9
SPE 37088 Geomechanical Design and Evaluation of a Horizontal Wellbore in Maracaibo Lake, Venezuela: Real-DriIling-Time Application Marisela Sanchez D., Intevep, S.A., Jose R. Cabrera S., Intevep, S.A., Carolina Coil, Maraven, S,A. COMSM 190S, Smkaty C4P.ba4wm EWinoam, he lhm papaf was pmpwad ku praaonmoon t ma 1 SS6 SPE Imanmond COnfaf*fwa on Hah0n81 Well Taatfmowy R.ld III C4DSfy fAnada, 1S.20 Wwmbw 1SSS. Thhpapuwa adacmbrpmonmmm MfmasOn by an SPS Pmgmm Canmtiaa folkwdffs IW.4.W d Canwnad inwfmbatmu aubmisodby Ihadfw(s).b ltanhdwl.ppq s -, k td ban ~ W Uw SodatY d Pahdoum Enginaam snd m wbjacl to wrractw by h wihor(s). Tha matafial, s praaantad, dc+s IX+ nacassanly mlhai ny paition dh Sac48q of PaImlaum En@wara, b omcefa, of mambwa Papafa prcsantad nt SPE maetings am wbjact la pubhcabon Wcw by Ed(tcoal Commmees of m+ .SocIety of P@trolaum Engiwm PwmIcsIw to -y m raa!rmfad 10 n Dbatmcf of not mom than 3M wxdt Illustrsfmm msy IKA ba CC.PIad Tha bstract should contain cmspuuous cknohwd~rn.nt d +am snd by WAOM th ~paf was pre8entad Wr!te Ltbrmmn, SPE, P O. Sox S.X?&S, Rlchardaon, TX 7S0S3-2S26 U.S A fax 01 .214.952.S4S5 Abstract A horizontal well was planned for a location in Maracaibo Lake, Venezuela, and it was required to asses its stability. A pilot vertical hole was drilled including an oriented core, Several laboratory and field techniques such as anelastic strain relaxation (ASR), differential strain analysis (DSA), acoustic anisotopy in the cores, breakouts, sonic logs and focal mechanisms were used to estimate the in-situ stress field. A cased-hole minifrac was available from a nearby well in the reservoir sand. While finishing the drilling of the pilot hole, running logs and cement-plugging, laboratory static and dynamic tests were performed for both, cap and reservoir sandstones. Linear elastic theory and Mohr-Coulomb failure criteria were used for the borehole stability analysis, Information from the rig site about mud weight used in unstable sections of the pilot was used to calibrate the linear elastic model and bound the maximun horizontal stress component. As a result of the analysis, safe mud weight limits to prevents collapse and lost of circulation were released to the drillers for both, the inclined and horizontal sections. The well was drilled without any stability problems. In this case it was shown that simple linear elastic models, when calibrated with field data, give reliable, first approximation values, specially useful when real-drilling-time answers are needed. The stability during production was studied using a 2-D finite element model with a generalized plasticity constitutive equation. A safe drawdown to prevent failure was determined. The well was completed open hole without any liner. It is producing above the riginal potential without any sanding or stability problems. Introduction Horizontal well activities in Venezuela started around the 80s and now the companies have agressive horizontal drilling programs. Even though there have been succesful cases, there have been some horizontal well failures, as well. llse problems have @n related to geological and petrophysical uncertainties, formation damage in mature reservoirs and collapses due to borehole instability. Programs considering vertical pilot holes with oriented coring have been deveioped to increase the chances of success in reservoirs in which very Iittie information has been gathered [1]. This approach has allowed to make timely evaluation of the reservoir rock and in situ stresses before the horizontal hole is drilled and therefore minimize risks from geomechanical and mud drilling design points of view. An example of such case was the planning of a horizontal well in a reservoir in the Maracaibo Lake area, Venezuela. This was the first horizontal well in this field and it was drilled with the purpose of draining the atic oil accumulated against an adjacent normal fault. The well was placed sub- parallel to the normal fault (with strike N36W approximately) as shown in Figure 1. The horizontal well was planned to be approximately parallel to the fault. It was difficult to asses the geomechanical risk for a horizontal well in this area without having an idea of the rock strength and the in situ stress field. Moreover, the regional stress environment in the Maracaibo Lake area is very complicated and it was not known if the horizontal well was going to be drilled in the most risky direction. Trying to decrease as much as possible the uncertainties, a vertical pilot hole with 60 feet oriented coring was drilled. Additionally, three hundred feet conventional coring was recovered for sedimentological studies, The pilot-hole and horizontal weli plan is presented in Figure 2. Sonic logs were added to the conventional petrophysical logging program to asses a strenght profile for the rock along the pilot hoie. A complete, but fast rwk mechanics testing program including static and dynamic measurements was 457

