Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 9, Part 4American Society of Mechanical Engineers, 1990 - Arctic regions |
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Page 65
... surface and the cold air . For simplicity , it is assumed that heat is lost from the ice surface only by convection . Radiation and sublimation are neglected . The differential heat balance equation for the top ice layer may be written ...
... surface and the cold air . For simplicity , it is assumed that heat is lost from the ice surface only by convection . Radiation and sublimation are neglected . The differential heat balance equation for the top ice layer may be written ...
Page 119
... surface at the end of the broken slab is not always in contact with the advancing plate . This is because earlier phases of crushing took place with a larger angle y , as shown in Figure 10. In order to describe the length of the ...
... surface at the end of the broken slab is not always in contact with the advancing plate . This is because earlier phases of crushing took place with a larger angle y , as shown in Figure 10. In order to describe the length of the ...
Page 120
... surface are assumed parallel and rigid . The relative tangential motion between the surfaces is ignored . The fluid flow in the gap is assumed not connected with the general fluid flow caused by the motion of the broken slab , the ...
... surface are assumed parallel and rigid . The relative tangential motion between the surfaces is ignored . The fluid flow in the gap is assumed not connected with the general fluid flow caused by the motion of the broken slab , the ...
Contents
OFFSHORE TECHNOLOGY PART | 3 |
ARCTIC STRUCTURES AND OPERATIONS II | 31 |
ICE STRUCTURE INTERACTION I | 75 |
Copyright | |
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analysis angle average Barents Sea beam behavior bergy bit Bohai Sea boundary conditions calculated Canada coefficient computed crack creep buckling crushing deflection deformation density displacement Dow's Lake drilling dynamic effect elastic energy equation ESARC experimental finite element finite element analysis flexural failure floating ice sheet floe fluid foundation fracture toughness freezing frequency grain heat Hobson's Choice horizontal ice cover ice forces ice island ice load ice shedding ice sheet ice temperature ice thickness iceberg icebreaking impact indentation indentor initial interaction locations maximum measured Mechanics method mode modulus Northumberland Strait notch nucleation numerical obtained Offshore parameters permafrost plane platform pore porosity predicted pressure Public Works Canada ratio response ridge saline sample sea ice SED criterion sensors shown in Figure Simulated Sinha soil solution specimens strain rate strength structure tests values vertical vibration Young's modulus