Closing_the_loop_R.pdf

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Transcript of Closing_the_loop_R.pdf

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  • Closing the Loop between geo&engineering in building

    calibration and history matching carbonate reservoir models?

    Patrick Corbett

    BG Group Professor

    Carbonate Petroleum Geoengineering

    AAPG Distinguished Lecture May 2014

    3

  • Fractured or not?

    Reservoir Engineering YES Well test response Negative skin Cross-flow

    Geology NO No fractured core No open fractures on image logs No significant losses

    4

  • Fractured or not?

    Reservoir Engineering YES >>> NO Well test response Negative skin >> not fractures >> double matrix Cross-flow >> not fractures >> double matrix

    Geology NO No fractured core No open fractures on image logs No significant losses

    5

  • Fractured or not?

    Reservoir Engineering YES Well test response Negative skin >>>> double matrix + fractures Cross-flow >>>> double matrix + fractures

    Geology YES Fractured core Open fractures on image logs Significant losses

    6

  • Closing the loop

    Highly heterogeneous carbonate reservoirs Fractured vs non-fractured well tests? Build a model without fractures Care to distribute RTs appropriately Check History Match without fractures Not conclusive but potentially useful Role for PLTs

    7

  • Dual porosity Horizontal well Closely bounded reservoir Negative skin

    Horizontal well Dual porosity Rectangular bounded Negative skin

    Horizontal well Dual porosity Infinite boundary Small positive skin

    Dual porosity Vertical well Negative skin

    A2

    0.01 1.0 100Time, hr

    1E+6

    1E+7

    Gas

    pot

    enti

    al, p

    sia/

    cp

    A1

    A3 A4

    0.1 10 1000

    Time, hr

    1E+6

    1E+7

    Gas

    pot

    enti

    al, p

    sia/

    cp

    0.1 10 1000Time, hr

    1E+6

    1E+7

    Gas

    pot

    enti

    al, p

    sia/

    cp

    0.1 10 1000Time, hr

    100

    1000

    Pres

    sure

    , psi

    a

    Fracture performance of well test??

    Kazemi et al, 20118

  • Composite log

    Layer 2

    Layer 3

    Layer 4

    Prograding ramp facies with higher frequency cycling

    Layer 1

    Kazemi et al, 20119

  • 11020 200 290 370 460 550 640

    Wel

    l bot

    tom

    hol

    e pr

    essu

    re, p

    sia

    A4

    A3

    A2

    A1

    Time, day

    Figure 10b

    Kazemi et al, 201110

  • 11020 200 290 370 460 550 640

    11020 200 290 370 460 550 640

    A1

    A2

    A3

    A4

    Wel

    l gas

    pro

    duct

    ion

    rate

    , MM

    sm3/

    day

    Wel

    l oil

    prod

    ucti

    on r

    ate,

    sm

    3/da

    y

    Time, day

    Time, day

    Figure 10a

    Kazemi et al, 201111

  • Facies Model

    Simple depositonal model with dolomite modification>>>PODS

    Kazemi et al, 201112

  • Well Location in Facies Model

    Interdigitation of Mid- to Outer- Ramp facies

    From Simpson, 2010

    Low PorosityIntragranular Porosity

    Foraminiferal Packstone

    Higher Inter XL Porosity

    Higher Permeability

    Un-dolomitised

    Strong primary control on property distribution

    Dolomitised

    Kazemi et al, 201113

  • Review of H Field Rock Types

    0.001

    0.010

    0.100

    1.000

    10.000

    100.000

    0.00 0.05 0.10 0.15 0.20 0.25 0.30

    Perm

    eabi

    lity

    mD

    Porosity

    L1L2L3L4

    0.001

    0.010

    0.100

    1.000

    10.000

    100.000

    0.00 0.05 0.10 0.15 0.20 0.25 0.30

    Perm

    eabi

    lity

    mD

    Porosity %

    H1H2H3H4

    0.001

    0.010

    0.100

    1.000

    10.000

    100.000

    0.00 0.05 0.10 0.15 0.20 0.25 0.30

    Perm

    eabi

    lity

    Porosity

    GB

    GN

    GPB

    GPN

    MWB

    MWT

    By facies?0.01

    0.1

    1

    10

    100

    0 0.05 0.1 0.15 0.2 0.25

    By well?

