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

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K.3 ENGINEERED SORPTION BARRIERS<br />

K.26<br />

In addition to retardation <strong>of</strong> radionuclide migration with an appropriate canister<br />

design or inert coating <strong>of</strong> the waste form, certain materials can be used to absorb or other-<br />

wise slow radionuclide migration from the package and the repository.<br />

Possible retardation mechanisms include surface adsorption, ion exchange, coprecipita-<br />

tion, and redox effects. The use <strong>of</strong> coprecipitation appears impractical as a retardation<br />

mechanism because <strong>of</strong> its rather selective nature and because a wide range <strong>of</strong> radionuclide<br />

chemical species must be retarded.<br />

K.3.1 Performance Requirements<br />

Solids selected for radionuclide adsorption, ion exchange, and redox effects in several<br />

combinations can be used for repository backfilling, for an overpack in the immediate vicin-<br />

ity <strong>of</strong> the canister exterior, and/or for a protective packing between the waste form and the<br />

interior surface <strong>of</strong> the canister (Karn-Bransle-Sakerhet 1978). The sorption material must<br />

be mechanically, thermally, and chemically stable in the repository environment. Also, it<br />

must be dry when in contact with the canister interior and in the waste form radiation field<br />

to prevent accelerated canister corrosion or pressurization. Good heat conducting proper-<br />

ties and relatively low permeability to ground water also are desirable sorption material<br />

characteristics. If the material is used for repository backfilling, it should have suffi-<br />

cient loadbearing capacity to prevent cavern ro<strong>of</strong> collapse onto stored wastes and to prevent<br />

major movement <strong>of</strong> the waste canisters. The organic contents <strong>of</strong> the filling material should<br />

be very low, probably less than 1%, to avoid radionuclide complexing and enhanced migration<br />

rates. Materials may be added to affect oxidation-reduction changes that retard radionu-<br />

clide migration. Radionuclide migration rates <strong>of</strong> the elements antimony, iodine, neptunium,<br />

plutonium, ruthenium, technetium, and uranium may be affected by changes in the redox poten-<br />

tial.<br />

K.3.2 Sorption Materials Performance<br />

Research sponsored by the Office <strong>of</strong> Nuclear <strong>Waste</strong> Isolation (ONWI) is determining sorp-<br />

tion coefficients <strong>of</strong> many minerals and rocks that may be <strong>of</strong> interest for sorption barrier<br />

use. Swedish (Allard et al. 1977, Haggblom 1977) and Canadian (Acres Consulting Services,<br />

Ltd. 1977) workers also have ongoing programs to investigate sorption <strong>of</strong> radionuclides in<br />

clays and rocks. Sorption investigations involving 19 radionuclides that are <strong>of</strong> interest<br />

in waste disposal operations were summarized in a 1976 EPA literature search (Ames and Rai<br />

1978).<br />

The solution species formed from the radionuclides <strong>of</strong> the various elements are a pri-<br />

mary control on their adsorption by a potential retardant. Possible solution species, based<br />

on existing thermodynamic data, are shown in Table K.3.1. Rocks, soils, and sediments are<br />

predominately cation exchange materials. The inorganic anion exchangers include the amor-<br />

phous hydrated oxides from iron, aluminum, and manganese, which are found naturally, and<br />

other synthetic anion exchange materials such as zirconia or titania. The environmental<br />

factors reported to effect radionuclide adsorption are summarized in Table K.3.2.

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