Characterisation of surface electrical charge and wettability in carbonates with application to controlled salinity waterflooding

M. D. Jackson, Jan Vinogradov

Research output: Contribution to conferencePaper

Abstract

It is well known that the wetting behavior of carbonate mineral surfaces is affected by their surface electrical charge (Strand et. al., 2006; Hiorth et. al., 2010) and that the surface charge in saturated porous media can be characterized using measurements of streaming potential (Jouniaux and Pozzi (1995); Delgado et. al., 2007). Streaming potentials in porous media arise from the charge separation that occurs in the electrical double layer at mineral-fluid interfaces (Hunter, 1981). If the fluid is induced to flow by an external potential (pressure) gradient, then some of the excess charge within the double layer is transported with the flow, giving rise to a streaming current. Divergence of the
streaming current density establishes an electrical potential, termed the streaming potential. The closest plane to the mineral surface at which flow occurs in the double layer is termed the shear plane; the electrical potential at this plane is termed the zeta potential. The relationships between streaming potential and surface electrical charge, and between surface electrical charge and wettability, suggest that measurements of streaming potential may be used to probe the wetting state of mineral surfaces in intact core samples. Previous studies have measured streaming potential in core samples saturated with oil, and with oil and brine, but the samples had not been aged to alter their wetting behavior (Alkafeef et. al., (2001); Alkafeef and Alajmi (2006); Vinogradov and Jackson (2001). Consequently, the relationship between streaming potential and wettability has not been investigated. Yet if streaming potential measurements, and the electrical properties interpreted from these measurements such as zeta potential and surface electrical charge, are affected by wettability in a direct and
quantifiable manner, then streaming potential measurements may be of great utility in characterizing wettability and processes that affect wettability. The aim of this paper is to determine whether wettability alteration in carbonate core samples leads to measurable changes in streaming potential.
Original languageEnglish
Number of pages10
Publication statusPublished - 2012
EventAAPG/SPE/SEG Hedberg Research Conference - SAINT-CYR SUR MER, France
Duration: 8 Jul 201213 Jul 2012

Conference

ConferenceAAPG/SPE/SEG Hedberg Research Conference
CountryFrance
CitySAINT-CYR SUR MER
Period8/07/1213/07/12

Fingerprint

streaming potential
wettability
salinity
carbonate
wetting
mineral
porous medium
fluid
electrical property
oil
density current
pressure gradient
brine
divergence
probe

Cite this

Jackson, M. D., & Vinogradov, J. (2012). Characterisation of surface electrical charge and wettability in carbonates with application to controlled salinity waterflooding. Paper presented at AAPG/SPE/SEG Hedberg Research Conference, SAINT-CYR SUR MER, France.

Characterisation of surface electrical charge and wettability in carbonates with application to controlled salinity waterflooding. / Jackson, M. D.; Vinogradov, Jan.

2012. Paper presented at AAPG/SPE/SEG Hedberg Research Conference, SAINT-CYR SUR MER, France.

Research output: Contribution to conferencePaper

Jackson, MD & Vinogradov, J 2012, 'Characterisation of surface electrical charge and wettability in carbonates with application to controlled salinity waterflooding' Paper presented at AAPG/SPE/SEG Hedberg Research Conference, SAINT-CYR SUR MER, France, 8/07/12 - 13/07/12, .
Jackson MD, Vinogradov J. Characterisation of surface electrical charge and wettability in carbonates with application to controlled salinity waterflooding. 2012. Paper presented at AAPG/SPE/SEG Hedberg Research Conference, SAINT-CYR SUR MER, France.
Jackson, M. D. ; Vinogradov, Jan. / Characterisation of surface electrical charge and wettability in carbonates with application to controlled salinity waterflooding. Paper presented at AAPG/SPE/SEG Hedberg Research Conference, SAINT-CYR SUR MER, France.10 p.
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abstract = "It is well known that the wetting behavior of carbonate mineral surfaces is affected by their surface electrical charge (Strand et. al., 2006; Hiorth et. al., 2010) and that the surface charge in saturated porous media can be characterized using measurements of streaming potential (Jouniaux and Pozzi (1995); Delgado et. al., 2007). Streaming potentials in porous media arise from the charge separation that occurs in the electrical double layer at mineral-fluid interfaces (Hunter, 1981). If the fluid is induced to flow by an external potential (pressure) gradient, then some of the excess charge within the double layer is transported with the flow, giving rise to a streaming current. Divergence of thestreaming current density establishes an electrical potential, termed the streaming potential. The closest plane to the mineral surface at which flow occurs in the double layer is termed the shear plane; the electrical potential at this plane is termed the zeta potential. The relationships between streaming potential and surface electrical charge, and between surface electrical charge and wettability, suggest that measurements of streaming potential may be used to probe the wetting state of mineral surfaces in intact core samples. Previous studies have measured streaming potential in core samples saturated with oil, and with oil and brine, but the samples had not been aged to alter their wetting behavior (Alkafeef et. al., (2001); Alkafeef and Alajmi (2006); Vinogradov and Jackson (2001). Consequently, the relationship between streaming potential and wettability has not been investigated. Yet if streaming potential measurements, and the electrical properties interpreted from these measurements such as zeta potential and surface electrical charge, are affected by wettability in a direct andquantifiable manner, then streaming potential measurements may be of great utility in characterizing wettability and processes that affect wettability. The aim of this paper is to determine whether wettability alteration in carbonate core samples leads to measurable changes in streaming potential.",
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note = "ExxonMobil Upstream Research Company are thanked for providing the core samples used in the experimental program, for flooding the cores with crude oil to establish the irreducible brine saturation, aging sample 1, and then flooding the cores with brine to establish the residual oil saturation. They are also thanked for granting permission to publish the results of the study. ; AAPG/SPE/SEG Hedberg Research Conference ; Conference date: 08-07-2012 Through 13-07-2012",
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N1 - ExxonMobil Upstream Research Company are thanked for providing the core samples used in the experimental program, for flooding the cores with crude oil to establish the irreducible brine saturation, aging sample 1, and then flooding the cores with brine to establish the residual oil saturation. They are also thanked for granting permission to publish the results of the study.

