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International Journal of Greenhouse Gas Control 28 (2014) 25–34 Contents lists available at ScienceDirect International Journal of Greenhouse Gas Control j ourna l h o mepage: www.elsevier.com/locate/ijggc Comparison of different methods for determining key parameters affecting CO 2 storage capacity in oil reservoirs Changlin Liao a,b,, Xinwei Liao a , Xiaoliang Zhao a , Hongna Ding a , Xiaopeng Liu c , Yongge Liu a , Jing Chen a , Ning Lu a a Petroleum Engineering Department, China University of Petroleum, Beijing, People’s Republic of China b PetroChina Research Institute of Petroleum Exploration and Development, Beijing, People’s Republic of China c Geological Exploration and Development Research Institute of CNPC, Chuanqing Drilling Engineering Company Limited, Chengdu, Sichuan, People’s Republic of China a r t i c l e i n f o Article history: Received 9 November 2012 Received in revised form 9 June 2014 Accepted 10 June 2014 Available online 28 June 2014 Keywords: Storage capacity Determination methods Oil reservoirs Stepwise regression Carbon sequestration a b s t r a c t Storing CO 2 in oil reservoirs is not only an effective method for reducing CO 2 emissions and greenhouse effects, but also a means to be more economical by enhancing oil recovery. The evaluation of CO 2 storage capacity in oil reservoirs which is very important for the implementation of CO 2 storage includes the evaluation of theoretical, effective, practical and matched storage capacities. Based on the volumetric balance theory, considering CO 2 dissolved in remaining oil and water, sweep efficiency and displacement efficiency, this paper utilizes three methods to calculate theoretical and effective CO 2 storage capacity in oil reservoirs, in which CO 2 volumetric sweep efficiency, oil recovery factor and sequestration factor are key parameters. This work presents a reservoir numerical simulation method, an empirical formula method, and a stepwise regression method. The feasibility, superiority and limitations of the methods for calculating these three key parameters and storage capacities including theoretical and actual CO 2 storage capacities were analyzed through simulated applications in three reservoirs of the Xinjiang Oilfield of China. The results indicated that the assessment results of stepwise regression has a high level of accuracy, and that this oilfield can provide a large storage capacity and is thereby worthy of further study. © 2014 Elsevier Ltd. All rights reserved. 1. Introduction The underground storage of carbon dioxide (CO 2 ), i.e., car- bon sequestration, is a promising method to reduce greenhouse gas emission. Many international institutions have been investing resources to evaluate geological CO 2 storage potential. There are five major geological systems that have been identified as the most promising targets for CO 2 storage: oil and gas reservoirs, saline for- mations, un-minable coal areas, shale, and basalt formations (IPCC, 2005). After significant exploration and development, oil reservoirs have been better characterized, which makes the estimation of CO 2 storage capacity in oil reservoirs simpler and more straightforward than in other geologic formations in normal situations. Corresponding author at: China University of Petroleum-Beijing, Mail Box 269, Changping, Beijing 102249, People’s Republic of China. Tel.: +86 010 8973 3223; fax: +86 010 8973 3223. E-mail address: [email protected] (C. Liao). Based on the volumetric balance theory, the fundamental assumption made in storage capacity calculations is that the vol- ume previously vacated by liquid recovery is fully available for CO 2 storage (Stevens et al., 2001; Bachu and Shaw, 2003). The Carbon Sequestration Leadership Forum (CSLF) presented a method to cal- culate theoretical storage capacity based on this assumption. The calculation is shown by Eq. (1) (CSLF, 2007). The volume of injected water, aquifer influx and produced water were considered in this equation. M CO 2 t = CO 2 r × [R fl × A × h × × (1 S wi ) V iw + V pw ] (1) The United States Department of Energy applied another method to calculate CO 2 theoretical storage capacity, based on CO 2 enhanced oil recovery theory and volumetric balance theory. The general form of the volumetric equation to calculate CO 2 theoreti- cal storage capacity in oil reservoirs is shown by Eq. (2) (Goodman et al., 2011). Table 1 summarizes the terms shown in Eqs. (1) and (2). M CO 2 t = CO 2 s × A × h × × (1 S wi ) × B o × E oil (2) http://dx.doi.org/10.1016/j.ijggc.2014.06.010 1750-5836/© 2014 Elsevier Ltd. All rights reserved.

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  • International Journal of Greenhouse Gas Control 28 (2014) 2534

    Contents lists available at ScienceDirect

    International Journal of Greenhouse Gas Control

    j ourna l h o mepage: www.elsev ier .com/ locate / i jggc

    Comparison of different methods for determiningaffectin

    Changlin ingXiaopenga Petroleum En ab PetroChina Re of Chinc Geological Ex CompPeoples Repub

    a r t i c l

    Article history:Received 9 NoReceived in reAccepted 10 June 2014Available online 28 June 2014

    Keywords:Storage capacityDetermination methodsOil reservoirsStepwise regreCarbon seques

    ly an onom

    capacity in oil reservoirs which is very important for the implementation of CO2 storage includes theevaluation of theoretical, effective, practical and matched storage capacities. Based on the volumetricbalance theory, considering CO2 dissolved in remaining oil and water, sweep efciency and displacementefciency, this paper utilizes three methods to calculate theoretical and effective CO2 storage capacityin oil reservoirs, in which CO2 volumetric sweep efciency, oil recovery factor and sequestration factorare key parameters. This work presents a reservoir numerical simulation method, an empirical formula

    1. Introdu

    The undbon sequesgas emissioresources tve major gpromising tmations, un2005). Afterhave been bstorage capthan in othe

    CorresponChangping, Befax: +86 010 8

    E-mail add

    http://dx.doi.o1750-5836/ ssiontration

    method, and a stepwise regression method. The feasibility, superiority and limitations of the methodsfor calculating these three key parameters and storage capacities including theoretical and actual CO2storage capacities were analyzed through simulated applications in three reservoirs of the XinjiangOileld of China. The results indicated that the assessment results of stepwise regression has a high levelof accuracy, and that this oileld can provide a large storage capacity and is thereby worthy of furtherstudy.

