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Low Salinity Waterflooding An Overview of Likely Mechanisms Jill Buckley EORI contractor Adjunct, Dept. of Chem. and Petroleum Eng. 15 January 2009

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  • Low Salinity Waterflooding

    An Overview of Likely Mechanisms

    Jill Buckley

    EORI contractorAdjunct, Dept. of Chem. and Petroleum Eng.

    15 January 2009

  • http://eori.uwyo.edu

    • Additional oil recovered from some (but not all) sandstone cores.

    • In studies with high permeability Berea sandstone cores, additional oil was recovered if and only if:

    core contained connate water

    oil phase was a crude oil

    core was not “fired” to remove clays

    Observations on Low Salinity Waterflooding

    Recovery (% OOIP)Connate HS MS LS

    Injected

    HS 50 65 80

    MS 50 71

    LS 56 80

  • http://eori.uwyo.edu

    0

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    0 5 10 15 20 25 30 35

    Brine injected, PV

    Rf,

    %O

    OIP

    0

    2

    4

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    8

    10

    12

    14

    ΔP (p

    si) o

    r pH

    Test A:R1/C1WP crude oil, Swi = 40.6%q = 2.6 ft/D

    R

    ΔP

    pH

    RIB(29,690 ppm)

    LSB(1,480 ppm)

    16.2%

    Low Salinity Waterflooding

  • http://eori.uwyo.edu

    Low Salinity Flooding MechanismsUniversity of Wyoming Mechanism Workshop

    12 – 23 May 2008Laramie, WY

    Outside Experts:

    Geoff Mason U Loughborough

    Koichi Takamura BASF

    Andrew Fogden Australian Nat U

    Norman Morrow, Xina Xie, Li Yu, Jill BuckleyNina Loahardjo, Wang Wei, Pu Hui, Xiuyu Wang

  • http://eori.uwyo.edu

    Suggested Mechanisms• Osmotic pressure

    • Limited release of mixed-wet particles

    • Salinity shock

    • Mineral dissolution

    • Emulsification/snap-off

    • Saponification

    • Particle-stabilized interfaces/lamellae

    • Multicomponent ion exchange

    • Surfactant-like behavior

    • Wettability alteration (more water-wet)

    • Wettability alteration (less water-wet)

    • Viscosity ratio

  • http://eori.uwyo.edu

    In a porous medium, there are multiple solid and fluid phases.

    Properties of interfaces between these phases change as brine composition changes.

  • http://eori.uwyo.edu

    Proposed Mechanism

    Description: Evidence for:

    Evidence against: Experiments needed:

  • http://eori.uwyo.edu

    Osmotic Pressure

    Description: Evidence for:

    Evidence against: Experiments needed:

    Rock may act as a semi- permeable membrane.

    +ΔP usually associated with low salinity injected brine and increased recovery.

    Increase only observed for crude oils--no increase in recovery with mineral oil

    Low salinity of both connate and injected water gives very high recovery even though there is no change in salinity.

    high salinityoillow salinity

    Tube with corners:

    Flow of oil plug depends on whether water can flow around the oil drop or high salinity phase expands.

  • http://eori.uwyo.edu

    Limited Release of Mixed-Wet Particles

    Description: Evidence for:

    Evidence against: Experiments needed:

    Tang and Morrow (1999)p

    oil

    water

    solid

    clays

    oil

    clay

    oil

    oilwater

    solid

    Fines not seen in all experiments, especially BP reservoir conditions tests.

    Tests to find and identify mixed-wet particles.

  • http://eori.uwyo.edu

    Salinity Shock

    Description: Evidence for:

    Evidence against: Experiments needed:

    Changes in flowing aqueous phase composition can be amplified by step changes in injected compositions.

  • http://eori.uwyo.edu

    Vaiyda and Fogler, 1992

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    Salinity Shock

    Description: Evidence for:

    Evidence against: Experiments needed:

    Changes in flowing aqueous phase composition can be amplified by step changes in injected compositions.

    Often see increase ΔP and recovery with step decrease in salinity.

    Secondary recovery is better for low salinity, without salinity shock.

    Additional investigation of salinity gradient effects.

  • http://eori.uwyo.edu

    Mineral Dissolution

    Description: Evidence for:

    Evidence against: Experiments needed:

    Reducing salinity increases solubility of some minerals.

    Tensleep core, which does not contain clay, responds to low salinity waterflooding. Cement dissolution may release dolomite particles.

    Micro CT visualization and AFM force measurements are in progress at ANU.

  • http://eori.uwyo.edu

    Tensleep rock

    quartz

    dolomite

    Swi =20% φ=14% k=14md (HSB); 9.5 md (LSB)

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    Registration[1]Size 762x460x573Dry: P=7.7%; Q=79.6%; D+A=12.6%Wet: P=7.6%; Q=79.6%; D+A=12.7%

    [1] Latham, S, Varslot, T & Sheppard, A. P., 2008. Image registration in Micro-CT experiments, to be submitted to the Proceedings of the Society of Core Analysts

