Skip to main content Accessibility help
×
Hostname: page-component-848d4c4894-ndmmz Total loading time: 0 Render date: 2024-04-30T20:44:11.575Z Has data issue: false hasContentIssue false

L1.2 - The van der Waals interaction spectrum

from LEVEL 1 - INTRODUCTION

Published online by Cambridge University Press:  08 January 2010

V. Adrian Parsegian
Affiliation:
National Institute of Child Health and Human Development, Maryland
Get access

Summary

What frequencies are important to the interaction of real materials? It is best to learn from example. If we can develop an intuition to know the significant frequencies of fluctuation, our partial ignorance of absorption spectra need not daunt us in computation or, better, this intuition might give us some idea about the accuracy of computation. Differences in dielectric response create the force; sampling-frequency density weights the contribution from higher frequencies; retardation snuffs out the highest frequencies first. These general features show up in specific examples. Water, hydrocarbon (liquid tetradecane), gold, and mica are not only popular materials in van der Waals force measurement but, as a group, they also display a wide variety of dielectric response. (See, e.g., tables in SubSection L2.4.D).

Their detailed energy-absorption spectra as functions of radial frequency ωR translate into smooth functions ε(iξ) of imaginary frequency. This blurring of details in ε(iξ) is one reason why it is often possible to compute van der Waals interactions to good accuracy without full knowledge of spectra (see Fig. L1.21).

To see how these different ε(iξ) functions combine to create an interaction, consider the case of two hydrocarbon half-spaces A = B = H across water medium m = W. First plot εH(iξ) and εW(iξ) as continuous functions [see Fig. L1.22(a)].

Type
Chapter
Information
Van der Waals Forces
A Handbook for Biologists, Chemists, Engineers, and Physicists
, pp. 61 - 64
Publisher: Cambridge University Press
Print publication year: 2005

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
×