Titlebook: High-Frequency Seafloor Acoustics; Darrell R. Jackson,Michael D. Richardson Book 2007 Springer-Verlag New York 2007 Geophysics.High-freque

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Geoacoustic Properties,fficult when the measured and required acoustic frequencies are substantially different. In spite of these problems, some generalizations can be made, and values of wave speed and attenuation as well as their gradients can be measured or predicted using physical and empirical models. This chapter wi

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Elastic Theories, chapter outlines elements of elasticity theory and notation needed for later discussion of modeling. Shear wave speed and attenuation are the two additional parameters required by elasticity theory compared to fluid theory. In situ and laboratory techniques commonly used to measure these parameters

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Sediment Volume Scattering,nov 1981b, D. Jackson et al. 1986a, Ivakin 1990, Hines 1990, D. Jackson and Briggs 1992, Gensane 1993, Lyons et al. 1994, Pace 1994, Boyle and Chotiros 1995b, Yamamoto 1996, Hines 1996, Pouliquen et al. 2000b, Pouliquen and Lyons 2002].

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nd practice. They play a key role in a variety of research areas, such as combinatorial optimization, approximation algorithms, computational complexity, graph theory, geometry, real algebraic geometry and quantum computing. This book is an introduction to selected aspects of semidefinite programmin

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Darrell R. Jackson,Michael D. Richardsonnd practice. They play a key role in a variety of research areas, such as combinatorial optimization, approximation algorithms, computational complexity, graph theory, geometry, real algebraic geometry and quantum computing. This book is an introduction to selected aspects of semidefinite programmin