Consider steady Poiseuille flow through a control volume with a circular cross section with radius
R, perimeter P , cross-sectional area A, and differential length dz. Assume a pressure gradient with
magnitude
is present. Write the net pressure on the control volume in terms of A, dz, and
. Write
the wall shear stress in terms of R and
. The sum of these forces is zero at equilibrium. Given this,
write the relation between R, A, and P .
For a circle, the relation between R, A, and P follows directly from geometry, and the analysis above
was not necessary. However, for a channel of unknown geometry but known A and P , the above
analysis allows us to derive the hydraulic radius rh.
Repeat the above analysis for a cross-section of unknown geometry but known A and P . To do this
analysis, you will have to assume that the surface stress is uniform, and define it as τ = 
. What is
the value of rh in terms of A and P ?
This analysis shows that the key approximation associated with using the hydraulic radius is the
assumption that the wall shear stress is uniform along the perimeter of the channel. For what
geometries is this assumption good? For what geometries is this assumption bad?