Reynolds decomposition

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In

.

Decomposition

For example, for a quantity ${\displaystyle u}$ the decomposition would be

$${\displaystyle u(x,y,z,t)={\overline {u(x,y,z)}}+u'(x,y,z,t)}$$

where ${\displaystyle {\overline {u}}}$ denotes the expectation value of ${\displaystyle u}$, (often called the steady component/time, spatial or

ensemble average

), and ${\displaystyle u'}$, are the deviations from the expectation value (or fluctuations). The fluctuations are defined as the expectation value subtracted from quantity ${\displaystyle u}$ such that their

The expected value, ${\displaystyle {\overline {u}}}$, is often found from an ensemble average which is an average taken over multiple experiments under identical conditions. The expected value is also sometime denoted ${\displaystyle \langle u\rangle }$, but it is also seen often with the over-bar notation.[3]

Direct numerical simulation, or resolution of the Navier–Stokes equations completely in ${\displaystyle (x,y,z,t)}$, is only possible on extremely fine computational grids and small time steps even when Reynolds numbers are low, and becomes prohibitively computationally expensive at high Reynolds' numbers. Due to computational constraints, simplifications of the Navier-Stokes equations are useful to parameterize turbulence that are smaller than the computational grid, allowing larger computational domains.^[4]

Reynolds decomposition allows the simplification of the Navier–Stokes equations by substituting in the sum of the steady component and perturbations to the velocity profile and taking the

See also

• Reynolds-averaged Navier–Stokes equations

References