Skip Navigation

The Quarterly Journal of Mechanics and Applied Mathematics 1981 34(3):361-381; doi:10.1093/qjmam/34.3.361
© 1981 by Oxford University Press
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Add to My Personal Archive
Right arrow Download to citation manager
Right arrowRequest Permissions
Google Scholar
Right arrow Articles by DENNIS, S. C. R.
Right arrow Articles by SINGH, S. N.
Right arrow Search for Related Content
Social Bookmarking
 Add to CiteULike   Add to Connotea   Add to Del.icio.us  
What's this?

THE STEADY FLOW OF A VISCOUS FLUID DUE TO A ROTATING SPHERE

S. C. R. DENNIS1, D. B. INGHAM2 and S. N. SINGH3

( 1Department of Applied Mathematics, University of Western Ontario London, Canada
2Department of Applied Mathematical Studies, University of Leeds Leeds, England
3Department of Mechanical Engineering, University of Kentucky Lexington, Kentucky, U.S.A. )

The viscous, incompressible, rotationally symmetric flow due to a sphere rotating with a constant angular velocity about a diameter is investigated. The equations of motion can be written in the form of three coupled, nonlinear, elliptic partial differential equations. These equations are expressed in finite-difference form using a specialized technique which is everywhere second-order accurate. Solutions of the finite-difference equations are presented for Reynolds numbers in the range 1 to 5000. No difficulties were encountered in obtaining numerical solutions at values of the Reynolds number higher than 5000, but in these cases the mesh size used was too crude to deal adequately with the boundary layers which form on the sphere.

The numerical results show how the theories which exist at both low and high Reynolds numbers are being approached. There is excellent agreement with previous numerical solutions up to a Reynolds number of 100 and with experimental results over the whole range of Reynolds numbers considered. The equatorial jet which develops with increasing Reynolds number agrees well with that predicted theoretically using the boundary-layer approximations. In the range considered there is no separation of the flow near the equator and the results give no indication that it is likely to occur at higher values of the Reynolds number.


Add to CiteULike CiteULike   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us    What's this?




Disclaimer:
Please note that abstracts for content published before 1996 were created through digital scanning and may therefore not exactly replicate the text of the original print issues. All efforts have been made to ensure accuracy, but the Publisher will not be held responsible for any remaining inaccuracies. If you require any further clarification, please contact our Customer Services Department.