Dr Harding4TH-SPE Paper 79695

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    Copyright 2003, Society of Petroleum Engineers Inc.

    This paper was prepared for presentation at the SPE Reservoir Simulation Symposium held inHouston, Texas, U.S.A., 35 February 2003.

    This paper was selected for presentation by an SPE Program Committee following review ofinformation contained in an abstract submitted by the author(s). Contents of the paper, aspresented, have not been reviewed by the Society of Petroleum Engineers and are subject tocorrection by the author(s). The material, as presented, does not necessarily reflect anyposition of the Society of Petroleum Engineers, its officers, or members. Papers presented atSPE meetings are subject to publication review by Editorial Committees of the Society ofPetroleum Engineers. Electronic reproduction, distribution, or storage of any part of this paperfor commercial purposes without the written consent of the Society of Petroleum Engineers isprohibited. Permission to reproduce in print is restricted to an abstract of not more than 300words; illustrations may not be copied. The abstract must contain conspicuousacknowledgment of where and by whom the paper was presented. Write Librarian, SPE, P.O.Box 833836, Richardson, TX 75083-3836, U.S.A., fax 01-972-952-9435.

    AbstractProduced water re-injection at high rates presents a coupled

    problem of reservoir flow, formation damage, stress alteration

    around the injector, and fracture propagation. Accurateprediction of permeability changes, fracture propagation

    pressure, and fracture dimensions is required for minimization

    of disposal costs and design of surface equipment. The paper

    presents the formulation and numerical implementation of acoupled reservoir, damage and geomechanical model which

    includes the above couplings. Details of the model are first

    described. A simple empirical damage model, calibrated tofield data is then presented. Finally, application of the

    complete model to high rate reinjection in the Masila Block in

    Yemen is presented. The model predictions show that it is

    feasible to sustain over 100,000 BWPD in a single Masiladisposal well by injecting above fracture pressure.

    Introduction

    Oil production operations often produce large volumes ofwater and high rate produced water re-injection (PWRI) isusually the best method of water disposal. However, injection

    wells can experience large reduction of injectivity due to

    plugging caused by solids and oil in water1,2. In particular, thecombination of total suspended solids (TSS) and oil-in-water

    (OIW) is particularly damaging2 and can cause equivalent

    skins on the order of 200 or more. Consequently, injection

    pressures increase with time and induced fracturing may takeplace.

    The prediction of injectivity and fracture propagation in

    injectors experiencing damage is a complex coupled problem

    including multiphase flow, geomechanics (stress changes)

    formation plugging, and fracture mechanics. This paper

    describes the formulation and numerical implementation of a

    model, which treats all of the above phenomena. The model isan extension of a previous coupled reservoir and

    geomechanics model3,4, combined with a dynamic fracture

    propagation feature and permeability reduction model. Thereare several possible approaches to fracture propagation

    modeling, which will be discussed in detail. The plugging

    mechanics is based on a simple, yet realistic model that can beeasily implemented in any conventional simulator.

    The formulation described here has been implemented in the

    GEOSIM modeling system and also in the Open Eclipse

    environment. The software has been used to model the PWRIinjection in the Masila block in Yemen, operated by Nexen

    Inc. Although the details of the engineering study are beyondthe scope of this paper, the methodology of conducting suchstudies and the consequences of the plugging mechanics for

    history matching will be presented in detail. The model shows

    in particular the importance of the coupling between theplugging, which generates increased pressure gradients, the

    associated poroelastic and thermoelastic stress changes, and

    the resulting fracture propagation pressure.

    Formulation of the modelThe coupled model consists of four main components:

    Fluid flow model

    Deformation and stress modelDynamic fracture model

    Permeability damage model

    Because the formulation of the first two components has been

    described previously3,4, this Section will give only a brief

    overview and highlight the couplings between them, followed

    by a detailed discussion of the fracturing and the damage

    model in the following Sections.

    Reservoir flow.

