Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 4; Volume 8, Part 4American Society of Mechanical Engineers, 1989 - Arctic regions |
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Page 72
... temperature range -50 ° C to -5 ° C decrease with increasing temperature but the rate of decrease is not as significant as that in the compression tests discussed in a previous section of this paper . If the energy release rate for ...
... temperature range -50 ° C to -5 ° C decrease with increasing temperature but the rate of decrease is not as significant as that in the compression tests discussed in a previous section of this paper . If the energy release rate for ...
Page 257
... temperature and humidity of the air surrounding individual droplets ( i.e. outside the boundary layer at the surface of the droplets ) are equal to those of the ambient air . This will be enhanced by wind and the continuous sweeping ...
... temperature and humidity of the air surrounding individual droplets ( i.e. outside the boundary layer at the surface of the droplets ) are equal to those of the ambient air . This will be enhanced by wind and the continuous sweeping ...
Page 258
... temperature of sail 6. Submergence of keel . 1. Ice Growth in Droplet From the ice shell theory , the surface temperature will fall below the solidification temperature to provide the thermal gradient necessary for heat transfer across ...
... temperature of sail 6. Submergence of keel . 1. Ice Growth in Droplet From the ice shell theory , the surface temperature will fall below the solidification temperature to provide the thermal gradient necessary for heat transfer across ...
Contents
OFFSHORE MECHANICS | 1 |
The Growth of Radial Cracks in Ice Sheets | 7 |
ICE FORCES | 11 |
Copyright | |
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analysis angle Arctic Engineering assumed Barents Sea Beaufort Sea behaviour berm Bjørnøya calculated coefficient Cole components computed Conference on Offshore constant constitutive equation damage evolution damage model deformation density depth determined diameter distribution dynamic effect energy equation experimental factor failure force fracture mechanics fracture toughness frequency friction function Geogrid grain horizontal ice floe ice load ice sheet ice thickness iceberg icebreaking impact increase indentor initial interaction keel material maximum measured Mechanics and Arctic Mellor microcracks modulus motion notch nucleation observed obtained ocean Offshore Mechanics parameters peak stress plane polycrystalline ice predicted pressure probability Proc radar ratio resistance ridge samples sea ice seabed shear shear stress ship shown in Figure simulation specimen spray ice strain rate strain tensor strength structure surface temperature tensile tensile stress tensor tests uniaxial compression variable vector velocity vertical wave Young's modulus