    2014 Elsevier Ltd. All rights reserved.

    ction

    erground storage of carbon dioxide (CO2), i.e., car-tration, is a promising method to reduce greenhousen. Many international institutions have been investingo evaluate geological CO2 storage potential. There areeological systems that have been identied as the mostargets for CO2 storage: oil and gas reservoirs, saline for--minable coal areas, shale, and basalt formations (IPCC,

    signicant exploration and development, oil reservoirsetter characterized, which makes the estimation of CO2acity in oil reservoirs simpler and more straightforwardr geologic formations in normal situations.

    ding author at: China University of Petroleum-Beijing, Mail Box 269,ijing 102249, Peoples Republic of China. Tel.: +86 010 8973 3223;973 3223.ress: [email protected] (C. Liao).

    Based on the volumetric balance theory, the fundamentalassumption made in storage capacity calculations is that the vol-ume previously vacated by liquid recovery is fully available for CO2storage (Stevens et al., 2001; Bachu and Shaw, 2003). The CarbonSequestration Leadership Forum (CSLF) presented a method to cal-culate theoretical storage capacity based on this assumption. Thecalculation is shown by Eq. (1) (CSLF, 2007). The volume of injectedwater, aquifer inux and produced water were considered in thisequation.

    MCO2t = CO2r [Rfl A h (1 Swi) Viw + Vpw] (1)

    The United States Department of Energy applied anothermethod to calculate CO2 theoretical storage capacity, based on CO2enhanced oil recovery theory and volumetric balance theory. Thegeneral form of the volumetric equation to calculate CO2 theoreti-cal storage capacity in oil reservoirs is shown by Eq. (2) (Goodmanet al., 2011). Table 1 summarizes the terms shown in Eqs. (1) and(2).

    MCO2t = CO2s A h (1 Swi) Bo Eoil (2)

    rg/10.1016/j.ijggc.2014.06.0102014 Elsevier Ltd. All rights reserved.g CO2 storage capacity in oil reservoirs

    Liaoa,b,, Xinwei Liaoa, Xiaoliang Zhaoa, Hongna D Liuc, Yongge Liua, Jing Chena, Ning Lua

    gineering Department, China University of Petroleum, Beijing, Peoples Republic of Chinsearch Institute of Petroleum Exploration and Development, Beijing, Peoples Republic ploration and Development Research Institute of CNPC, Chuanqing Drilling Engineeringlic of China

    e i n f o

    vember 2012vised form 9 June 2014

    a b s t r a c t

    Storing CO2 in oil reservoirs is not oneffects, but also a means to be more ec key parameters

    a,

    aany Limited, Chengdu, Sichuan,

    effective method for reducing CO2 emissions and greenhouseical by enhancing oil recovery. The evaluation of CO2 storage

  • 26 C. Liao et al. / International Journal of Greenhouse Gas Control 28 (2014) 2534

    Table 1Parameters for theoretical storage capacity estimation published in references.

    Parameter Units Description

    MCO2 t kg Theoretical storage capacityCO2r kg/m

    3 CO2 density under reservoirconditions

    R m3/m3 Total oil recovery factor onreservoir volume basis

    A m2 Oil reservoir areah m Oil reservoir thickness m3/m3 Oil reservoir porositySwi m3/m3 Initial water saturationViw m3 Cumulative volume of injected

    water and aquifer inuxVpw m3 Cumulative volume of

    produced waterCO2s kg/m

    3 CO2 density under standardconditions

    Bo standard m3/reservoir m3 Oil formation volume factorEoil m3-CO2/m3-OOIP Storage efciency factor that is

    derived from local CO2enhanced oil recovery (EOR)experience or reservoirsimulation, as the ratio ofstandard cumulative volume ofCO2 to standard volume oforiginal oil-in-place

    Others (Shaw and Bachu, 2006; Shen and Liao, 2009; Brennanet al., 2010to differentwere based

    In this volumetric implementjiang oilelcapacity calcalculated wto the Xinjiprovides a Xinjiang oil

    2. Calculat

    The techage capacit

    Fig. 1. Techno2007).

    There are four types in the pyramid theoretical, effective, practi-cal and matched storage capacities, and each of them is a subset ofthe previous one except theoretical capacity. The theoretical stor-age capacity (Bachu et al., 2007) represents the physical limit thatthe geologipyramid. Thacquired bying) cutoff concentratesome introare based obubble poinpore space

    The volulate storage2007). Howwater of thin the stora2002), was study, the Cby using ththe remain

    2.1. Calcula

    The theoree p2 disn in Fal poty. Aase ing opartsthat

    calchown

    the free-oirs ig ovmulaiginacurac) presented a number of various methods according reservoir development characteristics, but all of them

    on the volumetric balance theory.paper, CO2 dissolved in remaining oil and water,sweep efciency and displacement efciency were

    ed according to the development characteristics of Xin-d in China, while using theoretical and effective storageculations. The three key parameters Rf, Ef and SCO2 wereith three different methods, which have been applied

    ang oileld for storage capacity calculations. The workreference for the feasibility study of CO2 stored in the

    reservoirs.

    ion of storage capacity

    no-economic resource-reserve pyramid for CO2 stor-y (CSLF, 2005; Bachu et al., 2007) is shown in Fig. 1.

    into thand CO(showthe totcapacifree-phremainswept water

    Thewere ssum ofof the reservoodinthe cuand orthe ac-economic resourcereserve pyramid for CO2 storage capacity (CSLF,

    the storageoil reservoi(4), and theand (6) areremaining oinators of rand PWIP +priate methoil and watand they arfore, it is asremaining osweep efc

