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 210
... LOAD L normalized dynamic amplitude PEAK At TIME = L peak L peak fundamental frequency 1 fo At bias load TROUGH L trough t + At fo L dt Fig . 7 LOADING WAVEFORM CHARACTERIZATION Significant ice events were defined as those with ice loads ...
... LOAD L normalized dynamic amplitude PEAK At TIME = L peak L peak fundamental frequency 1 fo At bias load TROUGH L trough t + At fo L dt Fig . 7 LOADING WAVEFORM CHARACTERIZATION Significant ice events were defined as those with ice loads ...
Page 308
... load - deflection curve is called the secondary path . Real structures are " imperfect " . There are unavoidable minor irregularities in dimensions and material properties . The imperfections may trigger the new deformation pattern from ...
... load - deflection curve is called the secondary path . Real structures are " imperfect " . There are unavoidable minor irregularities in dimensions and material properties . The imperfections may trigger the new deformation pattern from ...
Page 92
... load combination and the actual loads . The theoretical characteristics of this integrated system is that the mathematicall model of load com- bination is formed by searching throughout all possi- ble load combinations in load space by ...
... load combination and the actual loads . The theoretical characteristics of this integrated system is that the mathematicall model of load com- bination is formed by searching throughout all possi- ble load combinations in load space by ...
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