Ivar KJELBERG
COMSOL Multiphysics(r) fan, retired, former "Senior Expert" at CSEM SA (CH)
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Posted:
1 decade ago
12 avr. 2013, 03:59 UTC−4
Hi
a comment to your model: use the boundary layers for the non slip condition walls, it changes the results
for your average heat flux, you can take the average energy out using the flow velocity as normalisation
And your model is really 2D-axi, it would solve quicker in 2d-axi so you have more time to play with the values
--
Good luck
Ivar
Hi
a comment to your model: use the boundary layers for the non slip condition walls, it changes the results
for your average heat flux, you can take the average energy out using the flow velocity as normalisation
And your model is really 2D-axi, it would solve quicker in 2d-axi so you have more time to play with the values
[math] \frac{\iint_A\;T\;\bold{u} \;dA} { \iint_A\;\bold{u}\;dA} [/math]
--
Good luck
Ivar
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Posted:
1 decade ago
13 avr. 2013, 01:54 UTC−4
Hi Ivar,
I've attached the geometry that I'm trying to implement the General Projection integration tool in. The objective is to be able to calculate the heat transfer coefficient along the length, so I need the average temperature at different cross-sectional locations. How would you go about achieving this in COMSOL? Would you write a MATLAB script or would you tackle it within the GUI? I think that I should be able to do some revolution integration with the general projection tool... but actually getting this to work I'm finding elusive, I'm finding the documentation is not clear as I see other users in the forum have discovered as well.
The reason I switched off the boundary layer mesh was that I found it was causing the velocity field to be unstable - I found that if I compared the max_exit_velocity/average_exit_velocity for a long duct it would give a different answer every time I increased the mesh density. When I used a swept triangular mesh the solution became stable as I increased the mesh density. I'm trying to recreate this in a neat way but it's made me distrustful of the boundary layer mesh!
Thank you for your advice,
Adam
Hi Ivar,
I've attached the geometry that I'm trying to implement the General Projection integration tool in. The objective is to be able to calculate the heat transfer coefficient along the length, so I need the average temperature at different cross-sectional locations. How would you go about achieving this in COMSOL? Would you write a MATLAB script or would you tackle it within the GUI? I think that I should be able to do some revolution integration with the general projection tool... but actually getting this to work I'm finding elusive, I'm finding the documentation is not clear as I see other users in the forum have discovered as well.
The reason I switched off the boundary layer mesh was that I found it was causing the velocity field to be unstable - I found that if I compared the max_exit_velocity/average_exit_velocity for a long duct it would give a different answer every time I increased the mesh density. When I used a swept triangular mesh the solution became stable as I increased the mesh density. I'm trying to recreate this in a neat way but it's made me distrustful of the boundary layer mesh!
Thank you for your advice,
Adam
Ivar KJELBERG
COMSOL Multiphysics(r) fan, retired, former "Senior Expert" at CSEM SA (CH)
Please login with a confirmed email address before reporting spam
Posted:
1 decade ago
14 avr. 2013, 10:57 UTC−4
Hi
well for me you should keep the boundary layer and identify why it goes unstable and rather fix that ;)
But then I take this comment back, because the projection operator do not work on other than thets, but you can always do a mesh convert on the domain as last mesh operation, then you keep the fine mesh along the edges, always cleaner, numerically
Another point, is it a half tube with symmetry conditions on the flat cut plane ? in which case you need to add "symmetry" BC, so that the flow remains invariant (and boundary normal = 0 ) along this boundary, also for the HT
In this case you probably do not need your projection variable either (I might have misunderstood though)
If you want to get an average per Z height you can also make a series of Data Set cut planes and integrate over these. Or use two projections: general projection on all domain from z,x,y to z,x, and another one on the flat boundary x,y=0,z from z,x to z and then combine both (the latter one can also be a linear projection from vertex source 1,11,2 to vertex destination 5,6
something like 1[K]*linproj1(genproj1(T[1/K])/genproj1(1))/linproj1(1)
as you can only go one DoF at the time, and projection only works on thets mesh check the doc
