An alternative method for modeling close-range
interactions between air guns
Daniel Barker
1
and Martin Landrø
1
ABSTRACT
We evaluated the problem of modeling the decay of the
primary pulse amplitudes of air-gun clusters caused by the
traditional assumption of sphericality. This was done by
generalizing the Rayleigh equation to work with arbitrary
bubble shapes, while retaining the assumption of incom-
pressibility. To approximate the coalescence of the bubbles,
we let the shapes be isosurfaces of the velocity potential.
With this method, it is possible to model the firing of clus-
tered air guns at any separation distance, including small dis-
tances that would cause two spherical bubbles to overlap. In
this way, we obtained results matching the relative decay
shown to be present for air-gun clusters. In addition, this
method also allowed a way of calibrating the model such
that effects created by the presence of the gun, compared
to just a single spherical air bubble, may be estimated
and included.
INTRODUCTION
The act of placing two or more air guns in close vicinity to each
other remains a popular way of shaping the seismic signal emitted in
marine seismic acquisition for several reasons. Historically, the
main reason has been the improved primary-to-bubble ratio ob-
served due to the interactions between the guns, but more recently,
the increased bubble time period has been used to create a source
signature, with enhanced low-frequent output (Hopperstad et al.,
2012). A side effect of this is that the primary amplitude of the clus-
ter will degrade compared to the primary amplitude of the single
guns alone, and it may be more important now than before to under-
stand exactly how the primary signal of the cluster will be affected
by separation distance and the number of guns used to optimize
these broadband sources by use of modeling. At the same time,
modeling the interactions by assuming spherical bubbles and modi-
fying the pressure surrounding the bubble by adding the acoustic
field propagated by other bubbles (Ziolkowski et al., 1982; Li et al.,
2011) will introduce problems at very close range, especially for
coalescing bubbles. For instance, by using spherical spreading,
one may experience that the hydrostatic pressure effect of another
bubble may be more than the pressure inside the bubble itself if its
radius is bigger than the original separation distance between the
guns. While this certainly could be improved by some form of cor-
rection, the general problem coming from the spherical assumption
and a fixed separation distance is not trivial to solve, and another
approach may be needed.
Strandenes and Vaage (1992) analyze by experiment how clus-
tering of air guns will change the primary amplitude, bubble time
period, and primary-to-bubble ratio compared to firing single guns
and introduce a dimensionless constant, defined by the separation
distance divided by an equilibrium radius, the latter being the theo-
retical radius at which the air bubble has hydrostatic pressure and
the temperature of the surrounding fluid. When comparing clusters
with the same constant, they find the relative results compared to
single guns to be equal, suggesting that this is a key parameter for
the dynamics. Barker and Landrø (2013) use this dimensionless
parameter, and a representation based on isosurfaces of the velocity
potential, to estimate the relative bubble time period, which
matched the general trend of the recorded data. Because their esti-
mate was based on an assumption of incompressibility, it seems that
the most important contributor to cluster dynamics may be the fluid
movement, rather than the traditional pressure field interaction,
when it comes to the bubble time period. This might also be the
case for the degradation of primary amplitudes due to clustering.
In this paper, we will concentrate on the primary amplitude, and
we investigate how it will decrease as clustered air guns are moved
closer toward each other. To be able to investigate this for coalesc-
ing bubbles, we will use an approach based on the isosurfaces that
Barker and Landrø (2013) present, but we extend the notion for use
in modeling. To investigate the effect on primaries, we also need a
Manuscript received by the Editor 5 April 2013; revised manuscript received 9 September 2013; published online 18 December 2013.
1
Norwegian University of Science and Technology (NTNU), Department of Petroleum Engineering and Applied Geophysics, Trondheim, Norway. E-mail:
daniel.barker@ntnu.no; mlan@ipt.ntnu.no.
© 2013 Society of Exploration Geophysicists. All rights reserved.
P1
GEOPHYSICS, VOL. 79, NO. 2 (MARCH-APRIL 2014); P. P1–P7, 12 FIGS.
10.1190/GEO2013-0141.1
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