SHAPE OF GRAIN BOUNDARY GROOVE ONPURE ICE SURFACE
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Dry Air
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In this work we studied the evolution of the groove that forms the grain boundary (BG) when it emerges to a free surface, in the presence of different processes of matter transport. By using a confocal microscope, the shape of the grain edge groove was obtained in an ice sample with orientation <1010>/50◦at −5◦C ; after keeping it 3 h in an environment with dry air. The shapes and depths of the grain boundary groove obtained experimentally, at regular time periods, were satisfactorily fitted considering a process of transport of matter developed by Srinivasan and Trivedi. In this model the transport of matter is mainly ruled by gaseous diffusion and not by surface diffusion.
1999 ◽
Vol 14
(6)
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pp. 2548-2553
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1995 ◽
Vol 450
(1940)
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pp. 569-587
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Keyword(s):
1986 ◽
Vol 44
◽
pp. 732-733
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