    MCO2t = MfMfree-phase C

    MCO2 in swep

    MCO2in sweptc system can accept, and it occupies the entire resourcee effective storage capacity (Bachu et al., 2007) can be

    applying a range of technical (geological and engineer-limits in a storage capacity assessment. This paper will

    on the theoretical and effective storage capacities withduction to their calculation methods. The calculationsn the assumption that reservoir pressure is above thet pressure of crude oil, and only oil and water in thewithout free gas.metric balance theory is commonly adopted to calcu-

    capacity (Bachu and Shaw, 2003, 2005; Bachu et al.,ever, the effect of CO2 dissolved in the remaining oil ande storage capacity, which is considerable and essentialge capacity calculation (Enick and Klara, 1990; Kovscek,not been taken into consideration in their studies. In thisO2 storage capacities of oil reservoirs were calculatede volumetric balance theory, and the CO2 dissolved ining oil and water was considered.

    tion of theoretical storage capacity

    retical storage capacity in oil reservoirs can be dividedarts: free-phase CO2, CO2 dissolved in the remaining oil,solved in the remaining water. The rectangular sketchesig. 2-12-3) are adopted to present the components ofre volume (entire rectangle) in the theoretical storagefter CO2 ooding, the total pore volume is lled withCO2, remaining oil and water. And the volume of theil and water are composed of two parts: swept and un-. In this way, the CO2 dissolved in the remaining oil andhad been swept by CO2 was considered.ulation model is shown by Eqs. (3)(6). The terms that

    in Eqs. (3)(6) are summarized in Table 2. Eq. (3) is thethree parts of the storage capacity. The storage capacityphase CO2 (Eq. (4)) is a derivation of Eq. (1). Most oiln the Xinjiang oileld have been developed by waterer a long period of time. The historical data such astive volume of injected water, produced water and oil,l oil-in-place are incomplete, which signicantly affectsy of the CO2 storage capacity calculation. Therefore,

    capacity is estimated based on the present situation ofrs. Therefore, the present oil-in-place is adopted in Eq.

    present water-in-place is adopted in Eq. (5). Eqs. (5) the storage capacities that CO2 dissolved in the sweptil and water respectively. The sweep efciency denom-emaining oil and remaining water are POIP (1 Rf)

    Viw Vpw respectively. However, there are no appro-ods to obtain the sweep efciencies of the remaininger. The two sweep efciency may have the same values,e near to the overall volumetric sweep efciency. There-sumed that the values of the sweep efciencies of theil and water are equal to that of the overall volumetriciency.

    ree-phase CO2 + MCO2 in sweptoil + MCO2 in sweptwater (3)

    O2 = CO2r[Rf POIP Viw + Vpw] (4)

    toil = CO2r Ef POIP (1 Rf ) mCO2 in oil (5)

    water = CO2r Ef (PWIP + Viw Vpw) mCO2 in water(6)

  • C. Liao et al. / International Journal of Greenhouse Gas Control 28 (2014) 2534 27

    Fig. 2. Rectangular sketches for showing the components of the total pore volume. Fig. 2-1 shows thecomponents of pore volume after CO2 ooding, Fig. 2-3 shows the components of the swept pore vovolume for effective storage capacity after CO2 ooding. The entire outer rectangle represents the tofree-phase CO2, remaining oil and water after CO2 ooding. Both the remaining oil and water were costorage capacity is part of the volume of the free-phase CO2, the swept remaining oil and the swept rem

    mCO2 inoil is calculated by Eqs. (7)(9) (Xue et al., 2005).

    mCO2 in oil =KP

    1 + KP44xTMave

    (7)

    ln K = 773.247 1T 273.15 18.5898 (8)

    = 0.00008286(T 273.15) 0.7287 (9)The mCO2 in water can be determined by the estimation model

    (Duan and Sun, 2003). This model was based on a specic particle

    Table 2Parameters for theoretical storage capacity estimation.

    Parameter Units Description

    Mfree-phase CO2 kg Mass of free-phase CO2MCO2 in sweptoil kg Mass of CO2 dissolved in the swept

    remaining oilMCO2 in sweptwater kg Mass of CO2 dissolved in the swept

    remaining waterRf m3/m3 Oil recovery factor from CO2

    ooding, dened as the ratio ofcumulative volume of produced oilto present oil-in-place (POIP)

    POIP PWIP Ef

    mCO2 in oil

    mCO2 in water

    K P osxT

    Mave

    T Swp

    Rw

    interactionequation ofwith tempefrom 0 to 2

    It was asvoir in this CO2 oodintinuous COsubstituted

    Mfree-phase C

    MCO2 in swep

    2.2. Estima

    Many pacapacity, sureduce the would mak

    tical 3 andore v4, the vo

    A calachu

    = Cmlculaubstim3 Present oil-in-placem3 Present water-in-placem3/m3 Overall volumetric sweep

    efciency, dened as the ratio ofswept pore volume to total porevolume

    m3-CO2/m3-oil CO2 solubility in oil at reservoirpressure and temperature

    m3-CO2/m3-H2O CO2 solubility in water at reservoirpressure and temperatureEquilibrium constant

    106 Pa Oil reservoir pressure(kg/m3 Oil density at standard condition

    theoreFig. 2-total pFig. 2-all threwater.CSLF (B

    MCO2e

    A caafter skg/kg Weight fraction of hydrocarboncomponents in oil

    kg/kg The secondary dissolvingcoefcient that indicates thedissolving capacity of CO2 in themixture composed of hydrocarboncomponents and CO2

    g/mol Average molecular weight ofhydrocarbon in oil

    K Oil reservoir temperaturem3/m3 Present average water saturation

    over entire pore volumem3-H2O/m3-PWIP Water recovery factor which is the

    ratio of the volume of waterproduced after CO2 ooding tovolume of the presentwater-in-place

    (12). DetailAppendix.