    By layer?

    By RRT?By GHE?

    Simpson, 2010

    How do we distribute properties?

    From full field model?

    Kazemi et al, 201114

  • Composite log

    Layer 2

    Layer 3

    Layer 4

    Based on given Log Porosity

    H Field Well H2

    NB: super-k >16%F >40mD?

    GHE Proportion Curve

    GHE Grouping

    Layer 2U

    Layer 2L

    Layer 1

    Use GHE grouping approach

    Kazemi et al, 201115

  • PLT Performance

    H2

    H A1

    H2

    16

  • H Field Model

    17

  • Distribution of Rock Types

    Kazemi et al, 201118

  • Cell dimension (m): 100X100X1Total number of cells: 95760Local grid refinement: 5X5X3

    Porosity

    Permeability

    Simulation Model

    Kazemi et al, 201119

  • Horizontal correlation length, m

    Ver

    tica

    l cor

    rela

    tion

    leng

    th, m

    1000500100

    13

    6

    PODS Distribution lengths

    Kazemi et al, 201120

  • SHORT CORRELATION

    LONG CORRELATION

    Example Models

    Kazemi et al, 201121

  • Storage capacity Flow capacity

    H100V1

    H100V3

    H100V6

    H500V1

    H500V3

    H500V6

    H1000V1

    H1000V3

    H1000V6

    REALISATIONS

    Kazemi et al, 201122

  • Kv/Kh0

    Kv/Kh= 0

    Short correlation length Long correlation length

    Bars

    Vertical Permeability

    Kazemi et al, 201123

  • Short correlation lengthLong correlation lengthHomogenous model

    Gas

    pot

    enti

    al

    Time, hr

    Numerical Well Tests

    Kazemi et al, 201124

  • H100V1 H1000V6

    Short correlation length vs. long correlation length

    Numerical PLT

    Kazemi et al, 201125

  • PorosityPermeabilityShort correlation length

    Long correlation length

    Full Field Model

    Kazemi et al, 201126

  • PorosityPermeability

    Short correlation length

    Long correlation length

    Full Field Model

    Kazemi et al, 201127

  • Full fieldSector modelShort correlation

    Full Field vs Sector Model

    Kazemi et al, 201128

  • Sector model

    Full field model

    Short correlation length Long correlation length

    Bars

    Full Field vs Sector Model

    Kazemi et al, 201129

  • Short correlation lengthLong correlation lengthShort correlation length, field

    Gas

    pot

    enti

    al

    Time, hr

    Long correlation length , field

    Full Field vs Sector Model

    Kazemi et al, 201130

  • Short correlation lengthLong correlation length

    Gas

    pot

    enti

    al

    Time, hr

    sector Full field GHElong

    GHEShort

    Next stage:PLT and WT history matching

    Kazemi et al, 201131

  • Poroperm data and effective RTs

    32

  • PC and Saturation Height

    0

    5

    10

    15

    20

    25

    30

    0.0 0.2 0.4 0.6 0.8 1.0

    Hei

    ght

    (m) a

    bove

    FW

    L

    Water Saturation

    Capillary Pressure Data

    Plug 1 (Por:=18.7%)

    Plug 2 (Por: =14.4%)

    Plug 3 (Por: 12.4%)

