Naslov
Precipitation of akaganéite and hematite particles in acidic pH media

Autori
Žic Mark ; Ristić Mira ; Musić Svetozar

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
Book of Abstracts: E-MRS 2007 Fall Meeting / Jean-François Hochepied, Urszula Narkiewicz, Markus Niederberger, Nicola Pinna (ur.). - Varšava, 2007, 164-164

Skup
E-MRS 2007 Fall Meeting

Mjesto i datum
Varšava, Poljska, 17.09.2007. - 21.09.2007

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
alfa-FeOOH; beta-FeOOH; alfa-Fe2O3; XDR; FT-IR; Mossbauer

Sažetak
Iron oxides (a common name for iron oxyhydroxides and oxides) are important materials which have found application in traditional and advanced technologies. These materials can be utilized as pigments, catalysts, sensors, carriers for waste metal cations, etc. Iron oxides also play an important role in natural aquatic systems, sediments and soils. Various methods of iron oxide synthesis using « wet» chemistry were reported, such as a slow or forced hydrolysis of Fe(III)-salt solutions, crystallization of ferrihydrite gel, sol-gel, microemulsion and crystallization induced by ultrasound, microwave or gamma-irradiation. As a rule, these syntheses are conducted at low concentrations of Fe(III)-salts. In that case it is relatively easy to obtain monodisperse particles ; these studies, however, are generally important from an academic standpoint. In the present work we have focused on precipitation from concentrated Fe3+ salt solutions partially neutralized with concentrated NaOH. The precipitation systems were autoclaved at 160 oC. The precipitation process was monitored by analysis of the precipitate by XRD, 57Fe Mössbauer and FT-IR spectroscopies, and FE SEM. The kinetics of the reference system showed a formation of beta-FeOOH (akaganéite) which was after a prolonged time transformed into alpha-Fe2O3 (hematite). The addition of Na2HPO4 (concentrations in the final volume 0.010, 0.025, or 0.050 M) at the beginning of the precipitation caused significant changes in the phase composition of the precipitates. An additional appearance of alpha-FeOOH (goethite) was observed as a direct result of adding Na2HPO4 to the precipitation systems. The specific adsorption of phosphates at acidic pH values, and the aggregation effect play an important role in the formation of particles in respect of their size and morphology. The formation of the end-product alpha-Fe2O3 was controlled by the dissolution/reprecipitation mechanism.

Izvorni jezik
Engleski

Znanstvena područja
Kemija

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