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.Ollg rallge shock \I'a\'('s (rolll a large cxployiol7 {lI/dcrl1'otcr: experilllellt and data<br />

2.3 OUTLINE PLAN OF THE EXPERIMENT<br />

The central concept of the experiment at sea is shown in the plan in<br />

Fig. 2.2 and cross-section in Fig. 2.3. The specific details of the<br />

listening equipment packages, such as the, instrument responses, package<br />

sizes etc, are described in the next chapter. The logistics of the<br />

experiment at sea required two ships: RMAS Salmaster and RMAS Goosander.<br />

Many of the underlying reasons and background information for adopting<br />

specific details in this plan are explained later in this report.<br />

It was decided to opt for six PUll-up Shallow Vater Seismometers<br />

(PUSSes) to be deployed on the sea bottom in a line between the coast and<br />

the shot point. The chosen shot point was located around 57°7N, 0045V.<br />

The recording great circle line extends from the coastal seismometer<br />

station at Tentsmuir in Fife (TMA in Fig. 2.2) , to the shot point. Each<br />

PUSS was to be deployed from the Salmaster in about 50-70 m of water.<br />

Once deployed each PUSS is self contained<br />

have to be retrieved after detonating the<br />

3-component geophone and one hydrophone.<br />

90 minutes of 4-channel data; this 90<br />

but is not disposable and would<br />

charge. Each PUSS contains one<br />

Each PUSS can record a total of<br />

minutes can be divided into<br />

pre-selected time windows of arbitrary length and 10 minutes was the<br />

selected option. Coordination of PUSS recording time windows and<br />

potential firing times of the explosion is obviously vital.<br />

One BGS sea bottom package was to be deployed by the Salmaster on the<br />

sea-bed in about 50-70 m of water on the shore-shot line (TMA to explosion<br />

in Fig 2.2). This package is not self contained. It would need to be<br />

cable- linked to the moored and stationery Salmaster, either directly or<br />

via mooring buoys. This cable would carry signals received at the BGS sea<br />

bottom package to recorders on board the Salmaster. The BGS sea bottom<br />

package contains one 3-component piezo-electric seismometer and one<br />

hydrophone. In addition, it was necessary for the recorder on the<br />

Salmaster to record an accurate time standard such as MSF transmitted from<br />

Rugby.<br />

A vertical hydrophone string (VHS) would also be deployed on the<br />

shore-shot line near to the BGS sea bottom package (Fig.2.3) and would be<br />

deployed by the Salmaster. The VHS would extend to the sea bottom and<br />

9

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