Skip to main content Accessibility help
×
Hostname: page-component-848d4c4894-pftt2 Total loading time: 0 Render date: 2024-06-01T02:51:33.949Z Has data issue: false hasContentIssue false

3 - Structure of vibrated powders – numerical results

Published online by Cambridge University Press:  06 October 2009

Anita Mehta
Affiliation:
Harvard University, Massachusetts
Get access

Summary

A microscopic description which focuses on the essential discreteness of grains is a fundamental part of understanding many fascinating features of a granular medium. Its response to vibration can be understood in terms of the competition between individual-particle and cooperative dynamical mechanisms intrinsic to the grains in a disordered assembly. We present below computer simulation results for some features of granular structure which depend only weakly on details of grain size or material, e.g. the finite range for the packing fraction or shaking-induced size segregation.

Details of simulation algorithm

In this section, we describe the details of the simulations first reported in. Simulations are performed for a bed of monodisperse hard spheres above a hard base at z = 0. The granular bed is periodic, with a repeat distance of L sphere diameters in two perpendicular directions x and y in the plane. Each primary simulation cell contains N spheres. A unidirectional gravitational field acts downwards, i.e. along the negative z-direction. Initially, spheres are placed in the cell using a sequential random close-packing procedure; the packing is then subjected to a series of nonsequential N-particle reorganisations. Each reorganisation is performed in three parts: first, a vertical expansion or dilation, second, a Monte Carlo consolidation, and finally a nonsequential close-packing procedure. We call each full reorganisation a shake cycle or, simply, a shake. The duration of model shaking processes as well as the lengths of other time intervals are measured in units of the shake cycle.

Type
Chapter
Information
Granular Physics , pp. 27 - 51
Publisher: Cambridge University Press
Print publication year: 2007

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
×