Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 18, Part 5American Society of Mechanical Engineers, 1999 - Arctic regions |
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Page 340
MODELING Computation Grid considered to be two - dimensional and the floe , for the sake of simplicity , is considered ... computations focusing on the very local behavior of floe . In a narrow area , the local characteristics of floes ...
MODELING Computation Grid considered to be two - dimensional and the floe , for the sake of simplicity , is considered ... computations focusing on the very local behavior of floe . In a narrow area , the local characteristics of floes ...
Page 342
... computations . The time series of the computational result is shown in Fig . 3. Figure 4 shows the time history of ... computation taking into account the tangential force ( Case 2-1 ) is compared with the computation in which tangential ...
... computations . The time series of the computational result is shown in Fig . 3. Figure 4 shows the time history of ... computation taking into account the tangential force ( Case 2-1 ) is compared with the computation in which tangential ...
Page 344
... computations . force value grows extremely high . There is no doubt that the improvement of water current analysis around the boundary is essential for the computation model , especially for DEM computation in small areas . CONCLUSIONS ...
... computations . force value grows extremely high . There is no doubt that the improvement of water current analysis around the boundary is essential for the computation model , especially for DEM computation in small areas . CONCLUSIONS ...
Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
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Allen Bay analysis angle Arctic Engineering ASME average boundary brittle calculated Canada channel coefficient component compressive cone Confederation Bridge Conference on Offshore contact area Copyright 1999 crack creep creep deformation crushed deformation density determined diameter distribution dynamic effect equation estimate failure stress Figure floes fracture frequency friction frozen soil full scale gas hydrate Grand Banks horizontal hydrodynamic ice block ice class ice conditions ice force ice loads ice pieces ice sheet ice strength ice thickness iceberg iceberg management icebreaker increase indentation tests indentor interaction layer level ice maximum measured Mechanics and Arctic mm/s Newfoundland Northern Sea Route observed Offshore Mechanics parameters peak Pechora Sea piers pipeline planetary boundary layer predicted pressure ratio Research resistance rubble Sakhalin salinity scantlings scour sea ice sensors shape shear ship shows speed stamukha surface temperature thrust torque values velocity vertical water depth width wind zone