1996, Marisela Sanchez, Jose. R. Cabrera, Geomechanical Design and Evaluation of a Horizontal Wellbore in Maracaibo Lake, Venezuela. Real-Drilling-Time Application

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  • SPE 37088

    Geomechanical Design and Evaluation of a Horizontal Wellbore in Maracaibo Lake,Venezuela: Real-DriIling-Time ApplicationMarisela Sanchez D., Intevep, S.A., Jose R. Cabrera S., Intevep, S.A., Carolina Coil, Maraven, S,A.

    COMSM 190S, Smkaty C4P.ba4wm EWinoam, he

    lhm papaf was pmpwad ku praaonmoon lt ma 1 SS6 SPE ImanmondCOnfaf*fwa onHah0n81 Well Taatfmowy R.ld III C4DSfy fAnada, 1S.20 Wwmbw 1SSS.

    Thhpapuwa adacmbrpmonmmmMfmasOn

    by an SPS Pmgmm Canmtiaa folkwdffs IW.4.W dCanwnad inwfmbatmu aubmisodby Ihadfw(s).b ltanhdwl.ppq ls

    -, k td ban ~ W Uw SodatY d Pahdoum Enginaam snd lm wbjacl towrractw by h wihor(s). Tha matafial, ls praaantad, dc+s IX+ nacassanly mlhai lnypaition d h Sac48q of PaImlaum En@wara, b omcefa, of mambwa Papafa prcsantad ntSPE maetings am wbjact la pubhcabon Wcw by Ed(tcoal Commmees of m+ .SocIety ofP@trolaum Engiwm PwmIcsIw to -y m raa!rmfad 10 ln Dbatmcf of not mom than 3Mwxdt Illustrsfmm msy IKA ba CC.PIad Tha lbstract should contain cmspuuouslcknohwd~rn.nt d +am snd by WAOM th ~paf was pre8entad Wr!te Ltbrmmn, SPE, P O.Sox S.X?&S, Rlchardaon, TX 7S0S3-2S26 U. S A fax 01 .214.952.S4S5

    AbstractA horizontal well was planned for a location in Maracaibo

    Lake, Venezuela, and it was required to asses its stability. Apilot vertical hole was drilled including an oriented core,Several laboratory and field techniques such as anelasticstrain relaxation (ASR), differential strain analysis (DSA),acoustic anisotopy in the cores, breakouts, sonic logs andfocal mechanisms were used to estimate the in-situ stressfield. A cased-hole minifrac was available from a nearby wellin the reservoir sand. While finishing the drilling of the pilothole, running logs and cement-plugging, laboratory static anddynamic tests were performed for both, cap and reservoirsandstones. Linear elastic theory and Mohr-Coulomb failurecriteria were used for the borehole stability analysis,Information from the rig site about mud weight used inunstable sections of the pilot was used to calibrate the linearelastic model and bound the maximun horizontal stresscomponent. As a result of the analysis, safe mud weight limitsto prevents collapse and lost of circulation were released tothe drillers for both, the inclined and horizontal sections. Thewell was drilled without any stability problems. In this case itwas shown that simple linear elastic models, when calibratedwith field data, give reliable, first approximation values,specially useful when real-drilling-time answers are needed.

