Skip to main content Accessibility help
×
Hostname: page-component-848d4c4894-xfwgj Total loading time: 0 Render date: 2024-06-17T02:36:21.087Z Has data issue: false hasContentIssue false

11 - Fluid Motion in Precessing Circular Cylinders

from Part 3 - Precession and Libration in Non-uniformly Rotating Systems

Published online by Cambridge University Press:  26 May 2017

Keke Zhang
Affiliation:
University of Exeter
Xinhao Liao
Affiliation:
Chinese Academy of Sciences
Get access

Summary

Formulation

Consider a viscous, incompressible, and homogeneous [in Equation (1.10)] fluid without the influence of an external force [f0 in Equation (1.10)] occupying a circular cylinder of radius and length d with aspect ratio. The cylinder, as depicted in Figure 11.1, rotates rapidly with an angular velocity, where

is constant, about its axis of symmetry and precesses slowly with an angular velocity that is fixed in an inertial frame (i.e., at an angle α, 0 < απ/2. In comparison to a precessing sphere or spheroid, it is the extra geometric parameter that enriches the dynamics of fluid motion in precessing cylinders.

We shall adopt cylindrical polar coordinates with s=0 representing the symmetry axis and z = 0 at the bottom surface along with the corresponding unit vectors fixed in the cylinder. In these coordinates, the precession vector is time-dependent in the form

where denotes the amplitude of the precession vector. It follows that the Poincaré forcing, required on the right-hand side of Equation (1.10), is

On inserting the expression for the overall angular velocity and into Equation (1.10), the equation of motion in the mantle or body frame governing the processionally driven flow in a circular cylinder reads as

where p is the reduced pressure containing all the gradient terms. The last term on the righthand side represents the Poincaré forcing which drives precessional flows against viscous dissipation.

On employing the depth d as the length scale, as the unit of time and as the unit of pressure, we obtain the dimensionless equations in the mantle frame describing fluid motion in a precessing cylinder

In the mantle frame of reference, the flow on the bounding surface S of a precessing cylinder is at rest, imposing

on the bottom z = 0 as well as on the top z = 1, and

on the sidewall.

Type
Chapter
Information
Theory and Modeling of Rotating Fluids
Convection, Inertial Waves and Precession
, pp. 164 - 212
Publisher: Cambridge University Press
Print publication year: 2017

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 coreplatform@cambridge.org 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
×