Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 4American Society of Mechanical Engineers, 1988 - Arctic regions |
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Page 121
... shows that vertical samples tend to become more brittle at lower strain rates than horizontal samples . The transition zone would probably be shifted towards higher strain rates for higher confining pressures . The columns need higher ...
... shows that vertical samples tend to become more brittle at lower strain rates than horizontal samples . The transition zone would probably be shifted towards higher strain rates for higher confining pressures . The columns need higher ...
Page 304
... shows that the temperature boundary layer thickness decreases as or | R | increases . Figure 5 shows the local Nusselt number as function of the inclination parameter & for various values of R and for q ( 0,1 ) and m = 0 . It shows that ...
... shows that the temperature boundary layer thickness decreases as or | R | increases . Figure 5 shows the local Nusselt number as function of the inclination parameter & for various values of R and for q ( 0,1 ) and m = 0 . It shows that ...
Page 338
... shows interaction between designing / building concepts and navigational practice . Fig . 1 shows variation in ice - in- duced loads exerted on the bottom structures of an ice - breaker evaluated from permanent deformations ( 1 ) ...
... shows interaction between designing / building concepts and navigational practice . Fig . 1 shows variation in ice - in- duced loads exerted on the bottom structures of an ice - breaker evaluated from permanent deformations ( 1 ) ...
Contents
OFFSHORE MECHANICS | 1 |
The Structure and Tensile Behavior of First Year Sea Ice and LaboratoryGrown Saline | 11 |
Effects of Temperature and Strain Rate on Uniaxial Compressive Strength of Naturally Formed Fresh | 19 |
Copyright | |
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analysis angle approximately Arctic assumed average beam boundary calculated coefficient Cold conducted Conference constant crack creep crushing curves deflection deformation dependence described determined developed direction drift dynamic effect elastic energy Engineering equation estimate experimental experiments factor failure field Figure flexural flow fracture friction function given grain heat horizontal ice force ice loads ice sheet ice velocity iceberg impact increase indentation indicates International island layer length limit linear material mean measured Mechanics method motion Norton Sound observed obtained ocean Offshore operating oriented parameters POSITION presented pressure properties range ratio reference region relative Report Research response saline samples scale sea ice shape ship shown shows specimen speed strain rate strength stress structure surface Table temperature tests theory thickness tion values variations vertical wind