The energy density of water and ice nucleation.
The energy density of water and ice nucleation.
复制标题
DOI:
10.1126/science.259.5100.1469
复制
发表时间:
1993-03
期刊:
影响因子:
56.9
通讯作者:
L. Wilen
中科院分区:
文献类型:
--
作者:
L. Wilen
M. Gavish et al. hypothesize (1) that nucleation is induced by large electric fields found in the narrow cracks of polar crystals. Their calculations show that an ice bilayer structure has a higher energy in a D-alanine crystal crevice than in a D, L-alanine crystal crevice, so they conclude that nucleation is facilitated by the latter crystals. What is pertinent to the nucleation process, how-ever, is the difference between the energy density of an ice nucleus and that of water in the crevice of each kind of crystal. Furthermore, a bilayer is not a likely shape for such an ice nucleus because of the heavy cost of surface energy relative to the gain in free energy that results from the chemical potential difference between ice and supercooled water. The bilayer nucleus described in the report would certainly be unstable relative to water unless ice preferentially wet the surface of the crystals. This would constitute surface freezing, which is not consistent with the usual surface melting of ice observed in nature (2). An estimate can be made of the difference in the electrostatic energy density (W) between a small spherical ice nucleus (3) and the same volume of water in an electric field. Following Jackson (4), one can write