
isotropic scalars, direct application of the EDQNM closure results in a co
variance spectrum that violates the Cauchy-Schwartz inequality; however, in
this case it is not as simple to construct a Langevin model that reproduce
s all of the spectral interactions that result from the EDQNM procedure. Ne
vertheless, we show that the same modification of the inverse time scale as
is done for the isotropic scalar results in an anisotropic scalar covarian
ce spectrum that is realizable for all times.