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Slow migration of detached fine particles over rock surface in porous media
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文摘

Long permeability stabilization periods during corefloods with alternate flow rates.

We attribute the long stabilization periods to slow drift of detached particles.

The mathematical model for slow fines drift is developed; the exact solution is derived.

Good agreement between laboratory data and analytical modelling.

Maximum retention concentration is defined for mono-layer of size-distributed fines.

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