Fig. 1. Well field location

Similar documents
EXERGY ANALYSIS FOR THE AHUACHAPAN AND BERLIN GEOTHERMAL FIELDS, EL SALVADOR

SUSTAINABILITY ANALYSIS OF THE BERLIN GEOTHERMAL FIELD, EL SALVADOR. Manuel Monterrosa, LaGeo El Salvador

FIRST SEVEN YEARS OF EXPLOITATION AT THE MIRAVALLES GEOTHERMAL FIELD

ANALYSIS OF TEMPERATURE AND PRESSURE MEASUREMENTS AND PRODUCTION DATA FOR BERLÍN GEOTHERMAL FIELD, EL SALVADOR

The model was developed on the TETRAD reservoir simulator.

TWENTY FIVE YEARS OF PRODUCTION HISTORY AT THE MOMOTOMBO GEOTHERMAL FIELD, NICARAGUA

Geothermal Development in El Salvador Update

The Momotombo Reservoir Performance upon 27 Years of Exploitation

MODELING OF THE MUTNOVSKY GEOTHERMAL FIELD EXPLOITATION IN CONNECTION WITH THE PROBLEM OF STEAM SUPPLY FOR 50 MWe PP

RESPONSE OF OLKARIA EAST FIELD RESERVOIR TO PRODUCTION

ANALYSIS OF WORKOVER TECHNIQUES IN GEOTHERMAL WELLS OF CERRO PRIETO FIELD, MEXICO

Numerical Analysis of MCY01 Production Well Mechanism: Understanding of Well Coughing Phenomenon and Irregular Productivity

30 Years of Tongonan-1 (Leyte, Philippines) Sustained Production

NOTICE CONCERNING COPYRIGHT RESTRICTIONS

NET POWER CAPACITY OF GEOTHERMAL WELLS VERSUS RESERVOIR TEMPERATURE A PRACTICAL PERSPECTIVE

Evolution of the Miravalles Geothermal Field in Costa Rica after Ten Years of Exploitation

The Geysers Geothermal Field, an Injection Success Story

The Geysers Geothermal Field, an Injection Success Story

Multiple Zone Geothermal Stimulation Case Study: Fluid Diversion Using Thermo-Degradable Zonal Isolation Materials

Iceland Deep Drilling Project IDDP

GEOCHEMICAL CHARACTERIZATION AND INTEGRAL ANALYSIS OF DATA LAS PAILAS GEOTHERMAL FIELD, COSTA RICA

Flow Testing Results from Habanero EGS Project

REASSESSMENT OF THE THELAMÖRK LOW TEMPERATURE GEOTHERMAL SYSTEM IN N-ICELAND FOLLOWING SUCCESSFUL DEEPENING OF WELL LÞN-10

IMPROVED POWER PRODUCTION EFFICIENCY OF HYDROTHERMAL RESERVOIRS USING DOWNHOLE PUMPS

Successful Perforation Operation Experience in a Geothermal Well of Salavatli Geothermal Field

CLASSIFICATION OF GEOTHERMAL SYSTEMS A POSSIBLE SCHEME

INJECTION EXPERIMENTS IN LOW-TEMPERATURE GEOTHERMAL AREAS IN ICELAND

Discrete Fracture Embedding to Match Injection Returns in a Single Porosity Model

RESERVOIR ENGINEERING AND GEOTHERMAL POWER PRODUCTION IN OLKARIA

PRELIMINARY RESERVOIR ENGINEERING STUDIES 0 F THE MIRAVALLES GEOTHERMAL FIELD, COSTA RICA

GEOTHERMAL RESOURCE ASSESSMENT CASE EXAMPLE, OLKARIA I

Benefits from the Utilization of a Calcium Carbonate Inhibition System for Production Wells at the Miravalles Geothermal Field

ABSTRACT. Figure 1. Geothermal areas of interes in Guatemala 2. AMATITLÁN GEOTHERMAL FIELD

