TY - JOUR
T1 - Structure and composition of the nanocrystalline phases in a MgO-TiO2 system prepared via sol-gel technique
AU - Bokhimi, X.
AU - Boldú, J. L.
AU - Muñoz, E.
AU - Novaro, O.
AU - López, T.
AU - Hernández, J.
AU - Gómez, R.
AU - García-Ruiz, A.
PY - 1999
Y1 - 1999
N2 - Samples in the MgO-TiO2 system were prepared via the sol-gel technique with titanium and magnesium ethoxides as precursors and HNO3 as hydrolysis catalyst. The analyzed magnesia to titania weight ratios were 0.1:0.9, 0.5:0.5, and 0.9:0.1 (0.05, 0.5, and 4.0 MgO: TiO2 molar ratios). Samples were characterized with X-ray powder diffraction, differential thermal analysis, and thermogravimetry. To quantify the concentration and the crystallography of the phases in the samples, their crystalline structures were refined by using the Rietveld method. In addition to periclase, anatase, and rutile, three intermediate compounds were observed: karooite (MgTi2O5), geikielite (MgTiO3), and qandilite (Mg2TiO4). The formation of the above crystalline phases in the samples occurred after an exothermic reaction at 200°C, and their dehydroxylation above 300°C. Karooite was abundant only in titania-rich samples, while geikielite and qandilite concentrations were high in the samples with equal magnesia to titania weight percent. Phase concentrations depended on the annealing temperature of the sample and its MgO content. Magnesium was soluble in anatase, but not in rutile; the solubility, however, was low.
AB - Samples in the MgO-TiO2 system were prepared via the sol-gel technique with titanium and magnesium ethoxides as precursors and HNO3 as hydrolysis catalyst. The analyzed magnesia to titania weight ratios were 0.1:0.9, 0.5:0.5, and 0.9:0.1 (0.05, 0.5, and 4.0 MgO: TiO2 molar ratios). Samples were characterized with X-ray powder diffraction, differential thermal analysis, and thermogravimetry. To quantify the concentration and the crystallography of the phases in the samples, their crystalline structures were refined by using the Rietveld method. In addition to periclase, anatase, and rutile, three intermediate compounds were observed: karooite (MgTi2O5), geikielite (MgTiO3), and qandilite (Mg2TiO4). The formation of the above crystalline phases in the samples occurred after an exothermic reaction at 200°C, and their dehydroxylation above 300°C. Karooite was abundant only in titania-rich samples, while geikielite and qandilite concentrations were high in the samples with equal magnesia to titania weight percent. Phase concentrations depended on the annealing temperature of the sample and its MgO content. Magnesium was soluble in anatase, but not in rutile; the solubility, however, was low.
UR - http://www.scopus.com/inward/record.url?scp=0000146848&partnerID=8YFLogxK
U2 - 10.1021/cm9900812
DO - 10.1021/cm9900812
M3 - Artículo
SN - 0897-4756
VL - 11
SP - 2716
EP - 2721
JO - Chemistry of Materials
JF - Chemistry of Materials
IS - 10
ER -