Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 4American Society of Mechanical Engineers, 1988 - Arctic regions |
From inside the book
Results 1-3 of 38
Page 2
... grain size , d1 is the unit of grain diameter , s is the stress exponent for the delayed elastic strain ( assumed to be unity ) , a is the inverse of relaxation time , & is the viscoplastic strain rate for unit stress o 。 and n ' is ...
... grain size , d1 is the unit of grain diameter , s is the stress exponent for the delayed elastic strain ( assumed to be unity ) , a is the inverse of relaxation time , & is the viscoplastic strain rate for unit stress o 。 and n ' is ...
Page 5
... Grain 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 ...
... Grain 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 ...
Page 56
... grains were counted in an area of 90 mm × 100 mm , giving an average grain area , a , of 6.01 mm2 which gives an equivalent grain diameter , d ( d = 2 √a / ) , of 2.77 mm . The corresponding average grain size obtained from the ...
... grains were counted in an area of 90 mm × 100 mm , giving an average grain area , a , of 6.01 mm2 which gives an equivalent grain diameter , d ( d = 2 √a / ) , of 2.77 mm . The corresponding average grain size obtained from the ...
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 | |
26 other sections not shown
Other editions - View all
Common terms and phrases
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