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 78
si dw h2 dp dx + w (hi dp ( 30 ) j $ Pressure distribution along the channel 人 + 124 dx x = L 16 Jo dx 12u dx hdp -W14 | . - S'úsdx = 0 12 124 dx x = 0 10 Taking the restriction w ( L ) = 0 and employing ( 29 ) gives the final weak ...
si dw h2 dp dx + w (hi dp ( 30 ) j $ Pressure distribution along the channel 人 + 124 dx x = L 16 Jo dx 12u dx hdp -W14 | . - S'úsdx = 0 12 124 dx x = 0 10 Taking the restriction w ( L ) = 0 and employing ( 29 ) gives the final weak ...
Page 121
The pressure , recorded from the central pressure cell P1 , also exhibited a sawtooth behavior . It always peaked early in the constant ocity tests and was immediately followed by a drastic decrease in pressure .
The pressure , recorded from the central pressure cell P1 , also exhibited a sawtooth behavior . It always peaked early in the constant ocity tests and was immediately followed by a drastic decrease in pressure .
Page 122
P to P10 Pressure Cells Sets of pressure cells were installed in rings on the indentor surface ( Figure 4 ) . To study the radial dependence of the pressure we use the average value of the three pressure transducers in a ring .
P to P10 Pressure Cells Sets of pressure cells were installed in rings on the indentor surface ( Figure 4 ) . To study the radial dependence of the pressure we use the average value of the three pressure transducers in a ring .
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Contents
OMAE99PA1135 | 19 |
OMAE99PA1141 | 39 |
PROPELLERICE INTERACTION | 53 |
Copyright | |
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