I am not sure to have fully understood your question ...Are you considering U as Reynolds averaged? Then
(uu)bar= UU + (u'u')bar you will model (u'u')bar as supplementary eddy viscosity tensor Td but it must be zero traced. Therefore, you decompose in isotropic and deviatoric tensors Td=(1/3)I *Trace(Td) + Td0 For incompressible flows, the isotropic part is simply summed to the pressure and you solve for a global scalar field whose gradients ensure the divergence-free velocity. Sorry if I did not get the right meaning of your question ... |
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