olivermsun
Science Advisor
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Maybe there's another way to think about this that will make it clearer.Loro said:Isn't it that if we're still considering the case of inviscid flow - it wouldn't sort itself out? The streamlines from in between the sheets would always have a higher H-quantity that the outside ones, no matter how far away from the sheets we look? (And in that way the infinite sheets would be a limiting case for the finite sheet problem)
Let's say that your inviscid flow is a "jet" flowing in the positive x direction which remains steady (and parallel) after it exits the channel formed by the sheets of paper. What this means (via Bernoulli or any other way you look at it) is that the velocity and pressure in the jet are constant for all x. It also means that jet and the "ambient" fluid have equal pressures along their boundary (otherwise, the flow would change shape). It doesn't really matter what you call static pressure and what you call dynamic pressure, since the pressure is constant throughout the flow (in fact, throughout the entire domain in your example).
If this is the scenario you're envisioning, then the sheets of paper are completely redundant. The pressure is equal on all sides of the sheets, and there will be no net force on the sheets.
However, if you have a clearly defined idea of an "ambient" pressure and some other thing going in your jet (so that, for example, there is a net inward force on the sheets) then you're going to have to explain how the jet joins with the ambient flow at the ends of the channel. There's will be a pressure differential somewhere, causing the flow to accelerate (or decelerate).