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Management of Commercially Generated Radioactive Waste - U.S. ...

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6.59<br />

Radionuclides might be sorbed by the host rock, which would substantially retard the<br />

waste transport within the lens. Sediments that might exist at the shoreline in the dis-<br />

charge zone could have useful sorption properties and retard radionuclides prior to dis-<br />

charge and dilution in the seawater.<br />

Ground-water Transport, Saline Zone Location. It has been suggested that <strong>of</strong>fshore<br />

islands may have essentially static saline ground water at depth, due to the absence <strong>of</strong><br />

hydraulic gradients at sea level. However, the residual or continuing effects <strong>of</strong> oceano-<br />

graphic, geothermal, climatological , or other changes may create flow. These effects would<br />

need to be examined prior to siting a repository in such a location (see Figure 6.1.11).<br />

Flow transport in the saline zone may be accompanied by dispersion and diffusion, which<br />

would result in reduced concentrations at a distance from the repository. The amount <strong>of</strong><br />

sorption <strong>of</strong> radionuclides in the host rock or on seabed sediments would depend on the parti-<br />

cular radionuclide, ground-water, and rock or sediment chemistry.<br />

Seawater Contamination. It appears that the principal discharge <strong>of</strong> wastes from an island<br />

repository would be into the seawater, possibly through sediments. Discharge might occur in<br />

a relatively concentrated near-surface zone if the waste were located in the freshwater lens.<br />

This could cause contamination <strong>of</strong> littoral and near-surface aquatic systems.<br />

Discharge from wastes located in the saline ground-water zone would likely be dispersed<br />

through the seabed if the thermal-convection effects were insufficient to distort the flow<br />

patterns significantly.<br />

Volcanism. Some islands, particularly those in island arcs and to a lesser extent oce-<br />

anic islands, are frequently highly active seismically and volcanically. Such activity could<br />

discharge the waste in either lava flows or into the atmosphere. Geologic data for the most<br />

recent volcanic event would be relied upon to establish inactivity before an island was<br />

selected as a disposal site.<br />

Potential Impacts<br />

In determining the potential impacts <strong>of</strong> island disposal over the long term, the follow-<br />

ing factors would be considered:<br />

* Corrosion, leaching, and transportation <strong>of</strong> radionuclides to the biosphere by the ground<br />

water<br />

* The influence <strong>of</strong> thermal effects on flow<br />

* Thermal/mechanical effects on permeability and porosity<br />

* Retardation <strong>of</strong> radionuclides on rock fractures and seabed sediments<br />

* Sediment and current movements<br />

* Pathways to man via marine organisms, typical marine activities, and island<br />

considerations.

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