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 111
... causes and external causes , the internal causes being the reaction of the microscopic structural parameters of the material while the external causes the environmental conditions and the loading cases , with the nature of the ...
... causes and external causes , the internal causes being the reaction of the microscopic structural parameters of the material while the external causes the environmental conditions and the loading cases , with the nature of the ...
Page 322
... causes changes in the settlement of the snowcover which is not only limited to the vicinity of the station . CONCLUSIONS An incremental approached was tried to simulate the settle- ment of a snowcover under distributed load . Using this ...
... causes changes in the settlement of the snowcover which is not only limited to the vicinity of the station . CONCLUSIONS An incremental approached was tried to simulate the settle- ment of a snowcover under distributed load . Using this ...
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