Reactions of nitrite with goethite and surface Fe(II)-goethite complexes

Chemodenitrification-the abiotic (chemical) reduction of nitrite (NO2−) by iron (II)-plays an important role in nitrogen cycling due in part to this process serving as a source of nitrous oxide (N2O). Questions remain about the fate of NO2− in the presence of mineral surfaces formed during chemodeni...

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Veröffentlicht in:The Science of the total environment 2021-08, Vol.782, p.146406-146406, Article 146406
Hauptverfasser: Dhakal, P., Coyne, M.S., McNear, D.H., Wendroth, O.O., Vandiviere, M.M., D'Angelo, E.M., Matocha, C.J.
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container_start_page 146406
container_title The Science of the total environment
container_volume 782
creator Dhakal, P.
Coyne, M.S.
McNear, D.H.
Wendroth, O.O.
Vandiviere, M.M.
D'Angelo, E.M.
Matocha, C.J.
description Chemodenitrification-the abiotic (chemical) reduction of nitrite (NO2−) by iron (II)-plays an important role in nitrogen cycling due in part to this process serving as a source of nitrous oxide (N2O). Questions remain about the fate of NO2− in the presence of mineral surfaces formed during chemodenitrification, such as iron(III) (hydr) oxides, particularly relative to dissolved iron(II). In this study, stirred-batch kinetic experiments were conducted under anoxic conditions (to mimic iron(III)-reducing conditions) from pH 5.5–8 to investigate NO2− reactivity with goethite (FeOOH(s)) and Fe(II)-treated goethite using wet chemical and attenuated total reflectance-Fourier transform infrared (ATR-FTIR) spectroscopy. Nitrite removal from solution by goethite was more rapid at pH 5.5 than at pH 7 and 8. Spectral changes upon nitrite adsorption imply an inner-sphere surface interaction (monodentate and bidentate) at pH 5.5 based on ATR-FTIR spectra of the nitrite-goethite interface over time. In iron(II)-amended experiments at pH 5.5 with high aqueous Fe(II) in equilibrium with goethite, nitrous oxide was generated, indicating that nitrite removal involved a combination of sorption and reduction processes. The presence of a surface complex resembling protonated nitrite (HONO) with an IR peak near ~1258 cm−1 was observed in goethite-only and iron(II)-goethite experiments, with a greater abundance of this species observed in the latter treatment. These results might help explain gaseous losses of nitrogen where nitrite and iron(II)/goethite coexist, with implications for nutrient cycling and release of atmospheric air pollutants. [Display omitted] •Nitrite sorption to goethite is more rapid at low pH.•Nitrite sorption occurs by a mixture of inner-sphere surface complexes to goethite.•Goethite-amended with iron(II) shows variable reactivity with respect to nitrite removal.•Nitrous oxide is produced during nitrite removal in high-Fe(II) amended treatments.
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Questions remain about the fate of NO2− in the presence of mineral surfaces formed during chemodenitrification, such as iron(III) (hydr) oxides, particularly relative to dissolved iron(II). In this study, stirred-batch kinetic experiments were conducted under anoxic conditions (to mimic iron(III)-reducing conditions) from pH 5.5–8 to investigate NO2− reactivity with goethite (FeOOH(s)) and Fe(II)-treated goethite using wet chemical and attenuated total reflectance-Fourier transform infrared (ATR-FTIR) spectroscopy. Nitrite removal from solution by goethite was more rapid at pH 5.5 than at pH 7 and 8. Spectral changes upon nitrite adsorption imply an inner-sphere surface interaction (monodentate and bidentate) at pH 5.5 based on ATR-FTIR spectra of the nitrite-goethite interface over time. In iron(II)-amended experiments at pH 5.5 with high aqueous Fe(II) in equilibrium with goethite, nitrous oxide was generated, indicating that nitrite removal involved a combination of sorption and reduction processes. The presence of a surface complex resembling protonated nitrite (HONO) with an IR peak near ~1258 cm−1 was observed in goethite-only and iron(II)-goethite experiments, with a greater abundance of this species observed in the latter treatment. These results might help explain gaseous losses of nitrogen where nitrite and iron(II)/goethite coexist, with implications for nutrient cycling and release of atmospheric air pollutants. [Display omitted] •Nitrite sorption to goethite is more rapid at low pH.•Nitrite sorption occurs by a mixture of inner-sphere surface complexes to goethite.•Goethite-amended with iron(II) shows variable reactivity with respect to nitrite removal.