Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 14, Part 4American Society of Mechanical Engineers, 1995 - Arctic regions |
From inside the book
Results 1-3 of 81
Page 101
This constitutive model is developed for the ductile behaviour of columnar grained sea ice and it takes into account the effects of crystal orientation , grain size , salinity and the kinetics of microcraking on the sea ice behaviour .
This constitutive model is developed for the ductile behaviour of columnar grained sea ice and it takes into account the effects of crystal orientation , grain size , salinity and the kinetics of microcraking on the sea ice behaviour .
Page 152
A complex interface intensity factor has been developed for the interface ( 28 ) , which is composed of the interface intensity factors due to the normal and shear components , K , and K2 , respectively : To outer contour inner contour ...
A complex interface intensity factor has been developed for the interface ( 28 ) , which is composed of the interface intensity factors due to the normal and shear components , K , and K2 , respectively : To outer contour inner contour ...
Page 235
Nevertheless it did develop very fast in the 1950s and 60s , but growth has gradually slowed and has now ceased at a ... 1995 OMAE - Volume IV , Arctic / Polar Technology ASME 1995 Between 1950 and 1970 Greenland developed very fast .
Nevertheless it did develop very fast in the 1950s and 60s , but growth has gradually slowed and has now ceased at a ... 1995 OMAE - Volume IV , Arctic / Polar Technology ASME 1995 Between 1950 and 1970 Greenland developed very fast .
What people are saying - Write a review
We haven't found any reviews in the usual places.
Contents
139 | 95 |
Mechanical Behavior of Ice Loaded Optical Ground Wires | 107 |
Influence of the Surface Liquid Film on Cylinder Icing Under Marine Conditions | 115 |
Copyright | |
9 other sections not shown
Other editions - View all
Common terms and phrases
activities analysis applied Arctic average axis beam boundary brine cable calculated caused coefficient cold compression considered constant crack deformation density dependent depth described determined developed direction distribution effect elastic energy Engineering equation estimated experiments failure field Figure floe flow force fracture freezing function given grain grain boundary Greenland heat ice cover ice load ice sheet iceberg increase initial International layer length limit liquid mass material maximum mean measured Mechanics mode natural observed obtained offshore operations parameters period possible present problem production region relative Research salinity sea ice sector shown shows snow solution specimen speed spray stations strain strength stress structure surface Table Technology temperature thickness towing transfer volume wave wind zone