Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 18, Part 5American Society of Mechanical Engineers, 1999 - Arctic regions |
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Page 104
... causes restrained deformation of longitudinal fibres and , accordingly , to normal stresses of restrained twisting O ... caused by spind : do not exceed ~ 30 % of σ ( r ) . Therefore , the value of σ ( r ) may be taken as an effective ...
... causes restrained deformation of longitudinal fibres and , accordingly , to normal stresses of restrained twisting O ... caused by spind : do not exceed ~ 30 % of σ ( r ) . Therefore , the value of σ ( r ) may be taken as an effective ...
Page 211
... caused either by the platform structural response or ice failure characteristics , or a combination of both ( Peyton , 1966a ) . Information on the measured ice loads have been reported in a number of confidential reports issued to Oil ...
... caused either by the platform structural response or ice failure characteristics , or a combination of both ( Peyton , 1966a ) . Information on the measured ice loads have been reported in a number of confidential reports issued to Oil ...
Page 227
... causes an upward motion of the ice sheet end , overriding the frictional restraint ) , and the ice will fail either ... caused by a combination of buckling and bending ( Haynes et al . 1983 ) . The time - varying in - plane force Ñ ( t ) ...
... causes an upward motion of the ice sheet end , overriding the frictional restraint ) , and the ice will fail either ... caused by a combination of buckling and bending ( Haynes et al . 1983 ) . The time - varying in - plane force Ñ ( t ) ...
Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
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Allen Bay analysis angle Arctic Engineering ASME average boundary brittle calculated Canada channel coefficient component compressive cone Confederation Bridge Conference on Offshore contact area Copyright 1999 crack creep creep deformation crushed deformation density determined diameter distribution dynamic effect equation estimate failure stress Figure floes fracture frequency friction frozen soil full scale gas hydrate Grand Banks horizontal hydrodynamic ice block ice class ice conditions ice force ice loads ice pieces ice sheet ice strength ice thickness iceberg iceberg management icebreaker increase indentation tests indentor interaction layer level ice maximum measured Mechanics and Arctic mm/s Newfoundland Northern Sea Route observed Offshore Mechanics parameters peak Pechora Sea piers pipeline planetary boundary layer predicted pressure ratio Research resistance rubble Sakhalin salinity scantlings scour sea ice sensors shape shear ship shows speed stamukha surface temperature thrust torque values velocity vertical water depth width wind zone