--
Good luck
Ivar
Hi
well for me you should keep the boundary layer and identify why it goes unstable and rather fix that ;)
But then I take this comment back, because the projection operator do not work on other than thets, but you can always do a mesh convert on the domain as last mesh operation, then you keep the fine mesh along the edges, always cleaner, numerically
Another point, is it a half tube with symmetry conditions on the flat cut plane ? in which case you need to add "symmetry" BC, so that the flow remains invariant (and boundary normal = 0 ) along this boundary, also for the HT
In this case you probably do not need your projection variable either (I might have misunderstood though)
If you want to get an average per Z height you can also make a series of Data Set cut planes and integrate over these. Or use two projections: general projection on all domain from z,x,y to z,x, and another one on the flat boundary x,y=0,z from z,x to z and then combine both (the latter one can also be a linear projection from vertex source 1,11,2 to vertex destination 5,6
something like 1[K]*linproj1(genproj1(T[1/K])/genproj1(1))/linproj1(1)
as you can only go one DoF at the time, and projection only works on thets mesh check the doc
--
Good luck
Ivar
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Posted:
1 decade ago
18 avr. 2013, 20:21 UTC−4
Ivar,
I've attached the model with the bulk average fluid temperature calculated with your suggestions implemented. I used two general projections:
1[K]*genproj2(genproj1(T[1/K])/genproj1(1))/genproj2(1)
So, I have genproj1() z,x,y to z,x, which is integration through the volume projected onto the 2D plane z,x,
And then genproj2() that gives an integration on the flat boundary x,y=0,z from z,x to z,
I drew myself a picture of how it works, I would not have worked that out from the manual! (I attached it as a .zip as well because I found I could not re-open the first file.)
Thank you very much for your help,
Adam
Ivar,
I've attached the model with the bulk average fluid temperature calculated with your suggestions implemented. I used two general projections:
1[K]*genproj2(genproj1(T[1/K])/genproj1(1))/genproj2(1)
So, I have genproj1() z,x,y to z,x, which is integration through the volume projected onto the 2D plane z,x,
And then genproj2() that gives an integration on the flat boundary x,y=0,z from z,x to z,
I drew myself a picture of how it works, I would not have worked that out from the manual! (I attached it as a .zip as well because I found I could not re-open the first file.)
Thank you very much for your help,
Adam
Ivar KJELBERG
COMSOL Multiphysics(r) fan, retired, former "Senior Expert" at CSEM SA (CH)
Please login with a confirmed email address before reporting spam
Posted:
1 decade ago
19 avr. 2013, 15:43 UTC−4
Hi
one thing to be aware off, the average is generally written
ave_of_a_field = integration_over_entity(your variable) / integration_over_entity(1)
but when you do a mapping you have a set of integrations, then you have always to consider the issue of integration of a value over s separate integration of the area, and the sum of the ( line integration / line integration of 1 = line length )
I'm not sure that in all generality, for any skewed surface in 3D you can swap integration and division.
But it seems certainly the case for you nice "cubic model well aligned on the Cartesian coordinates.
An example the aveop(T*(x<0)) to get the average temperature over the domain(s) for (x<0) IS NOT the same as the true "average" ave = intop(T*(x<0)) / intop((x<0)).
The former is giving you intop(T*(x<0)) / intop(1)
So check carefully the hypothesis when combining projections and complex formulas
--
Good luck
Ivar
Hi
one thing to be aware off, the average is generally written
ave_of_a_field = integration_over_entity(your variable) / integration_over_entity(1)
but when you do a mapping you have a set of integrations, then you have always to consider the issue of integration of a value over s separate integration of the area, and the sum of the ( line integration / line integration of 1 = line length )
I'm not sure that in all generality, for any skewed surface in 3D you can swap integration and division.
But it seems certainly the case for you nice "cubic model well aligned on the Cartesian coordinates.
An example the aveop(T*(x
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Posted:
1 decade ago
22 nov. 2013, 10:17 UTC−5
I actually made a mistake in the file I uploaded "BulkModel2.zip" the plot for the fluid should actually read:
genproj2(genproj1(T))/genproj2(genproj1(1))
I actually made a mistake in the file I uploaded "BulkModel2.zip" the plot for the fluid should actually read:
genproj2(genproj1(T))/genproj2(genproj1(1))