Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 7, Parts 4-6American Society of Mechanical Engineers, 1988 - Arctic regions |
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Page 304
... values of R , the inner region becomes smaller and the maximum values of normal com- ponent velocity become larger . Figure 4 shows that the temperature boundary layer thickness decreases as or R increases . Figure 5 shows the local ...
... values of R , the inner region becomes smaller and the maximum values of normal com- ponent velocity become larger . Figure 4 shows that the temperature boundary layer thickness decreases as or R increases . Figure 5 shows the local ...
Page 304
... values of Rl , the inner region becomes smaller and the maximum values of normal component velocity become larger . Figure 4 shows that the temperature boundary layer thickness decreases as & or | R | increases . Figure 5 shows the ...
... values of Rl , the inner region becomes smaller and the maximum values of normal component velocity become larger . Figure 4 shows that the temperature boundary layer thickness decreases as & or | R | increases . Figure 5 shows the ...
Page 261
... values the dilatancy will cause a decrease of pore - water pressures and consequently an increase in the shear resistance . In the case of a penetrating object of square thickness L the pore - water pressure drop P can be described as ...
... values the dilatancy will cause a decrease of pore - water pressures and consequently an increase in the shear resistance . In the case of a penetrating object of square thickness L the pore - water pressure drop P can be described as ...
Contents
ICE PROPERTIESII | 31 |
Simple Beam Tests on Type S3 Sea | 63 |
ICE DRIFT AND DYNAMICS | 69 |
Copyright | |
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analysis angle Arctic Engineering average beam Beaufort Sea Bering Sea buckling buoys Cold Regions compressive Conference on Offshore crack creep crushing curves deflection deformation density diameter drift dynamic effect elastic modulus equation estimated experimental factor failure flexural strength floe fracture toughness freshwater ice friction coefficient gauges geostrophic wind grain heat transfer horizontal ice drift ice force ice loads ice motion ice pressure ice sheet ice tests ice thickness ice velocity iceberg icebreaking impact increase indentation island layer linear measured Mechanics and Arctic method MIZEX model ice modulus Molikpaq normal force Norton Sound Ocean Offshore Mechanics oriented parameters pressure panel PVDF ratio reinforced ice Research samples scale sea ice sediments shear ship shown in Figure Sinha Sodhi specimen spray ice strain gauges strain rate strain tensor structure surface temperature tensor thermosyphon Timco tion uniaxial values vertical