Abstract
The reaction between strontium
carbonate and iron(III) oxide has been studied in a system open to the
atmosphere and in a vacuum. The extent of reaction was calculated from the
analysis of the solid products by X-ray diffraction and, in the case of the experiments
in vacuum, from the amount of carbon dioxide evolved from the system also. ��� In vacuum, the monoferrite SrFe2O4
results from the direct reaction of strontium carbonate and iron(III) oxide at
comparatively low temperatures, while the hexaferrite SrFe12O19
is formed by the reaction of Sr2Fe2O4 with
iron(III) oxide at higher temperatures. The formation of the ferrite Sr2Fe2O5
depends upon the prevailing atmosphere, since this compound was present only as
an intermediate phase when the experiments were carried out in air and not in
vacuum. Only three compounds of strontium, iron, and oxygen were found, namely
the ferrites SrFe2O4, Sr2Fe2O5,
and SrFe12O19. ��� The observataions appear to be explicable
in terms of Tammann temperatures.
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