Hostname: page-component-7b7567c8c-kwt9d Total loading time: 0 Render date: 2026-11-13T15:38:13.151Z Has data issue: false hasContentIssue false

Flow between rotating disks. Part 1. Basic flow

Published online by Cambridge University Press:  20 April 2006

A. Z. Szeri
Affiliation:
Department of Mechanical Engineering, The University of Pittsburgh, Pittsburgh, PA 15261
S. J. Schneider
Affiliation:
Department of Mechanical Engineering, The University of Pittsburgh, Pittsburgh, PA 15261
F. Labbe
Affiliation:
Department of Mechanical Engineering, The University of Pittsburgh, Pittsburgh, PA 15261
H. N. Kaufman
Affiliation:
Department of Mechanical Engineering, The University of Pittsburgh, Pittsburgh, PA 15261Research and Development Center, Westinghouse Electric Co., Beulah Rd, Pittsburgh PA 15235

Abstract

Laser-Doppler velocity measurements were obtained in water between finite rotating disks, with and without throughflow, in four cases: ω1 = ω2 = 0; ω2/ω1 = −1; ω2/ω1 = 0; ω2/ω1 = 1. The equilibrium flows are unique, and at mid-radius they show a high degree of independence from boundary conditions in r. With one disk rotating and the other stationary, this mid-radius ‘limiting flow’ is recognized as the Batchelor profile of infinite-disk theory. Other profiles, predicted by this theory to coexist with the Batchelor profile, were neither observed experimentally nor were they calculated numerically by the finite-disk solutions, obtained here via a Galerkin, B-spline formulation. Agreement on velocity between numerical results and experimental data is good at large values of the ratio RQ/Re, where RQ = Q/2πνs is the throughflow Reynolds number and Re = R22ω/ν is the rotational Reynolds number.

Information

Type
Research Article
Copyright
© 1983 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Article purchase

Temporarily unavailable