SC RE Chap9 Permeability Variations

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    Permeability - Its variationsPermeability - Its variations

    Adrian C Todd

    Heriot-Watt UniversityHeriot-Watt University

    DEPARTMENT OF PETROLEUM ENGINEERING

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    Introduction

    Seldom is a homoeneous roc! encountered"

    Reser#oir o$ten contains distinct units or

    la%ers o$ #ar%in roc! &ro&erties"

    Permea'ilit% is not necessaril% the same in alldirections"

    Permea'ilit% is anisotropic"

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    Introduction

    In sedimentar% roc!s #ertical &ermea'ilit% is less than

    hori(ontal &ermea'ilit%

    )ori(ontal &ermea'ilit% in the &rinci&al directions ma%

    also 'e di$$erent On reser#oir scale* thin strea!s o$ lo+ &ermea'ilit%

    material can reduce #ertical &ermea'ilit% to a lo+er #alue

    than roc! measurements miht indicate"

    Core anal%sis re&resents a microsco&ic scale +hereas

    +ell testin re&resents a macroscale 'eha#iour

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    ,ariation in

    Permea'ilit%

    Measurements $rom

    Mini-&ermeameter on

    sam&le $rom Leman

    Gas Field .U/0

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    ,ariation in Permea'ilit%

    ,ariation in a core can 'e

    considera'le The local &ro&erties re$lect the

    de&ositional &rocess o$ a

    considera'le &eriod

    Con#entional core anal%sis

    sam&le at 1 core &er $oot"

    A +ell test can re$lect

    &ermea'ilit% o#er tens o$ $eet"

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    A#erae Permea'ilit%

    Pro'a'le a#erae o$ a heteroeneous s%stemtends to+ards eometric mean"

    ( )navg 1 2 3 nk k k k ....k =

    ( )navg 1 2 3 nk k k k ....k =

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    A#erae Permea'ilit% - 2eds in Parallel-

    )ori(ontal s%stem re$lects sedimentar% nature o$

    roc!s

    Reason $or a#erae &ermea'ilit% is to rationalisesmall core sam&les +ith those measured at +ell test

    le#el"

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    2eds in Parallel-

    Linear $lo+A#erae &ermea'ilit% $romDarc%3s La+

    T 1 2 3Q Q Q Q= + +

    ( )1 1 1 21

    k A P PQ

    L

    =

    ( )i 1 2T

    A P PQ k

    L

    =

    ( ) ( ) ( )1 1 1 2 2 2 1 2 3 3 1 2T

    k A P P k A P P k A P PQ

    L L L

    = + +

    i i

    i

    k AkA

    =

    i i

    A

    i

    k hk

    h

    =

    Commonl% used to a#erae

    core anal%sis &ermea'ilities"

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    2eds in Parallel-Radial Circular $lo+

    Case o$ se#eral la%ers$lo+in simultaneousl% in a+ell

    ( )i i e wi

    e

    w

    2 h k P PQ

    r

    ln r

    =

    ( ) ( )( )T e w e w

    i 1 1 2 2 3 3e e

    w w

    2 h k P P 2 P PQ Q k h k h k h

    r rln lnr r

    = = = + +

    i i

    T

    h kk

    h

    = The #alue to 'e com&ared

    throuh +ell $lo+ tests

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    2eds in Series-

    Linear $lo+ Reser#oir ma% ha#e 'een$olded or $aulted"

    )ori(ontal la%ers no+#ertical"

    A#erae &ermea'ilit%o'tained '% addin&ressure dro& across each'ed"

    ( ) ( ) ( ) ( )1 4 1 2 2 3 3 4P P P P P P P P = + +

    ( ) 31 2 11 41 1 2 2 3 3 1

    Q LQ L Q L Q LP P

    k A k A k A kA

    = + + =

    i

    i

    Lk

    L

    k

    =

    This is the harmonic average

    permeability

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    2eds in Series-Radial

    $lo+ Natural #ariations in

    &ermea'ilit%" 4ell 'ore damae"

    Cleanin techni5ues"

    In6ection &rocesses

    ( )2 e 12

    e

    1

    2 k h P PQ

    rln

    r

    =

    ( )1 1 w1

    1

    w

    2 k h P PQ

    rln

    r

    =

    ( )avg e wT

    e

    w

    2 k h P PTotal flow: Q

    rln

    r

    =

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    2eds in Series-Radial $lo+

    ( ) ( ) ( )e w e 1 1 w

    Total pressure drop: P P P P P P = +

    e 1eT 12

    w w1

    avg 2 1

    r rrQ ln Q lnQ ln

    r rr

    2 k h 2 k h 2 k h

    = +

    T 1 2At steady state flow: Q Q Q= =

    e 1e

    w w1

    avg 2 1

    r rrln lnlnr rr

    k k k= +

    e

    wavg

    1 e

    w 1

    1 2

    rln

    rkr r

    ln lnr r

    k k

    =

    +

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    Modellin )eteroeneous S%stems