    This part of the system is a conventional 3-dimensional 3-phase black oil simulator. This model is the host or master

    SPE 79695

    Coupled Simulation of Reservoir Flow, Geomechanics, and Formation Plugging WithApplication to High-Rate Produced Water Reinjection

    R.C. Bachman, TAURUS Reservoir Solutions Ltd., T.G. Harding, Nexen Inc., A. (Tony) Settari, U. of Calgary and D.A.Walters, TAURUS Reservoir Solutions Ltd.

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    2 R.C. BACHMAN, T. HARDING, A. SETTARI AND D.A. WALTERS SPE79695

    for the other components. In the actual implementation, of the

    software, the host reservoir model can be either Eclipse 100 or

    the DE&S thermal reservoir simulator TERASIM.

    Deformation/stress model

    The model used is a continuum finite element code which

    solves the classical poro and thermoelasticity equations for

    nonlinear elasticity in an incremental fashion. The model alsohas elasto-plastic capabilities (discussed in Ref. 3) which have

    not been used in this work.

    In typical geomechanical applications, the main couplings

    between the flow and stress are through the changes in

    porosity (pore volume coupling) and through stress dependentpermeability (flow properties coupling). The first is dominant

    in compaction problems5, while the second is important in

    problems such as waterfloods in jointed media6.

    In PWRI problems, both of these couplings are of minorimportance until formation failure is induced around the

    fracture. However, there are additional couplings arising fromfracturing and damage mechanisms:

    Permeability reduction due to damage can be verylarge (especially close to the injector), and will

    completely overshadow any stress-dependent

    changes.

    Stress changes around the injector due to pressureand temperature changes cause time-dependent

    changes in fracture initiation and propagation

    pressure.

    Because the pressure gradients are a strong functionof the damage, there is a strong coupling between thedamage, time of the start of fracturing, and fracturing

    pressures.

    Modeling of induced fracturing in geomechanicsFracture modeling can be approached from either the fracture

    mechanics side, or the reservoir flow side.

    a) The conventional hydraulic fracturing models (intendedprimarily for stimulation treatments) focus on details of

    fracture geometry and other fracturing physics, and decouple

    the reservoir flow by the use of analytical leak-off models. Itis well known that this approach becomes inaccurate as the

    leak-off increases. The analytical reservoir treatment can be

    improved considerably7and incorporate the plugging effects8,9

    but ultimately such models are limited in generality.

    b) The alternative approach is to build a model of fracturing

    into a reservoir simulator to treat the leak-off implicitly. Such

    models have been known since the 1980s. Early examples10,11

    coupled 2-D analytical or pseudo-3D fracture geometrymodels with 3-D, 2-phase, thermal reservoir models.

    However, the coupling with stress was still not included andconsequently the fracture propagation pressure had to be

    specified.

    For PWRI problems, the stress coupling and its effect on

    fracture mechanics is significant. Therefore, the ultimate

    PWRI fracturing model consists of three fully coupled

    components: 1) Fracture mechanics model (computingfracture geometry, flow and heat transfer inside the crack), 2)

    reservoir model (computing flow, heat transfer and damage in

    the reservoir) and 3) geomechanics (computing stress-strain

    response of the reservoir and its surroundings to pressure and

    temperature changes, and loading on fracture face).

    Some of the important couplings between the components are:

    Pressure in the fracture is a boundary pressure forreservoir flow (leak-off)

    Fracture width and pressure are equal, respectivelyto the displacement and normal stress on the crack

    boundary in the stress model

    Pressure and temperature in the reservoir are loadsfor the stress solution

    Effective stress and volumetric strain determinereservoir permeability and porosity

    The modeling approach can be either to formulate the entire

    problem in a fully coupled manner, or in a modular fashion. In

    a fully coupled model, the couplings become internal

    compatibility conditions and are satisfied automatically, bu

    require internal iterative process. In the modular approachused in this work (see Fig. 2 of Ref. 4), the compatibility

    conditions can be satisfied by external iteration between the

    modules, or approximated. We will now describe two existing

    methods of implementing fracture modeling in the context of amodular system and discuss the outstanding issues for

    rigorous coupling. Both methods are based on the assumption

    that the primary interest in the modeling is to predict welproductivity or injectivity under fracturing conditions, and the

    fracture geometry details are not as critical.

