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Vorticity Transport in Turbulent Flows

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or∂ ? + u ⋅ ∇?= ? ⋅∇u+ ν∇2 ?∂t∂ ? + u ⋅ ∇?= d ⋅ ? + ν∇2 ?∂t(9)(10)where d is the deformation rate tensor.Dur<strong>in</strong>g a turbulent motion u and ? become random functions of space and time,and they may be decomposed <strong>in</strong>to a mean and fluctuat<strong>in</strong>g parts. i.e.,u = U + u′, Ui= ui, u′ i= 0 , (11)? = O + ? ′ , O = ? , ? ′ = 0 , (12)where U and O are the mean quantities and u ' and ?' are the fluctuat<strong>in</strong>g parts. As wasnoted before, a bar on the top of the letter stands for the (time) averaged quantity.Substitut<strong>in</strong>g (11) and (12) <strong>in</strong>to Equation (10) after averag<strong>in</strong>g we f<strong>in</strong>d the meanvorticity transport equation. That is∂Ω∂ti+ Uj∂Ω∂xji∂ω′iu′j= −∂xj∂ω′ju′i+∂xj+ Ωj∂U∂xij2∂ Ωi+ ν∂x∂xjj(13)Subtract<strong>in</strong>g (13) from (10) leads to the equation for the vorticity fluctuation field. That is∂ω′i∂t+ Uj∂ω′i= −u′j∂xj∂Ω∂xij− u′j∂ω′∂xij+ Ω d′jij+ ω′ Djij+ ω′ d′jij2∂ ω′i+ ν∂x∂xjj∂ω′iu′j+∂xj− ω′ d′jij(14)Equation (14) may be used to derive the mean square vorticity or dissipation ratetransport equations.ME6372G. Ahmadi

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