Startseite Neptunium incorporation into uranyl compounds that form as alteration products of spent nuclear fuel: Implications for geologic repository performance
Artikel
Lizenziert
Nicht lizenziert Erfordert eine Authentifizierung

Neptunium incorporation into uranyl compounds that form as alteration products of spent nuclear fuel: Implications for geologic repository performance

  • Peter C. Burns , Kathryn M. Deely und Suntharalingam Skanthakumar
Veröffentlicht/Copyright: 25. September 2009

Summary

Alteration of spent nuclear fuel in a geological repository under oxidizing conditions is likely to result in abundant uranyl compounds. Incorporation of radionuclides into the uranyl alteration phases may significantly reduce their mobility, thereby impacting repository performance. The following compounds have been synthesized from solutions containing from ∼10 to 500ppm Np5+: meta-schoepite, UO3·2H2O; Na-compreignacite, Na2[(UO2)3O2(OH)3]2(H2O)7; uranophane, Ca(UO2)2(SiO3OH)2(H2O)5; and β-(UO2)(OH)2. The structures of each involve sheets of uranyl polyhedra; the interlayers contain cations and H2O groups in Na-compreignacite and uranophane, only H2O in meta-schoepite, and β-(UO2)(OH)2 does not contain interlayer constituents. Synthesized powders were characterized by X-ray powder diffractometry, and were analyzed by ICP-AES (U, Na, Ca) and ICP-MS (Np). Aliquots of the powders were washed in 0.5M acetic acid to remove sorbed Np prior to analysis. The powders of meta-schoepite and β-(UO2)(OH)2 contained at most a few ppm Np5+. In contrast, powders of Na-compreignacite and uranophane contained Np5+ in proportion to the Np5+ concentration in the mother solution, and powders of each containing more than 400ppm Np5+ (of total Np + U) were obtained. Incorporation of Np5+ into uranyl compounds that form in a geological repository appears possible, and may impact the mobility of Np.

Published Online: 2009-9-25
Published in Print: 2004-3-1

© 2004 Oldenbourg Wissenschaftsverlag GmbH

Heruntergeladen am 14.10.2025 von https://www.degruyterbrill.com/document/doi/10.1524/ract.92.3.151.30491/html?lang=de
Button zum nach oben scrollen