Refracture Reorientation

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    FAST FAST 

    Project #3

    Refracture Reorientation inLenticular Reservoirs

    Daniel Benedict

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    Outline

    Resume` Reorientation theory

    Objectives Background odeling

    !e"t stes

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    Researcher Biograhy

    $ometo%n& Longmont' (O B)*c) in Petroleum +ngineering

    from (* in ,--, (ordillera +nergy Partners

    .ssociate +ngineer / (olorado

    Baker $ughes 0nte1 L2D2D +ngineer 4 5ulf ofe"ico

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     6heory of Reorientation

    Revie% reorientation

     6%o tyes of reorientationoccur 0mmediate stress 7eld changes

    through fracture and closure *tress 7eld changes over time

    through ressure dra%do%n

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    Reorientation methods

     6he ounds e"eriment8oschovidis' et al' ,---9

    0mmediate reorientation 2ilco" sandstone.toka shale

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    Reorientation methods

    :rom oschovidis' et al' ,---

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    Reorientation methods

     6he reservoir stress 7eld is alteredthrough the roduction of oil andgas over time)

     6he coinciding ore ressure droincurred in the reservoir %illchange the local e;ective stress7eld of the reservoir' making

    refracturing ossible)

     

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    Reorientation methods

    0n tight sands' theroduction comesfrom an ellitical

    area around thefracture

    +ncounter byassed

    ay that the ellisedoes not roduce

    Image Source: Devon Energy Corporation “Mid-ear !peration" Report and arnett S$a%e Sc$oo%&' () *+, ())(

    $ttp:media.corportate-ir.netmedia/fi%e"a"edvnpre"entation"ne0pre"S%ide1).jpg

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    Reorientation methods

    :ractureroagatesuntil virgin

    ressure>one isreached

    0mage *ource& Devon +nergy (ororation ?id/ @ear Oerations Reort and Barnett *hale*chool'A ,- C! ,--,' htt&media)corortate/ir)netmedia7lesasedvnresentationsne%res*lideE-)jg

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    Reorientation methods

    2hat if this henomenaoccurs in lenticular reservoirsF

     6his roject acts on theassumtion that reorientationhas occurred' and studies itsincremental bene7ts

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    Objectives

    *imulate roduction oflenticular sands that haveundergone fracture

    reorientation

    Perform sensitivity studies onthe inut arameters andanaly>e the results

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    Lenticular Reservoirs

    2hy lenticular reservoirsF

     6hese study areas have beenfocused on blanket/tyemarine sands

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    Lenticular Reservoirs

    :luvial sands have far less areale"tent' and in some cases' like inthe Piceance and 5reen River'

    micro/Darcy ermeability

    5reat verticallateral

    discontinuity Do%nsaced to G- acres in some

    areas

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    Lenticular Reservoirs

    Image Source: 2uu"raa& 4.5.& “Produced Ma""ive%y Staced 6enticu%ar Sand" of Co%orado7" Piceance a"in&'

    8a"9IPS& Spring ;;

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    Lenticular Reservoirs

    5eologic .dvantages *tress 7eld alignment Directional ermeability Reoriented fractures %ould cross

    direction of highest ermeability

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    Lenticular Reservoirs

    5eologic 1uestions !atural fractures

    Deletion Damage from stress changes Refracturing to ossibly energi>e

    matri"

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    Lenticular Reservoirs

    >igure (: 6oren?& *.C.& et al .:'>racture C$aracteri"tic" and Re"ervoir e$avior of Stre""-Sen"itive >racture Sy"tem" in

    >%at-6ying 6enticu%ar >ormation"&' paper SPE @(== pre"ented at t$e +nconventiona% 8a" 9ec$no%ogy

    Sympo"ium& 6oui"vi%%e& 2entucy& 1-( May ;1A.6auBac$& S.E.:'5ttriBute" of fracture net0or" in "e%ected

