Abstract
Perrhenate (ReO4-), as a TcO4- analogue, was incorporated into mixed-anion sodalites from binary solutions containing ReO4- and a competing anion Xn- (Cl-, CO32-, SO42-, MnO4-, or WO42-). Our objective was to determine the extent of solid solution formation and the dependence of competing ion selectivity on ion size. Using equivalent aqueous concentrations of the anions (ReO4-/Xn- molar ratio=1:1), we synthesized mixed-anion sodalites from zeolite and NaOH at 90°C for 96h. The resulting solids were characterized by bulk chemical analysis, powder X-ray diffraction, scanning electron microscopy, and X-ray absorption near edge structure (XANES) spectroscopy to determine crystal structure, chemical composition, morphology, and rhenium (Re) oxidation state. Rhenium in the solid phase occurred predominately as Re(VII)O4- in the sodalites, which have a primitive cubic pattern in the space group P4-3n. The refined unit-cell parameters of the mixed sodalites ranged from 8.88 to 9.15Å and showed a linear dependence on the size and mole fraction of the incorporated anion(s). The ReO4- selectivity, represented by its distribution coefficient (Kd), increased in the following order: Cl-<NO3-<MnO4- and CO32-<SO42-<WO42- for the monovalent and divalent anions, respectively. The relationship between the ReO4- distribution coefficient and competing anion size was nonlinear. When the difference in ionic radius (DIR) between ReO4- and Xn- (n=1 or 2) was greater than ~12%, then ReO4- incorporation into sodalite was insignificant. The results imply that anion size is the major factor that determines sodalite anion compositions. Given the similarity in chemical behavior and anion size, ReO4- serves as a suitable analogue for TcO4- under oxidizing conditions where both elements are expected to remain as oxyanions in the +7 oxidation state.
| Original language | English |
|---|---|
| Pages (from-to) | 138-143 |
| Number of pages | 6 |
| Journal | Chemical Geology |
| Volume | 395 |
| DOIs | |
| State | Published - Feb 4 2015 |
Funding
This material is based upon work supported by the U.S. Department of Energy (DOE) , Office of Science , Biological and Environmental Research , Subsurface Biogeochemical Research Program (SBR) , and was performed at Washington State University under contract No. DE-PS02-09ER65075 and at Oak Ridge National Laboratory under contract No. DE-AC05-00OR22725 . Portions of this work were supported by DOE, Office of Science, Basic Energy Sciences , Chemical Sciences, Biosciences, and Geosciences Division, Heavy Element Chemistry Program and were performed at Lawrence Berkeley National Laboratory under contract No. DE-AC02-05CH11231 . Portions of this work were performed at the Stanford Synchrotron Radiation Lightsource (SSRL), which is a DOE office of Science user facility operated by Stanford University. We are also indebted to the staff at the Franceschi Microscopy and Imaging Center at Washington State University for access to and assistance with the use of their SEM facilities.
Keywords
- Anion selectivity
- Distribution coefficient
- Mixed-anion sodalites
- Nuclear waste
- Perrhenate
- Pertechnetate, technetium-99
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