COSTA RICA COUNTRY UPDATE

NOTICE CONCERNING COPYRIGHT RESTRICTIONS

Geothermal Well Productivity: Why Hotter is Not Always Better

Geothermal Resources and Development in Guatemala Francisco Alberto Asturias

REINJECTION STRATEGY FOR GEOTHERMAL SYSTEMS

NOTICE CONCERNING COPYRIGHT RESTRICTIONS

INCREASED PRODUCTION LOAD IN TONGONAN GEOTHERMAL FIELD, PHILIPPINES: RESERVOIR RESPONSE AND FIELD MANAGEMENT STRATEGIES

THERMAL EXTRACTION ANALYSIS OF FIVE LOS AZUFRES PRODUCTION WELLS. Luis Quijano GPG Com. Fed. de Elec. Morelia, Mich.

Baigcng Hu. Thermal Engineering Depaarnent, Tsinghua University, Beijing, , P. R. China

Interpretation of the Injection and Heat Up tests at Sabalan geothermal field, Iran

V.L. Relativo-Fajardo, P.P. Gerona and D.O. Padua

Water Dependency of Geothermal Power Generation Systems

Production/Injection Optimization Using Numerical Modeling at Ribeira Grande, São Miguel, Azores, Portugal

Russell James. D.S.I.R., Wairakei Private Bag, Taupo New Zealand. Flow, kg s RADIAL FLOW CALCULATIONS

MASTERING REINJECTION IN THE HELLISHEIDI FIELD, SW-ICELAND: A STORY OF SUCCESSES AND FAILURES

Ahmad Yani PT. Pertamina Geothermal Energy Lahendong, Jl. Raya Tomohon no. 420, North Sulawesi

Recent Geothermal Well Work-Over Experiences at the Kawerau Geothermal Field, New Zealand

The Response to Exploitation of the Los Humeros (México) Geothermal Reservoir

Magma On the other hand, molten rock is under active volcanoes at accessible depths. The temperatures excess 650 o C.

NOTICE CONCERNING COPYRIGHT RESTRICTIONS

Experiences, Successes and Challenges in Sustaining Long-Term Production at the Tiwi Geothermal Field

SIMULATION AND PERFORMANCE ANALYSIS OF THE NEW GEOTHERMAL CO-GENERATION POWER PLANT (OV-5) AT SVARTSENGI

Utilizing Vertical Discharge Tests as an Effective Means for Well Decision Making at the Darajat Geothermal Field, Indonesia

Improved Efficiency of Solid Trap Installed in Brine Injection Pipeline of Leyte Geothermal Production Field, Philippines

Nodal Analysis Approach in Minimizing Pressure Losses to Improve Well Productivity

Geothermal Energy Future Development

Study of an EGS Power Plant Preliminary Feasibility Design by an Assumed Productivity Index

Steam Supply Sharing Through Steamline Interconnection The Tongonan Geothermal Field Experience, Philippines

Decline Curve Analysis for Production Forecast and Optimization of Liquid-Dominated Geothermal Reservoir

NOTICE CONCERNING COPYRIGHT RESTRICTIONS

Performance Analysis and Stimulation of Dry Steam Wells in Mak-Ban Geothermal Field, Philippines

Modelling of Injection into Geothermal Systems E. KAYA 1. Department of Engineering Science, University of Auckland, Auckland, NZ M.J.

Neutralization of Acid Fluids from Well H-43 (Superheated Steam), Los Humeros Geothermal Field, Mexico.

PHASES OF GEOTHERMAL DEVELOPMENT

- significant production increases and no temperature decrease in the wells around the injector. - almost complete vaporization of the injected water;

A SYSTEM DYNAMICS APPROACH FOR EGS SCENARIO ANALYSIS

Injection Management in Kawerau Geothermal Field, New Zealand

FLOW TESTING IN INDONESIA USING ALCOHOL TRACERS

Geothermal Energy in El Salvador

Measurement of Two Phase Flows in Geothermal Pipelines Using Load-Cells: Field Trial Results

STANFORD, CALIFORNIA SGP-TR-84 SG P-TR GEOTHERMAL RESERVOIR ENGINEERING. Stanford Un iver s i t y. Stanford, California

