Skip to main content Accessibility help
×
Hostname: page-component-7479d7b7d-qlrfm Total loading time: 0 Render date: 2024-07-13T04:54:45.872Z Has data issue: false hasContentIssue false

8 - A numerical example: drop pinch-off

from PART II - FORMATION OF SINGULARITIES

Published online by Cambridge University Press:  05 September 2015

J. Eggers
Affiliation:
University of Bristol
M. A. Fontelos
Affiliation:
Universidad Autónoma de Madrid
Get access

Summary

Numerical methods play an important role in our understanding of singularities. Simulations often provide crucial pointers to the local structure of a singularity, and they reveal which physical effects dominate near a singularity. In addition, the analytical descriptions that we are able to obtain encompass only the local structure of the solution. One often has to rely on numerics in order to capture how local singular solutions are connected on the global scale.

Regrettably, the development of numerical codes is often considered a pursuit best left to the specialist. Our aim is to highlight some of the fundamental ideas that go into the numerical description of singular behavior. As an example, we take the description of a capillary bridge of liquid collapsing under gravity (see Fig. 8.1), which we will describe in some technical detail. Two aspects are of particular importance:

Stability Solutions which are close to singular involve a wide range of time scales. As a result, great demands are placed on the stability of the numerical scheme being used. This issue is addressed by using so-called implicit numerical schemes.

Adaptability As the singularity is approached, the solution evolves on smaller and smaller length and time scales. It is crucial that the numerical scheme adapts to these changes, by adjusting the time step and by refining the computational grid in a small region around the singularity.

Finite-difference scheme

A liquid drop is held between two endplates of radius r0 which are a distance L apart; cf. Example 6.4 in Section 6.2. We solve equations (6.59), (6.57) on a grid zi, i= 1, . . ., k, which divides up the computational domain; see Fig. 8.2. Since the total length of the bridge is L, we have z1 = 0 and zk = L. The grid spacing between two points is denoted as below we discuss in more detail how is chosen to represent a given problem accurately. The radius h(z) is represented by its values on this grid.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2015

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
×