Hi Einstein,
I figured I would pick up our discussions here in a new thread. Let’s start out by talking to each other about the parameters of this design concept. You have begun by pointing out a very important aspect that is of utmost importance to model correctly:
Head pressure in any fluid is a pretty easy concept to model, based on the hydrostatic relationships. The head pressure for any fluid can be expressed in terms of the height of a column of that fluid, independent of the shape of the column at either end. For any height of a fluid “h” we can compute its head pressure over that height as:
P-head = (Fluid Density)g(fluid height) P = rhogh
So whatever the height of the device you wish to build, we can model the head pressure difference between the bottom and the top with respect to the height (h) between them.
The energy equation written in terms of fluid pressure could be represented as:
P-static + P-head + P-dynamic = Constant. OR
P-static1 + Phead1 + P-dynamic1 = P-static2 + Phead2 + P-dynamic2
OK, but this generalization is usually applied to a LEVEL flow (no head pressure difference). What you say is very true and is a basic model for aerodynamic flows that do NOT go through a change in height. Head pressure differences in non-level flow system changes this generalization.
Maybe I can convince you to think about this differently… You will note that as you go UP in altitude away from the earth’s sea level that the temperature goes DOWN. For example, when it is 85 Deg F at Huntington Beach, CA, it would be quite a bit cooler up in the mountains of SoCal near Big Bear. It would probably only be about 65-75 Deg F at altitude. This is consistent with how the atmosphere is actually structured. From Sea Level to about 36000 feet the temperature goes down linearly with height above sea level. And the other thing we notice as we go up in altitude and down in temperature: The air pressure goes down. This is because the density of air molecules is being lowered. This is why it is very handy to have a simple, Excel spreadsheet that models the ICAO standard atmosphere, as it can help you study atmospheric pressure questions.
Yes, this is the ICAO standard atmosphere model you are talking about. It is an exercise I give to my freshman AERO engineering students.
Any pressure differential due to height is handled by the head pressure equation I have given above. The only other force field that needs to be accounted for is the frictional fluid forces inherent in the boundary layer near the inner surfaces of the conduit. That would be called the frictional pressure losses and they would be added to the head pressure difference.
It is kind of simple, you know. That’s because head pressure only depends upon height within a fluid column. Look at the head pressure differential equation: Delta-P = densitygdelta-height. It does not depend at all upon how large of a vessel you have at the surface of the earth. Head pressure is only about height, not the shape of the vessel.
You’re absolutely right, it is fun! Before we think about the optimum pipe slope angle, let’s finalize some basics about what sort of altitude differences we could reasonably accomodate. There is a mountain in SoCal called Mt. Baldy, and it is roughly (give or take 200 feet) 10,000 feet above sea level. So if we ran a pipe up Mt Baldy from the ocean we could get a “head pressure” of atmosphere of about 10,000 feet. Using our equation and assuming that air density is constant at the sea level value (.002377 slugs/cubic feet), we could calculate a total head pressure of:
P-head = 764.78 Pounds per square foot. That would be the approximate head pressure differential between the bottom and the top of the pipe. That is the pressure exerted by that column of air.
OK, if we agree on a 10,000 foot head pressure differential, then we only need to talk about static pressures and dynamic pressures at each end in order to model this system. The ICAO standard atmosphere will tell us what the typical static pressures are for the atmosphere at 10,000 feet above sea level and at sea level. So the only thing that is left to answer is what are the velocities you wish to achieve at both the top and the bottom? That will establish the dynamic pressure requirement for the system.
RMT