    The stability during production was studied using a 2-Dfinite element model with a generalized plasticity constitutiveequation. A safe drawdown to prevent failure wasdetermined. The well was completed open hole without anyliner. It is producing above the riginal potential without anysanding or stability problems.

    Introduction

    Horizontal well activities in Venezuela started aroundthe 80s and now the companies have agressive horizontaldrilling programs. Even though there have been succesfulcases, there have been some horizontal well failures, as well.llse problems have @n related to geological andpetrophysical uncertainties, formation damage in maturereservoirs and collapses due to borehole instability. Programsconsidering vertical pilot holes with oriented coring havebeen deveioped to increase the chances of success inreservoirs in which very Iittie information has been gathered[1]. This approach has allowed to make timely evaluation ofthe reservoir rock and in situ stresses before the horizontalhole is drilled and therefore minimize risks fromgeomechanical and mud drilling design points of view.

    An example of such case was the planning of a horizontalwell in a reservoir in the Maracaibo Lake area, Venezuela.This was the first horizontal well in this field and it wasdrilled with the purpose of draining the atic oil accumulatedagainst an adjacent normal fault. The well was placed sub-parallel to the normal fault (with strike N36W approximately)as shown in Figure 1. The horizontal well was planned to beapproximately parallel to the fault.

    It was difficult to asses the geomechanical risk for ahorizontal well in this area without having an idea of the rockstrength and the in situ stress field. Moreover, the regionalstress environment in the Maracaibo Lake area is verycomplicated and it was not known if the horizontal well wasgoing to be drilled in the most risky direction. Trying todecrease as much as possible the uncertainties, a verticalpilot hole with 60 feet oriented coring was drilled.Additionally, three hundred feet conventional coring wasrecovered for sedimentological studies, The pilot-hole andhorizontal weli plan is presented in Figure 2.Sonic logs were added to the conventional petrophysicallogging program to asses a strenght profile for the rock alongthe pilot hoie. A complete, but fast rwk mechanics testingprogram including static and dynamic measurements was

    457

  • 2 M. SANCHEZ, J. CABRERA, C. COLL SPE 37088

    developed for mechanical characterization. Several laboratoryand field techniques were used to estimated the in-situ stressfield including breakout orientation [2], anisotropic sonic logs[3], Anelastic Strain Relaxation (ASR) [4], Differential StrainCurve Analysis (DSA) [5], Acoustic Shear Wave AmplitudAnalysis (SWAA) and Acoustic Velocity Anisotropy (AAA)[6] from samples and logs from the pilot hole. Informationfrom a minifrac [7] and density logs were gathered fromnearby vertical wells. The overall regional tectonicinformation was considered at the time of interpretation andintegration of the in-situ stress data. A borehole stability studywas carried out to define the mud-weight operational window.For the stability during perforation a linear elastic analyticalmodel was used [8]. The time available for this study was theone corresponding to the completion of coring, cementing,logging, and other operational procedures to be done beforethe kick-off of the inclined section, so this project wasdeveloped as a real-drilling-time application.

    The compatibility of the shales with drilling fluids wasdetermined, showing poor reactivity. Therefore, the water-based mud used for the inclined section would not affect thechemical stability of the shales. However, the mechanicalstability of the shales was not investigated. For the producingzone (horizontal section) a saline mud was designed andoptimized to minimize formation damage and ensure a highlyefficient mud-cake. The size distribution of pore throats wasdetermined by microscopic analysis and proper particle sizedistribution in the saline mud was used to prevent excessivefiltrate [9]. Tests of mud-cake efficiency on core from the payzone were also performed to verify the effectiveness of themud design.

    An open hole completion without any liner was suggestedand therefore, a study of wellbore stability during productionwas developed to determine a safe drawdown allowable forthis horizontal well. The model used for this estimations wasa 2D finite element model, plane strain, with several stress-strain constitutive laws such as linear elasticity, ehstic-perfectly plastic material, generalized plasticity [10].

