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UNDERSTANDING VARIATION IN PARTITION COEFFICIENT, Kd ...

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J.1.0 Background<br />

Appendix J<br />

Partition Coefficients For Uranium<br />

The review of uranium K d values obtained for a number of soils, crushed rock material, and<br />

single-mineral phases (Table J.5) indicated that pH and dissolved carbonate concentrations are the<br />

2 most important factors influencing the adsorption behavior of U(VI). These factors and their<br />

effects on uranium adsorption on soils are discussed below. The solution pH was also used as the<br />

basis for generating a look-up table of the range of estimated minimum and maximum K d values<br />

for uranium.<br />

Several of the studies identified in this review demonstrate the importance dissolved carbonate<br />

through the formation of strong anionic carbonato complexes on the adsorption and solubility of<br />

dissolved U(VI). This complexation especially affects the adsorption behavior of U(VI) at<br />

alkaline pH conditions. Given the complexity of these reaction processes, it is recommended that<br />

the reader consider the application of geochemical reaction codes, and surface complexation<br />

models in particular, as the best approach to predicting the role of dissolved carbonate in the<br />

adsorption behavior of uranium and derivation of K d values when site-specific K d values are not<br />

available for U(VI).<br />

J.2.0 Availability of K d Values for Uranium<br />

More than 20 references were identified that reported the results of K d measurements for the<br />

sorption of uranium onto soils, crushed rock material, and single mineral phases. These studies<br />

were typically conducted to support uranium migration investigations and safety assessments<br />

associated with the genesis of uranium ore deposits, remediation of uranium mill tailings,<br />

agriculture practices, and the near-surface and deep geologic disposal of low-level and high-level<br />

radioactive wastes (including spent nuclear fuel).<br />

A large number of laboratory uranium adsorption/desorption and computer modeling studies have<br />

been conducted in the application of surface complexation models (see Chapter 5 and Volume I)<br />

to the adsorption of uranium to important mineral adsorbates in soils. These studies are also<br />

noted below.<br />

Several published compilations of K d values for uranium and other radionuclides and inorganic<br />

elements were also identified during the course of this review. These compilations are also briefly<br />

described below for the sake of completeness because the reported values may have applicability<br />

to sites of interest to the reader. Some of the K d values in these compilations are tabulated below,<br />

when it was not practical to obtain the original sources references.<br />

J.2

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