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Extreme values of ice cover thickness and ice phenomena duration on lakes in Poland
Limnological Review, 2009 openaire
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Freezing phenomena in ice–water systems
Energy Conversion and Management, 2002The characteristics of solidification and melting are reviewed. The properties of water and ice and the phase diagram of water are discussed with special emphasis on ice density. A concise account of the freezing process and the Stefan problem is presented.
M. Akyurt, G. Zaki, B. Habeebullah
exaly +2 more sources
Modeling transport phenomena of ice slurry in an ice forming unit
International Journal of Refrigeration, 2016In this article, multiphase convective and solidification transport phenomena of ice slurry is investigated by developing a one-domain macroscopic model to simulate its formation in a rectangular ice forming unit. Convection, sedimentation, interfacial drag, permeability, remelting and viscosity variations are incorporated into this model through the ...
Ankit Mahato, Arvind Kumar
exaly +2 more sources
Diffusion and Relaxation Phenomena in Ice
The Journal of Chemical Physics, 1969The underlying mechanisms of several rate processes in ice are examined through cross comparisons of the processes with each other and with experimental observations. The assumption that the migration of orientational defects (Bjerrum faults) is the common origin of dielectric and elastic relaxation leads to a predicted ratio of dielectric-to-elastic ...
Lars Onsager, L. K. Runnels
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Snow‐and‐ice phenomena in the polar urals
Polar Geography and Geology, 1989Abstract Long‐term studies carried out in the test basin of the Bol'shaya Khadata River have allowed the authors to describe the complex of glacio‐nival phenomena typical of the rock tundra zone of the Polar Urals. It was found that the winters are characterized by snow drifting, which results in redistribution of snow at the macro‐ and especially the ...
V. G. Khodakov, Ye. A. Il'ina
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Journal of Colloid and Interface Science, 1967
Abstract Two new phenomena are described which would indicate directly two mechanisms of mass transfer along an ice surface. One is the neck formation observed between an ice sphere and a plane placed cose to but not in contact with it in an ice-saturated atmosphere.
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Abstract Two new phenomena are described which would indicate directly two mechanisms of mass transfer along an ice surface. One is the neck formation observed between an ice sphere and a plane placed cose to but not in contact with it in an ice-saturated atmosphere.
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Cratering phenomena on aircraft anti-icing films
Journal of Aircraft, 1996This article reports on a study of cratering effects in thin anti-icing films designed to protect aircraft surfaces from snow and ice accumulation while the aircraft is on the ground awaiting takeoff. These fluids primarily consist of a glycol used as a freezing point depressant, water, and to a small extent thickening and wetting agents.
J. La Due, M. R. Muller, M. Swangler
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Experimental and computational simulation of in-flight icing phenomena
Progress in Aerospace Sciences, 1998Abstract This paper reviews experimental and computational methods used for simulation of ice accretion on aircraft flying through icing conditions. Such methods were recently reviewed by the AGARD FDP Working Group 20 and the present paper represents a revised and updated version of parts of the Working Group report. To provide essential background,
R.J. Kind +4 more
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Multiscale Models of Sea Ice Phenomena
2019Sea ice can be viewed as a composite material over multiple scales. On the smallest scale, sea ice is viewed as a two-phase composite of ice and brine. On the mesoscale, one may consider pancake ice and slush as a viscoelastic composite. On the larger scale, one may consider the mix of ice floes and water.
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Modeling of ice phenomena in the mouth of the Vistula River
Acta Geophysica, 2014The mouth of the Vistula River, which is a river outlet located in tideless area, is analyzed. The Vistula River mouth is a man-made, artificial channel which was built in the 19th century in order to prevent the formation of ice jams in the natural river delta.
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