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 75
... fluid velocity is expressed as v ( x , y ) = u ( x , y ) i + v ( x , y ) j ( 4 ) ( 2 ) and on the lower and upper surfaces as ( 5 ) where is a reference pressure , p the actual pressure along the Po channel , μo the viscosity at ...
... fluid velocity is expressed as v ( x , y ) = u ( x , y ) i + v ( x , y ) j ( 4 ) ( 2 ) and on the lower and upper surfaces as ( 5 ) where is a reference pressure , p the actual pressure along the Po channel , μo the viscosity at ...
Page 171
... fluid motion due to oscillation of the structure is based on the linear potential theory with consideration of fluid compress- ibility . The associate boundary value problem for the potential function is solved using the boundary ...
... fluid motion due to oscillation of the structure is based on the linear potential theory with consideration of fluid compress- ibility . The associate boundary value problem for the potential function is solved using the boundary ...
Page 226
... fluid movement beneath the structure is ( a ) unrestricted and ( b ) restricted . The bottom - surface pressure due ... fluid is equal to the vertical velocity of the ice . Given that the depth Я of the fluid is constant , the vertical ...
... fluid movement beneath the structure is ( a ) unrestricted and ( b ) restricted . The bottom - surface pressure due ... fluid is equal to the vertical velocity of the ice . Given that the depth Я of the fluid is constant , the vertical ...
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