Chapter 2: The Biot theory of dynamic poroelasticity

PreviousNext No AccessAttenuation and Dispersion of Elastic Waves in Porous Rocks: Mechanisms and modelsChapter 2: The Biot theory of dynamic poroelasticityhttps://doi.org/10.1190/1.9781560803911.ch2 SectionsAboutPDF/ePub ToolsAdd to favoritesDownload CitationsTrack CitationsPermissions ShareFacebookTwitterLinked InReddit Abstract The Biot theory of dynamic poroelasticity is the subject of Chapter 2. The purpose of this chapter is three-fold: to give a detailed description of the global-flow mechanism described by this theory, to illustrate this mechanism with experimental data, and to present field equations and constitutive equations, which are employed in subsequent chapters to develop mathematical models of other attenuation mechanisms that occur in porous media with strong spatial heterogeneity. Permalink: https://doi.org/10.1190/1.9781560803911.ch2FiguresReferencesRelatedDetails Dec 2022 Pages: 536 ISBN (print):978-1-56080-390-4ISBN (online):978-1-56080-391-1 publication data© 2022 All rights reserved. This book or parts hereof may not be reproduced in any form without written permission from the publisher.Publisher:Society of Exploration Geophysicists HistoryPublished in print: 20 Dec 2022 CITATION INFORMATION (2022), "Chapter 2: The Biot theory of dynamic poroelasticity," Geophysical References Series : 31-101. https://doi.org/10.1190/1.9781560803911.ch2 Plain-Language Summary PDF DownloadLoading ...