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 22
... increase in resistance at low speeds was observed for a wedge bow , but not for a simplified icebreaker bow . The current study extends the speed range to lower speeds and the increase in resistance appears for an icebreaker bow . The ...
... increase in resistance at low speeds was observed for a wedge bow , but not for a simplified icebreaker bow . The current study extends the speed range to lower speeds and the increase in resistance appears for an icebreaker bow . The ...
Page 275
... increase in the icing load can be expected due to a stronger wind . However , the cause of the overestimation of the Chaîné model ( model C ) was investigated and might be related to the calculation of the ice loads from the hourly ...
... increase in the icing load can be expected due to a stronger wind . However , the cause of the overestimation of the Chaîné model ( model C ) was investigated and might be related to the calculation of the ice loads from the hourly ...
Page 303
... increase with speed , it can be seen that friction angle in most of the cases are almost constant for the slow tests ( velocity < 40 mm / s ) . The friction angle based on Meyerhof's theory is only valid for the low rates and the increase ...
... increase with speed , it can be seen that friction angle in most of the cases are almost constant for the slow tests ( velocity < 40 mm / s ) . The friction angle based on Meyerhof's theory is only valid for the low rates and the increase ...
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