Abstract
The microstructure of magnesia grains obtained from coarse crystalline and cryptocrystalline magnesites and from seawater and brines is illustrated and the influence of the amount and type of impurities on the development of periclase is discussed. The factors which affect direct peri‐clase‐periclase bonding in basic brick are reviewed; the microstructural effects of additions of sesquioxides are shown. The complex reactions between periclase and chromite spinel are considered with reference to direct periclase‐chromite bonding. The formation of secondary periclase is briefly described.
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