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1986 | Buch

The Marine Seismic Source

verfasst von: Gregg Parkes, Les Hatton

Verlag: Springer Netherlands

Buchreihe : Seismology and Exploration Geophysics

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Über dieses Buch

This book is about marine seismic sources, their history, their physical principles and their deconvolution. It is particularly accented towards the physical aspects rather than the mathematical principles of signature generation in water as it is these aspects which the authors have found to be somewhat neglected. A huge amount of research has been carried out by both commercial and academic institutions over the years and the resulting literature is a little daunting, to say the least. In spite of this, the subject is intrinsically very simple and relies on a very few fundamental physical principles, a somewhat larger number of heuristic principles and a refreshingly small amount of blunderbuss mathematics. As such it is still one of those subjects in which the gifted practical engineer reigns supreme and from which many of the important advances have originated. In Chapter 1 of the book, the underlying physics and concepts are discussed, including pressure and wave propagation, bubble motion, virtual images and the factors determining choice of source. In marine reflection seismology, almost all of the seismic data acquired currently is done with either the airgun or the watergun, which rely on the expulsion of air and water respectively to generate acoustic energy. As a consequence, the discussion in this chapter is geared towards these two sources, as is much of the rest of the book.

Inhaltsverzeichnis

Frontmatter
Chapter 1. Underlying Physics and Concepts
Abstract
The list of available marine seismic sources is extensive. Many have stood the test of time, whilst others have fallen by the wayside, then there are the countless variations on a theme. Technical details of the sources which are currently used most are given in the appendix. This will be updated periodically to keep it in line with the times. The methods used to generate acoustic waves in marine seismic sources can be grouped into four broad categories. These primary divisions are — chemical, mechanical, pneumatic/hydraulic, and electrical.
Gregg Parkes, Les Hatton
Chapter 2. Source Arrays and Directivity
Abstract
It is common for marine seismic sources to be deployed in groups or arrays. This is done for a variety of reasons. The most obvious of these is simply to increase the power of the source. The alternative of using increasingly larger sources is impractical because size increases of a single source are inevitably accompanied by changes in the characteristics (e.g. bandwidth) of the emitted pulse. In essence, therefore, a source system of ‘n’ times the power of a single source can be achieved by firing ‘n’ sources together as an array, whilst maintaining the basic pulse characteristics of the single source.
Gregg Parkes, Les Hatton
Chapter 3. Interaction and Wavefield Determination
Abstract
The previous chapters have concentrated on more general aspects of seismic sources, such as their physical properties, their variety and the basic principles of directivity. In this chapter, the subtleties of source interaction and some practical aspects of determining signatures in the presence of such interaction will be discussed.
Gregg Parkes, Les Hatton
Chapter 4. Practical Aspects of Wavefield Stability
Abstract
The previous chapters have described how the wavefield of a marine seismic source depends not only on the characteristics of the individual elements of the source but also upon the details of the geometry of the whole source system. Gross effects such as ghosting depend upon depth of deployment, interaction effects depend sensitively upon the relative positions of the elements, and directivity effects are a direct function of geometry. It follows that if the 3-dimensional wavefield of the array is to be stable, then the 3-dimensional geometry of the array must be stable. So geometry plays a major role in wavefield stability, however there are other factors which we can broadly group under the following headings :
(1)
The timing synchronisation accuracy of individual elements in an array.
 
(2)
The geometrical stability of the source deployment method.
 
(3)
The intrinsic stability of theacousticenergygeneration technique.
 
(4)
The weather.
 
Gregg Parkes, Les Hatton
Chapter 5. Source Signature Deconvolution
Abstract
The deconvolution of the seismic source signature has retained the interest of reflection seismologists from the earliest days of the science. Today, with the ever-increasing emphasis on temporal resolution, more is expected of the deconvolution process. The issue of whether such resolution is attainable with the information at hand is unanswered and quite often unaddressed. This is however beyond the scope of this textbook and will not be considered further.
Gregg Parkes, Les Hatton
Backmatter
Metadaten
Titel
The Marine Seismic Source
verfasst von
Gregg Parkes
Les Hatton
Copyright-Jahr
1986
Verlag
Springer Netherlands
Electronic ISBN
978-94-017-3385-4
Print ISBN
978-90-481-8425-5
DOI
https://doi.org/10.1007/978-94-017-3385-4