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Oceans of noise - Whale and Dolphin Conservation Society

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Energy source<br />

(Air gun array)<br />

28<br />

Sea surface)<br />

Hydrophone array<br />

(receivers /detectors)<br />

Figure 3.3. The basic components <strong>of</strong> a marine seismic reflection survey (the layers <strong>of</strong> the seabed<br />

are shaded).<br />

3.3.2. Marine seismic surveys<br />

Marine seismic surveys are commonly either two-dimensional (2-D) or three-dimensional (3-D),<br />

<strong>and</strong> the type <strong>of</strong> survey used not only affects the type <strong>of</strong> data collected but can also affect the<br />

extent <strong>and</strong> duration <strong>of</strong> exposure to high sound levels.<br />

Two-dimensional surveys employ a single airgun array <strong>and</strong> hydrophone streamer, <strong>and</strong> are<br />

conducted along single lines, or pre-determined tracks within an open grid, to produce a vertical<br />

slice or 2-D image through the earth's crust (McCauley 1994; Gull<strong>and</strong> <strong>and</strong> Walker 1998). The<br />

source in this type <strong>of</strong> survey is <strong>of</strong>ten made as strong as possible for maximum penetration<br />

(Gull<strong>and</strong> <strong>and</strong> Walker 1998). Two-dimensional seismic surveys provide little or no information<br />

about the true position <strong>of</strong> reflecting points in the sub-surface (Gull<strong>and</strong> <strong>and</strong> Walker 1998) <strong>and</strong> are<br />

typically used for speculative surveys covering large geographical areas (McCauley 1994).<br />

Three-dimensional seismic surveys are characterised by the need to record a grid <strong>of</strong> data, with<br />

each grid being close enough to allow processing along both grid axes (Gull<strong>and</strong> <strong>and</strong> Walker<br />

1998), <strong>and</strong> where each grid point is the centre <strong>of</strong> a grid cell (usually 25 m by 25 m). The<br />

appropriate processing grids can be used to produce a 3-D reconstruction <strong>of</strong> the traversed surface,<br />

giving a much higher resolution than conventional 2-D surveys. By their nature, 3-D surveys<br />

require accurate positioning <strong>and</strong> use multiple parallel hydrophone streamers <strong>of</strong>ten in conjunction<br />

with multiple airgun arrays. Tracklines are <strong>of</strong>ten separated by 50 or 100 m (McCauley 1994).<br />

Three-dimensional seismic surveys are typically used to define potential <strong>and</strong> / or existing<br />

hydrocarbon deposits <strong>and</strong> fewer exploration wells are needed as a result. However, there are now<br />

moves to use 3-D surveys for speculative exploration, with the extra cost being balanced by the<br />

quality <strong>and</strong> quantity <strong>of</strong> data produced (McBarnet 1993 in McCauley 1994).<br />

~12m

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