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 38
In blocked flow , the upper part of the propeller operated in the slow fluid of the separated wake of the blockage . This resulted in an effective decrease of the local advance coefficient of the blade sections and an associated ...
In blocked flow , the upper part of the propeller operated in the slow fluid of the separated wake of the blockage . This resulted in an effective decrease of the local advance coefficient of the blade sections and an associated ...
Page 64
In the calculations The reverse flow in the lower part of the recirculating cell has not been taken into account . This velocity is assumed to be very small compared to the velocity of the ocean current . We can derive the motion of the ...
In the calculations The reverse flow in the lower part of the recirculating cell has not been taken into account . This velocity is assumed to be very small compared to the velocity of the ocean current . We can derive the motion of the ...
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