Frazil Ice Formation

Frazil ice forms in flowing or turbulent water that has become supercooled by heat transfer to overlying air. This report investigates the influences of turbulence and water temperature on frazil ice formation. The rate and the quantity of frazil ice formed in a specified volume of supercooled water...

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Bibliographic Details
Main Authors: Ettema,R, Karim,M F, Kennedy,J F
Other Authors: IOWA INST OF HYDRAULIC RESEARCH IOWA CITY
Format: Text
Language:English
Published: 1984
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA147425
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA147425
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spelling ftdtic:ADA147425 2023-05-15T16:37:14+02:00 Frazil Ice Formation Ettema,R Karim,M F Kennedy,J F IOWA INST OF HYDRAULIC RESEARCH IOWA CITY 1984-07 text/html http://www.dtic.mil/docs/citations/ADA147425 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA147425 en eng http://www.dtic.mil/docs/citations/ADA147425 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost *ICE FORMATION *ICE MATHEMATICAL MODELS Frazil ice Text 1984 ftdtic 2016-02-20T23:27:45Z Frazil ice forms in flowing or turbulent water that has become supercooled by heat transfer to overlying air. This report investigates the influences of turbulence and water temperature on frazil ice formation. The rate and the quantity of frazil ice formed in a specified volume of supercooled water increase with both increasing turbulence intensity and decreasing water temperature. The influence of turbulence intensity on the rate of frazil ice formation, however, is more pronounced for larger initial supercooling. The turbulence characteristics of a flow affect the rate of frazil ice formation by governing the temperature to which the flow can be supercooled, by influencing heat transfer from the frazil ice to surrounding water, and by promoting collision nucleation, particle and floc rupture and increasing the number of nucleation sites. Larger frazil ice particles form in water supercooled to lower temperatures. The particles usually were disks, with diameters several orders greater than their thickness. Particle size generally decreased with increasing turbulence intensity. This report develops an analytical model, in which the rate of frazil ice formation is related to temperature rise of a turbulent volume of water from the release of latent heat of fusion of liquid water to ice. Experiments conducted in a turbulence jar with a heated, vertically oscillating grid served both to guide and too calibrate the mathematical analytic model as well as to afford insights into frazil ice formation. The formation of frazil ice was studied for temperatures of supercooled water ranging from -0.9 deg to -0.05 deg C. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
*ICE FORMATION
*ICE
MATHEMATICAL MODELS
Frazil ice
spellingShingle Snow
Ice and Permafrost
*ICE FORMATION
*ICE
MATHEMATICAL MODELS
Frazil ice
Ettema,R
Karim,M F
Kennedy,J F
Frazil Ice Formation
topic_facet Snow
Ice and Permafrost
*ICE FORMATION
*ICE
MATHEMATICAL MODELS
Frazil ice
description Frazil ice forms in flowing or turbulent water that has become supercooled by heat transfer to overlying air. This report investigates the influences of turbulence and water temperature on frazil ice formation. The rate and the quantity of frazil ice formed in a specified volume of supercooled water increase with both increasing turbulence intensity and decreasing water temperature. The influence of turbulence intensity on the rate of frazil ice formation, however, is more pronounced for larger initial supercooling. The turbulence characteristics of a flow affect the rate of frazil ice formation by governing the temperature to which the flow can be supercooled, by influencing heat transfer from the frazil ice to surrounding water, and by promoting collision nucleation, particle and floc rupture and increasing the number of nucleation sites. Larger frazil ice particles form in water supercooled to lower temperatures. The particles usually were disks, with diameters several orders greater than their thickness. Particle size generally decreased with increasing turbulence intensity. This report develops an analytical model, in which the rate of frazil ice formation is related to temperature rise of a turbulent volume of water from the release of latent heat of fusion of liquid water to ice. Experiments conducted in a turbulence jar with a heated, vertically oscillating grid served both to guide and too calibrate the mathematical analytic model as well as to afford insights into frazil ice formation. The formation of frazil ice was studied for temperatures of supercooled water ranging from -0.9 deg to -0.05 deg C.
author2 IOWA INST OF HYDRAULIC RESEARCH IOWA CITY
format Text
author Ettema,R
Karim,M F
Kennedy,J F
author_facet Ettema,R
Karim,M F
Kennedy,J F
author_sort Ettema,R
title Frazil Ice Formation
title_short Frazil Ice Formation
title_full Frazil Ice Formation
title_fullStr Frazil Ice Formation
title_full_unstemmed Frazil Ice Formation
title_sort frazil ice formation
publishDate 1984
url http://www.dtic.mil/docs/citations/ADA147425
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA147425
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA147425
op_rights APPROVED FOR PUBLIC RELEASE
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