Observation of the Fracture Plane of Potassium Iodide Formed at the Pressure-Induced Phase Transition
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概要
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The fracture plane of potassium iodide which experienced the phase transition athigh pressure was observed with the stereoscopic microscope at zero pressure, wherethe pressure was applied in the controlled rate and removed rapidly in various time in-tervals, At's, after the initiation of the phase transition was detected. The outerregion of the fracture plane observed, domain B, 'was bumpy and random, suggestingthat this region experienced the phase transition. However, the inner region of thefracture plane, domain F, was smooth, flat and considerably cleavable, indicatingthat this domain remained almostly at Bl in the case of very small At. Although in-creasing At did not alter the geometrical appearance of the fracture plane, thecleavability in phase F was rather lost, which leads us to the cccnclusion that the transi-lion following the formatiorn of domain B proce':ded over the entire volume of do-main F.
- 社団法人日本物理学会の論文
- 1988-04-15
著者
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FUJIWARA Hiroshi
Department of Bioregulatory Medicine, Graduate School of Medicine, Ehime University
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Negishi Saiko
Department Of Materials Science Faculty Of Science Hiroshima University
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Nomura Motoyuki
Department Of Materials Science Faculty Of Science Hiroshima University
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OKANO Yoji
Department of Materials Science,Faculty of Science,Hiroshima University
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Fujiwara Hiroshi
Department Of Bioregulatory Medicine Ehime University Graduate School Of Medicine
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Okano Yoji
Department Of Materials Science Faculty Of Science Hiroshima University
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Fujiwara Hiroshi
Department of Advanced Energy Engineering Sciences, Interdisciplinary Graduate School of Engineering Science, Kyusyu University
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