Abstract
To examine the reason for the formation and the structure of cubic ice in a restricted space, we measured the powder x-ray diffraction patterns of cubic ice formed within the mesopores of porous silicas as a function of pore size (4–70 nm). The results strongly suggest that cubic ice formed in the mesopores does not take a cubic structure as envisaged by König. It may be actually composed of very small crystallites of hexagonal ice that contains a large amount of growth faults depending on the crystallite size, that is, ice with disordered stacking sequence. Suppression of crystal growth of ice in the mesopores seems to be a vital factor for the formation and the stability of cubic ice.
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Dates
Type | When |
---|---|
Created | 20 years, 7 months ago (Jan. 15, 2005, 11 a.m.) |
Deposited | 2 years, 1 month ago (July 8, 2023, 8:06 p.m.) |
Indexed | 3 weeks, 1 day ago (July 30, 2025, 8:24 p.m.) |
Issued | 20 years, 7 months ago (Jan. 7, 2005) |
Published | 20 years, 7 months ago (Jan. 7, 2005) |
Published Online | 20 years, 7 months ago (Jan. 7, 2005) |
Published Print | 20 years, 6 months ago (Jan. 22, 2005) |
@article{Morishige_2005, title={The proper structure of cubic ice confined in mesopores}, volume={122}, ISSN={1089-7690}, url={http://dx.doi.org/10.1063/1.1836756}, DOI={10.1063/1.1836756}, number={4}, journal={The Journal of Chemical Physics}, publisher={AIP Publishing}, author={Morishige, Kunimitsu and Uematsu, Hiroaki}, year={2005}, month=jan }