Thermal behaviour of alumina precursor obtained by the aluminium sulphate-urea reaction in boiling aqueous solution

Ada K., Sarikaya Y., Alemdaroglu T., ÖNAL M.

CERAMICS INTERNATIONAL, cilt.29, sa.5, ss.513-518, 2003 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 29 Sayı: 5
  • Basım Tarihi: 2003
  • Doi Numarası: 10.1016/s0272-8842(02)00195-5
  • Dergi Adı: CERAMICS INTERNATIONAL
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.513-518
  • Anahtar Kelimeler: porosity, thermal properies, Al2O3, dehydration, dehydroxylation, EMULSION EVAPORATION TECHNIQUE, PHYSICOCHEMICAL PROPERTIES, HOMOGENEOUS PRECIPITATION, POWDERS, TEMPERATURE, BENTONITE, SIZE
  • Ankara Üniversitesi Adresli: Evet

Özet

An aqueous solution containing 0.1 M Al3+ and excess urea was boiled for 4 h to obtain an alumina precursor precipitate. The precursor precipitate was separated into several portions and each portion was heated at a different temperature for 4 h between 100-1100 degreesC. Thermally treated samples were investigated by X-ray diffraction (XRD) analysis, differential thermal analysis (DTA), thermogravimetric analysis (TGA) and scanning electron microscopy (SEM) techniques. The particle size distributions (PSD) and nitrogen adsorption-desorption isotherms at 77 K of the same samples were also determined. The XRD data showed that the previously amorphous precursor was transformed respectively into delta-Al2O3 at 850 degreesC and alpha-Al2O3 at 1100 degreesC. The TGA data were used to calculate the activation energies for the dehydration and dehydroxylation of the precursor according to the Coats-Redfern equation and the results were discussed. From the SEM and PSD data, it was determined that most of the precursor particles were agglomerated. The adsorption data were used to calculate the specific surface areas (A) and the desorption data were used to calculate the specific micropore-mesopore volumes (V). At 100 degreesC, the A and V values were respectively, 15 m(2) g(-1) and 0.030 cm(3) g(-1). They increased by increasing temperature and reached their maximum values of 117 m(2) g(-1) and 0.350 cm(3) g(-1) respectively at 900 degreesC and then decreased promptly at 1000 degreesC. (C) 2003 Elsevier Science Ltd and Techna S.r.l. All rights reserved.