Pregled bibliografske jedinice broj: 37345
Forced hydrolysis of Fe3+ ions in NH4Fe(SO4)2 solutions containing urotropin
Forced hydrolysis of Fe3+ ions in NH4Fe(SO4)2 solutions containing urotropin // Croatica chemica acta, 73 (2000), 2; 541-567 (međunarodna recenzija, članak, znanstveni)
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Naslov
Forced hydrolysis of Fe3+ ions in NH4Fe(SO4)2
solutions containing urotropin
Autori
Musić, Svetozar ; Šarić, Ankica ; Popović, Stanko ; Nomura, Kiyoshi ; Sawada, Tsuguo
Izvornik
Croatica chemica acta (0011-1643) 73
(2000), 2;
541-567
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
hydrolysis of Fe3+ ; NH4Fe(SO4)2 solutions ; urotropin ; iron-oxides
Sažetak
The effects of urotropin on the hydrolysis of Fe3+ ions in NH4Fe(SO4)2 solutions at 90°C were investigated using X-ray powder diffraction, 57Fe Mössbauer spectroscopy and Fourier transform infrared spectroscopy and transmission electron microscopy. Three concentrations of NH4Fe(SO4)2 solutions, 0.03, 0.1 and 0.5 M, with varying initial amounts of urotropin were used in the experiments. Chemical and structural properties of the precipitates strongly depended on the concentrations of the reactants and the time of hydrolysis. In the early stages of Fe3+ hydrolysis, samples were dominantly amorphous. a- FeOOH, a-Fe2O3 and NH4Fe3(OH)6(SO4)2 were crystalline phases detected in the precipitates ; however, the specific phase composition of each precipitate depended on the experimental conditions. The possible formation of schwertmannite was not proved in the precipitates. It was suggested that the particles of amorphous fraction, as well as a-FeOOH particles, contained significant amounts of sulphates on external and internal surfaces due to the specific adsorption. Regularity in the phase composition of the precipitates, as a function of the experimental conditions, was found. Crystallite sizes of oxides were estimated on the basis of the broadening of diffraction lines. Mössbauer spectroscopy indicated superparamagnetic behavior of a-FeOOH particles. Formation of a-FeOOH particles of colloidal dimensions was proved by transmission electron microscopy.
Izvorni jezik
Engleski
Znanstvena područja
Fizika, Kemija
POVEZANOST RADA
Ustanove:
Institut "Ruđer Bošković", Zagreb,
Prirodoslovno-matematički fakultet, Zagreb
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