Summary
The paper deals with the question whether the phases intermediate betweenγ- andβ-MnO2, which occur upon heating the former, possess the same type of random layer structure which has been proposed and confirmed earlier forγ-MnO2. In order to test that hypothesis, the powder diffraction pattern has been computed for five different values of the pyrolusite concentrationp in the random structure. The ensueing curves account for the main features of the intensity records of samples heated at different temperatures. The remaining discrepancies are definitely reduced if each record is compared with an appropriate weighted average of theoretical curves, indicating that in each sample the values ofp are distributed within a wide range.
Similar content being viewed by others
References
Brenet, J., J. P. Gabano and M. Seigneurin, C.R. du 16e Congr. Int. de Chimie Pure et Appl., p. 70, 1957.
Masataro Fukuda, National Technical Report4 (1958) 321.
Byström, A. M., Acta Chem. Scand.3 (1949) 163.
Wolff, P. M. de, Acta Cryst.12 (1959) 371.
Plomp, F. H., J. B. le Poole and P. M. de Wolff, Acta Cryst.13 (1960) 1095.
Warren, B. E., Phys. Rev.59 (1941) 693.
Strunz, H., Naturwiss78 (1943) 89.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Laudy, J.H.A., De Wolff, P.M. X-ray investigation of theγ-β transformation of MnO2 . Appl. Sci. Res. 10, 157–168 (1962). https://doi.org/10.1007/BF02928071
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF02928071