    MCO2e = C

    SCO2 = Ce

    Sfree-phase CO

    SCO2 in swept

    SCO2 in swept components of pore volume before CO2 ooding, Fig. 2-2 shows thelume after CO2 ooding, Fig. 2-4 shows the components of the poretal pore volume, including POIP and PWIP before CO2 ooding andmposed of swept and un-swept parts. The pore volume for effectiveaining water.

    theory for the liquid phase and a highly accurate state for the vapor phase, and has a broad applicationrature ranges from 0 C to 260 C and pressure ranges00 MPa.sumed that there was no aquifer beneath the oil reser-paper. The volume of injected and invaded water beforeg is not considered, and the method is limited to con-2 ooding, so Viw is zero. Thus, Eqs. (4) and (6) can be

    by Eqs. (10) and (11) respectively.

    O2 = CO2r POIP Rf + PWIP Rw (10)

    twater = CO2r Ef (PWIP Vpw) mCO2 in water(11)

    tion of effective storage capacity

    rameters out of considered in the theoretical storagech as buoyancy, mobility ratio and heterogeneity, couldpore volume available for CO2 storage (IPCC, 2005). Ite the effective storage capacity inevitably less than thestorage capacity. The rectangular sketches (shown in

    2-4) are adopted to illustrate the components of theolume in the effective storage capacity. As shown in

    e pore volume for effective storage capacity is part oflumes: the free-phase CO2, the swept remaining oil andculation of effective storage capacity was introduced by

    et al., 2007):

    Cb Ch Cw Ca MCO2t = Ce MCO2t (12)tion method for effective storage capacity is generatedtuting the results of Eqs. (3), (5), (10) and (11) into Eq.

    ed derived steps for Eqs. (13)(17) are shown in the

    O2r A h (1 Swp) SCO2 (13)

    (Sfree-phase CO2 + SCO2 in sweptoil + SCO2 in sweptwater)(14)

    2= Rf +

    Swp1 Swp Rw (15)

    oil = Ef (1 Rf ) mCO2 inoil (16)

    water = Ef Swp

    1 Swp (1 Rw) mCO2 in water (17)

  • 28 C. Liao et al. / International Journal of Greenhouse Gas Control 28 (2014) 2534

    Table 3Parameters for effective storage capacity estimation.

    Parameter Units Description

    MCO2e kg CmCbChCwCaCe

    SCO2SCO2 displaceSCO2 in oilSCO2 in wate

    The storstorage capshown in Eq

    2.3. Determ

    Rf, Ef andof theoreticcapacities, them.

    2.3.1. NumThe num

    method. Thinclude setreservoir mhistory maadopted toing CO2 storeservoirs a

    Numericestimation be chosen treservoir grwell trajectical dynamdata can offor the calcsituations, tpresented i

    2.3.2. EmpiThe thre

    empirical fotionship (Stprojects (Fiaccording tThe SCO2 cations, the w(Rice, 2007

    Rw =Swp

    where t is p

    2.3.3. StepwMathem

    sion methothe functiodent param

    Fig. 3. Oil recovery empirical relationship (Stevens et al., 1999).

    eters Rf, Ef and SCO2 were obtained from conceptual mod-numerical reservoirs which are established with differentndent parameters including permeability, heterogeneity,uration, uid mobility, injection and production pressures,oir pressure, and injection time. The stepwise regression wasd to establish the relationship between the dependent andndent parameters. This method will be helpful for evaluatingorage capacity in oil reservoirs.

    basic conceptual model for the numerical reservoir waserted pattern, including four production wells and a centralon well. Each grid block measured 25 m 25 m 2 m, overire grid of 37 25 5 cells. Top depth and reservoir temper-ere 1980 m and 335.3 K, respectively. Relative permeability

    are shown in Fig. 4. The three-parameter PengRobinsonon of state was used for ash calculation. Different concep-odels with different independent parameters of a numerical(kg-CO2-effective)/(kg-CO2-theoretical)(kg-CO2-effective)/(kg-CO2-theoretical) (kg-CO2-effective)/(kg-CO2-theoretical) (kg-CO2-effective)/(kg-CO2-theoretical) (kg-CO2-effective)/(kg-CO2-theoretical) (kg-CO2-effective)/(kg-CO2-theoretical)

    m3-CO2/m3-POIPm3-CO2/m3-POIP m3-CO2/m3-POIP

    r m3-CO2/m3-POIP

    age factor SCO2 from Eq. (14) reects the effective CO2acity in oil reservoir. Table 3 summarizes the termss. (12)(17).

    ination of key parameters

    SCO2 are the three key parameters for the calculational (Eqs. (3)(6)) and effective (Eqs. (13)(17)) storageand these three methods are introduced to determine

    erical reservoir simulationerical reservoir simulation is a mature and acceptede steps to establish a numerical reservoir simulationting up a geological model, establishing a numericalodel, and adjusting parameters of rock and uid throughtching. The Eclipse software (Schlumberger Ltd.) was

    establish a numerical model for accurately simulat-rage conditions, and the numerical models of three oilt the Xinjiang oileld were used.al reservoir simulation is considered as a very reliablemethod for reservoir development. Certain data shouldo establish an actual numerical reservoir model, such asid, earth coordinates of production and injection wells,ory, log interpretation, well test, well measures, histor-ic and other relevant data. For some oil reservoirs, thisten be difcult to obtain, which represents a challengeulation of the three parameters. Consequently, in somewo additional methods of parameter determination aren Sections 2.3.2 and 2.3.3.

    rical formulae key parameters Rf, Ef and SCO2 can be obtained byrmulae. The Rf can be obtained from an empirical rela-evens and Kuuskraa, 1999) derived from seven eld EORg. 3). At the Xinjiang oileld, Ef was assumed to be 0.58,o CO2 ooding that adopted by 2D visible experiment.n be calculated by Eqs. (14)(17). Among these equa-ater recovery factor Rw can be estimated by Eq. (18)

    paramels of indepeoil satreservadopteindepeCO2 st

    Thean invinjectithe entature wgraphsequatitual m).

