Why is there a velocity discontinuity next to a zero-velocity zone?
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I am modeling a pair of channels separated by a zero-velocity porous zone, through which only diffusion occurs. As you can see in this image, the flow profile is not parabolic, and has a velocity discontinuity. What can I do to have a continuous parabolic flow within both independent channels? I want to have a no-slip condition on the interface.
Here are the membrane properties that I am using:
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