Poission’s ratio from P- and S-wave traveltimes
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| Series | Geophysical References Series |
|---|---|
| Title | Problems in Exploration Seismology and their Solutions |
| Author | Lloyd P. Geldart and Robert E. Sheriff |
| Chapter | 13 |
| Pages | 485 - 496 |
| DOI | http://dx.doi.org/10.1190/1.9781560801733 |
| ISBN | ISBN 9781560801153 |
| Store | SEG Online Store |
Problem 13.7
Find Poisson’s ratio for the five events in Figure 13.7a.
Solution
Poisson’s ratio $ \sigma $ can be obtained from the ratio $ V_{\hbox{P}}/V_{\hbox{S}} $ using equation (10.2) Table 2.2a. Since $ z=V_{\hbox{P}}t_{\hbox{P}}=V_{\hbox{S}}t_{\hbox{S}} $, $ V_{\hbox{P}}/V_{\hbox{S}}=t_{\hbox{S}}/t_{\hbox{P}} $, we can get $ (V_{\hbox{P}}/V_{\hbox{S}}) $ from the traveltimes and then get $ \sigma $ using equation (10,2) (see Table 2.2a), that is,
$ {\begin{aligned}\sigma ={\frac {(V_{\hbox{P}}/V_{\hbox{S}})^{2}-2}{2[(V_{\hbox{P}}/V_{\hbox{S}})^{2}-1]}}.\end{aligned}} $
Measurements and calculations are listed in Table 13.7a.

| Event | $ t_{\hbox{P}} $ | $ t_{\hbox{S}} $ | $ \alpha /\beta $ | $ (\alpha /\beta )^{2} $ | $ \sigma $ |
|---|---|---|---|---|---|
| 1 | 0.39 | 0.96 | 2.46 | 6.05 | 0.40 |
| 2 | 0.62 | 1.50 | 2.42 | 5.86 | 0.40 |
| 3 | 0.74 | 1.65 | 2.23 | 4.97 | 0.37 |
| 4 | 0.80 | 1.83 | 2.29 | 5.24 | 0.38 |
| 5 | 0.99 | 2.16 | 2.18 | 4.75 | 0.37 |
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Also in this chapter
- S-wave conversion in marine surveys
- Equally inclined orthogonal geophones
- Guided (channel) waves and normal-mode propagation
- Vertical seismic profiling
- Effect of velocity change on VSP traveltime
- Mapping the vertical flank of a salt dome
- Poission’s ratio from P- and S-wave traveltimes