    0

    5

    10

    15

    20

    25

    30

    0.0 0.2 0.4 0.6 0.8 1.0

    Hei

    ght

    (m) a

    bove

    FW

    L

    Water Saturation

    Saturation Height Modelling

    GHE2

    GHE4

    GHE5

    33

  • Well H2

    Petrotype Model Calibration

    Layer 2

    Layer 4

    Layer 3

    2U

    2L

    34

  • Porosity Permeability

    Full Field RT based poroperm scenarios

    Kazemi et al, 201135

  • Porosity Permeability

    Full Field RT based poroperm scenarios

    Kazemi et al, 201136

  • Days

    Gas

    pro

    duct

    ion

    rate

    Oil

    prod

    ucti

    on r

    ate

    History

    History Match Gross Production

    Kazemi et al, 201137

  • 300 400 500 600 700 800 900 1000 1100 1200 1300 1400 1500 1600

    A1

    A2

    A4A3

    Time, hr

    Pres

    sure

    History

    Rate

    Pres

    sure

    Rate

    6000 8000 10000 12000 14000 3000 4000 6000 8000 10000

    400 600 8000 1000 12001000 3000 5000 7000 9000 1400 1600

    12000 14000 16000

    History

    History

    History

    History Match - Pressure

    Kazemi et al, 2011

    38

  • 1E-4 1E-3 0.01 0.1 1 10 100 10001E-4 1E-3 0.01 0.1 1 10 100 1000

    A1

    A2

    1E+6

    1E+7

    Gas

    pot

    enti

    al, p

    sia/

    cp 1E+8

    1E+6

    1E+7

    Gas

    pot

    enti

    al, p

    sia/

    cp 1E+8

    1E-3 0.1 10 1000

    1E-3 0.1 10 1000

    Time, hr

    History Match well rate

    Kazemi et al, 201139

  • 1E-5 1E-4 1E-3 0.01 0.1 1 10 100 10000.1

    1

    10

    1E-5 1E-4 1E-3 0.01 0.1 1 10 100 10000.1

    1

    10

    A3

    A4

    1E+7

    Gas

    pot

    enti

    al, p

    sia/

    cp1E

    +81

    10

    Pres

    sure

    , psi

    a

    1E-3 0.1 10 1000

    1E-3 0.1 10 1000

    1E-3 0.1 10 1000

    Time, hr

    History Match Well rate

    Kazemi et al, 201140

  • 1E-5 1E-4 1E-3 0.01 0.1 1 10 100 1000

    A2

    A11E

    +71E

    +8

    Gas

    pot

    enti

    al, p

    sia/

    cp1E

    +61E

    +7

    Gas

    pot

    enti

    al, p

    sia/

    cp

    1E-3 0.1 10 1000

    1E-3 0.1 10 1000

    Time, hr

    Model WT match

    Kazemi et al, 201141

  • A3

    A4

    1E+7

    Gas

    pot

    enti

    al, p

    sia/

    cp1E

    +81

    10

    Pres

    sure

    , psi

    a

    1E-3 0.1 10 1000

    1E-3 0.1 10 1000

    1E-3 0.1 10 1000Time, hr

    Model WT Match

    Kazemi et al, 201142

  • PLT Predictions

    Kazemi et al, 201143

  • Aternative match option

    Kazemi et al, 201144

  • Applied a new modelling strategy based on PODS Porosity Defined System for a carbonate reservoir.

    The effect of horizontal and vertical correlation length of PODS observed on WT response.

    Matching WT and PLT data in sector before going to full field modelling

    Sector model and full field model compare well

    WT and PLT Calibration of full field model

    Reasonable match achieved without incorporating any fractures

    H Field study conclusions

    45

  • SPE 166033: Using Near Wellbore Upscaling to Improve Reservoir Characterization and

    Simulation in Highly Heterogeneous Carbonate Reservoirs

    V. Chandra1,2, S. Geiger1,2 , P.W.M. Corbett1,2,4,R. Steele3, P. Milroy3 , A. Barnett3 , P. Wright3 , P. Jain3

    1Institute of Petroleum Engineering, Heriot-Watt University2International Centre for Carbonate Reservoirs

    3BG Group, Reading, U.K.4 Universidade Federal do Rio de Janeiro

    Acknowledgements:46

  • Key points of this research

    47

    Overall aim Using novel near wellbore upscaling (NWU) workflow to obtain

    improved permeability model of Field G

    Main conclusions Improved characterisation of key small-scale geological

    heterogeneities

    Revised permeability model eliminated the K-multipliersScientific impact Improved reservoir characterisation and simulation of

    carbonates using NWU workflow

    Chandra et al, 2012

  • Low relief anticline trap Thin oil rim, gas cap, deep seated aquifer Main HC bearing layers: Zone A, Zone B

    Field G Background

    E-W section: see gas over oil over water. See the two main reservoir layers (Image courtesy: Zoe Watt)

    48

    A/B Unconformity

    Chandra et al, 2012

  • Field G Simulation Model

    49Chandra et al, 2012

  • Field G Production Profiles: Oil, Gas and Water

    50Chandra et al, 2012

  • Re-evaluating Field G Permeability

    - DST K-transform >> core K-transform

    - Average K in geomodel ~ 20 mD and Ke in simulation model ~ 200 mD

    What was undersampled?How should it be modelled?