    Partially coupled approach

    The first is an extension of the partially coupled concept for

    modeling stimulation treatments (Settari et al. 1990). The

    fracture propagation is pre-computed using an uncoupled

    fracture mechanics model (such as the models discussed undera) above). For the coupling with reservoir, the fracture must

    lie in a grid plane of the flow model and it is represented in the

    flow model by increased transmissibilities, which arecalculated from the local fracture width. The stress model

    shares the mesh with the flow model; but the fracture width is

    typically not used as a displacement boundary condition in

    fracture plane. Since the transmissibilities are re-computed intime, the model can represent the dynamic process of fracturegrowth, or the propped or acidized fracture after the treatmen

    (essentially static except for the conductivity changes due to

    stress).

    This approach also ignores the effect of created fracture

    storage on pressure (this effect is however significant only

    when the fluid efficiency is high). Since the leak-off duringthe fracture propagation calculations is computed

    independently, there is no guarantee that it will be correct

    This will show up as a mismatch in computed injection

    pressures from the fracture mechanics and reservoir model: if

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    SPE 95695 COUPLED SIMULATION OF RESERVOIR FLOW, GEOMECHANICS AND FORMATION PLUGGING 3

    the predicted fracture growth rate is too small, coupling this

    fracture into the reservoir model will produce pressures which

    are too high and vice versa. Similarly, the poro andthermoelastic back stresses (also referred to as back

    stresses) are computed independently in the fracture model,

    and do not necessarily agree with the stresses on the fracture

    face computed by the stress model. In spite of these

    limitations, this method has been used extensively and can beapplied successfully to a number of problems if the models are

    tuned to produce the same pressure history13,14.

    Fully coupled approach with simplified fracture mechanics

    The second approach is similar to that presented recently for

    modeling waterfracs15. The idea is to use stress-dependentpermeability functions, which can represent the flow behavior

    of the fracture in a fully coupled manner. In the potential

    fracture plane (normal to the minimum effective stress), the

    permeability (or directly the flow transmissibility) is increased

    by several orders of magnitude as the effective stress normalto the fracture decreases. A typical function (permeability

    multiplier) is shown in Fig. 1.

    Fig. 1 Typical stress-dependent transmissibility functions

    to represent fracture in the flow model

    The shape of the curve can be related to the fracture width

    versus net pressure (i.e., stiffness) and its position to net

    pressure in the fracture. Imposing a maximum is necessary tomaintain the stability of the model. The coupled reservoir and

    stress model is then run without any reference to a fracture

    mechanics model, and the region where the flowtransmissibilities have reached large values is deemed to

    represent the fracture.

    This approach provides implicit coupling between reservoir

    stress and fracture propagation pressure (i.e., the back stress is

    implicit), However, the model lacks the fracture mechanicsfeatures. First, the crack opening is not included as a boundary

    condition on the stress model. In soft formations with small

    modulus and low fracture net pressure, the additional stress

    from the opening will be small. Second, the fracture volume is

    not represented. Again, this will not be a problem in high leak-

    off situation, but this aspect can be modeled rigorously byeffective stress dependent porosity of the fracture blocks

    Finally, the tip growth variables need to be introduced. This

    may be important in hard rock, if fracture propagates through

    a layered stress system (as it is usually the case), vertica

    growth through stress barriers may be poorly represented if thefracture opening is not included in the stress model. In the

    example of Fig. 2, where high stress layer is present within theperforated interval, the approach may produce two separate

    fractures while the true solution may be a single fracture

    Therefore the model will tend to exaggerate the confinement

    of the fractures.

    Confining

    stress

    Fracture mechanics

    model

    Stress dependent k

    model

    Fig. 2 Possible fracture geometry differences

    On balance, our experience indicates that for PWRI fracturing

    the reservoir flow and coupling with stress are more importanthan the fracture mechanics features, and therefore the coupled

    method was used in this work. Its most significant advantage

    for field applications is that it can model fractures in differentdirections (in Cartesian as well as in Corner Point Geometry

    grid), and within local grid refinement, as shown in Fig. 3.

