1974
DOI: 10.1016/0039-6028(74)90093-4
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The mobile water phase on ice surfaces

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Cited by 95 publications
(22 citation statements)
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“…It is easy to show using Eq. [5] and the known value of the icewater interfacial tension, γ = 33 mN/m (23), that the influence of the capillary curvature is two orders of magnitude smaller, compared with the disjoining pressure values and hence can be neglected. A thermocrystallization flux is caused by the latent heat of ice melting and is directed to the hot side according to the theory of mass transfer in frozen bodies (7).…”
Section: Tablementioning
confidence: 98%
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“…It is easy to show using Eq. [5] and the known value of the icewater interfacial tension, γ = 33 mN/m (23), that the influence of the capillary curvature is two orders of magnitude smaller, compared with the disjoining pressure values and hence can be neglected. A thermocrystallization flux is caused by the latent heat of ice melting and is directed to the hot side according to the theory of mass transfer in frozen bodies (7).…”
Section: Tablementioning
confidence: 98%
“…The difference between the disjoining pressure of a flat and a curved film, according to (7) is f = − (γ /r ), [5] where γ is the ice-water interfacial tension and r is the interlayer curvature, which is almost equal to the capillary radius, r . It is easy to show using Eq.…”
Section: Tablementioning
confidence: 99%
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“…Nuclear magnetic resonance (NMR) [26] spectroscopy suggested liquid layer fo rma ti on on ice: below the melting point there is a narrow absorption line, not the broad line one would expect from a periodic solid. Molecules at the surface between 20 and 0 °C rotate at a frequency five orders of magnitude greater than those in bulk ice, and about 1/25 as fast as those in liquid water.…”
Section: Diffraction Examination Of Premeltingmentioning
confidence: 99%
“…At present the hypothesis is accepted on the basis of several experimental evidences using NMR (Kvlividze et al, 1974), ellipsometry (Beaglehole and Nason, 1980), electrical (Jaccard, 1967;Maeno and Nishimura, 1978), and other measurements (Nakaya and Matsumoto, 1954;Jellinek, 1959;Golecki and Jaccard, 1977), and theoretical investigations by Fletcher (1962Fletcher ( , 1968, and Lacmann and Stranski (1972). The consensus view is that the layer is stable above about -20*10*.…”
Section: Growth Mechanismsmentioning
confidence: 99%