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 3
... values for the parameters based on the values given by Ashby and Duval are calculated . Young's modulus E. unit stress and the ratio of 。 to ar are assumed to have the same magnitudes as in Table 1 . Using dimensionless variables Ashby ...
... values for the parameters based on the values given by Ashby and Duval are calculated . Young's modulus E. unit stress and the ratio of 。 to ar are assumed to have the same magnitudes as in Table 1 . Using dimensionless variables Ashby ...
Page 79
... values in region I , larger values in region III and intermediate values in region II . The smallest values ( 0.4-0.6 ) occur in region IV , consistent with the notion that ice stress gradients , being larger here than elsewhere ...
... values in region I , larger values in region III and intermediate values in region II . The smallest values ( 0.4-0.6 ) occur in region IV , consistent with the notion that ice stress gradients , being larger here than elsewhere ...
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 ...
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