    Fig. 3 Possible fracture representations using the

    transmissibility modifier method

    Further work is ongoing to remove some of its limitations andto make it a fully coupled solution for general applications.

    1

    10

    100

    1000

    10000

    100000

    -600 -400 -200 0 200 400 600

    Effective stress normal to fracture

    Transmissibilitymultiplier

    Increasing net

    pressure in fracture

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    4 R.C. BACHMAN, T. HARDING, A. SETTARI AND D.A. WALTERS SPE79695

    The damage modelRigorous modeling of formation damage involves solving the

    equations for particle transport and entrainment in porousmedia. While such models have been developed16,17, they are

    currently too complex for full-field application and require

    parameters directly describing the physics, which are usually

    not readily available. For modeling purposes, it is desirable to

    have a simple model with few parameters, which can becalibrated directly against field injection data.

    Several authors18,19,20 postulated a model in which the

    permeability reduction at a given point in the media is

    expressed in a form:

    )1(

    1/ 0

    +=kk (1)

    where is some measure of the concentration of the particlesat that location. We now make an assumption that can berelated to the amount of the water that passed through thislocation. In a one-dimensional setting, this is simply

    =t

    dttQAtVt0

    )(/)()( (2)

    In a finite difference form, at the end of time step K,

    nK

    n

    nKK tQAVt = =1

    /)( (3)

    where Qnis the computed water flow rate through the area A

    during the time step n. Based on testing on field data described

    later, the above formula was further generalized to thefollowing:

    ))/(1(1

    1/

    min

    min0nAVR

    Rkk+=

    (4)

    where , n and Rminare the three parameters of the model.The parameter represents the intensity of the damage and is

    primarily related to the water quality (TSS and OIW) in

    combination with reservoir permeability. Increasing accelerates damage as shown on Fig. 4. The exponent n

    changes the shape of the damage curve as shown in Fig. 5.The factor Rminwas introduced because of field evidence that

    the damaged permeability does not decrease to zero but

    reaches an asymptotic minimum value, which in Eqn. (4)

    becomes kmin= k0Rmin(see Fig. 6).

    Laboratory tests on cores21 and field tests in the Masila

    Block22suggest that there is also a dependence of damage onflow velocity. Fines migration testing in the lab has indicated a

    dependence of permeability on flow velocity. In the field,

    there is little or no damage observed during production tests

    conducted immediately after drilling and completing disposal

    wells nor during low rate injection tests, while damage isdefinitely observed even in short duration high rate injection

    tests. This aspect is being investigated further.

    Damage model with constant n=1, Rmin=0

    0

    0.1

    0.2

    0.3

    0.4

    0.5

    0.6

    0.7

    0.8

    0.9

    1

    0.1 1 10 100

    Volume througput/Area

    (k)d

    amaged/(k)initial

    alpha=0.01

    alpha=0.1

    alpha=1.0

    Fig. 4 Effect of on damage function

    Damage model with constant =0.5, Rmin=0

    0

    0.1

    0.2

    0.3

    0.4

    0.5

    0.6

    0.7

    0.8

    0.9

    1

    0.1 1 10 100

    Volume througput/Area

    (k)damaged/(k)initial

    n=1.0

    n=0.6

    n=1.4

    Fig. 5 Effect of exponent non damage function

    Damage model with constant alpha=0.5, n=1

    0

    0.1

    0.2

    0.3

    0.4

    0.5

    0.6

    0.7

    0.8

    0.9

    1

    0.1 1 10 100

    Volume througput/Area

    (k)dam

    aged/(k)initial

    Rmin=0.0

    Rmin=0.1

    Rmin=0.2

    Fig. 6 Effect of residualRminon damage function

    Implementation

    Equation (4) was extended to 3-D flow and implemented in

    the flow calculation via another set of transmissibility

    multipliers (which are cumulative to those arising from

    fracture propagation). It should be noted that, in the use ofEqn. (4), a distinction must be made between in-situ reservoir

    water flow and injected water flow, because it is assumed that

    the flow of the in-situ water does not create damage. Trackingthe difference can be accomplished in two ways:

    a) Defining two water components in the model (e.g., by using

    the oil component for in-situ water and water componenfor injected water). This is often sufficient as the injection

    usually takes place into a water zone.

