Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 4; Volume 8, Part 4American Society of Mechanical Engineers, 1989 - Arctic regions |
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Page 199
... initial to the final equilibrium position . The translational motions are given in terms of distances from the origin of the F1 - triad while the rotational components , i.e. the orientations of the components of the B , vectors , are ...
... initial to the final equilibrium position . The translational motions are given in terms of distances from the origin of the F1 - triad while the rotational components , i.e. the orientations of the components of the B , vectors , are ...
Page 200
... initial and final positions . The initial position of the iceberg is similar to that in Figure 2a . A comparison of Figures 2c and 3c shows some very significant differences between the translational motions of the two icebergs ...
... initial and final positions . The initial position of the iceberg is similar to that in Figure 2a . A comparison of Figures 2c and 3c shows some very significant differences between the translational motions of the two icebergs ...
Page 201
... initial position with respect to the water plane . Its cross section is uniform in the B1 direction and is as shown . In its initial position the centre of the 13x11x13 box is 3 metres below the water surface , a depth that is fairly ...
... initial position with respect to the water plane . Its cross section is uniform in the B1 direction and is as shown . In its initial position the centre of the 13x11x13 box is 3 metres below the water surface , a depth that is fairly ...
Contents
OFFSHORE MECHANICS | 1 |
The Growth of Radial Cracks in Ice Sheets | 7 |
ICE FORCES | 11 |
Copyright | |
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analysis angle Arctic Engineering assumed Barents Sea Beaufort Sea behaviour berm Bjørnøya calculated coefficient Cole components computed Conference on Offshore constant constitutive equation damage evolution damage model deformation density depth determined diameter distribution dynamic effect energy equation experimental factor failure force fracture mechanics fracture toughness frequency friction function Geogrid grain horizontal ice floe ice load ice sheet ice thickness iceberg icebreaking impact increase indentor initial interaction keel material maximum measured Mechanics and Arctic Mellor microcracks modulus motion notch nucleation observed obtained ocean Offshore Mechanics parameters peak stress plane polycrystalline ice predicted pressure probability Proc radar ratio resistance ridge samples sea ice seabed shear shear stress ship shown in Figure simulation specimen spray ice strain rate strain tensor strength structure surface temperature tensile tensile stress tensor tests uniaxial compression variable vector velocity vertical wave Young's modulus