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 255
... soil and fills , the surface of the soil may exceed the melting point in summer . Traditional models for ice or frozen soils will have difficulty describing such a phenomenon , as the predicted rate of creep will be infinite in this ...
... soil and fills , the surface of the soil may exceed the melting point in summer . Traditional models for ice or frozen soils will have difficulty describing such a phenomenon , as the predicted rate of creep will be infinite in this ...
Page 258
... 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 time - dependent distribution of temperature in the ...
... 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 time - dependent distribution of temperature in the ...
Page 376
... soil friction , and the effect of surcharge of the spoil material in front of the moving keel . The above models are limited in that they do not reflect what has actually been observed from phenomenological studies . Icebergs do not ...
... soil friction , and the effect of surcharge of the spoil material in front of the moving keel . The above models are limited in that they do not reflect what has actually been observed from phenomenological studies . Icebergs do not ...
Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
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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