    Coring and Measurement of Mechanical Propertiesof the Rock

    The core for geomechanical testing was taken usingaiuminum barrei in order to minimize mechanical damageand it was preserved with conventional procedures. Ageological visual description was made at the rig-site and thecore was transported directly to the lab. Sandstone sampleswere taken at the depth correspondhg to the inclined section(cap rock) and at the pay zone. Figure 3 shows the depth ofcoring, together with the gamma ray iog, indicating the KOPand target point for the horizontal well. The results for theuniaxial and triaxial static testing are presented in Table I.The Mohr-Couiomb failure envelope was represented by a

    straight line for the rocks at the pay zone. This was notpossible for the rock at the KOP in which several envelopeswere drawn at different stress levels as is presented in Figures4 and 5. The line corresponding to the appropriate stress ieveiwas chosen (Fig 5) for the failure parameters for the caprock. The overbalance expected for this well was about 2000psi so the initial iinear envelope was considered to beapplicable to the conditions around the wellbore duringdrilling. However, it is known that for weaker rocks it isconvenient to consider a non-linear criterion [11]. Dynamicmeasurements were made under hydrostatic conditions [12]and during triaxial compression [6]. Comparison betweendynamic and static values for Young Modulus are presentedin Figure 6 together with the acoustic vaiues inferred from themechanical logging [13]. Laboratory dynamic vaiues werehigher than sonic log vaiues and static values by a factorranging from 1.2 to 2, respectively, at the measured points.

    In situ Stress Determination

    Most of the uncertainties in borehole stability problemsare reiated to the in-situ stress determination and rockstrength [14]. In this case a great effort was made to obtain areasonable estimate of magnitude and orientation of in-situstresses within the time limitations. Going from the regionaltectonic scenario to the iocal measurements was the approachin order to aid in the interpretation of local field and coretesting results. The structural history of the Maracaibo Basinis characterized by a complex structural system dominated byregional fauits. Repeated tectonic events and reactivation offaults are reported [15]. A perspective of the structural systemand results of focal mechanism studies for the region arepresented in Figure 7. The focai mechanisms allowed todetermine an orientation of the compressional principal axiswhich rotates from an E-W direction beiow 10 degrees ofNorth latitude to a transitional direction NW-SE and then toa NNE-SSW direction, The E-W orientation of thecompresional axis corresponds to the compression of theNazca piate and the NNE-SSW orientation resuits from themovements of the Caribbean plate agaist the South Americanplate [15], However, on a local basis the stresses may beredistributed depending on the proximity to iocal fauitssystems, making the interpretation difficult. The focalmechanism study also shows that at great depths principaistresses are not horizontal and vertical as is typicallyassumed. Whether this situation prevails at the upper layerswas difficult to asses at the time, but certainiy somesensibility analysis shouid be done in the models to considerthis possibility.

    Breakouts (3 inch size) were observed from the 4-armcaliper log run in the piiot hole together with an image log.The maximum elongation azimuth was 118 degrees (N62W)at 9500 feet. Therefore, the direction of the maximum

    458

  • SPE 370W GEOMECtiANICAL DESIGN AND EVALUATION Of A HORIZONTAL WELBORE IN MARACAISO LAKE, VENEZUEU REAL-DRILLING-llME APLICAllON 3

    principal stress component is interpreted as N28E. A soniclog with shear velocity anisotropy capability [13] showed amaximum stress direction between 15 and 20 degreesazimuth. This tool indicated a rotation in the direction ofmaximum stress to E-W at upper layers (depth). ASR testingwas also performed over three pieces of the oriented coreimmediately after the recovery [16]. The quality of the datawas not excellent and only one of these tests were consideredreasonably fair, resulting N135E. Anisotropic acousticvelocities and directional amplitude of acoustic shear wavesand differential strain curves [17] were obtained for this core.A summary of these results is shown in Figure 8. Note thatthe breakouts and anisotropic sonic log are showing a NNE-SSW trend. The ASR and differential strain analysis werecapable to see the maximum tectonic event in the area, whichis the E-W compression from the Nazca plate, The laboratorysonic tests @AA, SWAA), however, are showing thetransitional trend.