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N2 - It is well known that the wetting behavior of carbonate mineral surfaces is affected by their surface electrical charge (Strand et. al., 2006; Hiorth et. al., 2010) and that the surface charge in saturated porous media can be characterized using measurements of streaming potential (Jouniaux and Pozzi (1995); Delgado et. al., 2007). Streaming potentials in porous media arise from the charge separation that occurs in the electrical double layer at mineral-fluid interfaces (Hunter, 1981). If the fluid is induced to flow by an external potential (pressure) gradient, then some of the excess charge within the double layer is transported with the flow, giving rise to a streaming current. Divergence of thestreaming current density establishes an electrical potential, termed the streaming potential. The closest plane to the mineral surface at which flow occurs in the double layer is termed the shear plane; the electrical potential at this plane is termed the zeta potential. The relationships between streaming potential and surface electrical charge, and between surface electrical charge and wettability, suggest that measurements of streaming potential may be used to probe the wetting state of mineral surfaces in intact core samples. Previous studies have measured streaming potential in core samples saturated with oil, and with oil and brine, but the samples had not been aged to alter their wetting behavior (Alkafeef et. al., (2001); Alkafeef and Alajmi (2006); Vinogradov and Jackson (2001). Consequently, the relationship between streaming potential and wettability has not been investigated. Yet if streaming potential measurements, and the electrical properties interpreted from these measurements such as zeta potential and surface electrical charge, are affected by wettability in a direct andquantifiable manner, then streaming potential measurements may be of great utility in characterizing wettability and processes that affect wettability. The aim of this paper is to determine whether wettability alteration in carbonate core samples leads to measurable changes in streaming potential.

AB - It is well known that the wetting behavior of carbonate mineral surfaces is affected by their surface electrical charge (Strand et. al., 2006; Hiorth et. al., 2010) and that the surface charge in saturated porous media can be characterized using measurements of streaming potential (Jouniaux and Pozzi (1995); Delgado et. al., 2007). Streaming potentials in porous media arise from the charge separation that occurs in the electrical double layer at mineral-fluid interfaces (Hunter, 1981). If the fluid is induced to flow by an external potential (pressure) gradient, then some of the excess charge within the double layer is transported with the flow, giving rise to a streaming current. Divergence of thestreaming current density establishes an electrical potential, termed the streaming potential. The closest plane to the mineral surface at which flow occurs in the double layer is termed the shear plane; the electrical potential at this plane is termed the zeta potential. The relationships between streaming potential and surface electrical charge, and between surface electrical charge and wettability, suggest that measurements of streaming potential may be used to probe the wetting state of mineral surfaces in intact core samples. Previous studies have measured streaming potential in core samples saturated with oil, and with oil and brine, but the samples had not been aged to alter their wetting behavior (Alkafeef et. al., (2001); Alkafeef and Alajmi (2006); Vinogradov and Jackson (2001). Consequently, the relationship between streaming potential and wettability has not been investigated. Yet if streaming potential measurements, and the electrical properties interpreted from these measurements such as zeta potential and surface electrical charge, are affected by wettability in a direct andquantifiable manner, then streaming potential measurements may be of great utility in characterizing wettability and processes that affect wettability. The aim of this paper is to determine whether wettability alteration in carbonate core samples leads to measurable changes in streaming potential.

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