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

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5.90<br />

a few years. For purposes <strong>of</strong> this accident analysis the well(s) could operate for 50 years<br />

before being abandoned because <strong>of</strong> failure caused by cave-in and crushing and plugging <strong>of</strong><br />

piping with debris.<br />

This accidental repository intrusion, as in the case <strong>of</strong> the drilling accident, is based<br />

on the assumption that repository markers are either no longer evident, are misunderstood or<br />

ignored. Salt deposits are relatively plentiful and drilling to 600 m for salt seems<br />

highly unrealistic. No probabilities could be assigned to this event; it is presented only<br />

as a hypothetical "what if" accident.<br />

Ordinarily, once the brines are brought to the surface they are analyzed to determine<br />

the kinds and amounts <strong>of</strong> impurities such as calcium sulfate, calcium-magnesium carbonate,<br />

sulfides, etc., which would govern further processing to purify the salt. If radioactive<br />

waste is placed in repositories in salt formations, salt used for human consumption could<br />

be checked by radioanalysis as well (an institutionally administered precaution). Calcula-<br />

tions suggest that radioactivity would be determinable with <strong>of</strong>f-the-shelf gamma-ray spec-<br />

trometer apparatus on samples <strong>of</strong> a few hundred grams at concentrations <strong>of</strong> waste in salt<br />

existing after a few days <strong>of</strong> mining operation and with certainty by one month <strong>of</strong> mining<br />

operation.<br />

Assumptions <strong>of</strong> the scenario are that, although the salt stratum <strong>of</strong> the reference site<br />

is about 80 m thick, the salt removed is principally that from backfill, ceiling, pillars<br />

and floor where radioactive waste has been placed. In mining the repository.about 33 mil-<br />

lion tons <strong>of</strong> salt would have been removed for waste placement. This represents about one-<br />

fourth <strong>of</strong> the total salt volume in the mined area (in the scenario, the repository has been<br />

backfilled completely with salt; actually backfill <strong>of</strong> about 60% is presently planned). The<br />

total salt postulated to be solution mined over 50 years is then about 130 million tons.(a)<br />

This represents about 10% <strong>of</strong> the total salt contained in the salt stratum bounded by the<br />

repository area. If an equal amount <strong>of</strong> salt is mined in each <strong>of</strong> 50 years, the annual pro-<br />

duction would be about 2.6 million tons. In 1957 about 24 million tons <strong>of</strong> salt were pro-<br />

duced in the United States (Kaufmann 1960). Such a solution mining operation for salt would<br />

exceed the size <strong>of</strong> those presently in operation in the United States; a very large operation<br />

in the United States produces about 0.4 million tons annually and in Europe a very large<br />

operation may produce on the order <strong>of</strong> 1 million tons <strong>of</strong> salt annually.<br />

Given that 100 parts <strong>of</strong> water (at 20 to 100 C) by weight can dissolve 36 to 39 parts <strong>of</strong><br />

salt, then over a 50-yr period a stream flow <strong>of</strong> 210 /sec is required to dissolve that much<br />

(a) Although it is believed that radioanalysis <strong>of</strong> salt would result in termination <strong>of</strong> the<br />

operation soon after start-up, the scenario is developed based on removal <strong>of</strong> the repository<br />

salt over a 50-yr period. Amounts <strong>of</strong> wastes and salt brought to the surface<br />

over shorter periods <strong>of</strong> time are pro-rated based on water contact with all wastes by<br />

the end <strong>of</strong> 50 years. Consequences are based on the assumption that the presence <strong>of</strong><br />

radioactivity goes undetected for one year.

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