Pregled bibliografske jedinice broj: 540160
The effect of various metal cations on the formation of iron oxides in a highly alkaline medium
The effect of various metal cations on the formation of iron oxides in a highly alkaline medium // The 31st International Conference on the Applications of the Mössbauer effect, Kobe, Japan, September 25th-30th, 2011, Programme & Abstracts / Yoshida, Yutaka ; Nishida, Tetsuaki (ur.).
Kobe, 2011. str. 227-227 (poster, nije recenziran, sažetak, znanstveni)
CROSBI ID: 540160 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
The effect of various metal cations on the formation of iron oxides in a highly alkaline medium
Autori
Krehula, Stjepko ; Musić, Svetozar
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
The 31st International Conference on the Applications of the Mössbauer effect, Kobe, Japan, September 25th-30th, 2011, Programme & Abstracts
/ Yoshida, Yutaka ; Nishida, Tetsuaki - Kobe, 2011, 227-227
Skup
The 31st International Conference on the Applications of the Mössbauer effect (ICAME 2011)
Mjesto i datum
Kobe, Japan, 25.09.2011. - 30.09.2011
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
iron oxides; goethite; hematite; magnetite; Mössbauer spectroscopy
Sažetak
Natural and synthetic iron oxides may contain different amounts of various metal cations incorporated into their structure [1]. Such incorporation can modify some of the properties (magnetic, electrical, catalytic, adsorption, electrochemical, gas sensing, etc.) desired for commercial applications of iron oxides. The effect of the presence of various metal cations on the formation of iron oxides in a highly alkaline precipitation system was investigated using Mössbauer spectroscopy and other techniques. Uniform lath-like α-FeOOH particles precipitated in a highly alkaline medium with the addition of tetramethylammonium hydroxide (TMAH) were used as reference material [2]. Generally, the presence of varying amounts of metal cations in this precipitation system resulted in the following (Table I, Fig. 1): a) formation of α-FeOOH with incorporated metal cations (mainly at lower [Mn+]), characterized by changes in the unit-cell size and reduction in the hyperfine magnetic field (Fig. 2), often accompanied by changes in particle size and shape, b) formation of other iron oxides (α-Fe2O3 or ferrihydrite), ferrites (mainly at higher [Mn+]) or AgFeO2 (in the case of Ag+). In the case of platinum group metal cations (Ru3+, Rh3+, Pd2+, Ir3+ and Pt4+) longer autoclaving (24 hours) led to the reduction of cations to the metallic state (formation of platinum group metal nanoparticles) followed by the reduction of iron(III) oxides to magnetite, Fe3O4.
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