    b) Using a tracer tracking capability in the reservoir modelThis is more general as it retains all model capabilities and

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    SPE 95695 COUPLED SIMULATION OF RESERVOIR FLOW, GEOMECHANICS AND FORMATION PLUGGING 5

    allows injecting several produced water types with distinct

    plugging properties.

    The first method is used in the TERASIM based model, and

    the second in the Eclipse based one.

    Validation Gulf of Mexico data

    As an example, consider the data for the Gulf of Mexico(GOM) wells reported in Ref. 1. All wells were limited to

    injecting below fracture pressure, and temperature effects aresmall. This allows the testing of the damage model in a simple

    setting without stress or fracture coupling. The reservoir data

    is found in Ref. 1. Well A39 started injecting at 5000 BWPD

    but the injectivity decreased to below 1000 BWPD in less than

    a year. The decline was matched with the overall value of =0.12 (1/ft)n and n=1 as shown in Fig. 7. The value wasdecreased temporarily at early times to account for the acid

    jobs. At late times, damage was limited byRmin= 0.0002.

    Bullwinkle A39

    7400

    7600

    7800

    8000

    8200

    8400

    8600

    8800

    9000

    0 50 100 150 200 250 300 350 400 450

    time (days)

    BHP(psia)

    0

    1000

    2000

    3000

    4000

    5000

    6000

    7000

    8000

    InjRate(BWPD)

    BHP data

    Inj rate data

    Model match

    Fig. 7 Match of productivity decline GOM Well A39

    Well A42 has similar history and its match, shown in Fig. 8,

    was obtained with the same parameters as for A39. The well

    Bullwinkle A42

    7400

    7600

    7800

    8000

    8200

    8400

    8600

    8800

    9000

    0 50 100 150 200 250 300 350

    time (days)

    BHP

    (psia)

    0

    1000

    2000

    3000

    4000

    5000

    6000

    7000

    8000

    InjRate(BWPD)

    BHP data

    Inj rate data

    Model match

    Fig. 8 Match of productivity decline GOM Well A42

    had a high initial skin, which was accounted for by initialpermeability reduction close to the well. Matches of similar

    quality have been obtained for all other wells. The effect of

    the acid treatments performed in some of the wells can be

    modeled by the removal of the damage around the well.

    The method of treating the damage, although very simplified

    is remarkably realistic. Due to its empirical nature, the damage

    parameters must be obtained by history matching of field data

    or laboratory experiments. However, when the field injectioninvolves fracturing, the matching process is more complex, as

    will be shown next on the example of the Haru 4 well of theMasila project.

    Application high rate injection in the Masila Block

    The Masila injection project

    Canadian Nexen Petroleum Yemen Ltd. operates the Masila

    project in the Republic of Yemen on behalf of its partner

    Occidental Petroleum Ltd., Consolidated Contractors

    Company S.A.L. and the Government of the Republic ofYemen. Oil production comes mainly from the high porosity

    and permeability Upper Qishn sandstones of LowerCretaceous age. Currently, the operation produces 230,000

    BOPD and over 1,000,000 BWPD. The produced water is

    reinjected at matrix injection pressures mainly into the Upper

    Qishn section below the original oil-water contact in each

    field. The target injection horizon is the S2/S3 zone, which isconnected to the large regional aquifer, which underlies the

    producing areas. Despite the high quality of the reservoirs

    injectivity problems have hampered the project since inception

    and have prompted the investigation of causes of theseproblems and the development of remedies. Further details o

    the Masila operation and the analysis of water injectivity in

    the laboratory and field have been reported earlier21, 22.

