Hello, ;)
I am like in a stage of my project where I need to calibrate by trial and error my model. It's a region, with twin tunnels. The model has also discrete features (vertical faults), and the tunnel was modeled by deactivating elements. The mesh is fully non-structured.
I also have 10 obs points in the surface, and I ran FePEST and I got the best parameters (zonally constant) for one (out of two) lithologies modeled.
The thing is that, while the water heads are somewhat acceptable, the inflow in the tunnel is just too damn high for some reason, and it's far away from reality. FEFLOW is giving me that the water budget in the tunnels is like 170 lt/s, but the actual flow is around 100 times less this quantity... also, 170 lt/s in the tunnels is like almost 60% of the net recharge (!!!!). How is this possible?
It must be said that the recharge was set by using the In/Out flow top/bottom, by selecting the whole region a value of q=9.75E-9 [m/s], and the topographical area is 30761350 [m2] which is equivalent to 300 lt/s over the whole area.
The 'seepage face' boundary condition was set in the nodes of the tunnels. On surface, there are some small creeks as well and they were modeled by using the same BC.
Any comment or advice? I don't know what to do have some reasonable water budgets in the tunnel, there must be something wrong somewhere but I'm unable to detect it. I attach the geometry of the model, so you can see that it's unreasonable to have 60% of the recharge flowing in the tunnel.