Pregled bibliografske jedinice broj: 567194
The effect of iridium(III) ions on the formation of iron oxides in a highly alkaline medium
The effect of iridium(III) ions on the formation of iron oxides in a highly alkaline medium // Journal of alloys and compounds, 516 (2012), 207-216 doi:10.1016/j.jallcom.2011.12.052 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 567194 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
The effect of iridium(III) ions on the formation of iron oxides in a highly alkaline medium
Autori
Krehula, Stjepko ; Musić, Svetozar
Izvornik
Journal of alloys and compounds (0925-8388) 516
(2012);
207-216
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
iridium; goethite; hematite; magnetite; Morin transition; 57Fe Mössbauer spectroscopy
Sažetak
The effect of the presence of Ir3+ ions on the formation of iron oxides in a highly alkaline precipitation system was investigated using X-ray powder diffraction (XRD), 57Fe Mössbauer and FT-IR spectroscopies, field emission scanning electron microscopy (FE-SEM) and energy dispersive X-ray spectroscopy (EDS). Monodispersed lath-like α-FeOOH (goethite) particles precipitated by hydrothermal treatment in a highly alkaline medium with the addition of tetramethylammonium hydroxide (TMAH) were used as reference material. The presence of Ir3+ ions in the precipitation system strongly influenced the phase composition, magnetic, structural and morphological properties of obtained samples. The formation of α-Fe2O3 (hematite) along with α-FeOOH in the first stage of hydrothermal treatment and the transformation of α-FeOOH and α-Fe2O3 to Fe3O4 (magnetite) by a longer hydrothermal treatment was caused by the presence of Ir3+ ions. Ir3+ for Fe3+ substitution in the structure of α-FeOOH brought about changes in unit-cell dimensions, crystallinity, particle size and shape, hyperfine magnetic field and infrared bands positions. Ir3+ for Fe3+ substitution in the structure of α-Fe2O3 led to an increase in the temperature of the Morin transition ; Mössbauer spectroscopy showed the presence of α-Fe2O3 in the antiferromagnetically ordered state at 293 K.
Izvorni jezik
Engleski
Znanstvena područja
Kemija
POVEZANOST RADA
Projekti:
098-0982904-2952 - Sinteza i mikrostruktura metalnih oksida i oksidnih stakala (Ristić, Mira, MZOS ) ( CroRIS)
Ustanove:
Institut "Ruđer Bošković", Zagreb
Poveznice na cjeloviti tekst rada:
Pristup cjelovitom tekstu rada doi
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus