Abstract
Starting with wurtzite-type single crystals, AgI was investigated at room temperature and pressures up to 0.5 GPa by means of a polarizing light microscope and with the precession technique. Distinct orientation relations were observed between four different AgI phases that occur suc cessively under increasing pressure. At 0.35 GPa a reverse-obverse (111) twin of zincblende-type AgI is formed with twin plane parallel to the (001) plane of the wurtzite-type structure. The antilitharge type of AgI occurs at 0.39 GPa. Its tetragonal [001] direction runs parallel to one of the (100) directions of the zincblende type. At almost the same pres sure the transformation to the NaCl-type form takes place. This AgI modification shows also twinning on (111) and the basis vectors are oriented parallel to those of the zincblende type. The transition between the zincblende- and the anti litharge-type phase shows a hysteresis: The back transfor mation occurs at 0.35 GPa. NaCl-type AgI transforms di rectly to the zincblende-type form at approximately 0.2 GPa when pressure is released.The observed orientation relations between zincblende-, antilitharge- and NaCl-type AgI support transition mecha nisms that have been proposed earlier [Keen & Hull, J. Phys.: Condens. Matter5(1993) 23–32].
Subject
Inorganic Chemistry,Condensed Matter Physics,General Materials Science
Cited by
2 articles.
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