buckles plot

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Buckles Method used for estimation of Permeability

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    "Something hidden.

    Go and find it.Go and look behind the Ranges

    Something lost behind the Ranges.

    Lost and waiting for you. Go!"

    Rudyard Kipling - The Explorer

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    Using Buckles Plots to Aid Log

    Analysis

    By Kenneth Chaivre

    Wednesday June 25, 2008

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    PROBLEMS WITH ROUTINE LOG

    ANALYSIS

    High Sw wells may produce gas with very little or nowater

    Low Sw wells produce water or fail to produce.

    Similar looking wells produce differently. Leads to Changing m and n

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    Review of R. S. Buckles Paper - 1965

    Part of Volumetric Calculation is * (1-SW) * (1-SW) = *SW Buckles showed that * SW irr is a constant

    ( * SW is the Buckles Number

    or Bulk Volume Water)

    For Hand Calculations Constant is a quick andeasy way to calculate * (1-SW)

    Showed that * SW is related to grain size.

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    BUCKLES PLOT

    Transition

    SWirrTransition

    Low Perm

    High Perm

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    Parameters for Plot

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    BVW vs Grain Size and Lithology

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    Uses of the Buckles Plot

    Identify Swirr Zones for Analysisi.e. Calculate Capillary Pressure

    Identify One Type of Low Resistivity Pay Identify Stratigraphic Flow Units

    Environments of Deposition

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    Calculations with Swirr If Swirr is Known and

    If Permeability (k) can be estimated thenCapillary Pressure (Pc) can be estimated

    Pc= (19.5*Swirr^-1.7)*(k/100*Phie)^-0.45

    Height Above Free Water (H) can becalculated

    H= (.35 for gas)*(Pc)

    H= (.7 for medium oil) * (Pc)

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    Capillary Pressure

    Pore Throat Radius (r) can be calculated r = (108.1) / Pc

    Winland

    r35 Valuesdelineate commercial

    hydrocarbon reservoirs

    R35= 5.395 * ((K^0.588)/(100*PHIE^0.864))

    R35 < 0.5m (microns)Tight

    R35 > 0.5m (microns)Will Flow

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    BUCKLES IN PRACTICE

    DEPTH TO FREE WATER

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    Structure Carthage CVS G

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    ZONES SELECTED FOR H free water

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    MAUDE #13

    ZONES FOR DEPTH TO FREE WATER

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    RESULTS OF DEPTH TO FREE

    WATER

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    FREE WATER - CVS G

    200 400 FT DOWNDIP

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    Low Resistivity Pay Zones

    very fined grained rocks have high boundwater

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    ASHTON 2 UNIT #10 CVS F

    ASHTON 2 UNIT #10 CVS F

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    ASHTON 2 UNIT #10 CVS F

    BUCKLES

    BVW 0.049

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    RESULTS - 677mcf & 8.6 bw

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    STARR CO - FROST FIELD

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    STARR CO-VXBG

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    STARR CO - VXBG

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    STARR CO VXBG - NOT PERFD

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    STARR CO VXBG NOT PERFD

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    IDENTIFY FLOW UNITS

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    PETER 2 UNIT #10 CVS F

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    PETER 2 UNIT #10 CVS F

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    COTTON VALLEY FIELD

    Webster Parish, Louisiana

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    FIRST BANK OF PD - S Sarepta Field

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    FIRST BANK OF PD

    17 BCF

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    CLEMONS UTZ GRAY

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    CLEMONS UTZ GRAY

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    CLEMONS 1STGRAY

    CLEMONS 1ST GRAY

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    CLEMONS 1STGRAY

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    CLEMONS - UTZ VS 1STGRAY

    UTZ 1STGRAY

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    CLEMONS 3RD GRAY

    Thin Beds

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    CARTHAGE FIELD

    ENVIRONMENTS OF DEPOSITION

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    CARTHAGE - TYPE LOG

    Porosity PHI vs. Water Saturation Sw - Cotton Valley Sand Zone C,D,F,G

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    5%

    6%

    7%

    8%

    9%

    10%

    11%

    30% 35% 40% 45% 50% 55% 60% 65% 70% 75%

    Pay Avg Water Saturation Sw, %

    PayAvgPorosityPHI,%

    PHI vs. Sw -CVC PHI vs. Sw - CVG

    PHI vs. Sw - CVF PHI vs. Sw - CVD

    From Xindi Wang

    CARTHAGE CVS G St t

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    CARTHAGE CVS G Structure

    CARTHAGE BVW G with Structure

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    CARTHAGE BVW G with Structure

    Blue

    0.02 Red

    0.04

    Late Cotton Valle Time

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    Late Cotton Valley Time

    Cotton Valley SandWave reworked

    deltaic shoreline.

    Fine grained

    argillaceoussandstones

    CARTHAGE BVW G with Structure

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    CARTHAGE BVW G with Structure

    Blue

    0.02 Red

    0.04

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    MAUDE #4 LOG

    MAUDE #4

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    MAUDE #4

    CALLOW #9 LOG

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    CALLOW #9 LOG

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    CALLOW #9

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    MAUDE #4 CALLOW #9

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    CVS G Qgas vs BVW

    BVW

    Qgasfrom

    Production LogsFewer points

    Channel? Inarea of poorer

    production.

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    RESULTS IN CARTHAGE FIELD

    Perfing more and better zones

    Better Frac and completion techniques

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    Qgas vs Time

    Q t Ti

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    Qwtr vs Time

    TIME VS BW/MCF

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    TIME VS BW/MCF

    CONCLUSIONS

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    CONCLUSIONS

    Useful in Establishing Capillary Pressureo Use several equations to find depth to free water

    Differentiate Between Zones that Look Alikeon Logs but Produce Differently.

    o Help Establish Sw Cutoffso Different Rocks need Different Cutoffs

    Suggests Environment of Deposition

    Makes You Ask Questions

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    REFERENCES Buckles, R. S., 1965, Correlating and Averaging Connate Water Saturation

    Data: The Journal of Canadian Petroleum Technology, v. 5, p.42 -252

    Aguilera, R., 2002, Incorporating capillary pressure, pore throat aperture radii,height above free-water table and Winland r35 values on Pickett plots: AAPGBulletin V86 No. 4 p. 605-624

    Doveton, J. H., 1994, Graphical Techniques for the Analysis and display ofLogging Information: Chapter 2 Vol CA 2: p 23-46 Geologic Log Analysis Using

    Computer Methods

    Doveton, J. H., 1999, Integrated Petrophysical Methods for the Analysis ofReservoir Microarchitechurea Kansas Chester Sandstone Case Study: AAPG1999 Midcontinent Section, Transactions, Geoscience for the 21stCentury

    PfEFFEER Concepts: http://www.kgs.ku.edu/Gemini/Help/Pfeffer-theory

    Asquith, G. and Gibson C., 1983, Basic Well Log Analysis for Geologists: p.98

    http://www.kgs.ku.edu/Gemini/Help/Pfeffer-theoryhttp://www.kgs.ku.edu/Gemini/Help/Pfeffer-theoryhttp://www.kgs.ku.edu/Gemini/Help/Pfeffer-theoryhttp://www.kgs.ku.edu/Gemini/Help/Pfeffer-theory
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    THANKS

    Xindi Wang Christy Demel Pat Noon

    Matt Pickrel Randy Nesvold

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    QUESTIONS