Perrhenate incorporation into binary mixed sodalites: The role of anion size and implications for technetium-99 sequestration

被引:47
作者
Dickson, Johnbull O. [1 ]
Harsh, James B. [1 ]
Lukens, Wayne W. [2 ]
Pierce, Eric M. [3 ]
机构
[1] Washington State Univ, Dept Crop & Soil Sci, Pullman, WA 99164 USA
[2] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Div Chem Sci, Berkeley, CA 94720 USA
[3] Oak Ridge Natl Lab, Div Environm Sci, Oak Ridge, TN 37831 USA
关键词
Mixed-anion sodalites; Anion selectivity; Distribution coefficient; Perrhenate; Pertechnetate; technetium-99; Nuclear waste; RAY-ABSORPTION SPECTROSCOPY; TECHNETIUM; PERTECHNETATE; SPECIATION; BEHAVIOR; RHENIUM; NITRATE; NMR;
D O I
10.1016/j.chemgeo.2014.12.009
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
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 degrees C for 96 h. 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) O-4(-) in the sodalites, which have a primitive cubic pattern in the space group P (4) over bar 3n. The refined unit-cell parameters of the mixed sodalites ranged from 8.88 to 9.15 angstrom and showed a linear dependence on the size and mole fraction of the incorporated anion(s). The ReO4- selectivity, represented by its distribution coefficient (K-d), 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 similar to 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. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:138 / 143
页数:6
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