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Crystal Chemistry and Phase Relations in the Synthetic Minerals of Ceramic Waste Forms: I. Fluorite and Monazite Structure Phases

  • Gregory J. McCarthy
  • John G. Pepin
  • Dennis D. Davis
Part of the Advances in Nuclear Science & Technology book series (ANST)

Abstract

McCarthy (1–4) has suggested that synthetic minerals of the fluorite and monazite types are potentially ideal hosts for the lanthanide*-actinide** elements in nuclear wastes. He has synthesized numerous compositions of these structure types relevant to nuclear waste chemistries (1–5). Their geologic stability, radiation stability and high solid solution capacity for actinides have been previously discussed (1–10). The Ln and An elements are very important constituents of high level nuclear wastes (HLW) and transuranic wastes (TRU), and thus are receiving high priority consideration in the design of ceramic nuclear waste forms. The oxides of the Ln’s and An’s can constitute more than 50 weight percent (wt%) of some HLW formulations. Also included among the actinides are long-lived hazardous radionuclides such as Np-237, Pu-238 and Am-241. We discuss here crystal chemistry and recently determined phase relations data on synthetic fluorites and monazites in the context of designing synthetic minerals for HLW ceramics.

Keywords

Phase Relation Nuclear Waste Fluorite Structure Waste Form Nuclear Waste Management 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer Science+Business Media New York 1980

Authors and Affiliations

  • Gregory J. McCarthy
    • 1
  • John G. Pepin
    • 2
  • Dennis D. Davis
    • 2
  1. 1.Departments of Chemistry and GeologyNorth Dakota State UniversityFargoUSA
  2. 2.Materials Research LaboratoryThe Pennsylvania State UniversityUniversity ParkUSA

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