Impact of Inertia on the Stability of Two-phase Flow: a Pore-doublet Approach
ORAL
Abstract
Haine’s jumps, or rheons, occur during drainage in porous media at low capillary number and
are characterised by pinning of the interface at a constriction, before a quick and sudden
invasion of the next pore-body. During the jump, the interface’s speed is two to three orders of
magnitude above the average invasion speed. This raises the question: can inertia, usually
neglected during the invasion, play a role during those jumps? In this presentation, we will
focus on Haines jumps and the potential impact of localized inertial events on two-phase flows
in porous media.
Microfluidic devices, also called micromodels or aquifer-on-chips, are designed to mimic the
porous media and to allow for the direct observation of the fluid flow and interfacial dynamics.
In this work, particular interest is given to pore doublets, whose geometry is composed of two
parallel channels connected together at the inlet and the outlet. Their structure allows us to
reproduce the different regimes that appear during the drainage of a porous medium, as well
as to study the pore’s invasion mechanisms, such as Haine’s jumps.
We developed a pore-doublet model consisting in a set of equations resulting from the
integration of mass and momentum equations. The model accounts for inertia effects.
Simulations are then compared with experiments. The developed model, as well as the
experimental data, allows for a better understanding of the impact of inertia during two-phase flow. We
showed that, even for Reynolds numbers below one, after a jump, the menisci can oscillate
around their stable positions. If these oscillations, caused by the inertia of the fluid, are
important enough, they can help or inhibit the next Haine’s jump, altering the order in which the
pores are invaded. This can turn a stable drainage, where both channels are drained
simultaneously, to an unstable one where one pathway is preferentially invaded over the
other. We show that inertia must be considered when the density ratio or the aspect ratio
between the pore bodies and the constrictions is high.
are characterised by pinning of the interface at a constriction, before a quick and sudden
invasion of the next pore-body. During the jump, the interface’s speed is two to three orders of
magnitude above the average invasion speed. This raises the question: can inertia, usually
neglected during the invasion, play a role during those jumps? In this presentation, we will
focus on Haines jumps and the potential impact of localized inertial events on two-phase flows
in porous media.
Microfluidic devices, also called micromodels or aquifer-on-chips, are designed to mimic the
porous media and to allow for the direct observation of the fluid flow and interfacial dynamics.
In this work, particular interest is given to pore doublets, whose geometry is composed of two
parallel channels connected together at the inlet and the outlet. Their structure allows us to
reproduce the different regimes that appear during the drainage of a porous medium, as well
as to study the pore’s invasion mechanisms, such as Haine’s jumps.
We developed a pore-doublet model consisting in a set of equations resulting from the
integration of mass and momentum equations. The model accounts for inertia effects.
Simulations are then compared with experiments. The developed model, as well as the
experimental data, allows for a better understanding of the impact of inertia during two-phase flow. We
showed that, even for Reynolds numbers below one, after a jump, the menisci can oscillate
around their stable positions. If these oscillations, caused by the inertia of the fluid, are
important enough, they can help or inhibit the next Haine’s jump, altering the order in which the
pores are invaded. This can turn a stable drainage, where both channels are drained
simultaneously, to an unstable one where one pathway is preferentially invaded over the
other. We show that inertia must be considered when the density ratio or the aspect ratio
between the pore bodies and the constrictions is high.
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Presenters
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Nathan Bernard
CNRS
Authors
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Nathan Bernard
CNRS
-
Cyprien Soulaine
CNRS, Institut des Sciences de la Terre d'Orléans (ISTO)
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Sophie Roman
University of Orleans