    Rf (1 Swp) 1.8149912 10144e(665492.66)/t

    , (18)

    roduction time, year.

    ise regressionatics and statistics were used in the stepwise regres-d (Zhu, 2012). It has been widely adopted to establishnal relationship between the dependent and indepen-eters so as to analyze experimental data. Dependent

    reservoir wnumerical r

    The indeoil saturatireservoir pdimensionlparametersin the dimvertical andation coefof the permto characteEffective CO2 storage capacityCapacity coefcient effected by mobilityCapacity coefcient effected by buoyancyCapacity coefcient effected by heterogeneityCapacity coefcient effected by water saturationCapacity coefcient effected by aquifer strengthEffective capacity coefcient that incorporates thecumulative effects of all the other parametersStorage factorStorage factors for the free-phase CO2 in pore volumeStorage factors for CO2 dissolved in remaining oilStorage factors for CO2 dissolved in remaining waterere expressed using the basic conceptual model of aeservoir.pendent parameters, i.e., permeability, heterogeneity,on, uid mobility, injection and production pressures,ressure, and injection time were transformed to beess. The dimensionless equations of the independent

    are shown in Table 4. Table 5 summarizes the termsensionless equations. The permeability ratio between

    horizontal permeability (kv/h) and permeability vari-cient (Vk) were used to characterize the heterogeneityeability. The oilCO2 mobility ratio (Mog ) was adoptedrize the mobility of CO2 in the reservoir. Because the

  • C. Liao et al. / International Journal of Greenhouse Gas Control 28 (2014) 2534 29

    Fig. 4. Curves tive p

    Table 4The dimension

    Equations

    Kv/h = kv/khSop

    Mog =korgo

    korog

    Vk =

    PinjD = Pinj/PMPpD = Pp/PMMPrD = Pr/PMMtD = Vinj/POIP

    Table 5Parameters for

    Parameter

    kvkhkorgkoroo

    g

    hi

    kiPinjPMMPpPrVinj

    miscibility miscible presure, injectiThe dimenscumulativedimensionl

    BoxBehintroduced

    Table 6The values of d

    Levels

    Low IntermediateHigh of wateroil and gasoil relative permeability. Fig. 4-1 is the curves of wateroil rela

    less equations and denitions of the independent dimensionless parameters.Deni

    Ratio Presen

    Mobil

    n

    i=1ki(n

    i=1hiki/n

    i=1hi1)n

    i=1hi1

    2

    /

    (n

    i=1

    hiki/

    ni=1

    hi 1

    )Perme

    M DimenDimenDimen

    Dimen

    the dimensionless equations.

    Units Description

    m2 Vertical permeabilitym2 Horizontal permeabilitym2/m2 End-point relative permeability of CO2m2/m2 End-point relative permeability of oilPa s Oil viscosity at reservoir pressure and

    temperaturePa s CO2 viscosity at reservoir pressure and

    temperaturem Thickness of layer i, subscript i is the

    layer numberm2 Permeability of layer iPa Bottom hole injection pressurePa Minimum miscible pressurePa Bottom hole production pressurePa Average reservoir pressurem3 Cumulative volume of injected CO2 at

    reservoir pressure and temperature

    between CO2 and crude oil is determined by minimumssure, the dimensionless parameters of reservoir pres-on pressure and production pressure were introduced.ionless injection time tD was used to characterize the

    volume of injected CO2. The values of the independentess parameters are shown in Table 6.nken design (BBD) (Box and Behnken, 1960) wasto design the experiment. BoxBehnken experimental

    design is an(low, intermparameter tions are at that a BBD nexperimentcontained eparameter formed by E

    The stepparametric

    y = C0 +n

    i=

    The moparametersone througshown as fo

    Y =

    y1

    y2

    ...

    ym

    imensionless independent parameters corresponding to the three levels.

    Kv/h Sop Mog Vk

    0.1 0.40 27.5 0.05 0.55 0.55 51.75 0.455

    1 0.70 76.0 0.86 ermeability, and Fig. 4-2 is the curves of gasoil relative permeability.

    tions

    of vertical permeability to horizontal permeabilityt oil saturation, (1 Swp)ity ratio of CO2 displacing oil

    ability variation coefcient (Liu et al., 1993)

    sionless injection pressuresionless production pressuresionless reservoir pressuresionless injection time

    independent quadratic design requiring three levelsediate and high) for each independent dimensionless

    so as to capture quadratic effects. Treatment combina-midpoints of the process space, which essentially meansever uses all the extreme values at the same time. Theal design included 120 groups of simulations, whichight independent dimensionless parameters with each

    having three levels. All the simulation runs were per-clipse.wise regression method (Zhu, 2012) was applied in

    regression to establish the estimation model shown by

    1

    aixi +ij

    bijxixj +n

    i=1cix

    2i (19)

    del included multinomial and random error of the. This non-linear model can be converted into a linearh parameters substitution. The converted equation isllows:

    , X = (xij)mp, e =

    e1

    e2

    ...

    em

    , =

    1

    2

    ...

    p

    (20)

    PinjD PpD PrD tD

    1.21 0.61 0.89 0.21.305 0.705 0.985 0.71.40 0.80 1.08 1.2

  • 30 C. Liao et al. / International Journal of Greenhouse Gas Control 28 (2014) 2534

    Fig. 5. Relation graphs of predicted values and actual values. Fig. 5 1Fig. 5-3 are the relation graphs oThe straight lines in the gures represent places where predictive values are equal to actual values. Thepredicted and the actual values.

    Eq. (20) can be expressed by Eqs. (21) and (22).

    Y = X + e (21)

    Q () =m

    j=1

    Table 7Parameters fo

    Parameter

    y C0ai , bij , cixi , xj

    Y y1, y2 ,. . ., ymm X xijn p

    e e1 , e2 , . . ., em 1 , 2 , . . ., pQ()

    When Qthe regressregression cin Eqs. (19)

    = (X Y)1

    Ef anas thnt dimeter evel pwis

    Rf = 0.70 kv/h

    + 0.0 0.2

    1.8 228

    Ef = 1.25 kv/h+ 0.3 0.3

    0.3 .609SCO2 = 0. 52So

    + 0.0 + 0.

