Simultaneous incorporation of Mn and Al in the goethite structure

Two series of (Al,Mn)-substituted goethites were synthesized from ferrihydrite made in alkaline media, with different Al/Mn mole ratios ([Al + Mn]/Fe molar ratio up to 0.12). Powder X-ray diffraction and extended X-ray absorption fine structure (EXAFS) techniques were used to assess the structural c...

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Autor principal: Sileo, Elsa Ester
Publicado: 2007
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00167037_v71_n4_p1009_Alvarez
http://hdl.handle.net/20.500.12110/paper_00167037_v71_n4_p1009_Alvarez
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spelling paper:paper_00167037_v71_n4_p1009_Alvarez2023-06-08T14:38:46Z Simultaneous incorporation of Mn and Al in the goethite structure Sileo, Elsa Ester aluminum crystal structure goethite manganese Rietveld analysis X-ray diffraction Two series of (Al,Mn)-substituted goethites were synthesized from ferrihydrite made in alkaline media, with different Al/Mn mole ratios ([Al + Mn]/Fe molar ratio up to 0.12). Powder X-ray diffraction and extended X-ray absorption fine structure (EXAFS) techniques were used to assess the structural characteristics of the simultaneous substitution in goethite. XRD patterns revealed that all the obtained solids remain in a goethite-like structure. Rietveld refinement of X-ray diffraction data indicates that the increasing Mn substitution and consequent decrease of Al substitution causes an increase in the unit cell volume. This change is accompanied by the increment of the various Me-Me distances. XANES spectra at the Al and Mn K-edge confirm the octahedral coordination of Al and the trivalent oxidation state of the Mn ion in all the synthesized samples. EXAFS spectra at the Fe K-edge indicate that the local order around the Fe atom remains practically constant upon (Mn,Al) substitution. Measurements in the Mn K-edge show that distances Mn-Me suffer different changes with the increase in Mn substitution: a marked decrease in E and a slight decrease in E′, while DC remains constant. E and E′ values correspond to the distance between one Mn and one neighboring Me (Fe, Mn, Al) atom, both situated in two polyhedra linked by an edge. These polyhedra belong to the same double row of the goethite structure. DC value corresponds to the distance between one Mn and one Me (Fe, Mn, Al) atom, situated in two octahedral linked by one corner and belonging to two adjacent double chains. All the intermetallic distances are minor than the corresponding singly substituted goethites, this fact is attributed to the structure contraction due to the presence of Al(III) which restrains the axial distortion of Mn. Dissolution-time curves, resulting from exposure to 6 M HCl at 318 K, show that the dissolution rate slows with increasing Al substitution and consequent decrease of Mn substitution, and the shape of the curve becomes increasingly sigmoidal for mixed goethite with large Al content and Al-goethite. Dissolution kinetics of most samples are well described by the Kabai equation. Al dissolves almost congruently with respect to Fe, implying that it is homogeneously distributed in the structure. However, the convex χMn:χFe curve indicates that Mn tends to be concentrated in the outer layers of the goethite particles. © 2006 Elsevier Inc. All rights reserved. Fil:Sileo, E.E. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2007 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00167037_v71_n4_p1009_Alvarez http://hdl.handle.net/20.500.12110/paper_00167037_v71_n4_p1009_Alvarez
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic aluminum
crystal structure
goethite
manganese
Rietveld analysis
X-ray diffraction
spellingShingle aluminum
crystal structure
goethite
manganese
Rietveld analysis
X-ray diffraction
Sileo, Elsa Ester
Simultaneous incorporation of Mn and Al in the goethite structure
topic_facet aluminum
crystal structure
goethite
manganese
Rietveld analysis
X-ray diffraction
description Two series of (Al,Mn)-substituted goethites were synthesized from ferrihydrite made in alkaline media, with different Al/Mn mole ratios ([Al + Mn]/Fe molar ratio up to 0.12). Powder X-ray diffraction and extended X-ray absorption fine structure (EXAFS) techniques were used to assess the structural characteristics of the simultaneous substitution in goethite. XRD patterns revealed that all the obtained solids remain in a goethite-like structure. Rietveld refinement of X-ray diffraction data indicates that the increasing Mn substitution and consequent decrease of Al substitution causes an increase in the unit cell volume. This change is accompanied by the increment of the various Me-Me distances. XANES spectra at the Al and Mn K-edge confirm the octahedral coordination of Al and the trivalent oxidation state of the Mn ion in all the synthesized samples. EXAFS spectra at the Fe K-edge indicate that the local order around the Fe atom remains practically constant upon (Mn,Al) substitution. Measurements in the Mn K-edge show that distances Mn-Me suffer different changes with the increase in Mn substitution: a marked decrease in E and a slight decrease in E′, while DC remains constant. E and E′ values correspond to the distance between one Mn and one neighboring Me (Fe, Mn, Al) atom, both situated in two polyhedra linked by an edge. These polyhedra belong to the same double row of the goethite structure. DC value corresponds to the distance between one Mn and one Me (Fe, Mn, Al) atom, situated in two octahedral linked by one corner and belonging to two adjacent double chains. All the intermetallic distances are minor than the corresponding singly substituted goethites, this fact is attributed to the structure contraction due to the presence of Al(III) which restrains the axial distortion of Mn. Dissolution-time curves, resulting from exposure to 6 M HCl at 318 K, show that the dissolution rate slows with increasing Al substitution and consequent decrease of Mn substitution, and the shape of the curve becomes increasingly sigmoidal for mixed goethite with large Al content and Al-goethite. Dissolution kinetics of most samples are well described by the Kabai equation. Al dissolves almost congruently with respect to Fe, implying that it is homogeneously distributed in the structure. However, the convex χMn:χFe curve indicates that Mn tends to be concentrated in the outer layers of the goethite particles. © 2006 Elsevier Inc. All rights reserved.
author Sileo, Elsa Ester
author_facet Sileo, Elsa Ester
author_sort Sileo, Elsa Ester
title Simultaneous incorporation of Mn and Al in the goethite structure
title_short Simultaneous incorporation of Mn and Al in the goethite structure
title_full Simultaneous incorporation of Mn and Al in the goethite structure
title_fullStr Simultaneous incorporation of Mn and Al in the goethite structure
title_full_unstemmed Simultaneous incorporation of Mn and Al in the goethite structure
title_sort simultaneous incorporation of mn and al in the goethite structure
publishDate 2007
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00167037_v71_n4_p1009_Alvarez
http://hdl.handle.net/20.500.12110/paper_00167037_v71_n4_p1009_Alvarez
work_keys_str_mv AT sileoelsaester simultaneousincorporationofmnandalinthegoethitestructure
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