    Permea'ilit% #ariations can o$ten 'e traced $rom +ell

    to +ell"

    These #ariations ena'le a la%ered reser#oir s%stem to

    'e de#elo&ed

    Man% $ield demonstrate this la%erin"

    ,er% lare &ermea'ilit% #ariations

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    E7am&le o$ North Sea Field

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    Modellin )eteroeneous S%stems

    In some cases not &ossi'le to correlate &ermea'ilities $rom +ell

    to +ell"

    More di$$icult to &ut toether a reser#oir model "

    Modellin reser#oirs +ith a#erae &ro&erties can onl% 'e #alid i$8

    Reser#oir sands are homoeneous

    Random #ariations occur across sands

    Ordered distri'utions in one +ell do not correlate +ith other

    +ells"

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    Modellin

    )eteroeneous

    S%stems Permea'ilit% #ersus

    de&th used to 'e

    &resented on a lo-

    &ermea'ilit% de&th scale"

    Such a re&resentation

    can lead to misleadin

    #alues $or a#erae

    &ermea'ilit%

    Average permeability ?

    True permeability

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    Modellin4ater$loods

    -homoeneous

    #ersus la%ered"

    Process8

    4ater in6ected intoreser#oir to maintain

    &ressure"

    Good mo'ilit% ratio

    Piston li!e

    dis&lacement

    rw w

    ro o

    k !

    "o#ility $atio% " 1k !

    =

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    Modellin 4ater$loods -homoeneous s%stem

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    Modellin4ater$loods

    -homoeneous

    s%stem

    4ater 'rea!thouh

    Oil &roduction until

    'rea!throuh

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    Modellin 4ater$loods -la%ered s%stem

    La%ered &ermea'ilit% #ariations included in the model"

    Reservoir model includes thickness

    and rock properties of each layer

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    Modellin 4ater$loods -la%ered s%stem

    Water moving through high permeability layer

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    Modellin 4ater$loods -la%ered s%stem

    Water breakthrough after 1!! days

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    Modellin4ater$loods

    -la%ered

    s%stem

    Impact of gravity drainage

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    Modellin

    4ater$loods-la%ered s%stem

    "ottom of reservoir

    being s#ept by #ater

    due to gravity drainage

    Top of reservoir still

    contains oil at

    original saturation$

    Termed %attic oil&

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    Modellin 4ater$loods

    -la%ered s%stem' pro(ect not as attractive as1' simulation

    Water breakthrough in half the

    time$

    )eed for #ater treatment

    earlier

    *il recovery at

    breakthrough much less

    +uch longer times to reach

    lo#ere recoveries

    ,o#er vertical permeabilies

    make the case #orse

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    Modellin 4ater$loods -la%ered s%stem

    arly breakthrough

    Need to im&act hih &ermea'ilit% some distance into

    $ormation"

    Time settin &ol%mers are a serious consideration"

    Technical challenes and ris!s in their a&&lication"

    Attic oil?

    Gra#it% sereation"

    Use o$ lo+ densit% $luid" E"" Nitroen

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    La%ered Rese#oirs

    La%ered reser#oirs result $rom the de&ositional

    &rocess"

    Understandin the de&ositional &rocess can i#e

    insiht to the reser#oir enineerin im&lications"

    No+ more acti#it% o$ the interation o$ eoliicalscenarios and the de#elo&ment o$ realistic reser#oir

    simulation models"

    U&scalin* is no+ an interal &art o$ realistic model

    de#elo&ment

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    Im&act o$ Permea'ilit% Distri'ution on

    Dis&lacement Processk

    '

    .uper-homogeneous

    k

    '

    Worst case

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    Im&act o$ Permea'ilit% Distri'ution on

    Dis&lacement Processk

    'Tunnel

    k

    'Random

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    Characteristics o$ Reser#oirs +ith )ih

    Permea'ilit% Contrast 4ater $lo+s &re$erentiall% do+n hih &ermea'ilit% sections" Premature +ater 'rea!throuh"

    De$erment o$ oil &roduction"

    Ca&illar% &ressure e$$ects onl% enhance #ertical s+ee& e$$icienc%

    slihtl%"

    Not &er$oratin hih &ermea'ilit% sections has little success due to

    ra#it% $orces etc" 4ater $inds its +a% into hih &ermea'ilit% areas"

    Li$e o$ $ield loner than oriinal estimates on homoeneous

    &ro&erties"

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