    In the interpretation of the set of data available for in-situstress direction it is important to make an assessment of thequality of the information. A general quality indicator is thestandard deviation of the stress direction for a single test.Particularly for the ASR, art absolute magnitude of relaxationabove 100 microinches is necessary for a reasonableinterpretation[ 18]. For a strong stress anisotropy thedifferential strain analysis should be showing the threeprincipal stresses at 90 degrees apart. Breakouts should bedistinguished from washouts and wall geometry induced bynatural fractures or rock heterogeneity. Depending on thequality, a weight can be given to the data at the time ofintegrating conflicting data as is presented in Figure 8. Afterall these considerations, for this case a higher weight wasgiven to the breakouts, the anisotropic sonic log (DSI) and thelocal focal mechanism closer to the Lake area.

    It was evident that it is necessary to gather moreinformation about in situ stresses and also clarify the featuresthat each of the tests are capable of measure to explain thedifferent results.

    Magnitude of in situ stresses:

    A cased hole minifrac was performed at a nearby well. Amtdtirate tests was done before and downhole pressuremeasurements allowed to determine breakdown and closurepressures as 7650 psi and 5560, respectively. A back-analysis of the minifrac data was considered, ignoring theeffect of casing, cement and perforations, using the followingwell known equation :

    ~=%,-K@b-p.)-2p.This gave a first rough idea of maximum horizontal stressmagnitude. The resulting gradient was 0.78 psi/foot. Frombreakouts and from an instability event in which mud weight

    had to he raised from 66 to 72 pcf to enhance stability, it wasalso possible to obtain another bound by assuming shearfailure at the borehole. Another bound for the maximumhorizontal magnitude was determined by assuming shearfailure, such that the Mohr-Coulomb failure equation wasapplied and the maximum horizontal stress obtained by back-anal ysis:

    a,= co+or@$r)

    That is, knowing the strength of the rock, the pore pressureand the minimum in-situ stress magnitude and orientation,the maximum horizontal stress can be back-calculated. The Jfunction was solved using an elastic approach with theBORE3D model. The resulting gradient was 0.84 psi/foot.

    The vertical stress component was estimated from densitylogs of nearby wells resulting in a gradient of 0.95 psi/feet.The density logs covered part of the total depth; however, anuniform gradient was assumed because of lack of betterinformation.

    The results of measurement of in-situ stress field indicatedat this location a stress regime characterized by SvXSH>Sh,which is characteristic of a passive basin with typical featuresof normal faults. If the set of normal faults were responsiblefor the stress state at this point, then the minimum horizontalstress component would be perpendicular to the normal fault.However, it seems as a first approximation from the datagathered, that the minimum horizontal component isparallel to the normal fault.

    Stability analysis during drilling

    The aim of this analysis is to provide minimum mudweight required to prevent collapse and maximum mudweight required to avoid exceeding the fracture gradient as afunction of inclination and orientation of the well. Theanalysis consists in calculating the stress concentration in thevicinity of the wellbore, which are mainly function of rockproperties and in situ stresses (magnitude and orientationrelative to the wellbore, and comparing these stresses with afailure criterion for the rock. I%is analysis has been doneusing a linear elastic model and Mohr-Coulomb strengthcriterion. An impermeable borehole wall was considered, i.e.100 % efficient mud cake. This is supposed to be a gmdassumption is this case because the mud designed proved tomake an efficient mud cake in laboratory tests.

    By the time of the initiation of the inclined well, theorientation of the in situ stresses was based on preliminaryresults (maximum horizontal stress component sub-parallel to

    459

  • 4 M. SANCHEZ, J. CABRERA, C. COLL SPE 370ss

    the fault and to the horizontal well). The input parameters forthe inclined section and the target zone for the horizontalwell are listed in Table II. The operational mud weightwindow for these zones as a function of hole inclination arepresented in F@ures 9 and 10. This was the wome case forthe insitu stress regime considered aod the lowest weight thatthe saline mud can preset (typically around 80 PCO waswithin the safe values. Comparing these curves, it is seen theinfluence of rock parameters in the operational mud weightwindow. For inclinations higher than 40 degrees theoperational window is broader for the target zone. Therefore,it would be misleading to apply this information for mudweight values for the inclined section once the higherinclinations are achieved. These may often happen becausethe information is mostly recovered from the pay zone. SoNclogs can help on this task by offering a strength profile rdongthe well, but they should be properly calibrated to lead tomeaninfulg results. In this experience the sonic loginterpretation was more conservative than the linear elasticmodel, main] y because there was not time to perform acareful calibration of the log.

