Two-phase immiscible displacement of water by gas accounting for fines migration: analytical model for vertical equilibrium

Fuente: arXiv
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Main Authors: Shokrollahi, Amin, Prempeh, Kofi Ohemeng Kyei, Mobasher, Syeda Sara, Zeinijahromi, Abbas, Bedrikovetsky, Pavel
Format: Preprint
Published: 2025
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_version_ 1866909510476496896
author Shokrollahi, Amin
Prempeh, Kofi Ohemeng Kyei
Mobasher, Syeda Sara
Zeinijahromi, Abbas
Bedrikovetsky, Pavel
author_facet Shokrollahi, Amin
Prempeh, Kofi Ohemeng Kyei
Mobasher, Syeda Sara
Zeinijahromi, Abbas
Bedrikovetsky, Pavel
contents Fines migration during subterranean CO2 storage is considered as one of major contributors to formation damage and injectivity decline. The main formation damage mechanism by migrating fines is rock clogging by straining of particles in thin pore throats. The main mobilisation mechanism of attached natural reservoir fines is their detachment by capillary forces exerting from the advancing water-gas menisci. The mathematical model for displacement of water by injected CO2 from layer-cake reservoirs under fines mobilisation, migration and straining extends the classical vertical capillary-gravity equilibrium model, where hydrostatic pressure gradient is assumed in each phase. The analytical model generalises classical Buckley-Leverett problem, where the extended fractional flow accounts for permeability damage due to fines migration. We show the significant effect of fines migration on water displacement - while it decreases well injectivity, fines migration simultaneously increases reservoir sweep, increasing CO2 storage capacity.
format Preprint
id arxiv_https___arxiv_org_abs_2502_18035
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Two-phase immiscible displacement of water by gas accounting for fines migration: analytical model for vertical equilibrium
Shokrollahi, Amin
Prempeh, Kofi Ohemeng Kyei
Mobasher, Syeda Sara
Zeinijahromi, Abbas
Bedrikovetsky, Pavel
Geophysics
Fines migration during subterranean CO2 storage is considered as one of major contributors to formation damage and injectivity decline. The main formation damage mechanism by migrating fines is rock clogging by straining of particles in thin pore throats. The main mobilisation mechanism of attached natural reservoir fines is their detachment by capillary forces exerting from the advancing water-gas menisci. The mathematical model for displacement of water by injected CO2 from layer-cake reservoirs under fines mobilisation, migration and straining extends the classical vertical capillary-gravity equilibrium model, where hydrostatic pressure gradient is assumed in each phase. The analytical model generalises classical Buckley-Leverett problem, where the extended fractional flow accounts for permeability damage due to fines migration. We show the significant effect of fines migration on water displacement - while it decreases well injectivity, fines migration simultaneously increases reservoir sweep, increasing CO2 storage capacity.
title Two-phase immiscible displacement of water by gas accounting for fines migration: analytical model for vertical equilibrium
topic Geophysics
url https://arxiv.org/abs/2502.18035