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Common setup for p_rgh in complete open domains |
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September 14, 2020, 16:47 |
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#21 |
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Tobias Holzmann
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I don't think it is a solver-bug but there is probably something missing I don't get until now or there is no appropriate boundary condition (and I don't have time to investigate into that problem). So you have to check it out yourself.
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Keep foaming, Tobias Holzmann |
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October 6, 2021, 09:48 |
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#22 |
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Thiago Parente Lima
Join Date: Sep 2011
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Hi everybody,
I'm currently working on a problem of natural convection in a open domain using buoyantPimpleFoam and, as many of you, I faced the same problems on the outlet boundary, say, backflow, accelarating flow, divergence, etc. I tried different combinations of boundary conditions, most of them discussed here in this thread. Recently I found this work which suggests the combination for p_rgh/U of fixedFluxPressure/zeroGradient for the top boundary and totalPressure/pressureInletOutletVelocity for the sides and bottom boundaries. I tried those on a test case attached and I've got a good result for the flow field on outlet (see video). In my case the bottom part of the domain is a wall. The boundary conditions were the following: Pressure: p_rgh Code:
dimensions [1 -1 -2 0 0 0 0]; internalField uniform 101325; boundaryField { outlet { type fixedFluxPressure; value $internalField; } sides { type totalPressure; p0 $internalField; value $internalField; } heat { type fixedFluxPressure; value $internalField; } base { type fixedFluxPressure; value $internalField; } frontAndBack { type empty; } } Code:
dimensions [0 1 -1 0 0 0 0]; internalField uniform (0 0 0); boundaryField { outlet { type zeroGradient; } sides { type pressureInletOutletVelocity; inletValue uniform (0 0 0); value uniform (0 0 0); } heat { type noSlip; } base { type noSlip; } frontAndBack { type empty; } } Code:
dimensions [0 0 0 1 0 0 0]; internalField uniform 293.15; boundaryField { outlet { type inletOutlet; inletValue uniform 293.15; value uniform 293.15; } sides { type inletOutlet; inletValue uniform 293.15; value uniform 293.15; } heat { type fixedValue; value uniform 303.15; } base { type zeroGradient; } frontAndBack { type empty; } }
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Fields of interest: buoyantFoam, chtMultRegionFoam. Last edited by thiagopl; October 6, 2021 at 10:29. Reason: Deleting comments on the p_rgh file. |
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May 11, 2022, 04:27 |
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#23 |
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Marco Müller
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Location: Germany
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Just contributing my findings, since I had the same issue, in case someone will find it helpful:
- I was not able to solve my (steady state) problem with buoyantBoussinesqSimpleFoam. It seems to have a current (v2006 for me) implementation that makes it difficult to deal with openings, see: Wrong implementation of the Boussinesq assumption in heat transfer solvers - Using buoyantSimpleFoam worked fine for me (without momentumPredictor, which introduced the same artificial convection with middle speed velocities as buoyantBoussinesqSimpleFoam) - BC setup: --- lower opening ("inlet"): prghTotalPressure + pressureInletOutletVelocity --- upper opening ("outlet"): fixedFluxPressure + pressureInletOutletVelocity - lastly - since I also had forced convection inside my domain -, I successfully used the limitVelocity option to get a stable initialization |
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July 26, 2023, 09:30 |
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#24 |
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Following the release of OpenFOAM v11, I also want to share some recent tests I did about natural convection and open boundaries since I have been looking into it quite a lot. I think I finally have a decent setup for a steadystate simulation using the fluid solver of OF v11 (similar to buoyantSimpleFoam).
My case is a simple hot box inside a fully open domain, so the air can come and leave frome any side. I used OpenFOAM v11 because it includes a switch to initialize the hydrostatic pressure in fvSolution so you can use the ph_rgh field and the prghTotalHydrostaticPressure condition in p_rgh. In OpenFOAM v2306, there is a functionObject that does the same initialization but I have yet to try it Here are the boundary conditions: p Code:
internalField uniform 101325; boundaryField { #includeEtc "caseDicts/setConstraintTypes" ".*" { type calculated; value uniform 101325; } "(sky|bottom|walls)" { type calculated; value uniform 101325; } "vol.*" { type empty; } } Code:
internalField uniform 0; boundaryField { #includeEtc "caseDicts/setConstraintTypes" ".*" { type fixedFluxPressure; value $internalField; } bottom { type prghTotalHydrostaticPressure; meanValue $internalField; p0 $internalField; value $internalField; } sky { type prghTotalHydrostaticPressure; meanValue $internalField; p0 $internalField; value $internalField; } walls { type prghTotalHydrostaticPressure; meanValue $internalField; p0 $internalField; value $internalField; } "vol.*" { type empty; } } Code:
internalField uniform 0; boundaryField { ".*" { type fixedFluxPressure; value $internalField; } bottom { type fixedFluxPressure; meanValue $internalField; p0 $internalField; value $internalField; } sky { type fixedValue; meanValue $internalField; p0 $internalField; value $internalField; } walls { type fixedFluxPressure; meanValue $internalField; p0 $internalField; value $internalField; } "vol.*" { type empty; } } Code:
internalField uniform (0 0 0.0); boundaryField { #includeEtc "caseDicts/setConstraintTypes" ".*" { type fixedValue; value $internalField; } walls { type slip; } bottom { type zeroGradient; //inletValue uniform (0 0 0); value $internalField; } sky { type zeroGradient; //pressureInletOutletVelocity; inletValue uniform (0 0 0); value $internalField; } walls { type zeroGradient; //pressureInletOutletVelocity; inletValue uniform (0 0 0); value $internalField; } "vol.*" { type empty; } } Code:
internalField uniform 293.15; boundaryField { ".*" { type zeroGradient; value uniform 293.15; //value $internalField; } hot_walls { type fixedValue; value uniform 393.15; } "(sky|bottom|walls)" { type inletOutlet; inletValue uniform 293.15; value $internalField; } "vol.*" { type empty; } } Code:
