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 219
... internal and outer radii a and b , respectively ) , subjected to an internal pressure Osphere ; ra- dial cracks are assumed to emanate from the internal boundary . With increase in pressure these radial cracks stably increase in length ...
... internal and outer radii a and b , respectively ) , subjected to an internal pressure Osphere ; ra- dial cracks are assumed to emanate from the internal boundary . With increase in pressure these radial cracks stably increase in length ...
Page 251
... internal thermal resistivities can be considered negligible and the following expression should be used in the calculi : α 1 22 ; n π d In i + 1 d where d - internal diameter of the i - layer in the wall . The iteration method based on ...
... internal thermal resistivities can be considered negligible and the following expression should be used in the calculi : α 1 22 ; n π d In i + 1 d where d - internal diameter of the i - layer in the wall . The iteration method based on ...
Page 347
... internal ice stress . Considering the wind and current , the vertical structure of the planetary boundary layer near the ice surface is in the most general and complex case dominated by several interacting physical effects . Among these ...
... internal ice stress . Considering the wind and current , the vertical structure of the planetary boundary layer near the ice surface is in the most general and complex case dominated by several interacting physical effects . Among these ...
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