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Gaussian beams and dynamic ray equations

Under the Gaussian approximation the acoustic pressure along a ray beam is defined as [2,3]
\begin{displaymath}
P(s,n) = A \sqrt{ \frac {c(s)}{ r q(s) } } \times \exp\left[...
...a \left( \tau(s) + \frac {p(s)}{2q(s)}n^2 \right) \right]  ,
\end{displaymath} (4)

where $n$ represents the normal distance from the central ray and $A$ is an arbitrary constant, which can be fixed using an expansion of a point source into beams. After substitution into the Helmholtz equation one can obtain the dynamic ray equations [1,4,5]
\begin{displaymath}
\frac{dq}{ds} = c(s) p(s) \hskip5mm , \hskip5mm \frac{dp}{ds} = -\frac {c_{nn}}{c^2(s)} q(s)  ,
\end{displaymath} (5)

where [2]
\begin{displaymath}
c_{nn} = c_{rr} N_r^2 - 2 c_{rz} N_r N_z + c_{zz} N_z^2  ,
\end{displaymath} (6)


\begin{displaymath}
c_{rr} = \frac{\partial{^2c}}{\partial{r^2}} \hskip5mm , \hs...
...5mm
c_{rz} = \frac{\partial{^2c}}{\partial{r \partial z}}  ,
\end{displaymath}

and
\begin{displaymath}
N_r = c(s) \zeta(s) \hskip5mm , \hskip5mm
N_z = -c(s) \xi(s)  .
\end{displaymath} (7)

Initial conditions for $p(s)$ and $q(s)$ can be

\begin{displaymath}q(0) = 0 \hskip5mm\makebox{ and }\hskip5mm p(0) = 1  . \end{displaymath}

Thus, the acoustic pressure along the ray can be calculated as
\begin{displaymath}
P(s) = \phi_r \frac {A(s)}{\sqrt{r(s)}} e^{ -i\left[ \omega \tau(s) - \phi_c \right] }  ,
\end{displaymath} (8)

where the amplitude is given by [5]
\begin{displaymath}
A(s) = \left\vert \frac { c(s) \cos\theta_s }{ q(s) } \right\vert ^{1/2}  .
\end{displaymath} (9)

The factor $A(s)/\sqrt{r(s)}$ represents the ray amplitude due to cylindrical spreading; it should be multiplied by the decaying factor $\phi_r$ in order to account for the loss of energy due to boundary reflections; the factor $\phi_c$ represents the shift caused by the formation of caustics. Both $\phi_r$ and $\phi_c$ are described in the following subsection.


next up previous contents
Next: Boundary reflections and caustics Up: Theoretical background Previous: The Eikonal equations   Contents
Orlando C. Rodriguez 2008-06-03