•Nitrous oxide is produced during nitrite removal in high-Fe(II) amended treatments.</description><identifier>ISSN: 0048-9697</identifier><identifier>EISSN: 1879-1026</identifier><identifier>DOI: 10.1016/j.scitotenv.2021.146406</identifier><identifier>PMID: 33839658</identifier><language>eng</language><publisher>Netherlands: Elsevier B.V</publisher><subject>adsorption ; air ; Chemodenitrification ; Goethite ; Infrared spectroscopy ; iron ; Nitrite ; nitrites ; nitrogen ; nitrous acid ; Nitrous oxide ; Redox transformation ; Sorption</subject><ispartof>The Science of the total environment, 2021-08, Vol.782, p.146406-146406, Article 146406</ispartof><rights>2021 Elsevier B.V.</rights><rights>Copyright © 2021 Elsevier B.V. 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Questions remain about the fate of NO2− in the presence of mineral surfaces formed during chemodenitrification, such as iron(III) (hydr) oxides, particularly relative to dissolved iron(II). In this study, stirred-batch kinetic experiments were conducted under anoxic conditions (to mimic iron(III)-reducing conditions) from pH 5.5–8 to investigate NO2− reactivity with goethite (FeOOH(s)) and Fe(II)-treated goethite using wet chemical and attenuated total reflectance-Fourier transform infrared (ATR-FTIR) spectroscopy. Nitrite removal from solution by goethite was more rapid at pH 5.5 than at pH 7 and 8. Spectral changes upon nitrite adsorption imply an inner-sphere surface interaction (monodentate and bidentate) at pH 5.5 based on ATR-FTIR spectra of the nitrite-goethite interface over time. In iron(II)-amended experiments at pH 5.5 with high aqueous Fe(II) in equilibrium with goethite, nitrous oxide was generated, indicating that nitrite removal involved a combination of sorption and reduction processes. The presence of a surface complex resembling protonated nitrite (HONO) with an IR peak near ~1258 cm−1 was observed in goethite-only and iron(II)-goethite experiments, with a greater abundance of this species observed in the latter treatment. These results might help explain gaseous losses of nitrogen where nitrite and iron(II)/goethite coexist, with implications for nutrient cycling and release of atmospheric air pollutants. 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Questions remain about the fate of NO2− in the presence of mineral surfaces formed during chemodenitrification, such as iron(III) (hydr) oxides, particularly relative to dissolved iron(II). In this study, stirred-batch kinetic experiments were conducted under anoxic conditions (to mimic iron(III)-reducing conditions) from pH 5.5–8 to investigate NO2− reactivity with goethite (FeOOH(s)) and Fe(II)-treated goethite using wet chemical and attenuated total reflectance-Fourier transform infrared (ATR-FTIR) spectroscopy. Nitrite removal from solution by goethite was more rapid at pH 5.5 than at pH 7 and 8. Spectral changes upon nitrite adsorption imply an inner-sphere surface interaction (monodentate and bidentate) at pH 5.5 based on ATR-FTIR spectra of the nitrite-goethite interface over time. In iron(II)-amended experiments at pH 5.5 with high aqueous Fe(II) in equilibrium with goethite, nitrous oxide was generated, indicating that nitrite removal involved a combination of sorption and reduction processes. The presence of a surface complex resembling protonated nitrite (HONO) with an IR peak near ~1258 cm−1 was observed in goethite-only and iron(II)-goethite experiments, with a greater abundance of this species observed in the latter treatment. These results might help explain gaseous losses of nitrogen where nitrite and iron(II)/goethite coexist, with implications for nutrient cycling and release of atmospheric air pollutants. [Display omitted] •Nitrite sorption to goethite is more rapid at low pH.•Nitrite sorption occurs by a mixture of inner-sphere surface complexes to goethite.•Goethite-amended with iron(II) shows variable reactivity with respect to nitrite removal.•Nitrous oxide is produced during nitrite removal in high-Fe(II) amended treatments.</abstract><cop>Netherlands</cop><pub>Elsevier B.V</pub><pmid>33839658</pmid><doi>10.1016/j.scitotenv.2021.146406</doi><tpages>1</tpages><oa>free_for_read</oa></addata></record>
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source Elsevier ScienceDirect Journals
subjects adsorption
air
Chemodenitrification
Goethite
Infrared spectroscopy
iron
Nitrite
nitrites
nitrogen
nitrous acid
Nitrous oxide
Redox transformation
Sorption
title Reactions of nitrite with goethite and surface Fe(II)-goethite complexes
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