Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 7, Parts 4-6American Society of Mechanical Engineers, 1988 - Arctic regions |
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Page 222
... energy before ramming is transformed into many different forms of energies , as explained in Reference [ 5 ] . In such a case , however , it is assumed that the scantlings of the bow may allow it to to be considered rigid . The post ...
... energy before ramming is transformed into many different forms of energies , as explained in Reference [ 5 ] . In such a case , however , it is assumed that the scantlings of the bow may allow it to to be considered rigid . The post ...
Page 263
... energy waste by excluding a few constituents out of a full ice resistance . The problem is solved by the ... energy . The amount of this Presented at the Seventh International Conference on Offshore Mechanics and Arctic Engineering ...
... energy waste by excluding a few constituents out of a full ice resistance . The problem is solved by the ... energy . The amount of this Presented at the Seventh International Conference on Offshore Mechanics and Arctic Engineering ...
Page 335
... energy of 4.4 X 105 J ) and stops within semi - infinite ice . DYNA calculations displayed in Figure 12 show that the maximum kinetic energy of the ice ( rotational and translational motion within the target ) is only 8500 J ...
... energy of 4.4 X 105 J ) and stops within semi - infinite ice . DYNA calculations displayed in Figure 12 show that the maximum kinetic energy of the ice ( rotational and translational motion within the target ) is only 8500 J ...
Contents
ICE PROPERTIESII | 31 |
Simple Beam Tests on Type S3 Sea | 63 |
ICE DRIFT AND DYNAMICS | 69 |
Copyright | |
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analysis angle Arctic Engineering average beam Beaufort Sea Bering Sea buckling buoys Cold Regions compressive Conference on Offshore crack creep crushing curves deflection deformation density diameter drift dynamic effect elastic modulus equation estimated experimental factor failure flexural strength floe fracture toughness freshwater ice friction coefficient gauges geostrophic wind grain heat transfer horizontal ice drift ice force ice loads ice motion ice pressure ice sheet ice tests ice thickness ice velocity iceberg icebreaking impact increase indentation island layer linear measured Mechanics and Arctic method MIZEX model ice modulus Molikpaq normal force Norton Sound Ocean Offshore Mechanics oriented parameters pressure panel PVDF ratio reinforced ice Research samples scale sea ice sediments shear ship shown in Figure Sinha Sodhi specimen spray ice strain gauges strain rate strain tensor structure surface temperature tensor thermosyphon Timco tion uniaxial values vertical