1972 Volume 1972 Issue 9 Pages 1751-1754
The ultra-fine ferric oxides of 50 to 650 Å in diameter were examined by X-ray diffraction, differential thermal analysis, electron microscope and H2O adsorption in order to find the cor- relation of the ultimate and agglomerated structures of the ferric oxides with the heat of im- mersion in water, ΔHI.
It was shown that ΔHI is almost independent of the particle size, except B-500-1 and B500-2, samples which showed higher ΔHI values (Fig.2). These two samples were prepared by heating amorphous hydrous oxide at 500° C, and showed partial crystallization to α-Fe2O3 and considerable sintering. Higher ΔHI values of the sintered samples were interpreted by the' presence of interparticle micropores, through which H2O molecules are more easily permeable than N2 molecules. The surface activity incident to the structural change is also thought to be pertinent to the higher ΔHI.
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