TY - JOUR
T1 - Preparation of monodisperse platelet-type hematite particles from a highly condensed β-FeOOH suspension
AU - Sugimoto, Tadao
AU - Waki, Shuzo
AU - Itoh, Hiroyuki
AU - Muramatsu, Atsushi
PY - 1996/4/20
Y1 - 1996/4/20
N2 - This is the first report on preparation of monodisperse platelet-type hematite (α-Fe2O3) particles. As an application of the gel-sol method recently developed by one of the authors for the syntheses of general monodisperse particles, monodisperse platelet-type hematite particles (≈3 μm in diameter, ≈0.6 μm in thickness) have been prepared by aging a highly condensed suspension of fine akaganeite (β-FeOOH) particles in a strongly alkaline medium at 70 °C for 8 days in the presence of a concentrated electrolyte. The yield was almost 100%. Each particle was bound by {001} basal planes and {012} side planes as identified by the oriented particulate monolayer-X-ray diffraction method. The formation of the characteristic shape has been explained in terms of the specific adsorption of OH- ions. Systematic control of the mean size was shown to be possible by regulating the preparation temperature of Fe(OH)3 gel as a starting material for β-FeOOH. The growth of the platelet-type hematite particles proceeded through a dissolution-recrystallization mechanism from β-FeOOH.
AB - This is the first report on preparation of monodisperse platelet-type hematite (α-Fe2O3) particles. As an application of the gel-sol method recently developed by one of the authors for the syntheses of general monodisperse particles, monodisperse platelet-type hematite particles (≈3 μm in diameter, ≈0.6 μm in thickness) have been prepared by aging a highly condensed suspension of fine akaganeite (β-FeOOH) particles in a strongly alkaline medium at 70 °C for 8 days in the presence of a concentrated electrolyte. The yield was almost 100%. Each particle was bound by {001} basal planes and {012} side planes as identified by the oriented particulate monolayer-X-ray diffraction method. The formation of the characteristic shape has been explained in terms of the specific adsorption of OH- ions. Systematic control of the mean size was shown to be possible by regulating the preparation temperature of Fe(OH)3 gel as a starting material for β-FeOOH. The growth of the platelet-type hematite particles proceeded through a dissolution-recrystallization mechanism from β-FeOOH.
KW - akageneite
KW - gel-sol method
KW - hematite
KW - monodispersed particles
KW - platelet-type particles
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U2 - 10.1016/0927-7757(95)03454-4
DO - 10.1016/0927-7757(95)03454-4
M3 - Article
AN - SCOPUS:0342832968
SN - 0927-7757
VL - 109
SP - 155
EP - 165
JO - Colloids and Surfaces A: Physicochemical and Engineering Aspects
JF - Colloids and Surfaces A: Physicochemical and Engineering Aspects
ER -