Skip to main content Accessibility help
×
Hostname: page-component-68945f75b7-qf55q Total loading time: 0 Render date: 2024-08-05T18:35:42.942Z Has data issue: false hasContentIssue false

Appendix A

Published online by Cambridge University Press:  07 October 2011

William T. Sha
Affiliation:
Argonne National Labs
Get access

Summary

A staggered-grid computational system is widely used in numerical analysis. A family of COMMIX codes is no exception; the codes greatly benefited by using this system. In this system, all dependent nonflow variables (pressure, temperature, density, total energy, enthalpy, internal energy, mass fraction of phases, turbulent transport quantities, thermal physical properties, etc.) are calculated for the computational cell center (I, J, K) in three-dimensional orthogonal coordinates, and all flow variables (velocity components) are calculated for the surfaces of the computational cell (I ± 1/2, J ± 1/2, K ± 1/2). The computational cell is defined by the locations of cell volume faces, and a grid point is placed in the geometric center of each cell volume; cell sizes can be nonuniform. This type of construction of computational system is shown in .

Consider the control volume for a nonflow variable shown in . It is constructed around a grid point 0, which has grid points 1 (i − 1) and 2 (i + 1) as its west and east neighbors, 3 (j − 1) and 4 (j + 1) as its front and rear neighbors, and 5 (k − 1) and 6 (k + 1) as its south and north neighbors.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2011

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.

  • Appendix A
  • William T. Sha
  • Book: Novel Porous Media Formulation for Multiphase Flow Conservation Equations
  • Online publication: 07 October 2011
  • Chapter DOI: https://doi.org/10.1017/CBO9781139003407.014
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.

  • Appendix A
  • William T. Sha
  • Book: Novel Porous Media Formulation for Multiphase Flow Conservation Equations
  • Online publication: 07 October 2011
  • Chapter DOI: https://doi.org/10.1017/CBO9781139003407.014
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.

  • Appendix A
  • William T. Sha
  • Book: Novel Porous Media Formulation for Multiphase Flow Conservation Equations
  • Online publication: 07 October 2011
  • Chapter DOI: https://doi.org/10.1017/CBO9781139003407.014
Available formats
×