Synthesis and properties of titanomagnetite (Fe3−xTixO4) nanoparticles: A tunable solid-state Fe(II/III) redox system
[Display omitted] ► Fe3−xTixO4 nanoparticles (10–12nm) synthesized by aqueous precipitation. ► Composition, structure, magnetic properties of Fe3−xTixO4 nanoparticles determined. ► Ti(IV) incorporation in the unit cell up to a limit of x⩽0.38. ► Nanoparticles with higher x had a minor amorphous seco...
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Published in | Journal of colloid and interface science Vol. 387; no. 1; pp. 24 - 38 |
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Main Authors | , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Amsterdam
Elsevier Inc
01.12.2012
Elsevier |
Subjects | |
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Abstract | [Display omitted]
► Fe3−xTixO4 nanoparticles (10–12nm) synthesized by aqueous precipitation. ► Composition, structure, magnetic properties of Fe3−xTixO4 nanoparticles determined. ► Ti(IV) incorporation in the unit cell up to a limit of x⩽0.38. ► Nanoparticles with higher x had a minor amorphous secondary Fe(II)/Ti(IV) phase. ► Persistent segregation of Fe(II) to particle surfaces even after mild oxidation by dissolution.
Titanomagnetite (Fe3−xTixO4) nanoparticles were synthesized by room temperature aqueous precipitation, in which Ti(IV) replaces Fe(III) and is charge compensated by conversion of Fe(III) to Fe(II) in the unit cell. A comprehensive suite of tools was used to probe composition, structure, and magnetic properties down to site-occupancy level, emphasizing distribution and accessibility of Fe(II) as a function of x. Synthesis of nanoparticles in the range 0⩽x⩽0.6 was attempted; Ti, total Fe and Fe(II) content were verified by chemical analysis. TEM indicated homogeneous spherical 9–12nm particles. μ-XRD and Mössbauer spectroscopy on anoxic aqueous suspensions verified the inverse spinel structure and Ti(IV) incorporation in the unit cell up to x⩽0.38, based on Fe(II)/Fe(III) ratio deduced from the unit cell edge and Mössbauer spectra. Nanoparticles with a higher value of x possessed a minor amorphous secondary Fe(II)/Ti(IV) phase. XANES/EXAFS indicated Ti(IV) incorporation in the octahedral sublattice (B-site) and proportional increases in Fe(II)/Fe(III) ratio. XA/XMCD indicated that increases arise from increasing B-site Fe(II), and that these charge-balancing equivalents segregate to those B-sites near particle surfaces. Dissolution studies showed that this segregation persists after release of Fe(II) into solution, in amounts systematically proportional to x and thus the Fe(II)/Fe(III) ratio. A mechanistic reaction model was developed entailing mobile B-site Fe(II) supplying a highly interactive surface phase that undergoes interfacial electron transfer with oxidants in solution, sustained by outward Fe(II) migration from particle interiors and concurrent inward migration of charge-balancing cationic vacancies in a ratio of 3:1. |
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AbstractList | Titanomagnetite (Fe₃₋ ₓTiₓO₄) nanoparticles were synthesized by room temperature aqueous precipitation, in which Ti(IV) replaces Fe(III) and is charge compensated by conversion of Fe(III) to Fe(II) in the unit cell. A comprehensive suite of tools was used to probe composition, structure, and magnetic properties down to site-occupancy level, emphasizing distribution and accessibility of Fe(II) as a function of x. Synthesis of nanoparticles in the range 0⩽x⩽0.6 was attempted; Ti, total Fe and Fe(II) content were verified by chemical analysis. TEM indicated homogeneous spherical 9–12nm particles. μ-XRD and Mössbauer spectroscopy on anoxic aqueous suspensions verified the inverse spinel structure and Ti(IV) incorporation in the unit cell up to x⩽0.38, based on Fe(II)/Fe(III) ratio deduced from the unit cell edge and Mössbauer spectra. Nanoparticles with a higher value of x possessed a minor amorphous secondary Fe(II)/Ti(IV) phase. XANES/EXAFS indicated Ti(IV) incorporation in the octahedral sublattice (B-site) and proportional increases in Fe(II)/Fe(III) ratio. XA/XMCD indicated that increases arise from increasing B-site Fe(II), and that these charge-balancing equivalents segregate to those B-sites near particle surfaces. Dissolution studies showed that this segregation persists after release of Fe(II) into solution, in amounts systematically proportional to x and thus the Fe(II)/Fe(III) ratio. A mechanistic reaction model was developed entailing mobile B-site Fe(II) supplying a highly interactive surface phase that undergoes interfacial electron transfer with oxidants in solution, sustained by outward Fe(II) migration from particle interiors and concurrent inward migration of charge-balancing cationic vacancies in a ratio of 