In fluid dynamics, the Reynolds stress is the component of the total stress tensor in a fluid obtained from the averaging operation over the Navier–Stokes equations to account for turbulent fluctuations in fluid momentum.
Definition The velocity field of a flow can be split into a mean part and a fluctuating part using Reynolds decomposition. We write
u i = u i ¯ + u i ′ , {\displaystyle u_{i}={\overline {u_{i}}}+u_{i}',\,}
with u ( x , t ) {\displaystyle \mathbf {u} (\mathbf {x} ,t)} being the flow velocity vector having components u i {\displaystyle u_{i}} in the x i {\displaystyle x_{i}} coordinate direction (with x i {\displaystyle x_{i}} denoting the components of the coordinate vector x {\displaystyle \mathbf {x} } ). The mean velocities u i ¯ {\displaystyle {\overline {u_{i}}}} are determined by either time averaging, spatial averaging or ensemble averaging, depending on the flow under study. Further u i ′ {\displaystyle u'_{i}} denotes the fluctuating (turbulence) part of the velocity. We consider a homogeneous fluid, whose density ρ is taken to be a constant. For such a fluid, the components τ'ij of the Reynolds stress tensor are defined as:
τ i j ′ ≡ ρ u i ′ u j ′ ¯ , {\displaystyle \tau '_{ij}\equiv \rho \,{\overline {u'_{i}\,u'_{j}}},\,}
Another – often used – definition, for constant density, of the Reynolds stress components is:
τ i j ″ ≡ u i ′ u j ′ ¯ , {\displaystyle \tau ''_{ij}\equiv {\overline {u'_{i}\,u'_{j}}},\,}
which has the dimensions of velocity squared, instead of stress.
Averaging and the Reynolds stress To illustrate, Cartesian vector index notation is used. For simplicity, consider an incompressible fluid: Given the fluid velocity u i {\displaystyle u_{i}} as a function of position and time, write the average fluid velocity as u i ¯ {\displaystyle {\overline {u_{i}}}} , and the velocity fluctuation is u i ′ {\displaystyle u'_{i}} . Then u i = u i ¯ + u i ′ {\displaystyle u_{i}={\overline {u_{i}}}+u'_{i}} . The conventional ensemble rules of averaging are that
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