24 March 1999Mechanism of martensite γ'1 single-crystals formation during deformation of beta1-CuZnAl single crystals with oriented distribution of subgrain boundaries
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(beta) 1-CuZnAl single-crystals were subject to uniaxial tension with subgrain boundaries parallel to the direction of tension. A relation between individual stages of martensite (gamma) '1 single-crystals formation and changes of mechanical stress was determined. The stress was assessed on the basis of diffraction reflexes half-width measurement, measured on a Bond diffractometer, that ensured a precise assessment of even minute changes.
W. Bogdanowicz andKrystyna Wokulska
"Mechanism of martensite γ'1 single-crystals formation during deformation of beta1-CuZnAl single crystals with oriented distribution of subgrain boundaries", Proc. SPIE 3724, International Conference on Solid State Crystals '98: Single Crystal Growth, Characterization, and Applications, (24 March 1999); https://doi.org/10.1117/12.343017
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W. Bogdanowicz, Krystyna Wokulska, "Mechanism of martensite gamma'1 single-crystals formation during deformation of beta1-CuZnAl single crystals with oriented distribution of subgrain boundaries," Proc. SPIE 3724, International Conference on Solid State Crystals '98: Single Crystal Growth, Characterization, and Applications, (24 March 1999); https://doi.org/10.1117/12.343017