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Basics of Fluid Mechanics, 2014a

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562 CHAPTER 13. MULTI–PHASE FLOW<br />

Equation (13.76) can be integrated twice to yield<br />

U G = ΔP<br />

μ G L x2 + C 1 x + C 2 (13.77)<br />

This velocity pr<strong>of</strong>ile must satisfy zero velocity at the right wall. The velocity at the<br />

interface is the same as the liquid phase velocity or the shear stress are equal. Mathematically<br />

these boundary conditions are<br />

and<br />

U G (x = D) =0 (13.78)<br />

U G (x = h) =U L (x = h) (a) or (13.79)<br />

τ G (x = h) =τ L (x = h)<br />

(b)<br />

Applying B.C. (13.78) into equation (13.77) results in<br />

U G =0= ΔP<br />

μ G L D2 + C 1 D + C 2 (13.80)<br />

↩→ C 2 = − ΔP<br />

μ G L D2 + C 1 D<br />

Which leads to<br />

U G = ΔP<br />

μ G L<br />

(<br />

x 2 − D 2) + C 1 (x − D) (13.81)<br />

At the other boundary condition, equation (13.79)(a), becomes<br />

ρ L gh 2<br />

= ΔP (<br />

h 2 − D 2) + C 1 (h − D) (13.82)<br />

6 μ L μ G L<br />

The last integration constant, C 1 can be evaluated as<br />

C 1 =<br />

ρ L gh 2 ΔP (h + D)<br />

−<br />

6 μ L (h − D) μ G L<br />

(13.83)<br />

With the integration constants evaluated, the gas velocity pr<strong>of</strong>ile is<br />

U G = ΔP<br />

μ G L<br />

(<br />

x 2 − D 2) + ρ L gh 2 (x − D)<br />

6 μ L (h − D)<br />

−<br />

ΔP (h + D)(x − D)<br />

μ G L<br />

(13.84)<br />

The velocity in Equation (13.84) is equal to the velocity equation (13.64) when (x = h).<br />

However, in that case, it is easy to show that the gas shear stress is not equal to the<br />

liquid shear stress at the interface (when the velocities are assumed to be the equal).<br />

The difference in shear stresses at the interface due to this assumption, <strong>of</strong> the equal<br />

velocities, cause this assumption to be not physical.

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