Question About Fracture Property Scaling in Lower-Dimensional Elements #29152
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SirGardener
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Q&A Modules: Porous Flow
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First, thank you for providing such detailed documentation and examples for mixed-dimensional modeling. While implementing both DFN and CDFM models, we noticed some interesting behavior regarding property scaling that we'd like to discuss.
We're working with the example Flow and solute transport along 2D elliptical fractures embedded in a 3D porous matrix as a reference and implementing similar models. The documentation suggests scaling both permeability and porosity with aperture:
Observations
We've tested different scaling approaches and observed the following:
Configuration A (Double scaling as suggested in documentation):
k = (a²/12) * a # Permeability scaled with aperture
ϕ = 1 * a # Porosity scaled with aperture
Results:
DFN model:
CDFM model:
Configuration B (Single scaling):
k = (a²/12) * a # Permeability scaled with aperture
ϕ = 1 # Unscaled porosity (MOOSE handles volume scaling)
Results:
Both DFN and CDFM models:
Questions
Given that MOOSE automatically scales the volume term (and thus porosity) with aperture for lower-dimensional elements, is the additional manual scaling of porosity necessary or potentially problematic?
The observed behavior suggests that Configuration B (scaling only permeability) produces more physically reasonable results. Is this the intended approach?
Could the documentation be clarified regarding:
Additional Context
Our testing involved:
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