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 37
Typical advance coefficients for each operation were in the range of Js = 0.72 , Js = 0.65 , Js = 0.3 and Js = 0.15 ... At the lowest tested advance coefficient , J 0.2 , the thrust coefficient increased from K , 0.28 in uniform flow to ...
Typical advance coefficients for each operation were in the range of Js = 0.72 , Js = 0.65 , Js = 0.3 and Js = 0.15 ... At the lowest tested advance coefficient , J 0.2 , the thrust coefficient increased from K , 0.28 in uniform flow to ...
Page 86
Where the dependence of the advancing coefficient is only presented since the reflecting coefficient can be defined from the relation R ? + T2 = 1. It is shown that the advancing coefficient tends to zero T → 0.32 at y → 00 ...
Where the dependence of the advancing coefficient is only presented since the reflecting coefficient can be defined from the relation R ? + T2 = 1. It is shown that the advancing coefficient tends to zero T → 0.32 at y → 00 ...
Page 110
Indeed , the stress density function in the cable f ( Q ) , obtained from the ice thickness distribution ( Gumbel law , type 1 ) , used in nonlinear relationships Eqs . 1 , 2 and 3 is strongly nonsymmetrical ( coefficient of skewness ...
Indeed , the stress density function in the cable f ( Q ) , obtained from the ice thickness distribution ( Gumbel law , type 1 ) , used in nonlinear relationships Eqs . 1 , 2 and 3 is strongly nonsymmetrical ( coefficient of skewness ...
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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 interaction International layer length 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