    Cretaceou" "and"tone" of t$e 8reen River and San *uan a"in"&' Geological studies relevant to horizontal drilling:

    examples from western North America& Rocy Mountain 5""ociation of 8eo%ogi"t"& Denver& Co%orado ;;( A-

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    odeling

    (5 0+H simulator 5C0 interface

    Direct editing through )dat 7le as

    %ell Po%erful' yet ainless .ble to model naturally fracId

    reservoirs

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    odeling

    (5 Builder 5rid otions PJ6 roerties

    5as2ater model otion

    Rel Perm' non/Darcy Ko% 2ell events

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    odeling

    :irst stes 0ntroduce a fracture to the

    system (onstruct a cruciform fracture

    set in the reservoir Build fracture model at other

    angles ermeability' transmissibility

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    odeling isstes

    M!DE6 C!MPRESS.PSI

    P!R!SI9&

    PERM& MD 5RE5& 5CRES

    >R5CF56>-

    6E,89F&>9

    a"e   3*10^-6 0.12 0.02 80 500

    Cruciform   3*10^-6 0.12 0.02 80 500

    =@G a"e   3*10^-6 0.12 0.02 80 500

    =@G 6entic.   3*10^-6 0.12 0.01 33 250

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    odeling

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    odeling

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    odeling

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    odeling

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    odeling

    Project %asnIt 1uite thatsimle

    *o began the rocess ofre7nement and matching

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    odeling 2ith Lessistakes

    M!DE6 P!R& >R5CP!R&

    M59RIHPERM&

    MD

    >R5CPERM& MD

    E>>.PERM&

    MD

     5RE5& 5CRES

    E66I,DEH

    Hf& >9

    a"e   0.10 .00234 0.008 10000 2.63 40 263 250

    Cruciform   0.10 .00234 0.008 10000 2.92 40 293 250

    3)GJorigina%   0.10 .00234 0.008 10000 3.49 40 350 500

    3)GJorigina%   0.10 .00234 0.008 10000 2.92 20 758 250

    3)GJorigina%   0.10 .00234 0.008 10000 2.92 10 758 250

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    odeling

    Di;erent reservoircharacteristics for lenticularsands are being e"amined)

    ultile aroaches tried'%hich 0 %ill discuss)

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    odeling

    Original model contained onelayer

    :racture' matri" in the samesace

    Problems encountered in griddingnon/orthagonal fractures 6ransmissibility introduced

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    odeling

    Dual Porosity modelintroduced :lo% occurred from fracture to

    fracture and matri" to fractureonly

    Cnderrediction of recovery

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    odeling

    :inally' Dual Permeabilitymodel alied to scenarios atri"/atri" :lo% atri"/:racture :lo% :racture/:racture :lo%

    !atural :racture system

    introduced

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    odeling

    !atural fractures in the dualermeability model

    :racture system and matri"system oerate concurrently' butsearately' in the same sace'

    and on di;erent lanes' %ithindeendent arameters)

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    odeling

    2ith the natural fracturesystem' ermeability needs tobe scaled do%n)

    0n the (5 soft%are

     e;  =  frac M Nfrac total

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    odeling

    Nfrac = Jtf   Jbulk Jtf = Lres M $res M 2res M 82nf nf sacing9

    Jhf 

    :or simulation Jnf = 833IMGEIM33I9M8)--GQ-ISI9 Jnf = 3QS3)3S ftT3

    Jbulk = G)UQEGQMG-TS ftT3

    Nfrac = )--,3 JhfJbulk

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    odeling

     frac = G- Darcies to simulatein7nite conductivity

    :cd = 2fMf fmMHf  :or simulation

    :cd = 8)GMG-9 8EMG-T/Q M ,U-9 :cd = U-- /V essentially in7nite

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    odeling

    .dditional Parameters

    2ell 0nde"' M20 20 = 8,WMkMhM%frac9

    8L!8ReR%9*9 Re=geofacM8.reaPWM%frac9T)U

    2frac=GX geofac=)3SX skin=-

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    odeling

    . semi/analytical solution hasalready been develoed to testnumerical solutions for an

    in7nite/slab reservoir' 8(raig',--Q9)