dimensions [1 -1 -2 0 0 0 0]; value 101325; Code:
PIMPLE { momentumPredictor no; nNonOrthogonalCorrectors 1; //pRefCell 0; //pRefValue 0; //consistent yes; hydrostaticInitialisation yes; nHydrostaticCorrectors 10; } Code:
ddtSchemes { default steadyState; } gradSchemes { default cellLimited Gauss linear 1; } divSchemes { default none; div(phi,U) bounded Gauss linearUpwindV default; div(phi,K) Gauss linearUpwind default; div(phi,h) bounded Gauss linearUpwind default; div(phi,k) bounded Gauss linearUpwind default; div(phi,epsilon) bounded Gauss linearUpwind default; div(phi,omega) bounded Gauss linearUpwind default; div(((rho*nuEff)*dev2(T(grad(U))))) Gauss linear; } laplacianSchemes { default Gauss linear uncorrected; } interpolationSchemes { default linear; } snGradSchemes { default uncorrected; } wallDist { method meshWave; } Code:
thermoType { type heRhoThermo; mixture pureMixture; transport const; thermo hConst; equationOfState perfectGas; specie specie; energy sensibleEnthalpy; } dpdt off; mixture { specie { molWeight 28.96; } thermodynamics { Cp 1004.4; Hf 0; } equationOfState { rho 1.2; pRef 101325; } transport { mu 1.831e-05; Pr 0.705; } }
Here is a picture of the temperature field with the surface LIC representation of the velocity. It looks decent to me but I would like to have other opinions on this Cheers! |
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July 26, 2023, 16:54 |
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#25 |
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Thiago Parente Lima
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Hi Alczem,
Nice work. Although I posted this and also proposed this thread, which lead to conclusions, I still have problems in setting up natural convection problems in open domains. I found that OF v10 also includes this switch to initialize the hydrostatic pressure in fvSolution. I'm testing your setup, but in a transient case (good results by now!). I 'ill post the case here once I have conclusive results.
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Fields of interest: buoyantFoam, chtMultRegionFoam. |
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July 26, 2023, 17:01 |
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#26 |
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Hey!
I remember reading your various posts, I think I read almost every thread related to this kind of simulation Yep, the switch was already implemented in OF v10, but I mainly use the ESI version and only recently have I been using the foundation version which has some pros (and cons, still figuring it out!). From some posts (by Tobias Holzmann I think), it sounded as if free convection might only be properly simulated through transient computation, or at least using a transient initial state to initialize the steady run, which is... not encouraging! I tried local time stepping and large CFL numbers but it still so slow, especially if you are simulating fluids and solids in a CHT case hopefully some common setup will emerge from all our tests |
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July 27, 2023, 08:38 |
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#27 |
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Back again with a similar case to my previous post, only on a much larger domain (which is 2D now and triangles only, I meshed quickly with Salome and had to be fast).
The pressureInletOutletVelocity condition seems actually more stable than zeroGradient, but they achieve very similar results. A lot of undesired currents remain present near the boundaries and I did not manage to completely mitigate their effects. They are also present when the hot box was disabled to try to reach a perfectly still atmosphere. Overall I am pleased with the results, but it is slow: it takes more than 5000 iterations to have a satisfactory flow. Maybe the numerics need more tinkering and other boundary conditions can achieve similar results faster. I still take this as a win |
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October 5, 2023, 23:19 |
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#28 |
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Ali
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Hi Bodo1993,
It is about three years since your post. I hope you have had found a solution to this problem and are able to share it with me. I am facing exactly the same issue. Thanks, Ali |
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October 5, 2023, 23:33 |
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#29 | |
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Ali
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Quote:
Hi Bodo1993, It is about three years since your post. I hope you have had found a solution to this problem and are able to share it with me. I am facing exactly the same issue. Thanks, Ali |
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November 28, 2024, 06:57 |
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#30 |
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Hey!
I recently have had to work on buoyancy effects again, and I came back to this thread. I managed to slightly improve on my previous solution, so I figured I would share and hopefully get some feedback and see if others have managed to get their open boundaries to work Basically, I still use the hydrostaticPressure FO (pRef set to 0) from the ESI version to initialize ph_rgh, p_rgh and p. Boundary conditions are as follows:
Now the part I did not understand last time was how to let hot air leave the domain freely instead of "bouncing" on it. To achieve that, hRef has to be set to the height of the horizontal patch that will act as an outlet. Meaning that if you expect your flow to leave by the bottom boundary (in case of cold air), hRef should be set to the coordinate of that boudary. One more thing that I found useful: once the hydrostaticPressure FO has been run and the fields are initialized, we can disable it and use the readFields FO to read ph_rgh and be able to use the prghTotalHydrostaticPressure for p_rgh without needing to initialize ph_rgh again (because the FO will overwrite the existing pressure fields). I found this really neat to initialize a transient simulation with a steady-state run and keep using the prghTotalHydrostatic BC but without the need to overwrite the pressure fields at the start of the transient case (which is what would have happened if I used the hydrostaticPressure FO to access ph_rgh). The behavior of vertical patches is still a bit unclear to me, I intend to run more tests, maybe with a lateral wind pushing the hot plume in the side patches. I believe that concludes my quest for open boundaries with buoyancy... for now Maybe someone can tell us more on the proper way to treat buoyancy and boundaries in the future, but that is enough for me! |
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