    Produced water is currently reinjected into 24 vertical plus 4horizontal wells. These wells experience poor initia

    injectivity that decreases further as a result of impurities in the

    water that are impractical to remove through well headfiltration. Well acidizing or proppant fracturing the injectors

    provided only temporary increases in injectivity. Additiona

    disposal wells will be needed as water production continues toincrease. To meet future needs, Nexen plans to drill 4 to 6

    injection wells to allow for the additional wastewater disposal

    of approximately 500,000 BWPD. The present work wasundertaken to evaluate high rate produced water reinjection

    above formation parting pressure.

    A simulation study was conducted (and is currently beingupdated) to provide insight into the damage mechanism in theQishn sands, determine the injectivity and required wel

    spacing at fracture conditions, and ultimately predict the

    surface injection pressures at various target rates. In this way

    the injection project can be optimized with respect to numberof wells needed versus the cost for the surface equipment.

    In this paper, we only present the parts of this work thaillustrate the particular features of the coupled modeling and

    its results. The results of the engineering study including the

    details of the geomechanics will be published in a future

    article.

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    6 R.C. BACHMAN, T. HARDING, A. SETTARI AND D.A. WALTERS SPE79695

    Calibrating the model

    Two wells were used to calibrate the model: Camaal 30 andHaru 4.

    The Camaal 30 well was completed in the S2 zone, with net

    pay of 102 ft and permeability of 1307 md. Injection began

    June 26, 1999 and continued with some interruptions untilFeb.4, 2001. During that time a number of workovers took

    place, including filter changes, acid jobs and a propped fracjob. Conventional analysis using Hall plots and equivalent

    skin calculations clearly showed the temporary nature of

    injectivity improvement from these interventions. History

    matching established the damage parameters, but becauseCamaal 30 is a low injectivity well, more emphasis was

    placed on the Haru 4 calibration.

    The Haru 4 well is more representative of future injectors. The

    well is completed in water bearing S2 zone with net pay of 96ft and average permeability of 4300 md. The injection history

    from February 1, 1999 to January 6, 2001 is in Fig. 9, togetherwith an interpreted skin due to damage, assuming radial flow.

    Haru-4 - Injection Rate and BHP and interpreted damage skin

    0

    500

    1000

    1500

    2000

    2500

    3000

    0 100 200 300 400 500 600 700 800

    Time (days)

    BHP(psia),damageskinx10

    30000

    40000

    50000

    60000

    70000

    80000

    90000

    InjectionRate(stb/d)

    BHP

    skin from damageInjection Rate

    Fig. 9 Field data for Haru 4 and interpreted damage skin

    It was modeled with a single layer reservoir model coupled

    with a 5-layer geomechanical model, using a Cartesian grid.Permeability damage model was used and fracture propagation

    (if predicted by the model) could take place. Highly refined

    grid was used in the potential fracture path and the model wasset up to act in an infinite manner. Water was injected at a

    temperature of T = 27 deg F below reservoir temperature in

    all cases. A total of 701 days of injection was modeled. Itbecame quickly apparent that the couplings present in the

    physical system allow non-unique interpretation, if the

    pressure is the only data matched. Three major factors were

    identified:

    a) Thermal expansion coefficient aL. Its value controls the

    thermal stress component Twhich is added to the far-fieldconfining stress c. This in turn changes the fracture initiationand propagation pressure.

    b) Damage strength (parameters , n and Rmin). Increaseddamage accelerates fracturing, but also increases the

    poroelastic stress change pe, which increases fracturepressure.

    c) Friction pressure loss in the fracture pfric (part of the nepressure), directly related to fracture conductivity. In PWR

    injection, plugging occurs inside the fracture as well and can

    significantly increase injection pressures. If the fracture

    conductivity is finite, pfric increases significantly with

    fracture length xf.