    0n7nite conductivity desirable foreasiest match %ith analyticalsolution

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     6he *cenarios

    . %orking model is in lace' 0am adjusting sensitivities forthe follo%ing arameters&

    .sect ratios !umber of fractures :racture orientation :racture half/length :racture conductivity Reservoir area

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    ultile fracs' year ,

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    *ingle frac' year ,

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    ultile fracs' year 3

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    *ingle :rac' year 3

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    (omarison after G-years

    M!DE6 5rea&acre"

    8a"produced&

    mm"cf 

    8a"remaining&

    mm"cf 

    E>>.PERM&

    MD

    E66I,DEH

    Hf& >9

    Sing%e >rac   10 136.01 42.344 2.92 758 500

    3)GJorigina%   10 147.29 31.061 3.49 906 500

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    U-- foot fracture' year ,

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    ,U- foot fracture' year ,

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    U-- foot fracture' year 3

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    ,U- foot fracture' year 3

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    (omarison after G-yearsM!DE6 5rea&

    acre"8a"

    produced&mm"cf 

    8a"remaining&

    mm"cf 

    E>>.PERM&

    MD

    E66I,DEH

    Hf& >9

    3)GJorigina%   10 147.029 31.061 3.49 906 500

    3)GJorigina%   10 143.73 34.496 2.92 758 250

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    (ruciform fracture' year,

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    3-Y fracture' year ,

    if f

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    (ruciform fracture' year3

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    3-Y fracture' year 3

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    (omarison after G- years

    M!DE6 5rea&acre"

    8a"produced&

    mm"cf 

    8a"remaining&

    mm"cf 

    E>>.PERM&

    MD

    E66I,DEH

    Hf& >9

    ;)GJorigina%   40 536.23 892.17 2.92 293 250

    3)GJorigina%   40 461.67 966.06 2.92 293 250

    ,U- f t f t -

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    ,U- foot fracture' -acres

    ,U- f t f t ,-

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    ,U- foot fracture' ,-acres

    ,U- f t f t G-

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    ,U- foot fracture' G-acres

    ( i ft G-

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    (omarison after G-yearsM!DE6 5rea&

    acre"8a"

    produced&mm"cf 

    8a"remaining&

    mm"cf 

    E>>.PERM&

    MD

    E66I,DEH

    Hf& >9

    3)GJorigina%   40 461.67 966.06 2.92 293 250

    3)GJorigina%   20 239.13 117.79 2.92 758 250

    3)GJorigina%   10 143.73 34.496 2.92 758 250

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    .nisotroy' G&G

    i

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    .nisotroy' G&G-

    i --

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    .nisotroy' G&G--

    ( i ft G-

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    (omarison after G-yearsM!DE6 5rea&

    acre"8a"

    produced&mm"cf 

    8a"remaining&

    mm"cf 

     5ni"otropy E66I,DEH

    Hf& >9

    3)GJorigina%   10 143.73 34.496 1:1 758 250

    3)GJorigina%   10 155.54 22.623 1:10 758 250

    3)GJorigina%   10 156.42 21.795 1:100 350 250

    ( l i

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    (onclusions

    Refracture reorientation hasbeen theori>ed' studied insimulation' and roved ossible

    Reorientation in lenticularreservoirs has not been studied

     6he model has been enhanced

    to simulate changes in reservoirvariables

    ( l i

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    (onclusions

    :inal analysis is under%ay

    !umerical.nalytical resultse"ected shortly

    (riteria for selectioncandidates %ill be discussed

    6i li

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     6imeline

     

    January2006

    May2006

    January 2007 May2007

    Literature

    Review

    Preliminary X X X X XModeling

    - -- X XX XSensitivity

    Studies X XX XProject

    Completion

    [uestions and

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    FAST

    [uestions and(omments

    F