TY - JOUR
T1 - Synthesis and thermodynamics of uranium-incorporated α-Fe2O3 nanoparticles
AU - Lam, Andy
AU - Hyler, Forrest
AU - Stagg, Olwen
AU - Morris, Katherine
AU - Shaw, Samuel
AU - Velázquez, Jesús M.
AU - Navrotsky, Alexandra
N1 - Funding Information:
This work was supported by the U.S. Department of Energy, Office of Basic Energy Sciences, grant DE-FG02-97ER14749 (Thermodynamics of Minerals Stable near Earth's Surface). Support was also provided by the Nuclear Regulatory Commission (31310019M0009) through the Advancing Scientific Careers to Enhance Nuclear Technologies (ASCENT) program. We thank the University of California, Davis for start-up funding, as well as the Research Corporation for Science Advancement (RCSA 26780) through the Cottrell Scholar program. We also acknowledge funding support from the NSF through the Faculty Early Career Development Program (DMR-2044403). Diamond Light Source provided beam-time (SP17243), and the authors thank Steve Parry for his beamline assistance.
Funding Information:
This work was supported by the U.S. Department of Energy, Office of Basic Energy Sciences, grant DE-FG02-97ER14749 (Thermodynamics of Minerals Stable near Earth's Surface). Support was also provided by the Nuclear Regulatory Commission (31310019M0009) through the Advancing Scientific Careers to Enhance Nuclear Technologies (ASCENT) program. We thank the University of California, Davis for start-up funding, as well as the Research Corporation for Science Advancement (RCSA 26780) through the Cottrell Scholar program. We also acknowledge funding support from the NSF through the Faculty Early Career Development Program (DMR-2044403). Diamond Light Source provided beam-time (SP17243), and the authors thank Steve Parry for his beamline assistance.
Publisher Copyright:
© 2021
PY - 2021/12/1
Y1 - 2021/12/1
N2 - Hematite nanoparticles were synthesized with U(VI) in circumneutral water through a coprecipitation and hydrothermal treatment process. XRD, TEM, and EXAFS analyses reveal that uranium may aggregate along grain boundaries and occupy Fe sites within hematite. The described synthesis method produces crystalline, single-phase iron oxide nanoparticles absent of surface-bound uranyl complexes. EXAFS data were comparable to spectra from existing studies whose syntheses were more representative of naturally occurring, extended aging processes. This work provides and validates an accelerated method of synthesizing uranium-immobilized iron oxide nanoparticles for further mechanistic studies. High temperature oxide melt solution calorimetry measurements were performed to calculate the thermodynamic stability of uranium-incorporated iron oxide nanoparticles. Increasing uranium content within hematite resulted in more positive formation enthalpies. Standard formation enthalpies of UxFe2–2xO3 were as high as 76.88 ± 2.83 kJ/mol relative to their binary oxides, or -764.04 ± 3.74 kJ/mol relative to their constituent elements, at x = 0.037. Data on the thermodynamic stability of uranium retention pathways may assist in predicting waste uranyl remobilization, as well as in developing more effective methods to retain uranium captured from aqueous environments.
AB - Hematite nanoparticles were synthesized with U(VI) in circumneutral water through a coprecipitation and hydrothermal treatment process. XRD, TEM, and EXAFS analyses reveal that uranium may aggregate along grain boundaries and occupy Fe sites within hematite. The described synthesis method produces crystalline, single-phase iron oxide nanoparticles absent of surface-bound uranyl complexes. EXAFS data were comparable to spectra from existing studies whose syntheses were more representative of naturally occurring, extended aging processes. This work provides and validates an accelerated method of synthesizing uranium-immobilized iron oxide nanoparticles for further mechanistic studies. High temperature oxide melt solution calorimetry measurements were performed to calculate the thermodynamic stability of uranium-incorporated iron oxide nanoparticles. Increasing uranium content within hematite resulted in more positive formation enthalpies. Standard formation enthalpies of UxFe2–2xO3 were as high as 76.88 ± 2.83 kJ/mol relative to their binary oxides, or -764.04 ± 3.74 kJ/mol relative to their constituent elements, at x = 0.037. Data on the thermodynamic stability of uranium retention pathways may assist in predicting waste uranyl remobilization, as well as in developing more effective methods to retain uranium captured from aqueous environments.
KW - Calorimetry
KW - Hematite
KW - Iron oxides
KW - Uranyl
KW - Water remediation
KW - X-ray absorption spectroscopy
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U2 - 10.1016/j.jnucmat.2021.153172
DO - 10.1016/j.jnucmat.2021.153172
M3 - Article
AN - SCOPUS:85109952331
SN - 0022-3115
VL - 556
JO - Journal of Nuclear Materials
JF - Journal of Nuclear Materials
M1 - 153172
ER -