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

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6.95<br />

6.1.5.5 Potential Impacts over the Long Term (Postemplacement)<br />

Potential Events<br />

Long-term impacts with the greatest potential significance are related to'glacial<br />

phenomena that are not well understood. For example, ice dynamics and climatic variations<br />

affecting glaciation might be altered by waste disposal activities. Regardless <strong>of</strong> whether<br />

meltdown, anchored emplacement, or surface storage were used, potentially major modifica-<br />

tions in the delicately balanced glacial environment could occur.<br />

One <strong>of</strong> the major areas <strong>of</strong> uncertainty stems from our limited understanding <strong>of</strong> ice sheet<br />

conditions. Little is known <strong>of</strong> the motion <strong>of</strong> the continental ice sheets except for surface<br />

measurements made close to the coast (Gow et al. 1968). Three general types <strong>of</strong> flow have<br />

been defined--sheet flow, stream flow, and ice-shelf movement (Mellor 1959). Each type <strong>of</strong><br />

flow appears to possess a characteristic velocity. It is also believed that ice sheets where<br />

bottom melting conditions exist may move almost as a rigid block, by sliding over the bed-<br />

rock. Where there is no water at the ice-bedrock interface, it is believed that the ice<br />

sheet moves by shear displacement in a relative thin basal layer. The formation <strong>of</strong> large<br />

bodies <strong>of</strong> water from the waste heat could affect the equilibrium <strong>of</strong> such ice sheets.<br />

In addition, two potential problems concerning the movement <strong>of</strong> the waste are unique to an<br />

ice sheet repository. First, the waste container would probably be crushed and breached once<br />

it reached the ice/ground interface as a result <strong>of</strong> ice/ground interaction. Second, the waste<br />

might be transported to the sea by ice movement.<br />

Compared with other disposal schemes, the probability <strong>of</strong> human intrusion would be very<br />

low because the disposal area would be located in the most remote and inaccessible part <strong>of</strong><br />

the world, presently with a low priority for exploration <strong>of</strong> natural resources or habitation.<br />

The lack <strong>of</strong> human activity in these areas would markedly decrease the chance <strong>of</strong> humans dis-<br />

turbing waste material emplaced in an ice sheet. Conversely, because <strong>of</strong> the remoteness <strong>of</strong><br />

these areas they are relatively unexplored. Therefore they could attract considerable future<br />

resource exploration.<br />

Potential Impacts<br />

After the waste is emplaced and man's control is relinquished or lost, possible impacts<br />

fall into two broad categories. One <strong>of</strong> these relates to the reappearance <strong>of</strong> the radioactive<br />

waste in the environment, and the other involves the chance that the presence <strong>of</strong> waste would<br />

trigger changes in the ice sheets that would have worldwide consequences. For options that<br />

would place the waste within the ice or at the ice/ground interface, significant research<br />

would be required to predict future ice movements, accumulation or depletion rates, subsur-<br />

face water flow rates, frictional effects at the interface, and trigger mechanisms. A major<br />

purpose <strong>of</strong> this research would be to compare the degree <strong>of</strong> sensitivity <strong>of</strong> the predicted<br />

behavior to man's ability to forecast long-term situations such as global weather patterns,<br />

stability <strong>of</strong> the ice sheets, and sea-level changes.

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