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

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5.54<br />

chlorosis <strong>of</strong> young trifoliate leaves. Effects on vegetation will depend on air concentra-<br />

tion and time <strong>of</strong> exposure as well as humidity. Generally, an air concentration above<br />

10 Pg/m 3 will alter distribution and growth <strong>of</strong> plants (Bernstein and Hayward 1958). Because<br />

fenceline ground level concentrations for salt dust released from surface storage and<br />

handling operations will exceed this level, a significant affect would be expected. The<br />

deposition rates are in the range <strong>of</strong> 40 to 95 gm/m2/yr for observable leaf-burn on such<br />

plants as beans. Based on the assumptions made for determining salt depositions, mitigating<br />

procedures would be needed to reduce salt dispersal at least two orders <strong>of</strong> magnitude to<br />

ensure that emission concentrations are well below levels toxic to plant life. Once con-<br />

taminated, salt-affected soils will require special remedial measures and management prac-<br />

tices to restore them to their original productivity.<br />

Potentially, salt would be deposited as dust on the land and would also be transported<br />

by run<strong>of</strong>f to nearby surface waters. Salt concentrations on the order <strong>of</strong> 8000 parts per mil-<br />

lion (ppm) are lethal to freshwater fish under conditions <strong>of</strong> acute exposure (Jones 1964),<br />

and the recommended limit for chronic exposure is 80 ppm or 0.01 <strong>of</strong> the acute toxicity level<br />

(NAS 1972). The possibility exists for surface waters, particularly shallow, catch basin-<br />

type ponds, to receive amounts <strong>of</strong> salt sufficient to damage indigenous aquatic plants and<br />

animals. Resident species might also be replaced by more salt-tolerant forms.<br />

In addition to effects from dust deposition, localized effects occur from leaching<br />

around the surface storage area. Fluctuations in concentrations <strong>of</strong> soil salinity would<br />

depend on precipitation, drainage, seepage, wind and rain erosion rates, and salt concentra-<br />

tions in water and air that come into contact with the soil. Increased salinity around the<br />

storage area would decrease or eliminate plant growth, because high salt concentrations in<br />

soil reduce the rate at which plants absorb water. This would limit the use <strong>of</strong> vegetation<br />

to increase the aesthetic qualities <strong>of</strong> the storage area and to control dust.<br />

5.4.4.2 Ecological Effects for a Repository in Granite<br />

A deep geologic radioactive waste repository in granite would be potentially less eco-<br />

logically damaging than a salt repository and as a consequence would require fewer mitigat-<br />

ing measures. During construction, about 8 x 107 MT <strong>of</strong> rock would be mined and 4 x 107 MT<br />

would require disposal. For convenience <strong>of</strong> operation the granite would probably be crushed<br />

in the mine before being brought to the surface, thereby reducing the airborne dust contami-<br />

nation at the surface.<br />

Possible methods <strong>of</strong> disposal include removal for use in construction projects (e.g.,<br />

dams, highways) or surface disposal. Neither <strong>of</strong> these alternatives pose serious ecological<br />

problems. Apart from land use associated with surface storage <strong>of</strong> the mined material,<br />

several hundred tons <strong>of</strong> airborne particulates may be released yearly. Environmental release<br />

<strong>of</strong> this material to land or surface water could be limited by establishing a vegetation<br />

cover for the stored rock, and by proper draining and ponding the surface run<strong>of</strong>f.<br />

During construction <strong>of</strong> a granite repository, as with shale and basalt, water may enter<br />

either through downward flow from the overlying strata or through upwelling from lower

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