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Hi Emilia,
Refinement is not necessary the solution. You should look for the Mesh Quality.
How good is the mesh if you plot the Max. Interior Angle of triangles? For
example, if you do the refinement in bad-shaped triangles, then the situation
will become even worst.
Why are you using the Error Norm (max.)? Is your problem converging?
Get in touch with MIKE Support (mike.de@dhigroup.com) and discuss your case in
detail.
Best regards
Carlos Rivera
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Hi Rachit,
To understand better the case, can you elaborate how you are launching the
1000's simulations? Is this done under the FePEST framework? Or are you using
your own script to do the job? The issue with the MPI can be related to several
things, for example, you already have an MPI environment in place, which could
conflict with FEFLOW's one. Or the script is not properly terminating the MPI
instance.
Best regards
Carlos Rivera
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Hi Lucien,
If you are solving the groundwater flow equation with the option "Free" surface,
then FEFLOW assumes that the elevation of Slice 1 coincides with the phreatic
surface (Pressure = 0 kPa). Therefore, the model elevation will change
accordingly during the simulation. You can solve the groundwater flow equation
by using the "Phreatic" option or the Problem Class Richards. We have dedicated
free training course about all these options. You can register with the link
below:
https://www.theacademybydhi.com/course-sessions/feflow---behind-the-flow-11600061-142
Best regards
Carlos Rivera
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No, it is not possible. Hydrodynamics model for rivers cannot be solved with
steady-state concept. If you prefer to work in steady, then you would need to
operate only with FEFLOW, where the river heads are prescribed by the
Fluid-Transfer BC.
Best regards,
Carlos
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Hi Max,
The problem is that SAMG did not converge properly. I see you are working with a
RMS norm. This is practical for standard cases, but in situations, where you
have specific "hot spots" (e.g. not convergence directly at the BHE locations),
it will be much useful to work with a MAX norm. The Max norm will focus on the
spots with maximum error, presumably the BHE locations.
Alternatively, you can give a try with the direct solver PARDISO.
Best regards
Carlos Rivera
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Hi Tomás,
I recommend you to get in touch with MIKE support (mike.de@dhigroup.com). The
question is very generic and the fact of increasing the number of layers does
not clarify the changes of water balances. Indeed, the Multilayer Well is an
imposed source/sink. You would need to see this in the Rate Budget panel.
Best regards
Carlos
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Hi Sebastian, interesting question. You can change the direction of the gravity
vector, but not the magnitude.
I am wondering whether you could do a math trick by upscaling/downscaling other
parameters in order to achieve your purposes.
Cheers
Carlos
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Hi Adam,
Density-driven flow problems are hard to solve, but not impossible. Negative
concentrations are due to the poor discretization level and dispersivity values
assigned to the model. If I were you, I would do the model in steps. Does your
model run with constant head values (not tidal effects)? If no, this should be
fixed first.
You can take a look on the self-paced course below. There is a section covering
some information about numerical oscillations and their connections with the
mesh size and dispersivity.
https://www.theacademybydhi.com/course-sessions/feflow---getting-started-with-groundwater-quality-modelling-11600061-153
Best regards
Carlos Rivera
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Hi Abel,
The method is called getHistoryValues and you can find the documentation below:
https://dhi.github.io/ifm/api_doc.html?highlight=history#ifm.FeflowDoc.getHistoryValues
Best regards
Carlos Rivera
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Why don't you use directly the Monte Carlo functionality within FePEST
application? You can parallelize with a couple of clicks only..
Cheers
Carlos