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 87
... depends largely on DT and H. Whether ice motion grows or decays sub- stantially depends on a first critical value of the parameter DT ( when N = 1.45x10 - s -2s - 2 and H = 2.5m , this critical value is 5 ° C ) . When DTO is smaller ...
... depends largely on DT and H. Whether ice motion grows or decays sub- stantially depends on a first critical value of the parameter DT ( when N = 1.45x10 - s -2s - 2 and H = 2.5m , this critical value is 5 ° C ) . When DTO is smaller ...
Page 72
... depends on the pipeline length , and the distance and time steps . the number of time and distance steps is increased , the execution time will increase proportionally . If the distance and time steps are long , then model accuracy ...
... depends on the pipeline length , and the distance and time steps . the number of time and distance steps is increased , the execution time will increase proportionally . If the distance and time steps are long , then model accuracy ...
Page 246
... depends upon the actual uplift movement . Therefore , in order to control the upward creep of an " imperfect " pipe the uplift movement in each tempera- ture cycle should be limited to the " elastic " de for- mation characteristics of ...
... depends upon the actual uplift movement . Therefore , in order to control the upward creep of an " imperfect " pipe the uplift movement in each tempera- ture cycle should be limited to the " elastic " de for- mation characteristics of ...
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