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standardization of environmental data and information - International ...

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ecolonisation rates. If the area was recolonised in a week, recovery from a<br />

large-scale disturbance might be relatively fast. If it took ten years, recovery<br />

might be relatively slow. One thing that had been learned in regard to<br />

<strong>st<strong>and</strong>ardization</strong> <strong>and</strong> the design <strong>of</strong> monitoring <strong>and</strong> impact studies was that<br />

different components <strong>of</strong> the ecosystem would not respond in the same way<br />

<strong>and</strong> might need to be monitored with different techniques <strong>and</strong> time scales.<br />

Tailings discharge<br />

A question was raised about whether mining tailings were likely to<br />

be discharged at the surface or in mid-water. Smith replied that, as he<br />

understood current thinking, surface discharge should be minimized though<br />

some was inevitable. One approach, for purposes <strong>of</strong> discussion, might be<br />

that, since a big plume was being created by mining in the benthic boundary<br />

layer, the discharge should take place in the part <strong>of</strong> the environment<br />

already sullied.<br />

Mr. Lenoble observed that for the time being there was no<br />

regulation about this problem because most regulations dealt only with<br />

exploration. Companies active in this sphere were thinking <strong>of</strong> ways to<br />

reduce surface discharge but there had been little or no testing; they would<br />

have time to do that during the 15-year exploration phase. The discharge at<br />

the surface would come not only from the sediment but also from the fine<br />

particles <strong>of</strong> manganese hydroxide produced during the transportation <strong>and</strong><br />

manipulation <strong>of</strong> the nodules. There would in fact be another discharge, at<br />

the bottom during nodule collection, when some separation would take<br />

place between nodules <strong>and</strong> sediment to avoid raising most <strong>of</strong> the sediment<br />

to the surface, thereby reducing surface discharge. The problem at the<br />

bottom would be to try to discharge the sediment in such a way as to avoid<br />

making a big plume above the seabed <strong>and</strong> to avoid dispersion <strong>of</strong> the<br />

sediment by having the plume flatten quickly to the bottom.<br />

Another participant commented that the discharge level was more<br />

<strong>of</strong> an <strong>environmental</strong> than an engineering issue, since a system could be<br />

designed either way. It was premature to specify the level, given the lack <strong>of</strong><br />

<strong>environmental</strong> knowledge.<br />

Smith agreed that a recommendation as to the location <strong>of</strong> the<br />

discharge would be premature. However, perhaps the Workshop might<br />

propose some scenarios for discharge experiments. Otherwise, if there<br />

were only one or two cases <strong>of</strong> test mining, with no recommendations about<br />

discharge depth <strong>and</strong> monitoring, there would be no opportunity to study<br />

INTERNATIONAL SEABED AUTHORITY 80

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