    + 0.1 82(Vordinith

    5. Thted v, the[yi (1xi1 + 2xi2 + + pxip)]2 (22)

    r stepwise regression.

    Description

    Rf, taken pendeparamicant lthe ste

    66 + 0.2716PinjD 0.1468kv/h Sop + 0.001151kv/h Mog + 0.07318

    4611 kv/h tD + 0.8285Sop PpD + 0.1237Sop tD 0.2110Vk PinjD

    66(Sop 0.3794)2 0.7967(Vk 0.7191)2 0.00001665Mo2g 0.2

    8 0.2471kv/h Sop + 0.002169kv/h Mog + 0.1172kv/h Vk 0.3054359Sop tD + 0.001323Mog PinjD 0.2372Vk PinjD 0.2563Vk tD +

    416(kv/h 1.158)2 0.7520(Sop 0.3967)2 0.00003974Mo2g 06575 0.3143kv/h Sop + 0.1564kv/h tD 0.003718Sop Mog + 0.4601081 Mog Vk + 0.001024Mog tD 0.1993Vk PinjD 0.5189Vk tD410 PpD tD 0.1665(kv/h 1.057)2 1.729(Sop 0.6120)2 0.61

    Accpared win Fig. predicguresDependent parametersA constantRegression coefcientsIndependent parameters, i and j are the order number ofthe parameters, and i /= jMatrix of dependent parametersDependent parametersThe number of simulationsMatrix of independent parametersIndependent parameters or their combinationsthe number of independent parameters (x), n = 8The number of independent parameters and theircombinationsMatrix of random errorsRandom errorsMatrix of multinomial coefcientsMultinomial coefcientsSum of squared errors of each parameter

    matched, a0.9519, resptions obtainestimate Rfsionless paused withinvalues of sovariation teobtained ushave been awith differeence of Pinjcorrespond

    Rf, Ef anobvious at f predicted values and actual values for Rf , Ef and SCO2 respectively.se lines were used as the standard to measure matching between the

    () was at its minimum, the corresponding would beion coefcient. When X was a non-singular matrix, theoefcient was as follows. Table 7 summarizes the terms(23).

    X Y (23)

    d SCO2 obtained from the performed simulations weree dependent parameters. It is assumed that the inde-ensionless parameter would not affect the dependent

    when the signicant level is very low. The least signif-of p = 0.05 was used. Rf, Ef and SCO2 were calculated bye regression method. The equations are as the follows:

    Vk 0.2682kv/h PinjD606Vk tD 0.1629(kv/h 1.622)2

    P2pD 0.4109(tD 1.087)2

    (24)

    PinjD + 0.1702kv/h tD503PinjD tD + 0.07813PrD PpD6(Vk 0.8701)2 0.5066(tD 0.4603)2

    (25)

    p Vk 0.3406Sop PinjD4828PinjD tD

    k 0.6091)2 0.2247t2D

    (26)

    g to the above equations, predicted values were com-actual values to acquire their relational graphs, as showne straight lines in the gures represent places where thealues are equal to the actual values. As shown in those

    predicted and actual values of Rf, Ef and SCO2 are well

    nd their correlation coefcients are 0.9538, 0.9411 andectively. This demonstrates that the established equa-ed by the stepwise regression method can be used to, Ef and SCO2 . It should be pointed out that the dimen-rameters are limited in ranges. The correlations can be

    the ranges. Further studies need to be conducted if theme dimensionless parameters are beyond ranges. Thendency of Rf, Ef and SCO2 with different parameters areing the three equations. As shown in Fig. 6, four graphsdded to show the variation tendency of Rf, Ef and SCO2nt Kv/h, Sop, Mog and Vk respectively. Because the inu-

    D, PpD and PrD to Rf, Ef and SCO2 are insignicant, theiring graphs will not be given in this paper.d SCO2 increase with the increase of tD. The growth isthe beginning but the growth tapers off after tD = 0.8

  • C. Liao et al. / International Journal of Greenhouse Gas Control 28 (2014) 2534 31

    Fig. 6. Rf , Ef and SCO2 change with tD with different values of the parameters. Fig. 6 1Fig. 6-4 are the variation tendency of Rf , Ef and SCO2 with different Kv/h , Sop , Mog , Vk

    respectively. And Rf , Ef and SCO2 change with tD .

    Fig. 7. Rf , Ef and SCO2 change with tD with different values of the parameters. Rf and SCO2 are different with that of Fig. 6. The denominators of the new Rf , Ef and SCO2 are alltotal pore volume. Fig. 7-1Fig. 7-4 are the variation tendency of Rf , Ef and SCO2 with different Kv/h , Sop , M

    og , Vk respectively. And Rf , Ef and SCO2 change with tD .

  • 32 C. Liao et al. / International Journal of Greenhouse Gas Control 28 (2014) 2534

    Fig. 8. The abs on trends of the absolute differences respectively. The absolute differencesare the differe nimum values of Kv/h , Sop , Mog and Vk respectively.

    because of increase of In this papeduced oil towhich makpaper is seeratio of cumand reservomiscible precan achieveare still somsuch as homand well shof swept voing. Howevother refereto the usuapresented. recovery is If it is convethe value is

    In ordervalues whicare shown inew Rf andtors are all is higher thcorrelationsare shown iwhich corremum valueRf, Ef and SCences of thewith the incRf, Ef and SCences of thwith the incdecrease w