    Kh-multiplier required for history match : x20 in Zone A, x10 in Zone BPlus local well K and well PI multipliers

    Around 90% of the permeability missing !?

    Correct the K = Better Simulation Model = Better Production Forecast51

  • Removing the K-multiplier

    Can

    be r

    esol

    ved

    usin

    g re

    vise

    d K-

    mod

    el?

    All K-multipliers removed

    History matched case with K-multipliers

    52Chandra et al, 2012

  • Evaluating the Role of Meteoric Karst vs Burial Corrosion in an Offshore Indian Carbonate Field

    Michael OatesViswa Santhi Chandra

    Patrick Corbett

  • Outline

    Field G overview Evidence of late burial corrosion Impact on poro-perm Key conclusions

    Oates et al, 201254

  • Ramp foraminifera facies

    Depositional Facies

    Coskinolina

    1000 m

    Miliolids

    1000 mCoskinolinids and

    Alveolinids

    1000 m

    Platy corals

    1000 m

    Fine bioclastic Hash with Rotalid forams

    1000 m

    Fine bioclastic Hash with Echinoderm debris

    1000 m

    Nummulitids

    1000 m

    Discocyclinids

    1000 m

    Oates et al, 201255

  • Cold Karst ?Meteoric karstic porosity development caused the

    conduits?

    Diagenesis vs Permeability concepts

    Indication of dissolution porosity

    Solution enhanced stylolitesand associated fractures in well cores

    Evident high perm network, pervasive and stratiform

    Long producing data and tracer data indicating good lateral and vertical communication in reservoir

    The dissolution porosity +stylolites+associated fractures are the pervasive permeability network ?

    Hot Karst ?Late stage (hydro)thermal karstification could have

    formed the conduits?

    Oates et al, 201256

  • Proposed Paragenetic Sequence

    Transpressional tectonics at the end of Miocene

    Early stage extensive microporosityLate stage macroporosity along fractures, unconformities, vertical pipes

    Corrosive fluids penetrated the unloaded dissolution seams and stylolites predating the HC charge

    Unloading event

    Depositional setting:Ramp settingTransgressive stacking patterns

    Cementation+Compaction+Pressure dissolution=

    Very tight carbonate units

    Very common Associated with late

    carbonate cementscalcitedolomiteankeritesiderite

    Dissolution seamsStylolitesTension gashes

    Oates et al, 201257

  • Burial Corrosion- Field Scale

    (Modified from Esteban)Oates et al, 2012

    58

  • Burial Corrosion- Field Scale

    (Modified from Barnett et al . 2010)

    Oates et al, 2012

    59

  • Back to Basics: Key Observations from Core

    Stylolites and associated tension gashesCorrosion enhanced micro- and macro-porosity

    Corroded zone

    Matrix adjacent to corroded zone

    60

  • Post Stylolite Dissolution

    Fine vuggy porosity

    1 cm

    0.5 mm0.5 mm

    Extensive porosity along stylolites and microstylolites

    61

  • Corrosion along Stylolites and SAF

    Corrosion vs Stylolite CorrelationDensity of distribution of corroded zones is proportional to that of stylolites.

    2 cm

    Oates et al, 201262

  • Corrosion fluid front

    Corrosion fluid front

    Invasion of Corrosive Fluids

    Corrosion enhanced porosity

    Corrosion enhanced porosity

    Corrosion enhanced porosity

    Burial Corrosion Mechanism at Core Scale

    Oates et al, 201263

  • Post-Saddle Dolomite Dissolution

    Fractures with leached bladed calcite cement, saddle dolomite and dickite

    Saddle dolomite

    Bladed calcite cement

    Dickite

    Saddle dolomite in a fracture has undergone corrosion followed by dickite precipitation

    Dickite

    Corroded saddle dolomite

    0.5 mm 0.5 mm

    Oates et al, 201264

  • Dissolution of Tectonic Vein-filling Calcite

    Corroded calcite cement in a fracture

    0.5 mm

    Oates et al, 201265

  • Dickite and Pyrite

    Dickite is not common in carbonate reservoirs in general

    BUT it is a very common mineral phase in Field G

    Deeply etched stylolites and associated fractures

    pyrite nodules this size (up to 10mm across) are rare

    Dickite is a kaolin mineral thought to indicate the former activity of organic-rich acidic fluids

