Modelling of wettability alteration processes in carbonate oil reservoirs
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Liping Yu
1
, ,
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Hans Kleppe
1
, ,
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Terje Kaarstad
1
, ,
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Svein M. Skjaeveland
1
, ,
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Steinar Evje
2
, ,
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Ingebret Fjelde
2
,
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1.
University of Stavanger, NO-4036 Stavanger
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2.
International Research Institute of Stavanger (IRIS), Prof. Olav Hanssensvei 15, NO-4068 Stavanger
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Received:
01 September 2007
Revised:
01 November 2007
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76S05, 76R50, 76R05, 65M12, 35L65, 35K65.
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Previous studies have shown that seawater may alter the
wettability in the direction of more water-wet conditions in
carbonate reservoirs. The reason for this is that ions from the
salt (sulphat, magnesium, calsium, etc) can create a wettability
alteration toward more water-wet conditions as salt is absorbed on
the rock.
In order to initiate a more systematic study of this phenomenon a
1-D mathematical model relevant for spontaneous imbibition is
formulated. The model represents a core plug on laboratory scale
where a general wettability alteration (WA) agent is included.
Relative permeability and capillary pressure curves are obtained
via interpolation between two sets of curves corresponding to
oil-wet and water-wet conditions. This interpolation depends on
the adsorption isotherm in such a way that when no adsorption of
the WA agent has taken place, oil-wet conditions prevail. However,
as the adsorption of this agent takes place, gradually there is a
shift towards more water-wet conditions. Hence, the basic
mechanism that adsorption of the WA agent is responsible for the
wettability alteration, is naturally captured by the model.
Conservation of mass of oil, water, and the WA agent, combined with
Darcy's law, yield a 2x2 system of coupled parabolic
convection-diffusion equations, one equation for the water phase and
another for the concentration of the WA agent. The model describes
the interactions between gravity and capillarity when initial
oil-wet core experiences a wettability alteration towards more
water-wet conditions due to the spreading of the WA agent by
molecular diffusion. Basic properties of the model are studied by
considering a discrete version. Numerical computations are performed
to explore the role of molecular diffusion of the WA agent into the
core plug, the balance between gravity and capillary forces, and
dynamic wettability alteration versus permanent wetting states. In
particular, a new and characteristic oil-bank is observed. This is
due to incorporation of dynamic wettability alteration and cannot be
seen for case with permanent wetting characteristics. More
precisely, the phenomenon is caused by a cross-diffusion term
appearing in capillary diffusion term.
Citation: Liping Yu, Hans Kleppe, Terje Kaarstad, Svein M. Skjaeveland, Steinar Evje, Ingebret Fjelde. Modelling of wettability alteration processes in carbonate oil reservoirs[J]. Networks and Heterogeneous Media, 2008, 3(1): 149-183. doi: 10.3934/nhm.2008.3.149
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Abstract
Previous studies have shown that seawater may alter the
wettability in the direction of more water-wet conditions in
carbonate reservoirs. The reason for this is that ions from the
salt (sulphat, magnesium, calsium, etc) can create a wettability
alteration toward more water-wet conditions as salt is absorbed on
the rock.
In order to initiate a more systematic study of this phenomenon a
1-D mathematical model relevant for spontaneous imbibition is
formulated. The model represents a core plug on laboratory scale
where a general wettability alteration (WA) agent is included.
Relative permeability and capillary pressure curves are obtained
via interpolation between two sets of curves corresponding to
oil-wet and water-wet conditions. This interpolation depends on
the adsorption isotherm in such a way that when no adsorption of
the WA agent has taken place, oil-wet conditions prevail. However,
as the adsorption of this agent takes place, gradually there is a
shift towards more water-wet conditions. Hence, the basic
mechanism that adsorption of the WA agent is responsible for the
wettability alteration, is naturally captured by the model.
Conservation of mass of oil, water, and the WA agent, combined with
Darcy's law, yield a 2x2 system of coupled parabolic
convection-diffusion equations, one equation for the water phase and
another for the concentration of the WA agent. The model describes
the interactions between gravity and capillarity when initial
oil-wet core experiences a wettability alteration towards more
water-wet conditions due to the spreading of the WA agent by
molecular diffusion. Basic properties of the model are studied by
considering a discrete version. Numerical computations are performed
to explore the role of molecular diffusion of the WA agent into the
core plug, the balance between gravity and capillary forces, and
dynamic wettability alteration versus permanent wetting states. In
particular, a new and characteristic oil-bank is observed. This is
due to incorporation of dynamic wettability alteration and cannot be
seen for case with permanent wetting characteristics. More
precisely, the phenomenon is caused by a cross-diffusion term
appearing in capillary diffusion term.
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