    The operational window for the mud weight was releasedto the drillers by the time the pilot hole was being finished,which made possible its application in the field. Thehorizontal well was drilled with mud weight of 80 pcfwithout any stability problems. There is not a caliper log toverifjf if the hole was exactly in gauge, there is no evidence ofhole breakouts or washouts at both, the inclined andhorizontal sections.

    It is known that the linear elastic models can be overlyconservative, unless carefully calibrated with field data[ 14],and may overestimate the sensitivity of the hole stability towell trajectory [18]. Whether lower mud weights could beused safely and obtain in gauge holes in the field studied mustbe investigated as the horizontal well activities increase. Moredata for in situ stresses and post-analysis using other modelswill allow to have a better calibration and get moreeconomic designs.

    Stability during production

    An open hole completion without any liner was anopportunity in this well due the tehtively high strength of therock. Therefore, it was needed to determine a safe drawdownto avoid sanding or collapse of the hole. First attempt with thelinear elastic model predicted failure for any drawdownconsidered. The geomecam cal module of the program STARS[IO] was then used. This is a 2-D, plane strain program whichcan consider several constitutive models of the rock such aslinear elasticity, elastic perfectly plastic material and ageneralized plasticity model. A generalized plasticityconstitutive equation was used because it can model in a mom

    realistic way the rock behavior. The constitutive model isdescribe in reference [19].

    The modeling was done as if the horizontal well wetedrilled in the direction of the minimum in situ stress.Therefore, the transverse section of the hole will have asboundary stresses the vertical and the maximum horizontalstress components. Table II and Table 111present the strengthinput data and the parameters that define the constitutiveplasticity model [19]. These values were estimated from thestress-strain curves obtained in the lab. Figures 11, 12 and 13represent the maximum principal stresses induced around theborehole for three different drawdown values: 500 psi, 6(HIpsiand 800 psi. Note how the stress concentration and thestressed zones increase as the drawdown increases. To assesif these stress conditions lead to failure of the rock, the mostcritical stress state at the borehole wali was plotted in theMohr space to compare with the Mohr-Coulomb failurecriterion. As shown in Figure 14, as the drawdown increases,the points grow toward the failure, The analysis was carriedon up to a drawdown of 800 psi because this was a particularoperational restriction related to gas lift. Ihe horizontal wellis now producing 2tM0 SBPD steadily without sandingproblems or any stability problems.

    Conclusions and Recommendation

    Operational window for mud weight was given for thehorizontal well drilling during drilling time. This studyallowed to make an open hole completion without any linerfor a horizontal well in a sandstone reservoir for the fwsttime in Venezuela. This type of analysis should be done in anormal basis for horizontal wells to study its integrity duringdrilling and during production.

    The calibration of the linear elasticity model must berefined including more field data as horizontal drillingactivities are increased. This is important in order to be lessconservative and maintain, at the same time, the advantagesof simplicity, little computational and time effort of thesemodels. Calibration of the mechanical logs will also enhancestrength predictions from this source in order to obtain lessconservative designs for all the well profile and not justsome discrete point in which cores are available.

    The magnitude of the maximum horizontal stresscomponent can be estimated through back-calculations byconsidering plasticity models and geometry of the breakouts.

    It was evident in this horizontal well that the design ofmechanical sealers for the drilling mud minimizedformation damage, which is a vmy important issue in thistype of mature reservoitx. IWs is also a way to enhancestability of the well as the infiltration and extensive porepressure modification around the wellbore is pmwented.