    Oates et al, 201266

  • Highlights: Diagenetic Features

    2 cm

    (Courtesy Paul Wright )

    Oates et al, 201267

  • Key Observations from Core

    Key Characteristics of Corroded Zones:

    - Higher porosity

    - Higher mini-perm

    - Dark patches of highly conductive zones on image logs

    - High Uranium signature

    R1= unmodified limestone matrixR2= corroded matrix

    Oates et al, 201268

  • Corrosion Enhanced Porosity

    Collapse breccia porosityVuggy/Moldic porosityCorrosion along Stylolites and SAF

    BSEM images of typical corroded matrix with microporosity

    2 cm

    Oates et al, 201269

  • Reservoir Permeability Issues

    - DST K- transform >> core K- transform

    - Average K in geomodel ~ 20 mD and Ke in simulation model ~ 200 mD

    What was undersampled?How should it be modelled?

    Core and miniperm data

    Sample insufficiencySample bias towards tighter zones

    K-multiplier required for History match :

    x20 in A Zone x10 in B Zone Plus local well K and well PI multipliers

    Around 90% of the permeability missing !?

    Correct K = Better Simulation Model = Better Production Forecast

    Oates et al, 201270

  • Permeability Model Before and After Considering Corrosion Enhanced Porosity

    Geomodel using core K-transform After incorporating solution enhanced porosity features in the geomodel

    711000

    AFTER K-multiplier

    Geomodel permeability Modified permeability scenario

    100050

  • Simulation results

    72

    Cumulative oil production curves

  • Key Conclusions

    Distribution of high permeable corroded zones correlated with stylolites+fractures

    Evidence supports the occurrence of thermal karstification causing stratiform pervasive high permeable network

    The reservoir permeability model should be improved with considerations to late burial corrosion

    Oates et al, 201273

  • Near wellbore rock-typing and upscaling

    Chandra et al, 201474

    m-mm cm-dm m-km

  • 75

    Core vs upscaled permeability

    Corroded matrix porosity

    Leached stylolites and tension gashes in highly Corroded matrix

    Chandra et al, 2014

  • Poro-perm trends used for GeoPoDS

    Chandra et al, 201476

  • GeoPoDS saturation-height curves

    77

  • Near-wellbore upscaled permeability

    GeoPoDS J functions

    Improved RQI

  • GeoPoDS water-oil relative permeability

  • GeoPoDS gas-oil relative permeability

  • GeoPoDS summary

    GeoPoDS NWRT PHIE K-Transform Kv/Kh Sw-H function

    Kr curve

    Shale Shale 0.15 K = 663749*(PHIE)5.5071 y = 8E-07*(Kh)2 + 0.0016*(Kh)+ 0.878

    G2 G2

  • Now History match

    Chandra et al, 201482

  • Triple Porosity Systems

    Indian FieldN African Field

    No Fractures Needed in the Models for Reasonable History Matching

    Chandra et al, 2014Kazemi et al, 2011

    83

  • Field G Conclusions

    Mismatch between geological model and reservoir simulation modelled resolved

    Finer detail petrophysics Very high resolution NWB model Upscaled Rock Types ( GeoPODS) Improved History Match (without tuning) No significant fractures

    apart from the stylolite-related fractures that are incorporated in stylolite GeoPOD.

    84

  • Triple Matrix Porosity Systems

    Indian Field GNorth African Field H

    Three RTs only needed in the Models for Reasonable History Matching without need for fracture modelling 85

  • Conclusions

    Missing permeability in carbonates due to biased sampling and missing scale modelling

    Simulation model can show large corrections to geomodels to get history match

    Identifying key (3?) RT variations and upscalingthese can lead to improved history matching

    Use of upscaled RTs enabled through NWB modelling

    Consider Triple Matrix Porosity (GeoPODS) for heterogeneous reservoir models

    86

  • Acknowledgements Total Professorship (1994-2011) BG Group Professorship (2012-2017) Colleagues