ENVIRONMENTAL IMPACT ASSESSMENT OF GEOTHERMAL PROJECTS IN ICELAND

Enhanced Geothermal Systems (EGS): Comparing Water and CO 2 as Heat Transmission Fluids

Engineering Geothermal Systems in Oil and Gas Reservoirs. Susan Petty Bill Livesay Black Mountain Technology

Methods of Early Geothermal Energy Resource Assessment A Modern Conceptual and Mathematical Model

Challenges in the Design and Management of a 20-MW Geothermal Field: the Maibarara Geothermal Field (Philippines) Experience

A Comprehensive Well Testing Implementation during Exploration Phase in Rantau Dedap, Indonesia

ACID STIMULATION OF GEOTHERMAL RESERVOIRS

Reservoir Management at the Miravalles Geothermal Field, Costa Rica

ORMAT Nevada, Inc. Expansion and Improvements Raise Power Production 20%

SHALE FACTS. Production cycle. Ensuring safe and responsible operations

A SPREADSHEET FOR GEOTHERMAL DIRECT USE COST EVALUATION. Kevin Rafferty Geo-Heat Center

Evaluation of Water Produced from a Steam Dominated System, a Case Study from the Darajat Field

SuperWell. A Simple Well Bore Flow Simulator in Spreadsheet Format. Mike Timlin

EVALUATION OF MICROGRAVITY BACKGROUND AT THE UNDISTURBED OGUNI GEOTHERMAL FIELD, JAPAN

Micro-earthquake Observation Results in the Ogachi HDR Project

ALCOHOL TRACER TESTING AT THE MATSUKAWA VAPOR-DOMINATED GEOTHERMAL FIELD, NORTHEAST JAPAN

INTERPRETATION OF DRAWDOWN TEST DATA FROM OLKARIA DOMES GEOTHERMAL FIELD A CASE STUDY OF OW-907B, OW-912B AND OW-917

Production Performance Optimisation

RECENT ACTIVITIES AT THE CERRO PRIETO FIELD. 2 Lawrence Berkeley Laboratory Coordinadora Ejecutiva de Cerro Prieto

Maintenance history of surface pipes and plants case history of the Svartsengi geothermal plant

THE ROLE OF WELL TESTING IN GEOTHERMAL RESOURCE ASSESSMENT

Geothermal Power Capacity of Wells in Non-Convective Sedimentary Formations

Calculation of Geothermal Stored Heat from a Numerical Model for Reserve Estimation

PRELIMINARY STUDY OF DISCHARGE CHARACTERISTICS OF SLIM HOLES COMPARED TO PRODUCTION WELLS IN LIQUID-DOMINATED GEOTHERMAL RESERVOIRS

NEW HORIZONS FOR DESALINATION

White Paper: Shale Gas Technology. September Shale Gas Technology 2011 NRGExpert Page 1 of 8

Transcription:

-................... - PROCEDINGS, Twenty-First Workhop on Geothermal Rcaavoi Engln- Standford Univmfty, Standford, Catllomls, Jan- 22-24,1996 SGP-TR-151 SIMULATION STUDIES FOR WELLS AH-4bis/AH-17 and AH-18, AHUACHAPAN GEOTHERMAL FIELD. Manuel Ernest0 Monterrosa Recursos Geotermicos Comision Ejecutiva Hidroelictrica del Rio Lempa CEL PO box 2669 San Salvador, El Salvador. ABSTRACT. Well AH-4bi, at the Ahuachapan Geothermal Field is planned to be drilled on the same pad as the former AH-4. A simulation study was carried out for two casing dameters 13 5/8 and 9 5/8 in order to estimate its production and to know its economic feasibility. The simulation results indcate a high probability of production in the range of 7 Mwe, equivalent to 120 kg/s total mass flow rate, 1250 Idkg at 6 bar-a for the new well AH-4b;B. Well AH- 17 is good producer, during 199 1 after ten years of production, the well was shut-in due to silica scaling problems. A wellbore simulation was carried out in order to predct the new production condtions after the work-over, mainly to estimate the water flow rate in order to reduce the silica scaling. The results indcate a very low water flow rate. The match between the simulated and measured production curves after the work-over was successful. production of energy began in 1975 when the first 30 Mwe condensing unit came on line. During 1976 a second unit of 30 W e was installed. Finally during 198 1 thrid double-flash unit of 35 Mwe increased the total installed capacity to 95 Mwe. The steam production for power generation started in June 1975 when Unit 1 went into operation, which required the operation of the producer wells AH-1, AH-4, AH-6 and AH-7. During the exploitation period, the productivity of the field decreased due to a decline in the reservoir pressure and limited drilling of makeup wells. Wells AH-4, AH-17 are located in the central part of the field, well AH-18 is located at the southern part of the borefield, Figure 1 shows the well sites. The well AH-18 is located at the southern part of the actual bore field. CEL is planning to expand the borefield at this area and it is neccessary to estimate the possible production condtions at that zone. The results indicate a high probabilty of production at that area. The power potential is estimated at 3.5 Mwe per well at WHP 6 bar-a and the wells will not require induction. INTRODUCTION The Ahuachapan Geothermal Field is located 3 km away from The city of Ahuachapan at the eastern part of the country. The commercial Fig. 1. Well field location 101

