Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 14, Part 4American Society of Mechanical Engineers, 1995 - Arctic regions |
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Page 115
Qs2 = sensible heat flux density required to warm the non - freezing liquid to ( To + T ) / 2 W m ? ) sensible heat flux density evolved when frozen ice cools to TE ( W m ? ] 9 = liquid water content of the airstream [ kg mo ) K ...
Qs2 = sensible heat flux density required to warm the non - freezing liquid to ( To + T ) / 2 W m ? ) sensible heat flux density evolved when frozen ice cools to TE ( W m ? ] 9 = liquid water content of the airstream [ kg mo ) K ...
Page 120
8 shows the influence of cylinder diameter , D , on the icing mass flux , P ; É . The critical liquid water content at the Ludlam limit diminishes as the cylinder diameter increases because the heat transfer coefficient varies ...
8 shows the influence of cylinder diameter , D , on the icing mass flux , P ; É . The critical liquid water content at the Ludlam limit diminishes as the cylinder diameter increases because the heat transfer coefficient varies ...
Page 135
Lunardini , V.J. , 1981 , " Heat Transfer in Cold Climates " , Van Nostrand Reinhold , New York . flow through the packed bed . The freezing process is affected indirectly by changes in the resistance to the flow .
Lunardini , V.J. , 1981 , " Heat Transfer in Cold Climates " , Van Nostrand Reinhold , New York . flow through the packed bed . The freezing process is affected indirectly by changes in the resistance to the flow .
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Contents
139 | 95 |
Mechanical Behavior of Ice Loaded Optical Ground Wires | 107 |
Influence of the Surface Liquid Film on Cylinder Icing Under Marine Conditions | 115 |
Copyright | |
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activities analysis applied Arctic average axis beam boundary brine cable calculated caused coefficient cold compression considered constant crack deformation density dependent depth described determined developed direction distribution effect elastic energy Engineering equation estimated experiments failure field Figure floe flow force fracture freezing function given grain grain boundary Greenland heat ice cover ice load ice sheet iceberg increase initial International layer length limit liquid mass material maximum mean measured Mechanics mode natural observed obtained offshore operations parameters period possible present problem production region relative Research salinity sea ice sector shown shows snow solution specimen speed spray stations strain strength stress structure surface Table Technology temperature thickness towing transfer volume wave wind zone