Affiliation:
1. Civil & Environmental Engineering & Earth Sciences University of Notre Dame Notre Dame Indiana 46556 USA
2. Department of Chemistry & Biochemistry University of Notre Dame Notre Dame IN 46556 USA
3. Oak Ridge National Laboratory Oak Ridge TN 37831 USA
4. Current address: Actinide Analytical Chemistry Los Alamos National Laboratory Los Alamos NM 87545 USA
Abstract
AbstractPlutonium(IV) oxalate hexahydrate (Pu(C2O4)2 ⋅ 6 H2O; PuOx) is an important intermediate in the recovery of plutonium from used nuclear fuel. Its formation by precipitation is well studied, yet its crystal structure remains unknown. Instead, the crystal structure of PuOx is assumed to be isostructural with neptunium(IV) oxalate hexahydrate (Np(C2O4)2 ⋅ 6 H2O; NpOx) and uranium(IV) oxalate hexahydrate (U(C2O4)2 ⋅ 6 H2O; UOx) despite the high degree of unresolved disorder that exists when determining water positions in the crystal structures of the latter two compounds. Such assumptions regarding the isostructural behavior of the actinide elements have been used to predict the structure of PuOx for use in a wide range of studies. Herein, we report the first crystal structures for PuOx and Th(C2O4)2 ⋅ 6 H2O (ThOx). These data, along with new characterization of UOx and NpOx, have resulted in the full determination of the structures and resolution of the disorder around the water molecules. Specifically, we have identified the coordination of two water molecules with each metal center, which necessitates a change in oxalate coordination mode from axial to equatorial that has not been reported in the literature. The results of this work exemplify the need to revisit previous assumptions regarding fundamental actinide chemistry, which are heavily relied upon within the current nuclear field.
Funder
Basic Energy Sciences
National Nuclear Security Administration
Subject
General Chemistry,Catalysis,Organic Chemistry
Cited by
1 articles.
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