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Viscoelastic Waves in Layered Media

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  • Saadedin
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    • Sep 2018 
    • 35987 
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    Viscoelastic Waves in Layered Media





    Preface

    This book provides a self-contained mathematical exposition of the theory of

    monochromatic wave propagation in layered viscoelastic media. It provides analytic

    solutions and numerical results for fundamental wave-propagation problems in

    arbitrary linear viscoelastic media not published previously in a book. As a text

    book with numerical examples and problem sets, it provides the opportunity to teach

    the theory of monochromatic wave propagation as usually taught for elastic media

    in the broader context of wave propagation in any media with a linear response

    without undue complications in the mathematics. Formulations of the expressions

    for the waves and the constitutive relation for the media afford considerable generality

    and simplification in the mathematics required to derive analytic solutions valid

    for any viscoelastic solid including an elastic medium. The book is intended for the

    beginning student of wave propagation with prerequisites being knowledge of

    differential equations and complex variables.



    As a reference text, this book provides the theory of monochromatic wave

    propagation in more than one dimension developed in the last three to four decades.

    As such, it provides a compendium of recent advances that show that physical

    characteristics of two- and three-dimensional anelastic body and surface waves are

    not predictable from the theory for one-dimensional waves. It provides the basis for

    the derivation of results beyond the scope of the present text book. The theory is of

    interest in the broad field of solid mechanics and of special interest in seismology,

    engineering, exploration geophysics, and acoustics for consideration of wave propagation

    in layered media with arbitrary amounts of intrinsic absorption, ranging

    from low-loss models of the deep Earth to moderate-loss models for soils and weathered rock.


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