Appendices 5-13 - Nautilus Cares - Nautilus Minerals
Appendices 5-13 - Nautilus Cares - Nautilus Minerals
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