Pregled bibliografske jedinice broj: 328449
Influence of cobalt ions on the precipitation of goethite in highly alkaline media
Influence of cobalt ions on the precipitation of goethite in highly alkaline media // Clay minerals, 43 (2008), 1; 95-105 doi:10.1180/claymin.2008.043.1.07 (međunarodna recenzija, članak, znanstveni)
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Naslov
Influence of cobalt ions on the precipitation of goethite in highly alkaline media
Autori
Krehula, Stjepko ; Musić, Svetozar
Izvornik
Clay minerals (0009-8558) 43
(2008), 1;
95-105
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
cobalt ions ; goethite ; cobalt ferrite ; XRD ; Mossbauer ; FTIR ; FE-SEM ; EDS
Sažetak
The effects of cobalt ions on the precipitation of goethite in highly alkaline media were monitored using X-ray diffraction (XRD), Mossbauer, Fourier transform infrared (FTIR) and energy dispersive X-ray (EDS) spectroscopies and field emission scanning electron microscopy (FE-SEM)techniques. Tetramethylammonium hydroxide was used as a precipitating agent. The precipitates were collected after heating of the precipitation systems at 160 º ; ; C for 2 h. The XRD results showed the formation of goethite structure as a single phase up to r = 6.98 (where r = 100· ; ; [Co]/([Co]+[Fe])). Cobalt ferrite was found as an additional phase in the precipitates obtained at r = 9.09 and 13.04. Mossbauer spectroscopy showed the formation of solid solutions of a-(Fe, Co)OOH. The incorporation of cobalt ions into the goethite crystal structure was monitored by a decrease in the average hyperfine magnetic field (Bhf). The value Bhf i decreased linearly up to r = 5.66, whereas a nonlinear dependence was obtained at r = 6.98 to 13.04. Infrared (IR) bands corresponding to the bending vibrations dOH and gOH were shifted from 892 to 903 cm-1 and from 797 to 800 cm-1, respectively, up to r = 6.98. Fourier transform infrared spectroscopy lacked the sensitivity to monitor the effects of cobalt ions, demonstrated by the Mo¨ssbauer analysis. Cobalt incorporation into the crystal structure of goethite induced a gradual elongation of a-(Fe, Co)OOH particles along the crystallographic c axis. The formation of a-(Fe, Co)OOH nanowires was shown at r 56.98. These nanowires were ~700 nm long, whereas their diameter was ~15-20 nm. The majority of the cobalt ferrite particles were in the nanosize range, as observed by FE-SEM. On the basis of the Co/Fe ratio measured by EDS, it appears that the cobalt ferrite particles were not fully stoichiometric.
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
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