Skip to main content Accessibility help
×
Hostname: page-component-7479d7b7d-pfhbr Total loading time: 0 Render date: 2024-07-08T06:25:52.075Z Has data issue: false hasContentIssue false

Introduction

Published online by Cambridge University Press:  05 July 2015

Zhongying Chen
Affiliation:
Sun Yat-Sen University, Guangzhou, China
Charles A. Micchelli
Affiliation:
State University of New York, Albany
Yuesheng Xu
Affiliation:
Sun Yat-Sen University, Guangzhou, China
Get access

Summary

The equations we consider in this book are primarily Fredholm integral equations of the second kind on bounded domains in the Euclidean space. These equations are used as mathematical models for a multitude of physical problems and cover many important applications, such as radiosity equations for realistic image synthesis [18, 85, 244] and especially boundary integral equations [12, 177, 203], which themselves occur as reformulations of other problems, typically originating as partial differential equations. In practice, Fredholm integral equations are solved numerically using piecewise polynomial collocation or Galerkin methods, and when the order of the coefficient matrix (which is typically full) is large, the computational cost of generating the matrix as well as solving the corresponding linear system is large. Therefore, to enhance the range of applicability of the Fredholm equation methodology, it is critical to provide alternate algorithms which are fast, efficient and accurate. This book is concerned with this challenge: designing fast multi scale methods for the numerical solution of Fredholm integral equations.

The development and use of multi scale methods for solving integral equations is a subject of recent intense study. The history of fast multi scale solutions of integral equations began with the introduction of multi scale Galerkin (Petrov–Galerkin) methods for solving integral equations, as presented in [28, 64, 68, 88, 94, 95, 202, 260, 261] and the references cited therein. Most noteworthy is the discovery in [28] that the representation of a singular integral operator by compactly supported orthonormal wavelets produces numerically sparse matrices. In other words, most of their entries are so small in absolute value that, to some degree of precision, they can be neglected without affecting the overall accuracy of the approximation. Later, the papers [94, 95] studied Petrov–Galerkin methods using periodic multi scale bases constructed from refinement equations for periodic elliptic pseudodifferential equations, and in this restricted environment, stability, convergence and matrix compression were investigated.

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
×