
- •Contents
- •Series Preface
- •Introduction
- •Floating-Point Numbers
- •Computational Cost
- •Fidelity
- •Code Development
- •List of Open-Source Tools
- •Exercises
- •References
- •Derivation of the Wave Equation
- •Introduction
- •General Properties of Waves
- •One-Dimensional Waves on a String
- •Waves in Elastic Solids
- •Waves in Ideal Fluids
- •Thin Rods and Plates
- •Phonons
- •Tensors Lite
- •Exercises
- •References
- •Methods for solving the Wave Equation
- •Introduction
- •Method of Characteristics
- •Separation of Variables
- •Homogeneous Solution in Separable Coordinates
- •Boundary Conditions
- •Representing Functions with the Homogeneous Solutions
- •Green
- •Method of Images
- •Comparison of Modes to Images
- •Exercises
- •References
- •Wave Propagation
- •Introduction
- •Fourier Decomposition and Synthesis
- •Dispersion
- •Transmission and Reflection
- •Attenuation
- •Exercises
- •References
- •Normal Modes
- •Introduction
- •Mode Theory
- •Profile Models
- •Analytic Examples
- •Perturbation Theory
- •Multidimensional Problems and Degeneracy
- •Numerical Approach to Modes
- •Coupled Modes and the Pekeris Waveguide
- •Exercises
- •References
- •Ray Theory
- •Introduction
- •High Frequency Expansion of the Wave Equation
- •Amplitude
- •Ray Path Integrals
- •Building a Field from Rays
- •Numerical Approach to Ray Tracing
- •Complete Paraxial Ray Trace
- •Implementation Notes
- •Gaussian Beam Tracing
- •Exercises
- •References
- •Introduction
- •Finite Difference
- •Time Domain
- •FDTD Representation of the Linear Wave Equation
- •Exercises
- •References
- •Parabolic Equation
- •Introduction
- •The Paraxial Approximation
- •Operator Factoring
- •Pauli Spin Matrices
- •Reduction of Order
- •Numerical Approach
- •Exercises
- •References
- •Finite Element Method
- •Introduction
- •The Finite Element Technique
- •Discretization of the Domain
- •Defining Basis Elements
- •Expressing the Helmholtz Equation in the FEM Basis
- •Numerical Integration over Triangular and Tetrahedral Domains
- •Implementation Notes
- •Exercises
- •References
- •Boundary Element Method
- •Introduction
- •The Boundary Integral Equations
- •Discretization of the BIE
- •Basis Elements and Test Functions
- •Coupling Integrals
- •Scattering from Closed Surfaces
- •Implementation Notes
- •Comments on Additional Techniques
- •Exercises
- •References
- •Index

Two cases of interest are (1) normal incidence, θI = θT = βT = 0, and (2) when βT = π4. In the
case of normal incidence, the coefficients are |
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2ZP |
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S = 0 |
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R = |
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For case (2) the coefficients become |
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P = 0 |
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S = − |
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2ZS |
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R = |
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ZS + Z1 |
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In the case of normal incidence, only compression waves are excited, whereas in the second case only shear waves are excited.
5.5 Attenuation
Attenuation refers to a weakening of the wave amplitude. For cylindrical or spherical waves, the amplitude will weaken with distance from the source. This weakening is referred to as geometric spread. Interaction with the medium can lead to other types of attenuation by the processes of absorption or scattering. Mathematically this is accounted for by a complex wavenumber, κ = k + iα. Fluid media can exhibit a variety of attenuation strengths. At the micro level, the cause of attenuation is due to the interaction of waves and the particles in the medium. At a macro level, the effects are rolled up into the attenuation coefficient, α. This coefficient can depend on the frequency of the sound as well as on environmental factors such as temperature, relative humidity, and pressure. Attenuation acts opposite the direction of propagation, like air resistance for a moving object. In 3-dim a plane wave with attenuation is expressed as
exp i k ∙ x − αs |
(5.73) |
where s is the distance traveled along the propagation path or direction. The same result applies to a spherical wave, exp(−αR). The unit of the attenuation coefficient is m− 1. Models of the atmospheric attenuation of air and attenuation in water can be found in Refs. [6] and [4, 7], respectively.
5.6 Exercises
1.Sound in a fluid medium is incident on a thin layer of a solid medium of thickness L, with two Lamé parameters.
(a)Determine the boundary conditions at each interface of the solid medium.
(b)Solve for the transmission and reflection coefficients and the coefficients of the wave in the solid medium.
2.Calculate the 2-dim Fourier transform of the following spatial window functions.
(a)Step function, 1 for x
< Lx
2 and
y
< Ly
2, zero otherwise
(b)Circular step function, 1 for ρ < a, zero otherwise
(c)Radial quadratic window, 1 − (ρ/a)2 for ρ < a, zero otherwise
(d)What effect does the change in window have on the spectrum?
3.Given the transmission and reflection coefficient for a plane wave incident at the boundary of two media,
(a)Develop a procedure for modeling the transmitted and reflected field from a point source a distance, D, above the plane separating the medium.
(b)If possible work out the results analytically; otherwise write a procedure in the language of your choice.
References
[1]Körner, T. W., Fourier Analysis, Cambridge University Press, Cambridge, 1990.
[2]Press, W. H., Teukolsky, S. A., Vetterling, W. T., and Flannery, B. P., Numerical Recipes in C++, The Art of Scientific Computing, Second Edition, Cambridge University Press, Cambridge, 2005.
[3]Tolstoy, I. and Clay, C. S., Ocean Acoustics, Theory and Experiment in Underwater Sound, McGraw-Hill, New York, 1966.
[4]Ainslie, M. A. and McColm, J. G., A simplified formula for viscous and chemical absorption in sea water, J. Acoust. Soc. Am., Vol. 103, No. 3, pp. 1671–1672, 1998.
[5]Brekhovskikh, L. M., Waves in Layered Media, Academic Press, New York, 1960.
[6]Rickley, E. J., Fleming, G. G., and Roof, C. J., Simplified procedure for computing the absorption of sound by the atmosphere, Noise Control Eng. J., Vol. 55, No. 6, pp. 482–494, 2007.
[7]Fisher, F. H. and Simmons, V. P., Sound absorption in sea water, J. Acoust. Soc. Am., Vol. 62, No. 3, pp. 558–564, 1977.