# Difference between revisions of "Dominant frequencies of marine sources"

Series Geophysical References Series Problems in Exploration Seismology and their Solutions Lloyd P. Geldart and Robert E. Sheriff 7 221 - 252 http://dx.doi.org/10.1190/1.9781560801733 ISBN 9781560801153 SEG Online Store

## Problem 7.8

The dominant period of a marine seismic source is often determined by the source depth; this is the case when the second half-cycle of the downgoing wave is reinforced

Figure 7.7a  An air-gun array.

by the ghost reflection at the surface. Assuming that this is true for the source signatures in Figure 7.8a, determine their depths.

### Background

For discussion of reinforcement depth in marine recording, see problem 3.5. The ghost is the wave reflected at the surface (or at the base of the LVL) with a reversal of phase (see problem 3.8).

When a gas at high pressure is suddenly generated by an underwater explosion or injected into the water by an air gun at sufficient depth that the gas does not quickly escape into the air, oscillation occurs as the gas expands until stopped by the water pressure, then contracts until the gas pressure becomes very high,

Figure 7.8a  Far-field waveshapes of marine sources. (a) Single 120 in3 air gun; (b) array of air guns of different sizes selected to attenuate bubble effects by destructive interference; (c) sleeve exploder; (d) Vaporchoc; (e) Maxipulse; (f) Flexichoc; (g) water gun; (h) 5 kJ sparker. Curves are intended to show features of waveshape, not amplitude relationships. ${\displaystyle {\textit {B}}}$ indicates bubble effects; the interval between successive bubbles decreases with time; I indicates implosion (after Sheriff and Geldart, 1995)
Table 7.8a. Source depth from frequency.
${\displaystyle T}$ (ms) ${\displaystyle d}$ (m)
a) air gun 22 8
b) air-gun array 24 9
c) sleeve exploder 26 10
d) Vaporchoc 18 7
e) Maxipulse 24 9
f) Flexichoc 28 11
g) water gun 22 8
h) sparker 4 2

after which it expands again and the cycle is repeated. Each expansion is effectively a new activation of the source and so a new reflection sequence is generated. This phenomenon is called the bubble effect.

Air guns are described in problem 7.7, imploders, water guns, and sparkers in problem 7.4. Flexichoc${\displaystyle ^{\rm {TM}}}$, sleeve gun, Vaporchoc${\displaystyle ^{\rm {TM}}}$, and Maxipulse${\displaystyle ^{\rm {TM}}}$ are devices (now obsolete) designed to diminish the bubble oscillation. Flexichoc used the explosion of a small charge at the center of a steel cage that attenuated the bubble, the sleeve gun utilized the explosion of a propane-oxygen mixture inside a flexible chamber with the gases vented to the surface, Vaporchoc injected superheated steam into the water, and Maxipulse recorded the bubble oscillation for later processing to remove the bubble effects.

### Solution

The phase of a ghost is reversed by reflection at the surface, hence to reinforce the downgoing wavelet the ghost must return to the source at time ${\displaystyle T/2}$, where ${\displaystyle {\textit {T}}}$ is the period measured in Figure 7.8a. Therefore the depth of the source ${\displaystyle d=V_{w}T/4=380T}$ m, taking ${\displaystyle V_{w}={}}$ velocity in water ${\displaystyle {}=1500}$ m/s. The results are shown in Table 7.8a.