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Traveltime computations for dipping water-bottom multiple

In this Appendix I derive equations 39-45.

 
mul_sktch9
Figure 21
Sketch to show the computation of ts1 and ts2 for a non-diffracted multiple from a dipping water-bottom.
mul_sktch9
view

From triangle ABC in Figure [*] we immediately get
\begin{displaymath}
t_{s_1}=\frac{\tilde{Z}_s}{\cos(\alpha_s+\varphi)}\end{displaymath} (57)
and applying the law of sines to triangle ACD we get
\begin{displaymath}
t_{s_2}=\frac{t_{s_1}\cos\alpha_s}{\cos(\alpha_s+2\varphi)}=...
 ...cos\alpha_s}{V_1\cos(\alpha_s+\varphi)\cos(\alpha_s+2\varphi)}.\end{displaymath} (58)

 
mul_sktch10
Figure 22
Sketch to show the computation of tr2 and tr1 for a non-diffracted multiple from a dipping water-bottom.
mul_sktch10
view

Similarly, repeated application of the law of sines to triangles CDE and DEF in Figure [*] gives
\begin{eqnarray}
t_{r_2}&=&\frac{t_{s_2}\cos(\alpha_s+\varphi)}{\cos(\alpha_s+3\...
 ...s\cos\alpha_s}{V_1\cos(\alpha_s+3\varphi)\cos(\alpha_s+4\varphi)}.\end{eqnarray} (59)
(60)

 
mul_sktch11
Figure 23
Sketch to show the computation of $\tilde{Z}_s$ in equation 61.
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view

These equations are in terms of $\tilde{Z}_s$, which is not known. However, from Figure [*] we see that  
 \begin{displaymath}
\tilde{Z}_s=\tilde{Z}_D-h_D\sin\varphi,\end{displaymath} (61)
and $\tilde{Z}_D$ can be computed from the traveltime of the zero surface-offset trace, since, according to Figure [*]
\begin{displaymath}
t_m(0)=\frac{2\tilde{Z}_D}{V_1\cos\varphi}+\frac{2\tilde{Z}_...
 ...\varphi}=\frac{2\tilde{Z}_D(1+\cos(2\varphi))}{V_1\cos\varphi},\end{displaymath} (62)
from which it follows immediately that  
 \begin{displaymath}
\tilde{Z}_D=\frac{V_1t_m(0)\cos\varphi}{2[1+\cos(2\varphi)]}.\end{displaymath} (63)

 
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Figure 24
Sketch to show the computation of $\tilde{Z}_D$ in equation 63.
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Finally, we need to compute $\alpha_s$. Applying the law of sines to triangle ABC in Figure [*] we get
\begin{displaymath}
\sin(\alpha_s+2\varphi)=\frac{2h_D\cos(2\varphi)}{V_1t_m},\end{displaymath} (64)
from which we get
\begin{displaymath}
\alpha_s=\sin^{-1}\left[\frac{2h_D\cos(2\varphi)}{V_1t_m}\right]-2\varphi.\end{displaymath} (65)

 
mul_sktch16
Figure 25
Sketch to compute the takeoff angle of the source ray from a non-diffracted multiple from a dipping water-bottom.
mul_sktch16
view

D


next up previous print clean
Next: From dip to no Up: Alvarez: Multiples in image Previous: Computation of Image Depth
Stanford Exploration Project
11/1/2005