    Thus, the observed injection pressure pfduring fracturing can

    be written in a simplified manner as

    pf= c- T(T) + pe(dam) + pfric(dam, xf) (5)

    which illustrates the competing nature of these parameters. ForHaru 4, thermal expansion coefficient was not measured at the

    time. Based on literature data, a median value of a L= 0.648 x

    10-51/0F and a high value of 1.6 x 10-51/0F were selected

    The cases of low and high fracture conductivity wereconstructed by choosing the maximum of the fracture

    multipliers shown in Fig. 1 as 104

    and 105

    . The damageparameters were then varied to obtain a match for each caseFig. 10 shows the comparison of the pressure match for three

    cases:

    Case 1: Median aL= 0.648 x 10-5, low frac conductivity

    Case 2: High aL= 1.6 x 10-5, low frac conductivity

    Case 3: High aL= 1.6 x 10-5, high frac conductivity

    1500

    1700

    1900

    2100

    2300

    2500

    2700

    0 100 200 300 400 500 600 700 800

    time (days)

    BHP,

    dataandsimulated(psia)

    40000

    50000

    60000

    70000

    80000

    90000

    100000

    Observed BHP

    case 1

    Case 2

    Case 3

    inj rate

    Fig. 10 Comparison of pressure matches with three sets o

    coupling parameters

    These matches required different damage parameters as shown

    in Table 1. Case 1 had the lowest amount of thermal stress andtherefore required the smallest amount of damage (see Eqn

    (5)). In fact, the damage was not sufficient to initiate afracture. To maintain the match at late times, it was necessary

    to increase Rmin with time (reduce cumulative damage)

    Although we do not have a physical explanation for this

    phenomenon, it is in agreement with the conventional skin

    analysis shown in Fig. 9 where the skin decreases from 100 to65 during the second year. Case 2 had larger thermal stress

    Tand required more damage (pe) to match pf. Howeverbecause of the low fracture conductivity, the friction pressure

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    pfricwas significant, and the altered stress (i.e., c - T +pe) required was lower than pf. This resulted in a smallfracture of about 9 ft. Case 3 required much more damage asthe friction pressure was small and the altered stress needed to

    be higher than in Case 2 and close to the injection pressure.

    The effect of higher damage was to accelerate fracture

    propagation; the length at the end was 366 ft.

    Case (1/ft) n Rmin1 - median aL 0.0005 1 0.1

    2 - high aL,high conductivity 0.002 1 0.035

    3 - high aL,low conductivity 0.2 1 0.003

    Table 1 Damage parameters for the 3 matches

    The damage in the first two cases is localized close to the

    injector, while in Case 3 it reaches far into the reservoir. Inthis respect, Case 3 is considered less realistic. Apart from the

    oscillations due to fracture crossing block boundaries (which

    could be reduced by still finer gridding), the three matches are

    of similar quality, yet they produce a very different picture of

    the process. This demonstrates the danger of using coupled (orany) modeling with too little data. The ambiguity can be

    however dealt with as discussed below.

    Predictions for typical future injectors

    At this preliminary stage, all three scenarios were used to

    generate forecasts for injection rates up to 150,000 BWPD,

    and with different T, with the aim to determine the safesurface injection pressure (THP) specifications. At higher

    rates, all scenarios produced fracturing, but the predictedsurface pressures were somewhat different.

    For Case 1, the damage is low such that even the low

    fracture transmissibility results in high dimensionless fractureconductivity. The predicted BHP is insensitive to rate as

    shown on Fig. 11 for the case of T =27 oF. Therefore THP isprimarily a function of wellbore friction. For Case 2 there is a

    significant dependency on rate as well as on fracture length,

    and the BHP as well as THP continues to increase with time,

    as shown on Fig. 12 T =27 oF. For Case 3 the pressure alsoclimbs with time. In all cases, injection temperature has a

    large effect on BHP as shown in Fig. 13 for Case 1.

