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 5
... boundary sliding is only caused by the shear stress which acts in a direction parallel to the grain boundary , as shown in Figure 4 ( a ) . Grain Grain boundaries Grain * 1 ( a ) ( b ) × 2 Figure 4. ( a ) Grain boundary sliding caused ...
... boundary sliding is only caused by the shear stress which acts in a direction parallel to the grain boundary , as shown in Figure 4 ( a ) . Grain Grain boundaries Grain * 1 ( a ) ( b ) × 2 Figure 4. ( a ) Grain boundary sliding caused ...
Page 98
... boundary layer on the mean drift of pack ice : Application of simple model . J. Phys . Oceanogr . , 9 , 388-400 . McPhee , M.G. 1981 . An analytic similarity theory for the planetary boundary boundary layer stabilized by surface ...
... boundary layer on the mean drift of pack ice : Application of simple model . J. Phys . Oceanogr . , 9 , 388-400 . McPhee , M.G. 1981 . An analytic similarity theory for the planetary boundary boundary layer stabilized by surface ...
Page 301
... boundary conditions equation ( 30 ) are then solved as follows . For specified m , and Ray , k is guessed . Using equation ( 31 ) as starting values , the two integrals are integrated separately from the outer edge of the boundary layer ...
... boundary conditions equation ( 30 ) are then solved as follows . For specified m , and Ray , k is guessed . Using equation ( 31 ) as starting values , the two integrals are integrated separately from the outer edge of the boundary layer ...
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