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Title: Binding Geometries of Silicate Species on Ferrihydrite Surfaces

Abstract

Silicate sorption on ferrihydrite surfaces, as monomers, oligomers, and polymers, strongly affects ferrihydrite crystallinity, thermodynamic stability, and surface reactivity. How these silicate species bind on ferrihydrite surfaces is, however, not well understood. We have determined silicate binding geometries using a combination of X-ray absorption spectroscopy (XAS), differential atomic pair distribution function (d-PDF) analysis, and density functional theory (DFT) calculations. Silicon K-edge absorption pre-edges and DFT-predicted energies indicate that silicate forms monomeric monodentate–mononuclear (MM) complexes at low silicate sorption loadings. With increasing silicate loading, the pre-edge peak shifts to higher energies, suggesting changes in the silicate binding geometry toward multidentate complexation. The d-PDF analysis determines the Si–Fe interatomic distance to be ~3.25 Å for the high-loading samples. The DFT calculations indicate that such distance corresponds to an oligomer in the bidentate–binuclear (BB) binding geometry. The transition of the silicate sorption geometry accompanied by polymerization can affect stability of ferrihydrite and its adsorption and redox reactivity and increase the degree of Si isotopic fractionation upon silicate sorption on Fe oxides. MM monomeric complexes and BB oligomeric complexes should be used for surface complexation models predicting silicate sorption on Fe oxide surfaces.

Authors:
 [1]; ORCiD logo [2]; ORCiD logo [3];  [4];  [5]; ORCiD logo [6]; ORCiD logo [1]
  1. Univ. of Wyoming, Laramie, WY (United States)
  2. Univ. of Texas at El Paso, TX (United States)
  3. Umeå Univ. (Sweden)
  4. Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
  5. Univ. of Saskatchewan, Saskatchewan (Canada)
  6. Huazhong Agricultural Univ., Wuhan (China)
Publication Date:
Research Org.:
Argonne National Laboratory (ANL), Argonne, IL (United States). Advanced Photon Source (APS)
Sponsoring Org.:
DOE - BASIC ENERGY SCIENCESFOREIGN
OSTI Identifier:
1424771
Resource Type:
Accepted Manuscript
Journal Name:
ACS Earth and Space Chemistry
Additional Journal Information:
Journal Volume: 2; Journal Issue: 2; Journal ID: ISSN 2472-3452
Publisher:
American Chemical Society
Country of Publication:
United States
Language:
ENGLISH
Subject:
37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; Sorption; Oxides; Monomers; Silicon; Mathematical methods; silicate; ferrihydrite; binding geometry; polymerization; Si K-edge XANES spectroscopy; differential PDF analysis; DFT calculations

Citation Formats

Wang, Xiaoming, Kubicki, James D., Boily, Jean-François, Waychunas, Glenn A., Hu, Yongfeng, Feng, Xionghan, and Zhu, Mengqiang. Binding Geometries of Silicate Species on Ferrihydrite Surfaces. United States: N. p., 2018. Web. doi:10.1021/acsearthspacechem.7b00109.
Wang, Xiaoming, Kubicki, James D., Boily, Jean-François, Waychunas, Glenn A., Hu, Yongfeng, Feng, Xionghan, & Zhu, Mengqiang. Binding Geometries of Silicate Species on Ferrihydrite Surfaces. United States. https://doi.org/10.1021/acsearthspacechem.7b00109
Wang, Xiaoming, Kubicki, James D., Boily, Jean-François, Waychunas, Glenn A., Hu, Yongfeng, Feng, Xionghan, and Zhu, Mengqiang. Fri . "Binding Geometries of Silicate Species on Ferrihydrite Surfaces". United States. https://doi.org/10.1021/acsearthspacechem.7b00109. https://www.osti.gov/servlets/purl/1424771.
@article{osti_1424771,
title = {Binding Geometries of Silicate Species on Ferrihydrite Surfaces},
author = {Wang, Xiaoming and Kubicki, James D. and Boily, Jean-François and Waychunas, Glenn A. and Hu, Yongfeng and Feng, Xionghan and Zhu, Mengqiang},
abstractNote = {Silicate sorption on ferrihydrite surfaces, as monomers, oligomers, and polymers, strongly affects ferrihydrite crystallinity, thermodynamic stability, and surface reactivity. How these silicate species bind on ferrihydrite surfaces is, however, not well understood. We have determined silicate binding geometries using a combination of X-ray absorption spectroscopy (XAS), differential atomic pair distribution function (d-PDF) analysis, and density functional theory (DFT) calculations. Silicon K-edge absorption pre-edges and DFT-predicted energies indicate that silicate forms monomeric monodentate–mononuclear (MM) complexes at low silicate sorption loadings. With increasing silicate loading, the pre-edge peak shifts to higher energies, suggesting changes in the silicate binding geometry toward multidentate complexation. The d-PDF analysis determines the Si–Fe interatomic distance to be ~3.25 Å for the high-loading samples. The DFT calculations indicate that such distance corresponds to an oligomer in the bidentate–binuclear (BB) binding geometry. The transition of the silicate sorption geometry accompanied by polymerization can affect stability of ferrihydrite and its adsorption and redox reactivity and increase the degree of Si isotopic fractionation upon silicate sorption on Fe oxides. MM monomeric complexes and BB oligomeric complexes should be used for surface complexation models predicting silicate sorption on Fe oxide surfaces.},
doi = {10.1021/acsearthspacechem.7b00109},
journal = {ACS Earth and Space Chemistry},
number = 2,
volume = 2,
place = {United States},
year = {Fri Jan 05 00:00:00 EST 2018},
month = {Fri Jan 05 00:00:00 EST 2018}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record

Figures / Tables:

Figure 1 Figure 1: Silicate sorption isotherms at pH 4, 7 and 10, respectively, and their fits with the Langmuir equation (Qe = Qmax*kL*C/(1 + kL*C), where Qe is the amount of silicate sorbed, Qmax is the maximum sorption capacity, C is the equilibrium concentration, and KL is a constant related tomore » the binding strength) (a), and silicate adsorption kinetics on ferrihydrite surfaces with 1 mM Si at pH 4 (b).« less

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Figures/Tables have been extracted from DOE-funded journal article accepted manuscripts.