next up previous print clean
Next: Reflection seismology geometry Up: GETTING THE WAVES FROM Previous: GETTING THE WAVES FROM

Layers between two halfspaces

Let a stack of layers be sandwiched in between two halfspaces Figure 9.

 
8-9
8-9
Figure 9
Waves incident, reflected, and transmitted from a stack of layers between two half-spaces.
view

An impulse is incident from below. The backscattered wave is called C(Z) and the transmitted wave is called T(Z). We take these waves and load them into the multilayer equation (20).  
 \begin{displaymath}
\left[
 \begin{array}
{c}
 1 \\  C(Z) \end{array} \right]
\e...
 ...t]
\; \left[
 \begin{array}
{c}
 T(Z) \\  0 \end{array} \right]\end{displaymath} (21)

We may solve the first of (21) for the transmitted wave T(Z)  
 \begin{displaymath}
T(Z) \eq {\sqrt{Z}^k \Pi t \over F(Z)}\end{displaymath} (22)

and introduce the result back into the second of (21) to obtain the backscattered wave  
 \begin{displaymath}
C(Z) \eq {G(Z)T(Z) \over \sqrt{Z}^k \Pi t} \eq {G(Z) \over F(Z)}\end{displaymath} (23)

Let us be clear we understand the meaning of the solutions T(Z) and C(Z). They can be regarded two ways, either as functions of frequency $Z=e^{i\omega}$,or the polynomial coefficients (after dividing out the denominator F(Z)) as waveforms, as functions of time. Physical interpretations of F(Z) and G(Z) are on the right side of Figure 9.


next up previous print clean
Next: Reflection seismology geometry Up: GETTING THE WAVES FROM Previous: GETTING THE WAVES FROM
Stanford Exploration Project
3/1/2001