Proceedings of the ... International Conference on Offshore Mechanics and Arctic Engineering, Volume 5American Society of Mechanical Engineers, 2007 - Arctic regions |
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Page 310
y ni hi 이 EQUATIONS OF MOTION The fluid domain is the region consisting of the points ( x , y ) such that -hy < hi ... The two regions are occupied by two immiscible fluids , with p the density of the lower fluid and pi the density of ...
y ni hi 이 EQUATIONS OF MOTION The fluid domain is the region consisting of the points ( x , y ) such that -hy < hi ... The two regions are occupied by two immiscible fluids , with p the density of the lower fluid and pi the density of ...
Page 382
The behavior of the fluid - structure system is assumed to be twodimensional . A Cartesian coordinate system Oxz is defined here with the z - axis directed vertically upward and the x - axis being on the still water surface .
The behavior of the fluid - structure system is assumed to be twodimensional . A Cartesian coordinate system Oxz is defined here with the z - axis directed vertically upward and the x - axis being on the still water surface .
Page 383
By taking the second- and third - order derivatives about x on both sides of the mass continuity equation , Eq . ( 4 ) , we obtain the boundary conditions for the fluid motion under the ends of the beam as ( at x = xi , i = 1,2 ) ...
By taking the second- and third - order derivatives about x on both sides of the mass continuity equation , Eq . ( 4 ) , we obtain the boundary conditions for the fluid motion under the ends of the beam as ( at x = xi , i = 1,2 ) ...
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Contents
OCEAN SPACE UTILIZATION | 1 |
OMAE200729521 | 11 |
OMAE200729557 | 17 |
Copyright | |
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