The relationship between Mn oxidation state and structure in triclinic and hexagonal birnessites
Abstract
Because of their nanocrystallinity and high cation exchange capacities, birnessite phases can control the cycling of heavy metals in soils and groundwaters, and they also are implicated in the oxidation of transition metals in natural environments. Birnessite reactivity is determined by crystal structure and composition. Because birnessites typically are poorly crystalline, synchrotron-based absorption spectroscopy (EXAFS, XANES) often is utilized for structural characterization. For example, linear combination fitting (LCF) of X-ray absorption spectra typically is applied to quantify mixed triclinic and hexagonal birnessite phases. This approach is challenged, however, because the structures of the standards are not always plainly apparent. Moreover, it is difficult to distinguish birnessites with nanoscale intergrowths of hexagonal and triclinic endmembers from homogeneous birnessite structures of “intermediate triclinicity”. In this study, we explored these issues by synthesizing a host of cation-exchanged birnessite specimens whose long-range symmetrical character could be determined by X-ray diffraction without ambiguity. Through a combination of Fourier transform infrared spectroscopy (FTIR), extended X-ray absorption fine structure (EXAFS), and X-ray photoelectron spectroscopy (XPS), we have examined the relationships among structural symmetry, Mn oxidation state, and interlayer composition. Our results confirm prior models that as the concentration of Mn3+ increases, the departure from hexagonal symmetry alsomore »
- Authors:
-
- Pennsylvania State Univ., University Park, PA (United States)
- Smithsonian Inst., Washington, DC (United States)
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
- Publication Date:
- Research Org.:
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States). Environmental Molecular Sciences Lab. (EMSL); Argonne National Lab. (ANL), Argonne, IL (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC), Basic Energy Sciences (BES). Chemical Sciences, Geosciences & Biosciences Division; USDOE Office of Science (SC), Biological and Environmental Research (BER); National Science Foundation (NSF); USDOE Office of Science (SC), Basic Energy Sciences (BES)
- OSTI Identifier:
- 1773815
- Alternate Identifier(s):
- OSTI ID: 1506722
- Report Number(s):
- PNNL-SA-135583
Journal ID: ISSN 0009-2541
- Grant/Contract Number:
- AC05-76RL01830; AC02-06CH11357; EAR-1147728; EAR-1552211; AC06-76RLO-1830
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Chemical Geology
- Additional Journal Information:
- Journal Volume: 479; Journal ID: ISSN 0009-2541
- Publisher:
- Elsevier
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; 58 GEOSCIENCES; birnessite; manganese oxide; triclinic; hexagonal; Mn oxidation state; FTIR; EXAFS; XRD; XPS
Citation Formats
Ling, Florence T., Post, Jeffrey E., Heaney, Peter J., and Ilton, Eugene S. The relationship between Mn oxidation state and structure in triclinic and hexagonal birnessites. United States: N. p., 2018.
Web. doi:10.1016/j.chemgeo.2018.01.011.
Ling, Florence T., Post, Jeffrey E., Heaney, Peter J., & Ilton, Eugene S. The relationship between Mn oxidation state and structure in triclinic and hexagonal birnessites. United States. https://doi.org/10.1016/j.chemgeo.2018.01.011
Ling, Florence T., Post, Jeffrey E., Heaney, Peter J., and Ilton, Eugene S. Wed .
"The relationship between Mn oxidation state and structure in triclinic and hexagonal birnessites". United States. https://doi.org/10.1016/j.chemgeo.2018.01.011. https://www.osti.gov/servlets/purl/1773815.
@article{osti_1773815,
title = {The relationship between Mn oxidation state and structure in triclinic and hexagonal birnessites},
author = {Ling, Florence T. and Post, Jeffrey E. and Heaney, Peter J. and Ilton, Eugene S.},
abstractNote = {Because of their nanocrystallinity and high cation exchange capacities, birnessite phases can control the cycling of heavy metals in soils and groundwaters, and they also are implicated in the oxidation of transition metals in natural environments. Birnessite reactivity is determined by crystal structure and composition. Because birnessites typically are poorly crystalline, synchrotron-based absorption spectroscopy (EXAFS, XANES) often is utilized for structural characterization. For example, linear combination fitting (LCF) of X-ray absorption spectra typically is applied to quantify mixed triclinic and hexagonal birnessite phases. This approach is challenged, however, because the structures of the standards are not always plainly apparent. Moreover, it is difficult to distinguish birnessites with nanoscale intergrowths of hexagonal and triclinic endmembers from homogeneous birnessite structures of “intermediate triclinicity”. In this study, we explored these issues by synthesizing a host of cation-exchanged birnessite specimens whose long-range symmetrical character could be determined by X-ray diffraction without ambiguity. Through a combination of Fourier transform infrared spectroscopy (FTIR), extended X-ray absorption fine structure (EXAFS), and X-ray photoelectron spectroscopy (XPS), we have examined the relationships among structural symmetry, Mn oxidation state, and interlayer composition. Our results confirm prior models that as the concentration of Mn3+ increases, the departure from hexagonal symmetry also increases. Rietveld refinements indicate that the Jahn-Teller distortions associated with Mn3+ induce systematic variations in unit-cell parameters, particularly an increase in the α-axis and the β angle of the unit cell. Interlayer cation composition also controls structural distortions, and Ca-rich birnessites showed less deviation from hexagonality than did Na-, K-, and Ba-birnessites. Our linear combination fits of X-ray absorption spectra sometimes yielded misleading results, reinforcing the difficulty and importance of selecting appropriate standards.},
doi = {10.1016/j.chemgeo.2018.01.011},
journal = {Chemical Geology},
number = ,
volume = 479,
place = {United States},
year = {Wed Jan 17 00:00:00 EST 2018},
month = {Wed Jan 17 00:00:00 EST 2018}
}
Web of Science
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