Hello, I'm doing some work to get permeability in 2D porous media by LBM.

And I'm considering Zou/He pressure BC in my inlet/outlet, because my geometry may not be periodic (I read some papers about effective body force for pressure gradient BCs and understood that method can be used in periodic geometry).

To validate my LBM code, I'm doing compare analytic solution and numerical solution about Poiseuille flow between plates. And I saw weird phenomena.

When, inlet velocity reach to outlet, velocity in outlet become greater than inlet. So, magnitude of velocity seems to propagate outlet to inlet. (=magnitude of velocity seems to be reversed)

I guess this phenomena comes from Zou/He pressure BCs. Because unknown population of inlet (or outlet) comes from known population, when population from inlet(or outlet) reaching to outlet( or inlet), flow should be reversed.

So, my question is "Is this phenomena right?/ Should I consider streaming from neighboring node in inlet/outlet?". Because, in my common sense, flow formed opposite direction to pressure gradient quite seems weird(It is creeping flow). (But it shows good result when comparing analytic solution)

And when I'm not considering streaming from neighboring node(just do overwriting to initial value), result was not good and fully developed flow can not be formed.

I needs you guess advice.

Thank you for your reading.

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