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Appendices 5-13 - Nautilus Cares - Nautilus Minerals

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2 Methods<br />

2.1! Source modelling<br />

Cavitation in water occurs when the pressure in a particular location drops below the<br />

saturated water vapour pressure. Bubbles of water vapour then form - the water<br />

effectively boils, but due to a lowering of pressure, rather than the increase in water<br />

vapour pressure with temperature. When these bubbles move into a region of higher<br />

pressure they implode violently, producing a sharp, impulsive sound.<br />

For a propeller, there is a low pressure region on the forward face of each blade which can<br />

(and usually does) result in the continuous formation of cavitation bubbles, which<br />

subsequently move into a region of higher pressure and implode. The combined effect of<br />

the implosion of many cavitation bubbles is high intensity, broadband noise, usually<br />

modulated at the propeller blade rate (the shaft rotation rate multiplied by the number of<br />

blades).<br />

Because of its importance for passive sonar detection of ships and submarines, cavitation<br />

noise has been extensively studied (see eg. Ross, 1987), however this has been in the<br />

context of ships travelling at speed, rather than ships holding station on DP. The source<br />

model used in this report is therefore based on measurements made by one of the authors<br />

of underwater sound levels produced by a rig tender (Pacific Ariki) on DP (McCauley<br />

1998). The characteristics of the Pacific Ariki are given in Table 1, and the measured,<br />

third octave source spectrum is shown in Figure 2. The Pacific Ariki is a much smaller<br />

vessel than the proposed mining vessel (see Table 1). Levels have therefore been<br />

extrapolated to those to be expected for a larger vessel by assuming that a constant<br />

proportion of the mechanical power is converted to acoustic power. This relationship has<br />

been found to hold reasonably well for surface vessels operating at their normal cruising<br />

speed (Ross 1987). The source level corrections given in Table 1 are therefore given by:<br />

Correction 10<br />

( P % vessel<br />

) 10 log<br />

&<br />

# (dB)<br />

' PAriki<br />

$<br />

where P vessel is the total installed thruster power on the vessel, and P Ariki is the total<br />

installed thruster power on Pacific Ariki. The resulting source spectrum is shown in<br />

7

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