The actual power scheme requires the increasing of the steam production of the field. CEL is planning to carry out some projects or activities in that sense. As part of these activities, the work-over for well AH-17, the drilling of well AH-4bis and, the drilling of make-up wells represent an important target for the reservoir engmeering studles. WELL AH-4 bis. The previous well AH-4 was drilled from June to August 1972, the well site is in the central part of borefield with coordinates 310,835 E and 412,470 N; the casing program was as follows: Hole diameter Depth Casing size Depth 26" 52m 20" 50 m 17 %,, 485 m 13 318" 481.5 m The simulation study was carried-out using the wellbore simulator HOLA. This simulator was developed by Orkustofnun (Iceland); HOLA reproduces the measured flowing temperature and pressure profiles in flowing wells and determines the relative contribution of each feed zone for a given dwharge condtion (Bjornsson, 1992). The flow within the well assumes steadystate conditions at all times, but time changmg reservoir pressures are allowed. The output curves and some temperature and pressure profiles of well AH-4 were considered as initial or matching con&tions due to the lack of flowing profiles. Figure 2 and 3 shows the total mass flow rate and mixture enthalpy for several output test measured at the former well. Well AH-4 was considered a good producer with a total mass flow rate close to 130 kgk, 23.5 kg/s of steam, 18 % of dryness, 1300 kjkg of enthalpy for a Well Head Pressure of 7 bar-a ( Withersp.n, 1977). The main feed zone was located between 480 to 600 m depth. In June 1975 well AH-4 went on line in order to contribute the operation of Unit 1. The power capacity of this well was close to 12 Mwe during that period. Due to possible casing corrosion and poor cementing, CEL in 1982 decided to carry out the work-over operation, the objective was to change the casing design and repair the casing damaged. After it was repaired, the feed zone was cemented. The permeability and the production rates of the well changed and became very low. In order to increase the steam production of the actual borehole field, CEL is considering drilling a new well on the same pad of the previous AH-4 well, 50 m SE away from the previus well to intersect the original feed zone and fracture for the former well, considering no effect of the cementing no more than 20m away from the center of the previous well (CEL, 1992). - m 88............ \ 0 1 0,, ',,, /,,,,, j,,,,, / 5 10 15 20 WHP (bar-a) Fig. 2. Output test, well AH-4 The former well, since its start into operation was affected by the pressure drawdown and boiling around the well as observed in Fig. 2 and Fig. 3 but after the work-over the permeability of the well was very low. The main assumptions and input data used for the simulator were: a) The production zone is located at 640m depth with a Productivity Index (PI) of 0.9E-'' kg/slm3 similar to well AH-4. 102

