Author:
DRAAD A. A.,NIEUWSTADT F. T. M.
Abstract
A pipe flow facility with a length of 32 m and a diameter of 40
mm has been designed
in which a laminar flow of water can be maintained for Reynolds numbers
up to
60 000. Velocity measurements taken in this facility show an asymmetric
velocity
profile both in the vertical as well as horizontal direction with velocities
that deviate
strongly from the parabolic Hagen–Poiseuille profile. The cause of
this asymmetry is
traced back to the influence of the Earth's rotation. This is confirmed
by means of
a comparison of the experimental data with the results from a perturbation
solution
and from a numerical computation of the full nonlinear Navier–Stokes
equations. The
physical background of this unforeseen result lies in the fact that a Hagen–Poiseuille
flow is governed by a force equilibrium and inertia forces are everywhere
negligible.
This implies that the Coriolis force can be balanced only by a viscous
force. So even
the small Coriolis force due to the Earth's rotation causes a large
velocity distortion
for a case such as ours where the kinematic viscosity is small.
Publisher
Cambridge University Press (CUP)
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics
Cited by
29 articles.
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