Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 18, Part 5American Society of Mechanical Engineers, 1999 - Arctic regions |
From inside the book
Results 1-3 of 33
Page 47
... channel made through fast ice . The experience of Russian navigators showed that the age and state of the channel plays a rather significant role when escorting the ships via such kind of routes ( Arikainen & Chubakov , 1987 ; Gotsky ...
... channel made through fast ice . The experience of Russian navigators showed that the age and state of the channel plays a rather significant role when escorting the ships via such kind of routes ( Arikainen & Chubakov , 1987 ; Gotsky ...
Page 49
... channel axis is connected with that at the edge by a linear equation . For constructing a more accurate formula it is necessary to have special observation data which are , unfortunately , absent . h2 = chax - hiev ( 8 ) where hed and ...
... channel axis is connected with that at the edge by a linear equation . For constructing a more accurate formula it is necessary to have special observation data which are , unfortunately , absent . h2 = chax - hiev ( 8 ) where hed and ...
Page 94
... channel transit also generates reasonably high loads , at about 8 degrees blade pitch . Blade bending moment ( at 0.35R ) is plotted versus pitch angle in Figure 8. Bending moments are higher in the broken channel than in level ice ...
... channel transit also generates reasonably high loads , at about 8 degrees blade pitch . Blade bending moment ( at 0.35R ) is plotted versus pitch angle in Figure 8. Bending moments are higher in the broken channel than in level ice ...
Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
24 other sections not shown
Other editions - View all
Common terms and phrases
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