    3. Exampleoilelds re

    XinjiangAutonomou(Fig. 9). It ilike low perability and

    water in most reservoirs is relatively simple and uid prop-are relatively favorable. The oil is of low density and lowty, and is classied as light oil. The high pressure, low poros-

    permeability and strong heterogeneity make some parts ofeld ee re

    valieters.20, of thlace .253educervo

    106

    e is ndention, umeoir fere ate par

    numegreetersulate2005ptabtainolute differences of Rf , Ef and SCO2 change with tD . Fig. 8 1Fig. 8-3 show the variatint values of Rf , Ef and SCO2 respectively, which correspond to the maximum and mi

    CO2 breakthrough. Rf, Ef and SCO2 increase with theSop, and decrease with the increase of Kv/h, Mog and Vk.r, oil recovery is dened as the ratio of cumulative pro-

    POIP. POIP is often the oil-in-place after water ooding,es it less than OOIP. Therefore, the oil recovery in thismingly higher than the oil recovery that dened as theulative produced oil to OOIP. The injection pressureir pressure in many models are higher than minimumssure. Therefore, most oilCO2 systems in these models

    miscibility which can leads to higher oil recovery. Theree other situations that can achieve higher oil recovery,ogeneous reservoir, low density and viscosity of the oil,ot wells. All these situations can easily lead to increaselume which may further result in oil recovery increas-er, the oil recovery in this paper has rarely been used innces. For comparison, the oil recovery can be convertedl oil recovery. An example of this conversion has beenPOIP is 0.7 times of OOIP after water ooding. The oil0.25 after CO2 ooding, with the denominator of POIP.rted to the oil recovery with the denominator of OOIP,

    70% of the oil recovery, i.e. 0.175. to compare with Ef, Rf and SCO2 were converted to theh the denominators are total pore volume. The trendsn Fig. 7. The overall trends are the same as Fig. 6, but the

    SCO2 are less than the former because their denomina-total pore volume. Ef is higher than Rf and SCO2 . And Rfan SCO2 . In order to analyze the further trends of these, the curves of the absolute differences of Rf, Ef and SCO2n Fig. 8. The absolute differences values of Rf, Ef and SCO2 ,spond to Vk, Kv/h and SCO2 respectively, are the maxi-s. It indicates that the most inuential parameters onO2 are Vk, Kv/h and Sop respectively. The absolute differ-

    three key parameters, corresponding to Kv/h, increase

    oil anderties viscosiity, lowthe oil

    Thrsen toparam0.160cosity of in-pis 335The irrage resis 7.3 reservindepesaturafrom nreservters weof thes

    Thewise rparamto simet al., be acceities obrease of tD, which indicates that the inuence of Kv/h toO2 increase with the increase of tD .The absolute differ-e three key parameters, corresponding to Vk, decreaserease of tD, showing the inuence of Vk to Rf, Ef and SCO2ith the increase of tD.

    storage capacity calculation of Xinjiangservoirs

    oileld is in the northern part of Xinjiang Uygurs Region in China with an area of 13.487 104 km2s a representative oileld characterized with featuresmeability, low porosity, and high pressure. Both perme-porosity show strong heterogeneity. The distribution of

    Fig. 9. Locatiocolored regionThe dashed linborder line of difcult to develop via water ooding.servoirs in Xinjiang oileld (CN, XS and BQ) were cho-date the three methods for estimating the three key. Their locations are shown in Fig. 9. The porosity isand permeability is 4.7 101559.74 1015 m2. Vis-e oil is 1.1 1034.4 103 Pa s. The specic gravityoil is 0.7240.814. The original reservoir temperature51.45 K and its pressure is 20.6 10629.5 106 Pa.ible water saturation ranges from 30.4% to 47%. Aver-ir depth is 22252597.5 m, and the development area39.7 106 m2. Reservoir thickness is 6.910.8 m. Oil7.54 10928.83 109 m3. The average values of thet parameters including permeability, heterogeneity, oiluid mobility and reservoir pressure were obtainedrical reservoir simulations and were used to depict theatures. Then, the independent dimensionless parame-tained through the dimensionless formulae. The valuesameters for the three oil reservoirs are shown in Table 8.erical reservoir simulation, empirical formula and step-ssion methods were used to estimate the three key. The numerical simulation has been adopted widely

    CO2 storage in formations (Kumar et al., 2004; Ozah; Jahangiri and Zhang, 2012), and has been proven tole. Therefore, it is assumed that the CO2 storage capac-ed through the numerical reservoir simulation are then of the three reservoirs (BQ, XS and CN) in Xinjiang oileld. The light- is the uplift belt, and the dark-colored region is the depression belt.e depicts the boundaries of the regions, and the solid line means thethe oileld.

  • C. Liao et al. / International Journal of Greenhouse Gas Control 28 (2014) 2534 33

    Table 8The values of independent dimensionless parameters of example reservoirs in Xinjiang oileld.

    Reservoir kv/h Sop Mog Vk PinjD PpD PrD tD

    BQ 0.1 0.47 41.9 0.28 1.42 0.79 1.01 0.47CN 0.13 0.45 37.4 0.35 XS 0.11 0.56 44.8 0.24

    Table 9Calculated values of the key parameters and their corresponding storage capacitiesusing three different methods for three reservoirs in Xinjiang oileld.

    Reservoir Numericalsimulation

    Empiricalformula

    Stepwiseregression

    Rf , m3/m3 BQ 0.46 0.54 0.49CN 0.52 0.59 0.47XS 0.43 0.49 0.40

    Ef , m3/m3 BQ 0.56 0.58 0.54CN 0.65 0.58 0.70XS 0.59 0.58 0.53

    SCO2 , kg/kg BQ 0.32 0.38 0.35CN 0.41 0.46 0.43XS 0.37 0.42 0.35

    POIP, 109 m3 BQ 28.83 28.83 28.83CN 22.46 22.46 22.46

    MCO2 t , 109 kg

    MCO2e , 109 k

    standard vacapacities olation modeIt shows thacloser to themula. SCO2 imakes CN rcal and effePOIP in genregression mthe numeriative errorseffective stomethod is 3is 4.1218.76.02% and 1method is hthat the stethe CO2 sto

