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 18
Page 13
Flexural strength of sea ice ( 0 ) was evaluated using the bulk salinity ( S1 ) and temperature ( Ti ) of ice as follows . Kouenbad 0.1 o = 1.76exp ( -5.88 ( valC.S ) ( 1 ) 0.0 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 vB = S / 100 { 49.185 / abs ...
Flexural strength of sea ice ( 0 ) was evaluated using the bulk salinity ( S1 ) and temperature ( Ti ) of ice as follows . Kouenbad 0.1 o = 1.76exp ( -5.88 ( valC.S ) ( 1 ) 0.0 0.0 0.2 0.4 0.6 0.8 1.0 1.2 1.4 vB = S / 100 { 49.185 / abs ...
Page 258
The specific gravity , the initial soil concentration , and the salinity of the frozen soil are assumed to be a function of the depth referred to measurements ( Masterson , 1998 ) and are plotted in Figure 4 .
The specific gravity , the initial soil concentration , and the salinity of the frozen soil are assumed to be a function of the depth referred to measurements ( Masterson , 1998 ) and are plotted in Figure 4 .
Page 283
The salinity at a depth of 0.23 m , the centre of the ... One manifestation of the effects of lower salinity and lower temperature in saline ice is the decrease in ductility and hence an increase in brittleness . Low - salinity , colder ...
The salinity at a depth of 0.23 m , the centre of the ... One manifestation of the effects of lower salinity and lower temperature in saline ice is the decrease in ductility and hence an increase in brittleness . Low - salinity , colder ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
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 compressive 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 ice force ice loads ice sheet ice thickness iceberg icebreaker included increase indentation indentor interaction International layer length material maximum mean measured Mechanics method observed obtained occurred Offshore operations parameters peak performance predicted present pressure Proceedings propeller range ratio region Report Research resistance salinity scale scour shape shear ship shown shows soil speed stamukha strain strength stress structure surface Table temperature tests thrust torque values vertical wave width wind zone