Effect of Turbulent Fluctuations on Mean Flow: Reynolds-Averaging In a turbulent flow, we can define the mean, steady flow as: T 1 u ( x, y , z ) = lim ∫ u ( x, y , z , t )dt T →∞ T 0 This allows us to split the flow properties into a mean and a fluctuating part: u ( x, y , z , t ) = u ( x, y , z ) + u′( x, y , z, t ) v ( x, y , z , t ) = v ( x, y , z ) + v′( x, y , z, t ) w( x, y , z, t ) = w( x, y , z ) + w′( x, y , z, t ) p ( x, y , z , t ) = p ( x, y , z ) + p′( x, y , z, t ) mean part turbulent fluctuating part Note: the mean of u ′ is zero: u − u = u′ 1 T →∞ T lim T 0 T T 1 u′dt T →∞ T ∫ 0 ∫ {u − u }dt = lim 1 lim ∫ udt − u = u′ T 0 T →∞ u ⇒ − u = u′ uN =0 ⇒ u′ = 0 ⇐ mean of fluctuations is zero. Now, we will develop equations which govern the mean flow and try to develop some insight into how the fluctuations alter the mean flow equations. Let’s start with incompressible flow and look at the x − momentum: x − momentum: ∂ 2u ∂ 2u ∂ 2u 1 ∂p ∂u ∂u ∂u ∂u +u +v +w =− +ν 2 + 2 + 2 ρ ∂x ∂t ∂x ∂y ∂z ∂y ∂z ∂x Let’s look at the “averaging” of this equation in time to develop an equation for the mean flow. Effect of Turbulent Fluctuations on Mean Flow: Reynolds-Averaging ⇒ 1 T →∞ T lim T ∫ [ x − mom]dt or 0 x − mom time-average of x-momentum The first term is: 1 ∂u 1 ∂ (u + u′) lim ∫ dt = lim ∫ dt T →∞ T T →∞ T ∂t ∂t 0 0 T But, T ∂u = 0 thus: ∂t T T ∂u′ 1 ∂u 1 ∂u′ = dt dt = lim ∫ ∫ T →∞ T T →∞ T ∂t ∂t T 0→∂t∞ 0 lim Just as u′ = 0 , we will assume ∂u ′ = 0. ∂t End result: ∂u =0 ∂t Let’s skip over to the pressure term and look at its average: ∂p ∂p ∂p′ ∂p ∂p ∂p′ = + ⇒ = + ∂x ∂x ∂x ∂x ∂x ∂x ∂p ∂p ∂p′ = + ∂x ∂x ∂x ∂p ∂p ∂p′ = + ∂x ∂x ∂x But, p ′ = 0 thus: ∂p ∂p = ∂x ∂x Similarly, ∂ 2u ∂ 2u ∂ 2u ∂ 2u ∂ 2u ∂ 2u + + = + + ∂x 2 ∂y 2 ∂z 2 ∂x 2 ∂y 2 ∂z 2 16.100 2002 2 Effect of Turbulent Fluctuations on Mean Flow: Reynolds-Averaging Combining these into x − mom , we now have: ∂ 2u ∂ 2u ∂ 2u 1 ∂p ∂u ∂u ∂u u +v +w =− +ν 2 + 2 + 2 ∂x ∂y ∂z ∂y ∂z ρ ∂x ∂x must still work this out Let’s work out the last term: u ∂u ∂u ∂u ∂u ∂u ∂u +w +v =u +w +v ∂z ∂y ∂x ∂z ∂y ∂x That’s the easy part. Now, consider u Question: What does u a) u ∂u ∂x b) u ∂u′ ∂u + u′ ∂x ∂x c) u ∂u ∂u ′ + u′ ∂x ∂x d) none of the above 16.100 2002 ∂u : ∂x ∂u equal in terms of u & u′ only? ∂x 3