gsminmag Mineralogical Magazine Mineralogical Magazine 0026-461X Mineralogical Society 10.1180/minmag.1966.035.274.08 On the Oriented Conversion of Ca(OH)2 to CaO Chatterji S. M.Sc., D.Phil. Jeffery J. W. Ph.D., F.Inst.P. Birkbeck College Crystallography Laboratory, University of London 6 1966 35 274 867 870 25 1 1966 Copyright © 1966, The Mineralogical Society 1966 Summary

In order to study the orientational relationship between Ca(OH)2 and CaO, the transformation was carried out in stages inside an electron microscope by condensing the electron beam, and the process was monitored by electron diffraction. It has been found that at the initial stage all the hexagonal spots of Ca(OH)2 split into two ; on further heating one set of spots disappear. The remaining set of spots corresponds to the CaO structure, which has an orientational relationship to the hydroxide structure. To estimate the degree of orientation, a sample of brucite was treated in a similar way to the Ca(OH)2; a comparison shows that a high degree of orientation is preserved in the conversion of Ca(OH)2 to CaO. This observation is contrary to earlier reports.