Presion Capilary Historia de La Saturacion

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    Capillary Pressure andSaturation History

    Capillary Pressure in

    Reservoir Rock

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    DRAINAGE AND IMBIBITION

    CAPILLARY PRESSURE CURVES

    Drainage

    Imbibition

    Swi Sm

    Sw

    Pd

    Pc

    0 0.5 1.0

    Modified from NExT, 1999, after

    DRAINAGE

    Fluid flow process in which the saturationof the nonwetting phase increases

    IMBIBITION

    Fluid flow process in which the saturationof the wetting phase increases

    Saturation History - Hysteresis

    - Capillary pressure depends on both directionof change, and previous saturation history

    - Blue arrow indicates probable path from

    drainage curve to imbibition curve at Swt=0.4- At Sm, nonwetting phase cannot flow,resulting in residual nonwetting phasesaturation (imbibition)

    - At Swi, wetting phase cannot flow, resulting inirreducible wetting phase saturation (drainage)

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    Saturation History

    The same Pc value can occur at more than

    one wetting phase saturation

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    Rock Type

    Rock Type (Archies Definition - Jorden and Campbell)

    Formations that ... have been deposited under similar

    conditions and ... undergone similar processes of laterweathering, cementing, or re-solution....

    Pore Systems of a Rock Type (Jorden and Campbell)

    A given rock type has particular lithologic (especially pore

    space) properties and similar and/or related petrophysical andreservoir characteristics

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    Thomeers Parameters for

    Capillary Pressure Curves Thomeers Data

    Mercury Injection - drainage

    Very high capillary pressures

    (Vb)P The (assymptotically approached) fraction of bulk

    volume occupied by mercury at infinite capillary pressure

    (similar to previous parameter, irreducible wetting phase

    saturation)

    Pd Displacement Pressure, capillary pressure required to

    force nonwetting phase into largest pores (same aspreviously discussed)

    G Parameter describing pore-size distribution (similar to

    previous parameter, 1/. Increasing G (or decreasing ),

    suggests poor sorting, and/or tortuous flow paths)

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    Modfied from Jordan and Campbell, 1984, vol. 1

    Figures 2.4 and 2.5

    PT = PORE THROATP - PORE

    (Vb)p =is the fractional volume occupied by Hg atinfinite pressure, or total interconnected pore volume.

    pdis the extrapolated Hg displacement pressure (psi);pressure required to enter largest pore throat.

    Gis pore geometricalfactor; range in size and

    tortuosity of pore throats.

    Large pd= small pore thorats

    Large G= tortuous, poorlysorted pore thorats

    .

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    7/16Modfied from Jordan and Campbell, 1984, vol. 1

    Note variation in pore properties and permeability within a formation

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    Modfied from Jordanand Campbell,

    1984, vol. 1

    Figure 2.8

    size: lower finesorting: verywell sorted

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    Modfied from Jordan

    and Campbell, 1984, vol. 1

    Figure 2.9

    size: lower finesorting:moderately

    sorted

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    Modfied from Jordan

    and Campbell, 1984, vol. 1

    Figure 2.10

    size: uppervery finesorting:

    moderatelysorted

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    Modfied from Jordan

    and Campbell, 1984, vol. 1

    Figure 2.11

    -effect ofsignificantcementing

    and clay

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    Modfied from Jordanand Campbell, 1984, vol. 1;after Neasham, 1977

    Figure 2.12

    Effect ofDispersed Clays

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    Capillary Pressure in Reservoirs

    A B

    Reservoir, o

    Aquifer, w1

    2

    3

    Pc = po-pw = 0

    Pressure

    Depth

    dpw=wg/D dh

    Free

    WaterLevel

    dpo=og/D dh

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    Fluid Distribution in Reservoirs

    Gas & Water

    Gas density = g

    Oil, Gas & Water

    Oil & Water

    Oil density = o

    Water

    Water density = w

    A

    h1

    h2B

    Free Oil Level

    Free Water Level

    Capillary pressure differencebetween

    oil and water phases in core APc,ow= h1g(w-o)

    Capillary pressure differencebetween

    gas and oil phases in core BP

    c,go= h

    2g(

    o-

    g)

    Modified from NExT, 1999, modified after Welge and Bruce, 1947

    Fault

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    RELATION BETWEEN CAPILLARY

    PRESSURE AND FLUID SATURATION

    Free Water Level

    Pc

    PdOil-Water contact

    Hd

    Heig

    htAboveFreeWaterL

    evel(Feet)

    0 50 100Sw(fraction)

    0 50 100

    Sw(fraction)

    0

    Modified from NExT, 1999, after

    Pc

    0 50 1000

    Pd

    Sw(fraction)

    Lab Data

    -Lab Fluids: ,

    -Core sample: k,

    J-Function

    J-Function

    - for k,

    Reservoir Data

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    Saturation in

    Reservoir vs. Depth

    Results from two

    analysis methods (after ABW)

    Laboratory capillary

    pressure curve

    Converted to reservoir

    conditions

    Analysis of well logs Water saturation has

    strong effect on resistivity

    curves (future topic)