3:1. [Display omitted] ► Fe3−xTixO4 nanoparticles (10–12nm) synthesized by aqueous precipitation. ► Composition, structure, magnetic properties of Fe3−xTixO4 nanoparticles determined. ► Ti(IV) incorporation in the unit cell up to a limit of x⩽0.38. ► Nanoparticles with higher x had a minor amorphous secondary Fe(II)/Ti(IV) phase. ► Persistent segregation of Fe(II) to particle surfaces even after mild oxidation by dissolution. Titanomagnetite (Fe3−xTixO4) nanoparticles were synthesized by room temperature aqueous precipitation, in which Ti(IV) replaces Fe(III) and is charge compensated by conversion of Fe(III) to Fe(II) in the unit cell. A comprehensive suite of tools was used to probe composition, structure, and magnetic properties down to site-occupancy level, emphasizing distribution and accessibility of Fe(II) as a function of x. Synthesis of nanoparticles in the range 0⩽x⩽0.6 was attempted; Ti, total Fe and Fe(II) content were verified by chemical analysis. TEM indicated homogeneous spherical 9–12nm particles. μ-XRD and Mössbauer spectroscopy on anoxic aqueous suspensions verified the inverse spinel structure and Ti(IV) incorporation in the unit cell up to x⩽0.38, based on Fe(II)/Fe(III) ratio deduced from the unit cell edge and Mössbauer spectra. Nanoparticles with a higher value of x possessed a minor amorphous secondary Fe(II)/Ti(IV) phase. XANES/EXAFS indicated Ti(IV) incorporation in the octahedral sublattice (B-site) and proportional increases in Fe(II)/Fe(III) ratio. XA/XMCD indicated that increases arise from increasing B-site Fe(II), and that these charge-balancing equivalents segregate to those B-sites near particle surfaces. Dissolution studies showed that this segregation persists after release of Fe(II) into solution, in amounts systematically proportional to x and thus the Fe(II)/Fe(III) ratio. A mechanistic reaction model was developed entailing mobile B-site Fe(II) supplying a highly interactive surface phase that undergoes interfacial electron transfer with oxidants in solution, sustained by outward Fe(II) migration from particle interiors and concurrent inward migration of charge-balancing cationic vacancies in a ratio of 3:1. |
Author | Pearce, C.I. Qafoku, O. Arenholz, E. Kukkadapu, R.K. Rosso, K.M. Gorski, C.A. Heald, S.M. Liu, J. Henderson, C.M.B. |
Author_xml | – sequence: 1 givenname: C.I. surname: Pearce fullname: Pearce, C.I. email: carolyn.pearce@pnnl.gov organization: Pacific Northwest National Laboratory, Richland, WA 99352, USA – sequence: 2 givenname: O. surname: Qafoku fullname: Qafoku, O. organization: Pacific Northwest National Laboratory, Richland, WA 99352, USA – sequence: 3 givenname: J. surname: Liu fullname: Liu, J. organization: Pacific Northwest National Laboratory, Richland, WA 99352, USA – sequence: 4 givenname: E. surname: Arenholz fullname: Arenholz, E. organization: Advanced Light Source, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA – sequence: 5 givenname: S.M. surname: Heald fullname: Heald, S.M. organization: Argonne National Laboratory, Argonne, IL 60439, USA – sequence: 6 givenname: R.K. surname: Kukkadapu fullname: Kukkadapu, R.K. organization: Pacific Northwest National Laboratory, Richland, WA 99352, USA – sequence: 7 givenname: C.A. surname: Gorski fullname: Gorski, C.A. organization: Swiss Federal Institute of Aquatic Science and Technology, Eawag, Ueberlandstrasse 133, 8600 Duebendorf, Switzerland – sequence: 8 givenname: C.M.B. surname: Henderson fullname: Henderson, C.M.B. organization: Science and Technology Facilities Council, Daresbury Laboratory, Warrington WA4 4AD, UK – sequence: 9 givenname: K.M. surname: Rosso fullname: Rosso, K.M. organization: Pacific Northwest National Laboratory, Richland, WA 99352, USA |
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► Fe3−xTixO4 nanoparticles (10–12nm) synthesized by aqueous precipitation. ► Composition, structure, magnetic properties of Fe3−xTixO4... Titanomagnetite (Fe₃₋ ₓTiₓO₄) nanoparticles were synthesized by room temperature aqueous precipitation, in which Ti(IV) replaces Fe(III) and is charge... |
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SubjectTerms | ambient temperature chemical analysis Chemistry Colloidal state and disperse state Dissolution Electron transfer Exact sciences and technology General and physical chemistry iron magnetic properties Magnetite Master Curve nanoparticles oxidants Physical and chemical studies. Granulometry. Electrokinetic phenomena Site occupancy spectroscopy Surface physical chemistry titanium transmission electron microscopy Ulvöspinel X-ray magnetic circular dichroism |
Title | Synthesis and properties of titanomagnetite (Fe3−xTixO4) nanoparticles: A tunable solid-state Fe(II/III) redox system |
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