Hello,
I am on vacation so I only reply quickly... A few thoughts:
Your velocity map gives ONLY the velocity upstream and downstream of the tubes, not the discharge through them. If your bottom is deeper upstream of the southern tube then what you get does not sound illogical.
Do you reach a steady state?
What does the listing say? You should have, for each printout, the value through each tube, that's the best way to control your results.
Finally, don't forget that the "tube" function has some limitations:
- only rectangular dimensions
- discharge is computed based on water levels and not on energy levels as it should be in theory
The latter can maybe lead to some "oscillations" with the discharge alterning in the two tubes (possibily with high approaching velocities, just a guess, never tried such a configuration, I might be wrong) with for example:
- higher u/s water level at tube 1 => Q1 increases and Q2 decreases
- as Q1 increases, u/s velocity V1 also increases and water level decreases until WL 2 > WL 1, and same phenomenon at tube 2, and so on...
As a last word, I would actually use tubes to model a bridge only if I can't do it with the classical method (with openings in the mesh and the piles as island), ie. in the case when the flow is expected to reach the deck.
The best solution would be a coupled model 1D-2D Mascaret-TELEMAC-2D as bridges are easily modelled in 1D models (this works well with MIKE FLOOD with DHI software). But I don't know if a coupled version is in the pipe or not...
Best regards
PL