Immobilizing Pertechnetate in Ettringite via Sulfate Substitution
Author(s) -
Sarah A. Saslow,
Sébastien Kerisit,
Tamás Varga,
Sebastian T. Mergelsberg,
Claire L. Corkhill,
Michelle M.V. Snyder,
Nancy M. Avalos,
Antonia S. Yorkshire,
Daniel J. Bailey,
Jarrod V. Crum,
R. Matthew Asmussen
Publication year - 2020
Publication title -
environmental science and technology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.851
H-Index - 397
eISSN - 1520-5851
pISSN - 0013-936X
DOI - 10.1021/acs.est.0c03119
Subject(s) - ettringite , sulfate , substitution (logic) , pertechnetate , chemistry , geochemistry , geology , nuclear chemistry , materials science , technetium , metallurgy , organic chemistry , cement , computer science , portland cement , programming language
Technetium-99 immobilization in low-temperature nuclear waste forms often relies on additives that reduce environmentally mobile pertechnetate (TcO 4 - ) to insoluble Tc(IV) species. However, this is a short-lived solution unless reducing conditions are maintained over the hazardous life cycle of radioactive wastes (some ∼10,000 years). Considering recent experimental observations, this work explores how rapid formation of ettringite [Ca 6 Al 2 (SO 4 ) 3 (OH) 12 ·26(H 2 O)], a common mineral formed in cementitious waste forms, may be used to directly immobilize TcO 4 - . Results from ab initio molecular dynamics (AIMD) simulations and solid-phase characterization techniques, including synchrotron X-ray absorption, fluorescence, and diffraction methods, support successful incorporation of TcO 4 - into the ettringite crystal structure via sulfate substitution when synthesized by aqueous precipitation methods. One sulfate and one water are replaced with one TcO 4 - and one OH - during substitution, where Ca 2+ -coordinated water near the substitution site is deprotonated to form OH - for charge compensation upon TcO 4 - substitution. Furthermore, AIMD calculations support favorable TcO 4 - substitution at the SO 4 2- site in ettringite rather than gypsum (CaSO 4 ·2H 2 O, formed as a secondary mineral phase) by at least 0.76 eV at 298 K. These results are the first of their kind to suggest that ettringite may contribute to TcO 4 - immobilization and the overall lifetime performance of cementitious waste forms.
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