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Title: Macroscopic and microscopic behaviors of Mn(II) (ad)sorption to goethite with the effects of dissolved carbonates under anoxic conditions

Abstract

Manganese and its compounds have been extensively researched because of their far-reaching roles in a wide range of biogeochemical processes in natural systems. The (ad)sorption behavior of Mn(II), however, is poorly understood despite its important role as the primary reaction step for surface-catalyzed Mn(II) oxidation that is the principal abiotic process forming various Mn (oxyhydr)oxides in nature. Here, we systematically examined Mn(II) (ad)sorption to one of the most common natural sorbents, goethite, in oxygen- and carbonate-free systems. Traditional sorption edge and isotherm experiments were conducted by varying sorbate-to-sorbent ratio (0.027–15 μmol∙m-2) and solution pH (pH 5.0–9.0). The effects of dissolved carbonates on Mn(II) sorption were also assessed in a range of naturally prevalent concentrations (0.5–10 mM NaHCO3). The Mn(II) uptake on goethite followed a typical Langmuir isotherm in the absence of dissolved carbonates, with increasing maximum adsorption capacities (Γmax) from 0.19 at pH 6.5 to 3.4 μmol∙m-2 at pH 9.0. The presence of dissolved carbonates raised the extent of Mn(II) adsorption, which appeared to be directly correspondent to that of the adsorption of dissolved carbonates. Extended X-ray absorption fine structure (EXAFS) analysis indicated that Mn(II) predominantly formed inner-sphere binuclear bidentate surface complexes. Mn(II) uptake became deviated from the Langmuir modelmore » and showed a clear indication of surface precipitation when the Mn(II) sorption density (Γ) exceeded a threshold value in a given solution composition. This secondary Mn(II) phase was identified as rhodochrosite using X-ray diffraction (XRD) and transmission electron microscope (TEM). Furthermore, it would be plausible that a minor fraction of adsorbed Mn(II) coexisted with the secondary rhodochrosite according to a linear combination fitting (LCF) of the X-ray absorption near edge structure (XANES) spectra of Mn reference and samples. These systematic investigations of the macroscopic and microscopic behaviors of Mn(II) (ad)sorption to goethite provide a critical avenue for disentangling surface-catalytic Mn(II) oxidation processes, which ultimately lead to the formation of diverse Mn (oxyhydr)oxides in the environment.« less

Authors:
ORCiD logo [1]; ORCiD logo [2];  [2]; ORCiD logo [3];  [4]
  1. Yonsei Univ., Seoul (Korea, Republic of)
  2. Kyushu Univ., Fukuoka (Japan)
  3. Argonne National Lab. (ANL), Argonne, IL (United States)
  4. Yonsei Univ., Seoul (Korea, Republic of); Pohang Univ. of Science and Technology (POSTECH) (Korea, Republic of)
Publication Date:
Research Org.:
Argonne National Laboratory (ANL), Argonne, IL (United States)
Sponsoring Org.:
National Research Foundation of Korea (NRF); Japan Society for the Promotion of Science (JSPS) - KAKENHI; USDOE Office of Science (SC), Basic Energy Sciences (BES). Chemical Sciences, Geosciences, and Biosciences Division
OSTI Identifier:
1617647
Alternate Identifier(s):
OSTI ID: 1615557
Grant/Contract Number:  
AC02-06CH11357
Resource Type:
Accepted Manuscript
Journal Name:
Geochimica et Cosmochimica Acta
Additional Journal Information:
Journal Volume: 277; Journal Issue: C; Journal ID: ISSN 0016-7037
Publisher:
Elsevier; The Geochemical Society; The Meteoritical Society
Country of Publication:
United States
Language:
English
Subject:
37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; manganese; goethite; oxidation; heterogeneous catalysis; sorption isotherm

