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 9
Page 48
... pass ; c ) plan view at the moment of the ship pass First of all we should make some necessary assumptions . According to ( Gorbunov & Losev , 1978 ) , the lateral influence of island is expressed by empirical formula : D = 0.9√w ( 1 ) ...
... pass ; c ) plan view at the moment of the ship pass First of all we should make some necessary assumptions . According to ( Gorbunov & Losev , 1978 ) , the lateral influence of island is expressed by empirical formula : D = 0.9√w ( 1 ) ...
Page 295
... Pass to the east , or the Avalon Channel to the west . The relatively constant water depth in this region is particularly advantageous for the iceberg management operations . Although the " target " is large ( approximately 280km in ...
... Pass to the east , or the Avalon Channel to the west . The relatively constant water depth in this region is particularly advantageous for the iceberg management operations . Although the " target " is large ( approximately 280km in ...
Page 344
... Passes the Water ) DEM ( Structure Stops the Water ) Experiment 0.1 0.15 0.2 0.25 0.3 Velocity of Water [ m / s ] Fig . 11 : Average ice force acting on the structure ; comparison between experiment and computations . force value grows ...
... Passes the Water ) DEM ( Structure Stops the Water ) Experiment 0.1 0.15 0.2 0.25 0.3 Velocity of Water [ m / s ] Fig . 11 : Average ice force acting on the structure ; comparison between experiment and computations . force value grows ...
Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
24 other sections not shown
Other editions - View all
Common terms and phrases
analysis angle applied Arctic ASME assumed average blade block boundary calculated Canada channel coefficient component conducted considered constant Copyright crack creep crushed dependence depth determined direction distribution effect Engineering equation estimate experiments factor failure field Figure floes flow force frequency friction function given height horizontal ice force ice loads ice sheet ice thickness iceberg icebreaker included increase indentation indentor interaction International layer length material maximum mean measured Mechanics method Newfoundland observed obtained occurred Offshore operations parameters peak performance predicted present pressure propeller range ratio region Report Research resistance salinity scale scour shape shear ship shown shows similar soil speed stamukha strain strength stress structure surface Table temperature tests thrust torque values vertical wave width wind zone