    Sebastian Geiger, Alireza Kazemi Students

    Viswasanthi Chandra International Centre for Carbonate Reservoirs

    DynaCARB Project Schlumberger (Ecplise), Geomodelling (SBED),

    CMG (CMOST, IMEX )

    87

  • Fractured Reservoir Myths

    Majority of fractures have a high angle origin but only to bedding (Lewis, HWU) Is use of curvature good OK for thinly bedded systems (Couples, HWU) Is fracture porosity always low (1-2%) yes generally but not always (Quenes,

    Sigma3) is the fractal model a good one there are length scales, layering and the

    mechanical stratigraphy is important (Couples, HWU; Riva GE Plan), Mechanical fractures follow existing fracture patterns (Alverellos, Repsol) Thermal Fracturing in low permeability rocks also high permeability sandstones

    (Tovar, IES) Continuum fracture models vs Discrete Fracture models upscaling DFN is very

    challenging (Geiger, HWU) There is no REV in fractured reservoirs except possibly at the seismic bin scale

    (Quenes, Sigma3) and at the bed scale (Couples, HWU; Riva GEPlan) Basement provide seals and migration barriers but not if fractured (Hartz, Det

    Norske Oljeselskap) Ruger equation can give fracture orientation and density simple laboratory

    models show this equation sometimes holds (Chapman, Edinburgh University)

    Source: EAGE-SBGf Fracture workshop Rio Nov 201388

  • Fracture Reservoir Agreement

    Fractures are difficult to locate but easy to predict with the correct structural model (Lewis, HWU)

    Fracture Models should be driven by data and concepts (Riva, GE Plan)

    Fractures develop though complex history of burial and many stress episodes(Bezerra, UFRN; Betotti (TUDelft)

    Lithology and facies have an impact on fracture distributions (Cazarin, Petrobras)

    Need to model fractures in 3D (Hartz, Det Norske Oljeselskap; Moos, Baker-Hugues)

    A multidisciplinary approach to tackle fractures is necessary

    Source: EAGE-SBGf Fracture workshop Rio Nov 201389

  • All reservoirs are fractured!

    What Gary Couples and I can agree on: We think all carbonates are fractured, but the

    fractures MAY not be playing a major role in flow

    So All reservoirs are fractured and some fractures are useful for flow

    And Sometimes reservoirs that appear fractured may actually have very high matrix contrasts

    90

  • ReferencesChandra, Corbett, Hamdi and Geiger, 2011, Improving Reservoir Characterisation and Simulation with Near Well boremodelling, SPE 148104, SPE Reservoir Characterisation and Simulation Conference, 9-11 October, Abu Dhabi.

    Kazemi, Corbett, and Wood, 2012, New approach for geomodeling and dynamic calibration of carbonate reservoirs usingporosity determined system (PODS). Presented at 74th EAGE conference and Exhibition, Copenhagen, Denmark, 4-7 June2012.

    Chandra, Geiger, Corbett, Steele, Milroy, Barnett, Wright, Jain, 2012, Using Near Well Bore Upscaling to improve reservoircharacterisation and simulation in highly heterogeneous carbonate reservoirs, SPE 166033, SPE Reservoir SimulationConference

    Oates, Chandra, and Corbett, 2013, Evaluating the role of meteoric karst vs burial corrosion in an offshore IndianCarbonate Field, AAPG

    Chandra, Corbett, Hamdi, and Geiger. 2013. Improving Reservoir Characterisation and Simulation with Near-WellboreModeling. SPE Res Eval & Eng 16 (2): 183-193. SPE-148104-PA. May.

    Chandra, V., Steele, R., Milroy, P., Corbett, P.W.M. and Geiger, S. 2013b. Using near-wellbore modelling and dynamiccalibration to improve permeability modelling in a giant carbonate field. Oral presentation at 75th EAGE Conference &Exhibition incorporating SPE EUROPEC 2013, TU 14 15

    Chandra, Wright, Barnett, Steele, Milroy, Corbett, Geiger and Mangione, 2014, Evaluating the Impact of a Late BurialCorrosion Model on Reservoir Permeability and Performance in a Mature Carbonate Field Using Near Wellbore Upscaling,Geol Soc Spec Publication Fundamental Controls on Fluid Flow in Carbonates: Current Workflows to EmergingTechnologies (Paper accepted for publication)

    91