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Title: The solubility of (UO[sub 2])[sub 3](PO[sub 4])[sub 2][center dot]4H[sub 2]O(s) and the formation of U(VI) phosphate complexes: Their influence in uranium speciation in natural waters

Journal Article · · Geochimica et Cosmochimica Acta; (United States)
;  [1]
  1. Royal Institute of Technology, Stockholm (Sweden)

Uranium is commonly associated in natural waters with O-containing ligands both in the aqueous and the solid phases. Phosphate is present in most of these systems; however, the thermodynamics of the U(VI)-H[sub 3]PO[sub 4] system are poorly known, particularly in the pH range of interest 6 to 9. Hence, the effect of phosphate on the migration of uranium in natural waters is not well understood. We have investigated the solubility of a well-characterized U(VI)-phoshpate phase in the pH range 3 to 9: (UO[sub 2])[sub 3](PO[sub 4])[sub 2][center dot]4H[sub 2]O(s). Analysis of these data indicates the formation of the predominant species UO[sub 2]HPO[sub 4](aq) and UO[sub 2]PO[sub 4] in the pH range 4-9. Their formation constants as well as the solubility constant of (UO[sub 2])[sub 3](PO[sub 4])[sub 2][center dot]4H[sub 2]O(s) have been determined. From the same experiments we have established the equilibrium constant of the hydroxide complex UO[sub 2](OH)[sub 3][sup [minus]]. A discussion of the hydrolysis of U(VI) is also reported. The effect of phosphate on the mobility of U in natural waters is assessed in the light of these new data. They indicate that in the pH range of most natural waters, 6 to 9, U(VI) will be associated to aqueous phosphate complexes when the total concentration ratio [PO[sup 3[minus]][sub 4]]T/CO[sup 2[minus]][sub 3]T is greater than 10[sup [minus]1].

OSTI ID:
7030941
Journal Information:
Geochimica et Cosmochimica Acta; (United States), Vol. 56:12; ISSN 0016-7037
Country of Publication:
United States
Language:
English