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standardization of environmental data and information - International ...

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?? Classification <strong>of</strong> facies types should be verified by looking at their<br />

surface with a video system.<br />

?? Samples should be gathered <strong>and</strong> tested onboard for various<br />

properties.<br />

?? Finally, laboratory testing <strong>and</strong> modelling should be conducted.<br />

In conclusion, he suggested that the large-scale <strong>and</strong> sediment<br />

parameters he had described be used also as an <strong>environmental</strong> framework<br />

for defining the benthic communities.<br />

SUMMARY OF DISCUSSION<br />

Sonar mapping anomalies<br />

A participant from the Korea Ocean Research <strong>and</strong> Development<br />

Institute (KORDI) said his organisation, using a 12 kHz side-scan sonar<br />

system on a manganese nodule field, had found a substantially higher<br />

backscattering strength than Wiedicke had reported. This was a st<strong>and</strong>ard<br />

frequency used in Hydrosweep <strong>and</strong> many other deep-water systems. As<br />

KORDI had generally found a greater abundance <strong>of</strong> nodules, his people had<br />

thought at first that this might be due to reflection from the nodules<br />

themselves. Another possible explanation, however, was that, because the<br />

wavelength at 12 kHz was much bigger than the nodule, the effect might be<br />

due to the physical property <strong>of</strong> the substrate 10 or 20 metres below the<br />

nodules; thus, besides a reflection directly from the nodules, it was also<br />

coming from the upper substrate.<br />

Wiedecke-Hombach replied that similar observations had been<br />

recorded in the Pacific Ocean with other kinds <strong>of</strong> side-scan sonar systems;<br />

strange features had been found that could not be observed on the surface.<br />

The effect had been ascribed to interference <strong>of</strong> the signal wavelength <strong>and</strong><br />

its penetration into the uppermost sediment layer. A side-scan sonar<br />

system should be geared to the particular target; with small nodules, higher<br />

frequencies might have to be used so that nodule distribution would not be<br />

confused with sediment properties.<br />

164 INTERNATIONAL SEABED AUTHORITY

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