Abstracts for Annual Meeting of the Mineralogical Society of Japan
2005 Annual Meeting of the Mineralogical Society of Japan
Session ID : K4-03
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Evaporation rate anisotropyof forsterite
*Naoko MatsumotoHiroko NagaharaKazuhito OzawaShogo TachibanaMaho Yamada
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Abstract

Evaporation anisotropy of a synthetic single crystal of forsterite was investigated by high temperature vacuum experiments at temperatures from 1500 °C to 1750 °C. Anisotropy of evaporation rate is significant at temperatures below 1730 °C, where the rate is largest on (001), intermediate on (100), and smallest on (010) surfaces. The activation energies are 641, 592, and 570kJ/mole for (100), (010), and (001) surfaces, respectively. The anisotropy of evaporation rate is negligible at temperature above 1740 °C, where a different type of evaporation pits appears with a high density on the (010) surface.

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© 2005 Japan Association of Mineralogical Sciences
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