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pressure problem |
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| Dec23-05, 09:16 AM | #1 |
| Dec23-05, 11:04 AM | #2 |
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Assuming that P3 is at the same elevation as P1, then the pressure P3 = P1, which would seem to contradict the pressure due to the height (2 m) of water above between P4 and P3.
I'll have to get back to this later. |
| Dec23-05, 11:50 AM | #3 |
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| Dec23-05, 01:01 PM | #4 |
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pressure problemThere must be a gradient of pressure for the fluid to move. |
| Dec23-05, 01:29 PM | #5 |
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| Dec23-05, 03:41 PM | #6 |
| Dec23-05, 05:12 PM | #7 |
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The surrounding air is at atmospheric pressure, so the water at the siphons exit has to be atmospheric pressure, and actually is might be slightly higher due to interatomic forces which are responsible for surface tension.
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| Dec24-05, 06:21 AM | #8 |
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The boundary condition P=Patm is usually employed in bernoulli problems as a mechanical constraint at outflowing jets into the atmosphere. This boundary constraint is only valid at high Reynolds number, when [tex]\partial P/\partial r[/tex] is negligible. The assumption underlying is the boundary layer flow. The exiting jet flow would be described by Prandtl boundary layer equations, developing an annular boundary layer due to air viscosity. At high Re, this boundary layer is thin enough to assume the internal pressure in the jet core is the same than the external surrounding pressure (pressure remains constant radially across the layer). The existance of this layer is unavoidable. Because of that one always assume a flow discharge as an irreversible process, because this layer is an entropy generator, and some kinetic energy is ultimately dissipated. The condition P=Patm would not be longer valid at small Re (Stokes flow), or at very high Mach (in supersonic flow) where the hydrostatic boundary condition is not felt by some fluid particles due to the hyperbolicity of the flow. |
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