Mössbauer Spectroscopy 2013
DOI: 10.1002/9781118714614.ch18
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Mössbauer Spectroscopy in Study of Nanocrystalline Iron Oxides From Thermal Processes

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Cited by 5 publications
(3 citation statements)
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“…When fitting, widely accepted physicochemical models for ε-Fe 2 O 3 and α-Fe 2 O 3 were adopted and appropriately adjusted. 9,80 The appearance of the Mössbauer spectral profile of ε-Fe 2 O 3 reflects its crystal structure; each sextet corresponds to respective ε-Fe 2 O 3 crystallographic sites. Since all three octahedral and one tetrahedral sites in ε-Fe 2 O 3 are fully occupied with Fe 3+ ions, their sextets show relative spectral areas equal to 1 : 1 : 1 : 1 (with an assumption of an identical Mössbauer-Lamb factor for all the four different sites).…”
Section: Resultsmentioning
confidence: 99%
“…When fitting, widely accepted physicochemical models for ε-Fe 2 O 3 and α-Fe 2 O 3 were adopted and appropriately adjusted. 9,80 The appearance of the Mössbauer spectral profile of ε-Fe 2 O 3 reflects its crystal structure; each sextet corresponds to respective ε-Fe 2 O 3 crystallographic sites. Since all three octahedral and one tetrahedral sites in ε-Fe 2 O 3 are fully occupied with Fe 3+ ions, their sextets show relative spectral areas equal to 1 : 1 : 1 : 1 (with an assumption of an identical Mössbauer-Lamb factor for all the four different sites).…”
Section: Resultsmentioning
confidence: 99%
“…The sextet present in the spectra could be attributed to iron oxide (i.e. α-Fe 2 O 3 ) (Tuček et al, 2013).…”
Section: Mössbauer Spectroscopymentioning
confidence: 96%
“…The most frequently occurring polymorphs are alpha (α‐Fe 2 O 3 ) and gamma (γ‐Fe 2 O 3 ) form, mineralogically known as hematite and maghemite, respectively. The other two polymorphs, beta (β‐Fe 2 O 3 ) and epsilon (ε‐Fe 2 O 3 ), are very rare and due to the role of surface energy, they can exist only in the form of nano‐objects …”
Section: Introductionmentioning
confidence: 99%