Skip to main content Accessibility help
×
Hostname: page-component-78c5997874-t5tsf Total loading time: 0 Render date: 2024-11-16T17:22:32.705Z Has data issue: false hasContentIssue false

6 - Centrifugal stability

Published online by Cambridge University Press:  06 July 2010

W. O. Criminale
Affiliation:
University of Washington
T. L. Jackson
Affiliation:
University of Illinois, Urbana-Champaign
R. D. Joslin
Affiliation:
Office of Naval Research, Arlington
Get access

Summary

Polar coordinates

As has been mentioned earlier, there are many flows that require the formulation of the stability problem to be cast in coordinate systems other than Cartesian. For example, pipe flow is perhaps the most notable example. Then, there is the case that is now referred to as stability of Couette flow and has been examined both theoretically and experimentally by Taylor (1921, 1923). In this case, concentric cylinders rotate relative to each other to produce the flow. Free flows, such as the jet and wake, can be thought of as round rather than plane. If the boundary layer occurs on a curved wall, then Görtler vortices result. All of these examples can be described in terms of polar coordinates. And, at the outset, it should be recognized that, not only will the governing mathematics be different from that that has been used up to this point but the resulting physics may have novel characteristics as well.

The prevailing basis for the flows that have been examined heretofore has been that the flows are parallel or almost parallel. Then, the solutions for the disturbances were all of the form of plane waves that propagate in the direction of the mean flow or, more generally, obliquely to the mean flow. And, as we have learned, if solid boundaries are present in the flow, viscosity is a cause for instability. Now there are flows that will have curved streamlines and this leads to the possibility of a centrifugal force and its influence must be considered.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2003

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.)

Save book to Kindle

To save this book to your Kindle, first ensure [email protected] is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×