b) The flowing enthalpy for the new well is between 1250 to 1650 kjkg. c) Due to the pressure drawndown, the flowing pressure in the well will be close to 16-18 bar-a and the reservoir pressure is 20 bar-a (actual average pressure of the reservoir). output curves for different liner dmneters with constant 1250 kjkg enthalpy. Figure 6 shows an integrated curve for 6 bar-a constant well head pressure and enthalpy between 1250 to 1650 Hkg. 20 1000 5 10 15 20 WHP (bar-e) Fig. 3. Discharging enthalpy, well AH-4 8 10 12 WHP (bare1 Fig. 5. Simulated curves for different liner diameter Figure 4 shows the matching curve for the simulation adjustment. 80-6iaul.bdr.unlll850WIkpJ 20 / 1 1,,,,,,, 1,,,,,,,,,,,,,I I I,,,,,,,, 7 8 9 10 11 12 13 1 28 10 15 20 WHP (bar-o) Fig. 4. Simulated and measured output curves An important role for this simulation is to make a decision about the new well desing, as well as, the new production rate and the estimated output curve for this well. Figure 5 shows the simulated LInner d lameter ( Inch) Fig. 6. Flow rate for different liner diameter. The results of the study suggest the follow a) The bottom hole depth of the new well will reach 700 m in order to mantain the same production rates as the former well. 103

b) The casing design will require 13 518 production casing down to 300-400 m depth just on the cap rock of the reservoir and 9 518 slotted linner down to the bottom hole. c) The production of the well AH-4bi. will reach 7 MWe for the actual reservoir conditions and similar permeability as the former well; but the liner Qameter is reduced to 7 5/8 the production will be 40% lower than 9 518. WELL AH-17. Well AH-17 is located in the central part of the actual borehole field, its coorqnates are 310,781 E; 411,697 N, elevation 773 masl. It was drilled from June to August 1976, the casing desing is the following: main target was to evaluate the liquid phase production and its changes for different WHP. It was also necessary estimate the new production parameter in order to evaluate the silica scaling inside the casing. Again the wellbore simulator HOLA was used for this work. Two flowing profiles carried out with scaling into the well during 1992 were used for matching purposes. Well AH-17 was modelled with a 7.5 scaling Qameter and 100 m scaling length as observed in Figure 7. -u I 1 1 7 r 1 : Jlt Hole size Depth (m) Casing size Depth (m) 17 % 105 13 318 104 12?4 452 9 518 450 8 %, 1200 7 518 440-1200 The main production zone for this well was located at 480 m depth just on the steam cap of the reservoir. From October 1976 to June 1978 this well was used as an injection well due to the lack of a Qsposal channel and injection wells. In 1981 a work-over operation was carried out in order to install slotted linner into the open hole. As this well produces dry steam, in 1981 it was connected to the power station. In 1991 after almost 10 years of continuous production, the well showed silica scaling in the production casing and steam pipeline. AccorQng to CEL s studies and Consultants recommendations (Electroconsult, 1993), the silica scaling could be reduced by increasing the WHP (change on the production characteristics) in order to increase the liquid phase, in this case the silica could be diluted and could move together with the liquid phase. Fig. 7. Simulated and measured curves, well AH-17. The matching was achieved with a Productivity Index equal to 0.23e-10 k8/s.m3, the main feed zone was located between 475 to 600 m and a very low permeability at the bottom. After the work-over operations, the mass flow rate from the well will tend to increase, Figure 8 shows the simulated output test for well AH-17 without scaling. The figure also shows the simulated curve with two measured output curves after the work-over operation, in both cases the error between the measured and simulated curves is less than 20 %. LI In 1994 CEL carried out the work-over in well AH-I7 in order to clean and remove the silica scaling from the production casing. A simulation study has been prepared in order to simulate the production and the output test. The 1 04