    Fig. 10. Relatiical formula an

    limited. Thethat it has a

    4. Discussi

    Most oilwater oodwater produCO2 in remthe heterogwhich is caciency musmethods ofreservoirs i

    obtacuratparamlabletual

    caperimin. T

    conethoe uti

    the

    clus

    ed otion aininere XS 7.54 7.54 7.54BQ 13.96 15.22 14.59CN 12.99 13.53 12.54XS 3.77 4.03 3.53

    g BQ 5.71 6.78 6.24CN 5.55 6.22 5.91XS 1.70 1.93 1.61

    lues in this paper. The theoretical and effective storagef the reservoirs were estimated according to the calcu-l of CO2 storage capacity. The result is shown in Table 9.t Rf, Ef and SCO2 obtained by the stepwise regression are

    numerical simulation as compared to the empirical for-n CN reservoir is higher than in other reservoirs whicheservoir more suitable for storing CO2. The theoreti-ctive storage capacities of the reservoirs increase witheral. CO2 storage capacities obtained by the stepwiseethod are very close to the results obtained through

    cal simulation. As shown in Fig. 10, most of the rel- of theoretical storage capacity are less than that of

    can beand acthose is avaiconcepstorageon expto obtastrictlysion mit can blacking

    5. Con

    Bascalculain remSCO wrage capacity. The relative error of stepwise regression.089.12%, and that of the empirical formula method5%. The average relative errors of the two methods are0.73%. Therefore, the accuracy of stepwise regressionigher than the empirical formula method. This suggestspwise regression method is more suitable to evaluaterage capacity of Xinjiang oileld when needed data is

    ve errors of the storage capacities of the three reservoirs in the empir-d stepwise regression methods.

    2lation, empused to detison of the numerical rever, it requdata. A reducision of theon experimso, some arbe strictly poor. The sreservoir sitive blocks after whichdoes not reresults are

    Acknowled

    This wogram of ChiNational M006 and 2involved ineditor and t1.32 0.61 0.89 0.611.39 0.72 1.12 0.52

    calculated CO2 storage capacity of the oileld shows very large storage potential.

    on

    reservoirs in Xinjiang oileld have been developed viaing, and most of them are experiencing a stage of highction. To store CO2 in such reservoirs, the dissolution of

    aining oil and water should be considered. Consideringeneity of permeability as well as the gravity separation,used by the density variation of oil and CO2, sweep ef-t be contemplated. In the present work, the calculation

    CO2 storage capacity were based on Rf, Ef and SCO2 of then the Xinjiang oileld. The three key parameters aboveined in different ways. For oil reservoirs with abundante data, the numerical simulation method can determineeters with relatively high precision. When less data

    , the stepwise regression method based on numerical reservoir simulation can be utilized to estimate CO2acity. The empirical formula method is mainly basedental and empirical data, which are sometimes difcultherefore, applicable conditions of this method must besidered before application. Because the stepwise regres-d requires less data and has a wide range of application,lized to predict storage capacity for oil reservoirs when

    required data.

    ions

    n the volumetric balance theory, this work presentedmodels for CO2 storage capacity with the CO2 dissolvedg oil and water considered. In these models, Rf, Ef andthe three key parameters. Numerical reservoir simu-irical formula, and stepwise regression methods wereermine these parameters in the models. After compar-results obtained from the three different methods, theeservoir simulation method is the most reliable. How-ires substantial geological, reservoir and experimentalced amount of data would impact the accuracy and pre-

    results. The empirical formula method is mainly basedental and empirical data. Less data is required, but evene still difcult to acquire. Its applicable condition mustconsidered. And the estimation accuracy is relativelytepwise regression method is based on the numericalmulation method, and only requires small representa-of the oil reservoir to build the numerical simulation

    many parameter values can then be obtained easily. Itquire a substantial amount of data, but the calculationaccurate.

    gements

    rk was supported by the National Basic Research Pro-na (973 program, grant no. 2011CB707302), and Chinese

    ajor Science and Technology Projects (2011ZX05016-011ZX05009-004-001).We are grateful to all staff

    these projects, and also thank the journal associatehe reviewers.

  • 34 C. Liao et al. / International Journal of Greenhouse Gas Control 28 (2014) 2534

    Appendix A

    Detailed derived steps for Eqs. (13)(17)Eqs. (3), (5), (10), (11), (12) are shown as follows:

    MCO2e = Ce MCO2t (12)

    MCO2t = Mfree-phase CO2 + MCO2 in sweptoil + MCO2 in sweptwater (3)

    MCO2 in sweptoil = CO2r Ef POIP (1 Rf ) mCO2 in oil (5)

    Mfree-phase C

    MCO2 in swept

    When Eqequation is

    MCO2t = C+ Ef PO+Ef (P

    where, POIP

    PWIP = A

    PWIP Vpw(The secondCO2 oodin

    The twoEq. (3-1-1)

    MCO2 t = CO2r

    + Ef A

    + Ef (A

    = CO2r A

    + Ef (1

    = CO2r A

    where,

    Sfree-phase CO

    SCO2 in swept

    SCO2 in swept

    The SCO2

    SCO2 = Ce

    Then, Eq. (3-1-1) can be simplied as follows

    MCO2t = CO2r A h (1 Swp) SCO2Ce

    After substituting the last equation into Eq. (12), Eq. (13) isobtained.

    MCO2e = Ce MCO2t = CO2r A h (1 Swp) SCO2 (13)

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    Comparison of different methods for determining key parameters affecting CO2 storage capacity in oil reservoirs1 Introduction2 Calculation of storage capacity2.1 Calculation of theoretical storage capacity2.2 Estimation of effective storage capacity2.3 Determination of key parameters2.3.1 Numerical reservoir simulation2.3.2 Empirical formula2.3.3 Stepwise regression

    3 Example storage capacity calculation of Xinjiang oilfield's reservoirs4 Discussion5 ConclusionsAcknowledgementsAppendix AReferences