  • http://eori.uwyo.edu

    Emulsifcation/Snap-off

  • http://eori.uwyo.edu

    5

    10

    15

    20

    25

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    35

    40

    45

    50

    55

    5 15 25 35 45 55

    Predicted API

    °API

    1.4

    1.42

    1.44

    1.46

    1.48

    1.5

    1.52

    1.54

    1.56

    1.58

    1.6

    5 15 25 35 45 55

    RI@

    20°C

    0

    2

    4

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    8

    10

    12

    0 10 20 30 40 50 60

    API Gravity

    mg

    KO

    H /

    g oi

    l

    0

    2

    4

    6

    8

    10

    12

    0 10 20 30 40 50 60

    API Gravity

    mg

    KO

    H /

    g oi

    l

    Crude Oil Composition ~ 300 Samples

    ACID NUMBER

    BASE NUMBER

    RI vs °API

    SARA vs °API

  • http://eori.uwyo.edu

    5

    10

    15

    20

    25

    30

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    40

    45

    50

    55

    5 15 25 35 45 55

    Predicted API

    °API

    1.4

    1.42

    1.44

    1.46

    1.48

    1.5

    1.52

    1.54

    1.56

    1.58

    1.6

    5 15 25 35 45 55

    °API

    RI@

    20°C

    0

    2

    4

    6

    8

    10

    12

    0 10 20 30 40 50 60

    API Gravity

    mg

    KO

    H /

    g oi

    l

    0

    2

    4

    6

    8

    10

    12

    0 10 20 30 40 50 60

    API Gravity

    mg

    KO

    H /

    g oi

    l

    Wyoming Crude Oil Composition (20 samples)

    ACID NUMBER

    BASE NUMBER

    RI vs °API

    SARA vs °API

  • http://eori.uwyo.edu

    The Way Forward

    Can we find a model rock?Reservoir cores often respond to low salinity waterflooding, but are hard to obtain, limited in quantity, heterogeneous, and sometimes poorly consolidated.

    Outcrop rocks have some advantages, but have been exposed to oxidation and to low salinity rainwater. Some Berea cores (higher permeability) respond to low salinity waterflooding, but the core material that is currently available from the quarry is lower in permeability and does not respond consistently.

  • http://eori.uwyo.edu

    The Way Forward

    Address baseline problem in reservoir cores

    Response to low salinity my be greater in a secondary waterflood than in tertiary mode, but the baseline is shifting.

  • http://eori.uwyo.edu

    The Way Forward

    Fundamental studies

    Can we create a micromodel that includes kaolinite?

    Force measurements in low and high salinity environments.

    Micro CT visualization of particle movement.

  • http://eori.uwyo.edu

    The Way Forward

    Suggestions for improved laboratory procedures

    Add back pressure regulation

    Add pressure measurements in imbibition tests

  • Low Salinity Waterflooding

    An Overview of Likely Mechanisms

    Jill Buckley

    EORI contractorAdjunct, Dept. of Chem. and Petroleum Eng.

    15 January 2009

  • http://eori.uwyo.edu

    Viscosity Ratio

    Description: Evidence for:

    Evidence against: Experiments needed:

    Is kaolin dispersed in brine or formation of emulsions increasing viscosity and sweep efficiency?

    Use glycerol to viscosify brine or toluene to reduce oil viscosity.

    Use a back pressure regulator to facilitate use of low viscosity oils.

  • http://eori.uwyo.edu

    Saponification

    Description: Evidence for:

    Evidence against: Experiments needed:

    If pH of flowing aqueous phase is high enough, saponification of esters from the oil phase can cause mass transfer from oil to water and decrease IFT.

    We are not seeing consistent increases in pH and pH never gets high enough to release fines or reduce IFT significantly.

    An increase in pH was observed in early low salinity tests.

    ester + NaOH = alcohol + organic acid

    Characterization of effluent brine composition.

    Crude oil compositional information.

  • http://eori.uwyo.edu

    Surfactant-like Behavior

    Description: Evidence for:

    Evidence against: Experiments needed:

    Increasing temperature should have the same effect.

    Tor Austad says adsorbed materials are surfactants, salted out by high salinity that comes off the surface in low salinity water, forms micelles or is transferred to the oil phase. Calls this “salting in.”

    mixed wettingsolid

    water

    oil

    decreasesalinity

  • http://eori.uwyo.edu

    Multicomponent Ion Exchange

    Description: Evidence for:

    Evidence against: Experiments needed:

    BP patent: [Ca2+]inj / [Ca2+]connate < 1

    Lager et al., 2006; BP patent, 2007

    Secondary results for Injected = Connate.Recovery is better with low salinity even though ion exchange has already taken place.

    Evidence of Ca2+ in oil? Difficult to measure.

    0

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    0 1 2 3 4 5 6 7Pore volume

    Chl

    orid

    e co

    ncen

    trat

    ion

    (ppm

    )

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    Mag

    nesi

    um c

    once

    ntra

    tion

    (ppm

    )

    Chloride Mg

  • http://eori.uwyo.edu

    0

    5

    1 0

    1 5

    2 0

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    bene

    fit c

    ompa

    re to

    w

    ater

    flood

    resu

    lts (%

    )

    1 2 3 4 5 6 8 9 10 11 12 13 14 15 16 17 18

    Low Salinity WaterfloodingSlide Number 2Slide Number 3Slide Number 4Slide Number 5Slide Number 6Slide Number 7Slide Number 8Slide Number 9Slide Number 10Slide Number 11Slide Number 12Slide Number 13Tensleep rockRegistration[1]Slide Number 16Slide Number 17Slide Number 18Slide Number 19Slide Number 20Slide Number 21Slide Number 22Low Salinity WaterfloodingSlide Number 24Slide Number 25Slide Number 26Slide Number 27Slide Number 28