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Published online 12 March 2007
Published in Soil Sci Soc Am J 71:329-335 (2007)
DOI: 10.2136/sssaj2006.0159
© 2007 Soil Science Society of America
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Theoretical Solid/Solution Ratio Effects on Adsorption and Transport: Uranium(VI) and Carbonate

John M. Phillippia, Vijay A. Loganathana, Melissa J. McIndoea, Mark O. Barnetta,*, T. Prabhakar Clementa and Eric E. Rodenb

a Dep. of Civil Engineering, 238 Harbert Engineering, Center Auburn Univ., Auburn, AL 36849
b Dep. of Geology and Geophysics, Univ. of Wisconsin, 1215 W. Dayton St., Madison, WI 53706


Figure 1
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Fig. 1. Calculated adsorption isotherms in the absence of carbonate. A, B, and C correspond to the cases shown in Table 2.

 

Figure 2
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Fig. 2. Calculated adsorption isotherms as a function of solid/solution ratio with total carbonate of 0.01 M. G, H, and I correspond to the cases shown in Table 2.

 

Figure 3
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Fig. 3. Calculated adsorption isotherms with solid/solution ratio set at 3.33 g L–1 with carbonate concentration varying from 0.0 to 0.01 M. A, D, and G correspond to the cases shown in Table 2.

 

Figure 4
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Fig. 4. Calculated adsorption isotherms at a solid/solution ratio of 333 g L–1. O, C, and I correspond to the cases shown in Table 2.

 

Figure 5
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Fig. 5. Calculated percentage of surface sites occupied by the adsorbed species at a solid/solution ratio of 333 g L–1 and total carbonate (CTCO3) = 0.01 M, Case I in Table 2.

 

Figure 6
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Fig. 6. Calculated percentage of surface sites occupied by the adsorbed species at a solid/solution ratio of 333 g L–1 and total carbonate (CTCO3) = 0.01 M in the absence of U(VI)–carbonate aqueous complexes, Case O in Table 2.

 

Figure 7
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Fig. 7. Calculated total aqueous carbonate vs. solid/solution ratio with a total carbonate of 0.01 M (pH = 7, ionic strength I = 0.1 M). The total aqueous carbonate is dependent on the solid/solution ratio, but all of the points (I–IV) still fall on the carbonate adsorption isotherm (Fig. 8).

 

Figure 8
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Fig. 8. Calculated adsorption isotherm for carbonate at a solid/solution ratio of 333 g L–1 (Case M in Table 2). In the absence of U(VI), the carbonate isotherm is independent of the solid/solution ratio (not shown). Points I to IV correspond to the same points as in Fig. 7.

 





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