Abstract
POLYGONIZATION has been studied hitherto by means of two different methods: Guinier and co-workers1 used refined X-ray methods, which, however, only permit the detection of orientation differences without localizing the domain responsible for a particular spot; Cahn and others2, on the other hand, used etching techniques to make visible the polygon boundaries. The mean difference of orientation was estimated from the radius of curvature of the bent specimen and the width of the domains.
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References
Guinier, A., and Tennevin, J., “Progress in Metal Physics”, 2 (edit. by B. Chalmers. Interscience Publishers, New York, 1950).
Cahn, R. W., J. Inst. Metals, 76, 121 (1949); see also “Progress in Metal Physics”, 2. Dunn, C. G., and Daniels, F. W., Trans. Amer. Inst. Met. Eng., 191, 147 (1951).
Konobejewski, S., and Mirer, I., Z. Krist., 81, 69 (1932).
Françon, M., Revue d'Optique, 31, 65 (1952).
Cottrell, A. H., “Dislocations and Plastic Flow in Crystals” (Oxf. Univ. Press, 1953).
Tolansky, S., “Multiple Beam Interferometry of Surfaces and Thin Films” (Oxf. Univ. Press, 1948).
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AMELINCKX, S. Direct Observation of Polygonization in Rocksalt. Nature 173, 993–994 (1954). https://doi.org/10.1038/173993b0
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DOI: https://doi.org/10.1038/173993b0
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