    460

  • SPE 37tma GEOMECHANICAL DESIGN MD EVALUATION G A HORIZWWM ~E IN MARACNSO ME, VENEZUEIA: REAL-ORILUN&TIME APLICATKX 5

    Nomenclature:

    PoKm

    OHcrhGrdco, 1$

    PbEv

    UcsToCp,crw. @Pn

    a

    m

    = reservoir pore pressure.= poroelastic parameter (1S K< 2).= vertical in situ stress coqtponent.= maximum horizontal in situ stress component.= minimum horizontal in situ stress component.= radial stress at the borehole wall.= tangential stress at the borehole wall.= cohesion and fnction angle from A40hr-Coulomb

    strenght criterion..= Breakdown pressure.= Youngs modulus.= Poissons ratio.= unconfined compressive strength= tensile strength of the rock.= peak and residual cohesion

    = initial and peak fnction angles,= cohesion softening parameter= friction hardening parameter= yieidfinction curvature

    AcknowledgmentsThe authors wish to thank the management of INTEVEP,S.A. and MARAVEN S. A., for permission andencouragement to public this paper, and also the manycolleagues who participated in this study in the differentdisciplines: Alberto Munoz, Maria de Blundum, GediGonzalez, Jose Luis Zkit, Gilberto Lopez, Maria G.Faustino, Jose A. Natera, Jose A. Linarez, Lemniz Zerpa,Kerin Urrecheaga, Jose Guzman, Ivanka Kancev, JesusBetancotrrt, Jose Castillo and Entique Poleo.

    References

    1. Skopek, R.A. Rock Characterization in Reservoirs Targeted forHorizontal Drilling JPT, December, 1993.

    2. Zoback, M.D. , Moos D. , Mastin L. and Anderson, R. WellBore Breakouts and In Situ Stress , Journal of GeophysicalResearch. Vol. 90, No. B7, pages 5523-5530, June 10, 1985.

    3. Schrdmberger, Wireline & Testing, DSI SoNco dipolar deCizathzrniento por lmagenes

    4. El Rabaa, A.W.M. and Meadows, D.L. Laboratory and FieldApplication of the Strain Relaxation Method, paper SPE15072 presented at the 56th California Regional Meeting of theSPE, Oakland CA, April 2-4, t 986.

    5. Strickland, F.G. and Ren N.K.; Predicting the lrr-Sittr Stressfor Deep Wells Using Differential Strain Curve Anatysis,paper SPE presented at the 1980 SPEJDGE on UnconventionalGas Recovery, Pittsburgh, May 18-21.

    6.

    7.

    8,

    9.

    10.

    11.

    12.

    13.

    14.

    15.

    16.

    17.18.

    19.

    Ter-ratek, Static and Dynamic Properties and In-Situ StressDirection, Unidad @o Treco Maraven, S.A., Caracas.February 1996.Economies, M., J., and Nolte K., G.fl Reservoir Stimulation,Second Edition. Prentice Hall, Englewood Cliffs, New Jersey07632, 1989.

    Da Fontoura, S., Bore3D, Version 1.02, Release Alpha, UsersManual, Rock Mechanics Consortium Report, RMC-92 13,University of Oklahoma, 1992.Kancev, L, Guzman J.H.,Polco, E., Feranactez, D., Castillo J.,Betamcourt, J.S. Prrrebas de Dafio de Forrnacion con IodoThixsat en el pozo VLC-1 184, INTEVEP Intemat Report, inprogress, 1996.Rodriguez, H., Fung, L.S-K, Silva, R., zerp~ L. and Wan,R.G.,Themral Simulation of Horizontal Wellbore Stability inUnconsolidated Heavy Oil Reservoirs, paper SPE 37102presented at 1996 International Conference of Horizontal WellTechnology, Calgary, Canada.Mclean, M.R. and Addis, M. A,: Wellbore Stability Anatysis:

    A Review of Current Methods of Anatysis and llseir FieldApplication paper SPE 19941 presented at the 1990IADC/SPE Drilling Inference, Houston, Feb.27-March.2.Sanchez D, M., Cabrera J. R., Munoz R., A. , Faustino M.,Natera J. Diseno Integmdo del Pozo Horizorrtat VLCI 184,hrtemal INTEVEP Internal Report, in progress, 1996.Schhtmberger-GeoQuest., VICI 184 Bkque 111,Resumen deProcesarniento e tnterpretacion, Maraven, S. A., Caracas.,Febmary 16, 1996.Morita, N. Uncertainty Anatysis of Borehole StaMlityProblems, paper SPE 30502 presented at the AnnualTechnical Conference & Exhibition, Datlas, October 22-25,1995.Malave G. Deforrnacion Corticaf y Sisrnicidad SupeKlcial

    Reciente en el Occidente de Venezuela lmplicacionesTectonics Regionafes. INTEVEP Internal Report INT-03279,96.Halliburton., ASR Testing at the Maracaibo Lake, Venezuela,Well VLC-I 184, Maraven S. A., Ciudad Ojeda (LasMorochas), Zulia, Venezuela., January 14, 1996.Abass H. Personnal Communication , 1996.Law, N.C. and McLean, M.R. Assessing the Impact of

    Trajectory on Wells Drilled in an Overthrust Region pap?rSPE 30465 presented at the 1995 SPE Annual TechnicalConference and Exhibition, Dallas Oct. 22-25.CMG, Wellbore Stability Simulation for Vertical andHorizontal Wells, INTEVEP S.A. Dec., 1995.

    461

  • 6 M. SANCHEZ, J. CABRERA, C. COLL SPE 37066

    Depth(feet)

    9483109483294846

    9483 1095773957729579795801095772

    Confining Peak Youngs Poissonpressure Stress Modulus Ratio

    (psi) (Psi) (10 bpsi) (10 bpsi)

    o258255259979

    00

    258255847527

    551115415209492632141603995147522659032549

    1,52 0,382,45 0,162,00 0,112,27 0,131,66 0,351,26 0,255,00 0,283,06 0,213,39 0,14

    Table I. Uniaxial and Triaxial Testing Results.

    Table II. Geomechanical Input Parameters

    462

  • SPE 37088 GEOMECHANICAL DESIGN ANO EVALUATION OF A HORIZONTAL WELBORE IN MARACAIBO IAKE, VENEZUEIJ! REAL-DRILLING-TIME APPLICATION 7

    ,

    Fig. 1 Location of the Horizontal Well in theField

    lm 1s,oOO

    *MO I

    l

    Ak Imh 9.7W mm- B7ar

    3-L...Fig 2. Well Profile and Completion Design.

    +-=-+ CORINGrrzs=--l I ~ w~K.O.P

    -d,!. .= em t TrmmalsJ

    4-4ShaSecomD.s677 Tri.walsas HORIZONTALTARGET- muadcama.m *am.

    Fig

    Fig 3. Depth of coring in the Vertical Pilot Hole.

    463

  • 8 M. SANCHEZ, J. CABRERA, C. COLL SPE 37088

    Fig 7. Focal Mechanisms Analysis.

    -wA/iNosl

    w DoL FOCALMm-l.

    o

    Fig 8. In situ Stress Analysis from Different Sources.

    Fig 10. Operational Window the for Pay Zone (mudweight vs. inclination).

    . .......s . . .. m.,.,=.,,,,. . .. ,,.. .,, .... .

    ~.. ..,-. .-AZ-!-.,. ., ..w., !; .;. . ..-,, . . .

    Fig 11. Maximum Effective Principal Stress atDrawdown = 500.

    464

  • SPE 37088 GEOMECHANICAL OESIGN AND EVALUATION W A HCfUZONTAL WELSCX?E IN MARACN80 MI(E, VENEZllE~ REAL.DRKLIN5TIME APLICAllON 9

    Fig 12. Maximum Effective Principal Stress atDrawdown = 600,

    Ii

    StKlu

    00 swo MmrBma120u092soo 03mo 35ao

    Noru181strc.s%psiFlg 14. Mohr-Coulomb Failure Envelop

    Showing Sress State for IncreasingDrawdown Conditions.

    Fig 13. Maximum Effeetive Principal Stress atDrawdown = 800.

    465