Skip to main content Accessibility help
×
Hostname: page-component-7bb8b95d7b-cx56b Total loading time: 0 Render date: 2024-09-05T06:16:14.666Z Has data issue: false hasContentIssue false

Appendix to Chapter I

Published online by Cambridge University Press:  07 September 2010

Get access

Summary

Ao.—EXPRESSION IN GENERALIZED CO-ORDINATES FOR POISSON's EXTENSION OF LAPLACE's EQUATION.

(a) In § 491 (c) below is to be found Poisson's extension of Laplace's equation, expressed in rectilineal rectangular co-ordinates ; and in § 492 an equivalent in a form quite independent of the particular kind of co-ordinates chosen : all with reference to the theory of attraction according to the Newtonian law. The same analysis is largely applicable through a great range of physical mathematics, including hydro-kinematics (the “ equation of continuity” §192), the equilibrium of elastic solids (§734), the vibrations of elastic solids and fluids (Vol. II.), Fourier's theory of heat, &c. Hence detaching the analytical subject from particular physical applications, consider the equation

where p is a given function of x, y, z, (arbitrary and discontinuous it may be). Let it be required to express in terms of generalized co-ordinates, the property of U which this equation expresses in terms of rectangular rectilinear co-ordinates. This may be done of course directly [§ (m) below] by analytical transformation, finding the expression in terms of, for the operation. But it is done in the form most convenient for physical applications much more easily as follows, by taking advantage of the formula of § 492 which expresses the same property of U independently of any particular system of co-ordinates. This expression is

where ∬dS denotes integration over the whole of a closed surface S, ∭ dB integration throughout the volume B enclosed by it, and δU the rate of variation of U at any point of S, per unit of length in the direction of the normal outwards.

(b) For B take an infinitely small curvilineal parallelepiped having its centre at (£, £', £“), and angular points at

Let be the lengths of the edges of the parallelepiped, and a, a', a” the angles between them in order of symmetry, so that R'R” sin, are the areas of its faces.

Let DU, D'U D“U denote the rates of,variation of U, per unit of length, perpendicular to the three surfaces £= const., £' = const., £” = const., intersecting in (£,£', £“) the centre of the parallelepiped.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2009
First published in: 1883

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
×