Mikko Brummer
Senior Member
- Joined
- May 16, 2006
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- 575
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- Finland
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If you add the free stream (uniform flow) vectors into the vectors shown in the first case, you end up in the flow field of the second case (as far as I understand).
There is no difference between moving fluid vs. moving wing. Why do you want to simulate them time dependent while the problem is totally stationary (unless you want to simulate velocity changes)?
There is no difference between moving fluid vs. moving wing. Why do you want to simulate them time dependent while the problem is totally stationary (unless you want to simulate velocity changes)? For a CFD simulation it is typically much easier to use a stationary wing in a steady flow field. Then you can view the results in any frame of reference you like. In most CFD softwares changing frame of reference for post processing is very easy.
I didn't find anything surprising in the zero lift situation. You can see the same from streamlines as well. Of course the flow has to go around the wing with higher velocity and horizontal component in the velocity.
Mikko, I'm a bit confused by the boundary conditions on the upper and lower surface of the model. It looks like the problem is calculated for the viewing area frame by frame, and the upper and lower boundary is sourcing and sinking the material willy nilly. Are there constraints on the boundary's ability to source and sink material? And are these applied in one dimension only (mass balance) of two dimensions (mass and energy). Just eyeballing it, there appears to be an energy balance mismatch.
Shouldn't there be more updraft in front of the wing?
it's like the flow that goes out from the bottom comes back in from the top - not very realistic, but it makes for a faster simulation when the domain can be smaller.
You probably can read the streamlines so well, but I don't. I think the common belief would be the foil just pushes the water neatly aside as it slices through the water, not that it first shoves water forward and out, then the water is bending back on the rear part of the foil at nearly straight angles... I never anticipated it from the streamlines...
Streamlines exist in three dimensional flows.Streamlines are quite easy to read. The principle is that the excact same volume flow goes between each streamline. It's like a set of channels. Thus the flow turns with the channel and the narrower the channel is the higher the velocity. Don't confuse streamlines with vectors. Stremlines only exist in 2D.
Why can't periodic boundary conditions be used? Both periodic outer boundary conditions and constant outer boundary conditions will affect the results. The further the outer boundaries are from the foil/sail the less the influence of either type of outer boundary condition will be.Yes the foil pushes (or slows down) water in front of it and drags (or slows down) water behind it in the wake. Even a flat plate would do that due to friction, but a thick foil does it more.
That is the reason why you should never put the log transducer close to the keel. It will read differently depending on the leeway. If the transducer is off the center, it will also show differently on different tacks. I would put the transducer at least one chord lenght in front the keel unless it becomes too close to bow.
If you want to model foils or sails accurately, you need to have a long part of the domain after the foil and you can't use periodic boundary conditions. If you can't use steady state, just calculate long enough until the flow is steady state with constant boundary conditions (set the incoming velocity and keep the foil stationary).
Perhaps you are confusing "streamlines" with "stream function". Stream function is a 2D concept, and lines of constant stream function are 2D streamlines.
Why can't periodic boundary conditions be used? Both periodic outer boundary conditions and constant outer boundary conditions will affect the results. The further the outer boundaries are from the foil/sail the less the influence of either type of outer boundary condition will be.
A pathline is the trajectory of a single fluid particle; ie the path a single fluid particle takes over time.Yes I was confusing them. I think in Fluent streamlines are called pathlines (for zero mass particles). In 2D they are the same, if equally spaced stream/pathlines are used in constant incoming velocity.
rather awkward when your purpose is to model circulation.Just for grins, what would happen if you reversed the y component of the flow when you pumped it back in at the top?
The arrows in Mikko's videos and images appear to show the direction of the velocity but not the magnitude.