Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9830107 | Journal of Crystal Growth | 2005 | 8 Pages |
Abstract
By observing the crystal shapes and kinetics of ice Ih growing at high pressures from the melt, it was found that the prism {101¯0} faces undergo a roughening transition at approximately -16âC and 160 MPa (1600 bar) in H2O ice, and -14âC and 180 MPa (1800 bar) in D2O ice. At temperatures above the roughening transition, the prism facets completely vanished and the curves of growth rate versus growth drive were linear. In contrast, below the roughening temperature, regions of prism facets existed and the growth rate curves were approximately quadratic. The basal {0001} faces persisted up to 0âC and gave approximately quadratic growth rate curves. The melting curves of ice Ih for H2O and D2O were accurately measured by direct observations of the solid-liquid coexistence equilibrium and found to agree with previous results obtained with other methods.
Related Topics
Physical Sciences and Engineering
Physics and Astronomy
Condensed Matter Physics
Authors
Minoru Maruyama,