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

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6.14<br />

Sealing. Standard oil field practices for cementing in casing have satisfactorily iso-<br />

lated deep high-pressure gas zones from shallower formations and from the surface for time<br />

periods measured in decades. Plugs <strong>of</strong> cement or other materials have been emplaced in aban-<br />

doned oil and gas wells, both cased and uncased, and have maintained integrity over similar<br />

periods <strong>of</strong> time. In these instances, it is not uncommon for the casing to corrode prior to<br />

plug deterioration.<br />

Logging/Instrumentation. Borehole geophysical logging techniques in existence and cur-<br />

rently under development will permit the logging and analyses <strong>of</strong> a number <strong>of</strong> parameters<br />

critical to the emplacement <strong>of</strong> radioactive waste in very deep holes. Caliper, acoustic,<br />

televiewer, and other borehole geophysical devices are regularly used to verify the presence<br />

and distribution <strong>of</strong> fractures in well bores. Electrical logs, neutron porosity loss recor-<br />

ders, and other devices are used to verify the presence <strong>of</strong> water. Temperature logs and spin-<br />

ner logs are used to detect water flow. While all <strong>of</strong> this equipment can be used from depths<br />

<strong>of</strong> hundreds to thousands <strong>of</strong> feet, none <strong>of</strong> these tools can function at the temperatures<br />

[between 200 and 300 C (390 and 570 F)] and pressures anticipated at depths around 10,000 m,<br />

because <strong>of</strong> the electronics contained in the probe.<br />

While rudimentary development <strong>of</strong> in situ stress measurements has been accomplished, the<br />

down-hole techniques would require significant improvement.<br />

Issues and R&D. Requirements<br />

Depth <strong>of</strong> Hole. The hole depth required for adequate isolation from the biosphere would<br />

have to be determined by the geologic medium <strong>of</strong> interest and by the history and physical con-<br />

dition <strong>of</strong> that medium. Sedimentary rocks in some instances are considered as potential VDH<br />

locations, but only where they are considered to be lower in elevation than circulating<br />

groundwater, such as deep basins or hydrologically stable synclines. Crystalline rocks may<br />

be the best geologic medium for VDH disposal. Usable hole depth in crystalline rock would be<br />

influenced by the depth <strong>of</strong> ground-water circulation within that rock. Ground-water circula-<br />

tion in weathered granite near the surface in a humid environment will generally be signifi-<br />

cantly greater than in fresh granite in an arid to semiarid environment.<br />

R&D is required to determine the depth required in various geologic media to minimize the<br />

possiblity <strong>of</strong> significant circulation to ground-water systems. The top <strong>of</strong> the emplaced waste<br />

would still have to be significantly below possible contact with circulating ground water,<br />

and would have to be properly plugged and sealed against such contact.<br />

Drilling. The discussion <strong>of</strong> the present state <strong>of</strong> development <strong>of</strong> drilling makes it clear<br />

that emplacement <strong>of</strong> nuclear waste in very deep holes is not possible at this time given that<br />

(1) the waste canisters will be 31 to 36 cm (12 to 14 in.) in diameter and (2) the depth re-<br />

quired for isolation from the biosphere may be as great as 10,000 m. If it is assumed that<br />

these two criteria are valid for the conceptual system, then a number <strong>of</strong> problems related to<br />

drilling would have to be solved to attain emplacement in very deep holes. The key issue is<br />

whether it will be possible to develop the technology to drill to 10,000 m with a bottom hole

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