40 7 7 :- 35...... my ma :.... Dei IW - Smul*darrr. 30...... -... 9 20-101 5 1 5 1 0, I ( /, I l l, I l l I l l, 5 10 15 20 WHP (bar-a) Fig. 8. Simulated and measured output curves, well AH-17. The simulation results suggest only dry steam production with dryness over 90% (mist flow pattern) for a wide range of WHP, therefore the change in the operation parameters will not increase the liquid phase flow rate for the well AH-17, perhaps due to the steam cap production. WELL AH-18 Well AH-1 8 is located at the southern part of the actual borehole field, its coordnates are 309,745 E, 412,852 N and elevation 926 masl. The well was drilled from March to May 1977 and the casing desing is presented in the following table:... Hole size Depth (m) Casing size Depth (m) 17 %, 108 13 318 105 12 % 625 9 518 624 8 %, 1256 7 518 614-1256 southeastern areas. The target for the simulation stuqes is based on the estimation of the production rates of the new wells. In fact we have been using similar Productivity Index to those of other production wells in the field. It is also necessary to analize the reason for the low production rate for well AH-18 to determine if the new wells will require induction. Agam, wellbore simulator HOLA was used for this work but due to the lack of data on production flow rates or flowing profiles, the matching process was carried out using the static profiles considering a normal temperature and pressure drawdown and some dlscharge data. An upper production zone at 800m and another one at a depth of 1200 m was used for the simulation, correlating it with the circulation losses during drilling. The Productivity Indexes from the simulation were O.lE- and 0.1E m3 to match with -3 bar-a and 24 kg/s flow rate as measured during a test in Aug. 1984. If well AH- 18 or the new well in this area could maintain a long term Qscharge and considering the same PI for the required WHP (6 bar-a), to connect the well to the power plant, the simulator indlcates the total flow rate will reach 7 kg/s with 12% of dryness. In that situation the feasibility of the operation can not be economical. Figure 9 shows the HOLA results. Despite the unsuccessful production results from AH-18, its the high measured temperature and the temperature contours suggest an upflow at this area, in thls sense a PI of twice that of the production wells in the field was used (e.i. 0.2 E- m3). A flow test report indicates low flow rate and production declining with time (few hours). The mass flow rate ranges from 24 to 3 1 kg/s and the enthalpy is about 1030 Hkg. Several injectivity test inqcate 1.6 lts/skg/cm2g for the Injectivity Index, this index is lower that of other wells in the field. Within the scope of the Ahuachapan Stabilization Project, CEL is considering drilling new production wells at the south and 105

production characteristics for flowing wells at low cost and time. This simulator represent a very useful tool for the reservoir engineering stuqes. 0 The simulation study for well AH-%k inqcates hgh probablity of obtaining a good production well with total flow rate close to 40 kgs, 1250 Idkg enthalpy for a WHP of 6 bar-a. The power capacity will reach 7 Mwe with the actual reservoir conqtions. If the linner Qameter is changed from 9 518 to 7 518 the production could be reduced to 40% of the total production from the well. hme ih - 01 Fig. 9. Simulation results well AH-18, WHP 6 bar-a and equal PI. The results indicate flow rates of 60 kgk, 15% dryness and 9 kg/s of steam. The power capacity for each well will reach 3.5 Mwe with 6 bar-a WHP. The wells may not require air induction. The results are shown in the Figure 10. 0 The new production characteristic of well AH- 17 without scaling have been estimated and the liquid phase rate calculated for several well-head conditions. Furthermore, the liquid phase production will be less than 10-5 % of the total mass, therefore in this manner it be difficult to reduce the silica scaling. 0 The low production rate of well AH-18 is due to the low surrounqng permeability, the high temperature indicates a convective zone nearby, with higher permeability and an upflow area, in the case that higher permeability is found, the WHP will be hgher, hence the well will not require induction, and CEL believes the new wells will be good producer. REF ERENCES. Bjornsson Grimur, Arason Pordur and Bodvarsson Gudmundur, Sept. 1992. The Wellbore Simulator HOLA, User s Guide. CEL, EstuQo de Factibilidad Pozo AH-4bis, Octubre 1992, Internal report. Fig. 10. Simulation results, well AH-18, WHP 6 bar-a and double PI. CONCLUSIONS 0 A wellbore simulator HOLA has been successufully used to estimate the main ELC Electroconsult SPA, Aug 1993. Informe de Msion de Enfoque Programa Integral de Estabilizacion del Campo Geotermico de Ahuachapan. Witherspoon Paul, May 1979. Analysis of Reservoir Behavior at Ahuachapan Geothermal Field. 106