    Case 1 Forecast - Infinite Reservoir, BHP for Various Rates for DT=27 deg F

    2000

    2200

    2400

    2600

    2800

    3000

    3200

    3400

    0 200 400 600 800 1000 1200 1400 1600 1800 2000

    time (days)

    BHPinjpressure(psia)

    Q=100,000, BH inj pressure

    Q=125,000, BH inj pressure

    Q=150,000, BH inj pressure

    Fig. 11 BHP dependence on rate for Case 1, T =27

    oF

    Case 2 Forecast, infinite reservoir, BHP for various rates, DT=27 deg F

    2000

    2200

    2400

    2600

    2800

    3000

    3200

    3400

    0 200 400 600 800 1000 1200 1400 1600 1800 20

    time (days)

    BHPinjpress

    ure(psia)

    Q=100,000, BH inj pressure

    Q=125,000, BH inj pressure

    Q=150,000, BH inj pressure

    Fig. 12 BHP dependence on rate for Case 2, T =27oF

    Case 1 Forecast - Infinite Reservoir, BHP for Various DT, Qw=150,000 stb/d

    2000

    2200

    2400

    2600

    2800

    3000

    3200

    3400

    0 200 400 600 800 1000 1200 1400 1600 1800 20

    time (days)

    BHPinjpressure(psia)

    DT=17 Deg F, BH inj pressure

    DT=27 Deg F, BH inj pressure

    DT=37 Deg F, BH inj pressure

    Fig. 13 BHP dependence on T, Case 1, Q=150,000 BWPD

    Design consequences

    It is obvious that due to the complexity of the process, as

    many uncertainties as possible must be eliminated to design

    high rate re-injection projects. First, data for aLcan be easilymeasured. Second, the damage can be calibrated by matching

    injection tests below fracture pressure where the fracture

    aspects do not interfere (like in the GOM example above)

    Finally, for injection in fracture mode, analysis of steprate/fall-off tests and fracture diagnostics methods can be used

    to determine fracture dimensions and conductivity by other

    means, thus leaving only the damage as a matching parameter.

    The above principles were followed in a subsequent study. Asa result, an essentially unique match for Haru 4 was obtained

    and the uncertainties of the THP predictions were significantly

    reduced. As a result, it was possible to recommend ANSI 600standard for the surface equipment design that will result in

    significant cost savings for the operator.

    Conclusions1) A numerical model solving in a coupled fashionmultiphase flow, geomechanics (stress changes), formation

    plugging, and fracture mechanics has been developed.2) A simple, flexible model of permeability damage was

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    8 R.C. BACHMAN, T. HARDING, A. SETTARI AND D.A. WALTERS SPE79695

    formulated and implemented in the reservoir flow part of the

    system. It is capable of reproducing the injectivity loss

    observed in Gulf of Mexico and Masila Block wells.3) The factors controlling injection pressure match are thefracturing, the degree of reservoir permeability damage and

    thermal stresses, which are dependent on the rock thermal

    expansion coefficient (T).

    4) Multiple interpretations of the field injection pressures arepossible, with trade-off between the thermal stress magnitude,poroelastic stress induced by permeability damage, and

    fracture conductivity. However, if laboratory data on T isavailable, history match can be used to characterize the

    plugging mechanics.

    5) Accurate prediction of injection pressure is critical as itdirectly impacts facilities and pipeline design specifications.Forecasting with the calibrated model indicated that 100,000

    BWPD injectors should be possible without exceeding ANSI

    600 standard for surface equipment design.

    6) Due to the cumulative permeability damage, the onlyfeasible method of maintaining injectivity in high rate

    produced water re-injection is sustained fracturing.

    NomenclatureA = flow area (m2)

    aL = linear thermal expansion coefficient (1/deg C)

    k = permeability (md)

    k0 = undamaged permeability (md)n = exponent in damage equation

    pf = fracture propagation pressure (kPa)

    Q = injection rate (m3/d)Rmin = maximum damage parameter in Eqn. (4)

    V = cumulative water flow through area A (m3)

    = damage strength parameter in Eqn. (4) = coefficient in Eqn. (1)T = thermal stress (kPa)pe = poroelastic stress (kPa)pfric = friction pressure in the fracture (kPa)T = temperature difference (reservoir-inj) (deg C)c = undisturbed confining stress on fracture (kPa) = particle concentration (kg/m3)

    AcknowledgementsThe authors wish to thank Nexen Inc. and its partners in the

    Masila Project, Occidental Petroleum Ltd., Consolidated

    Contractors Company S.A.L. and the Government of the

    Republic of Yemen, for the permission to publish this paper.

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