Citation Formats

Namgung, Seonyi, Guo, Binglin, Sasaki, Keiko, Lee, Sang Soo, and Lee, Giehyeon. Macroscopic and microscopic behaviors of Mn(II) (ad)sorption to goethite with the effects of dissolved carbonates under anoxic conditions. United States: N. p., 2020. Web. doi:10.1016/j.gca.2020.03.036.
Namgung, Seonyi, Guo, Binglin, Sasaki, Keiko, Lee, Sang Soo, & Lee, Giehyeon. Macroscopic and microscopic behaviors of Mn(II) (ad)sorption to goethite with the effects of dissolved carbonates under anoxic conditions. United States. https://doi.org/10.1016/j.gca.2020.03.036
Namgung, Seonyi, Guo, Binglin, Sasaki, Keiko, Lee, Sang Soo, and Lee, Giehyeon. Sat . "Macroscopic and microscopic behaviors of Mn(II) (ad)sorption to goethite with the effects of dissolved carbonates under anoxic conditions". United States. https://doi.org/10.1016/j.gca.2020.03.036. https://www.osti.gov/servlets/purl/1617647.
@article{osti_1617647,
title = {Macroscopic and microscopic behaviors of Mn(II) (ad)sorption to goethite with the effects of dissolved carbonates under anoxic conditions},
author = {Namgung, Seonyi and Guo, Binglin and Sasaki, Keiko and Lee, Sang Soo and Lee, Giehyeon},
abstractNote = {Manganese and its compounds have been extensively researched because of their far-reaching roles in a wide range of biogeochemical processes in natural systems. The (ad)sorption behavior of Mn(II), however, is poorly understood despite its important role as the primary reaction step for surface-catalyzed Mn(II) oxidation that is the principal abiotic process forming various Mn (oxyhydr)oxides in nature. Here, we systematically examined Mn(II) (ad)sorption to one of the most common natural sorbents, goethite, in oxygen- and carbonate-free systems. Traditional sorption edge and isotherm experiments were conducted by varying sorbate-to-sorbent ratio (0.027–15 μmol∙m-2) and solution pH (pH 5.0–9.0). The effects of dissolved carbonates on Mn(II) sorption were also assessed in a range of naturally prevalent concentrations (0.5–10 mM NaHCO3). The Mn(II) uptake on goethite followed a typical Langmuir isotherm in the absence of dissolved carbonates, with increasing maximum adsorption capacities (Γmax) from 0.19 at pH 6.5 to 3.4 μmol∙m-2 at pH 9.0. The presence of dissolved carbonates raised the extent of Mn(II) adsorption, which appeared to be directly correspondent to that of the adsorption of dissolved carbonates. Extended X-ray absorption fine structure (EXAFS) analysis indicated that Mn(II) predominantly formed inner-sphere binuclear bidentate surface complexes. Mn(II) uptake became deviated from the Langmuir model and showed a clear indication of surface precipitation when the Mn(II) sorption density (Γ) exceeded a threshold value in a given solution composition. This secondary Mn(II) phase was identified as rhodochrosite using X-ray diffraction (XRD) and transmission electron microscope (TEM). Furthermore, it would be plausible that a minor fraction of adsorbed Mn(II) coexisted with the secondary rhodochrosite according to a linear combination fitting (LCF) of the X-ray absorption near edge structure (XANES) spectra of Mn reference and samples. These systematic investigations of the macroscopic and microscopic behaviors of Mn(II) (ad)sorption to goethite provide a critical avenue for disentangling surface-catalytic Mn(II) oxidation processes, which ultimately lead to the formation of diverse Mn (oxyhydr)oxides in the environment.},
doi = {10.1016/j.gca.2020.03.036},
journal = {Geochimica et Cosmochimica Acta},
number = C,
volume = 277,
place = {United States},
year = {Sat Apr 04 00:00:00 EDT 2020},
month = {Sat Apr 04 00:00:00 EDT 2020}
}

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Kinetics of rhodochrosite crystal growth at 25°C: The role of surface speciation
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In Situ Infrared Speciation of Adsorbed Carbonate on Aluminum and Iron Oxides
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Formation of Cd precipitates on γ-Al2O3: Implications for Cd sequestration in the environment
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Evidence for a Dynamic Cycle between Mn and Co in the Water Column of a Stratified Lake
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X-ray Absorption Near Edge Structure Study of Lead Sorption on Phosphate-Treated Kaolinite
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