+ All Categories
Home > Documents > ) P'UNvGEOTHbKMALVENTURE · 2018-08-02 · PGV respectfully submits the following documentation for...

) P'UNvGEOTHbKMALVENTURE · 2018-08-02 · PGV respectfully submits the following documentation for...

Date post: 08-May-2020
Category:
Upload: others
View: 3 times
Download: 0 times
Share this document with a friend
22
/- . \ '\) P'UN"vGEOTHbKMAL VENTURE A Hawaii Partnership December 9, 1991 Mr. William Paty Chairperson state of Hawaii Department of Land P.O. Box 621 Honolulu, Hawaii Dear Mr. Paty: and Natural Resources 96809 Subject: Puna Geothermal Venture Project Well Kapoho state 1-A (KS 1-A) Upon review of the drilling and testing results from the Puna Geothermal Venture (PGV) field development to date, PGV has decided to convert well KS 1-A from a production well to an injection well. The geologic rationale for this decision is detailed in the Hydrogeologic Model of the Puna Geothermal Venture Geothermal Resource Update dated October 22, 1991, which was submitted to your office on October 24, 1991. The conversion of the KS 1-A well into an injection well will require execution of a 'I'esting and Injection Program as specified in the Underground Injection Permit No. 1529. This program was subtllitted to the Hawaii state Department of Health (DOH) and copied to your office for review and approval on November 25, 1991. The conversation of the KS I-A well into an injection well is not expected to require further modification to the well at this time. -:Richard P esident Geothermal Venture cc: C. Hew, DOH J. Lewin, DOH D. Nakano, DLNR M. Tagamori, DLNR E. Tanaka, DLNR 91208.011 101 Aupuni Street, Suite 1014-8, Hilo, Hawaii 96720 (808) 961-2184 Facsimile (808) 961-3531
Transcript

/-. ~\/ \ '\) ~

P'UN"vGEOTHbKMAL VENTUREA Hawaii Partnership

December 9, 1991

Mr. William PatyChairpersonstate of HawaiiDepartment of LandP.O. Box 621Honolulu, Hawaii

Dear Mr. Paty:

and Natural Resources

96809

Subject: Puna Geothermal Venture ProjectWell Kapoho state 1-A (KS 1-A)

Upon review of the drilling and testing results from the PunaGeothermal Venture (PGV) field development to date, PGV hasdecided to convert well KS 1-A from a production well to aninjection well. The geologic rationale for this decision isdetailed in the Hydrogeologic Model of the Puna GeothermalVenture Geothermal Resource Update dated October 22, 1991, whichwas submitted to your office on October 24, 1991.

The conversion of the KS 1-A well into an injection well willrequire execution of a 'I'esting and Injection Program as specifiedin the Underground Injection Permit No. 1529. This program wassubtllitted to the Hawaii state Department of Health (DOH) andcopied to your office for review and approval on November25, 1991.

The conversation of the KS I-A well into an injection well is notexpected to require further modification to the well at thistime.

~~~~~~:.-:RichardP esidentGeothermal Venture

cc:C. Hew, DOHJ. Lewin, DOHD. Nakano, DLNRM. Tagamori, DLNRE. Tanaka, DLNR

91208.011

101 Aupuni Street, Suite 1014-8, Hilo, Hawaii 96720 • (808) 961-2184 • Facsimile (808) 961-3531

~/iJrld-

PUNA GEOTHnRMAL VENTURbA Hawaii Partnership

November 25, 1991

t.. ,"

Dr. John Lewin, M.D.Directorstate Department of HealthP.O. Box 3378Honolulu, Hawaii 96801

Dear Dr. Lewin:

SUbject: Puna Geothermal Venture ProjectUnderground Injection Control (UIC)UIC Application No. UH-1529

.. \

.... '~. ~

-.... \..,'

i;,:~;~--'\

.....,.-'

,"

Pursuant to the Authority to Construct Underground InjectionWells issued to Puna Geothermal Venture (PGV) by the StateDepartment of Health on March 16, 1990 in the form of a letter,PGV respectfully submits the following documentation for yourreview and approval:

1. Production and Injection Well Casing MonitoringProgram, dated November 21, 1991;

2. KS-3 Testing and Inspection program, dated November 21,1991; and

3. KS-IA Testing and Inspection program, datedNovember 21, 1991.

The acceptance of these reports, along with the geologic reportand the Hydrologic Monitoring program, constitute the completionof requirements for a Permit to Operate injection wells KS-IA andKS-3 under the UIC.

91194.011

101 Aupuni Street. Suite 101~-B. Hilo. Hawaii 96720 • (808) 961-2184 • Facsimile (808) 961-3531

November 25, 1991Page 2

Your timely review and acceptance of these documents is greatlyappreciated. If there are any questions regarding thissUbmittal, or the request for a permit to operate the injectionwells, please feel free to contact me in the Hilo office at961-2184.

Venture

Enclosures

cc:C. Hew, DOH'i5. Nakano, DLNRM. Tagamori, DLNR

91194.011

PUNA GEOTHERMAL VENTURE

KS-IA TESTING AND INSPECTION

PURPOSE:

To test injection capacity and inspect the mechanical integrity of KS-1 A to convert KS-1A from aproduction to an injection well.

PROCEDURE:

Run static temperature survey, perform injection test and inspect casing to assure the integrity of thecompletion and the injectivity of the well.

1. Rig up to run PT surveys and injection test.

a. Run water line from water well to the location.b. Rig up Howco V-12 to wing valve and water line.c. Install lubricator on 3" swab valve. Install personnel stand.d. Discontinue injection at least 48 hours prior to testing so that well can retain a stable

shut-in condition.e. Notify DLNR & DOH representatives at lease 24 hours prior to testing so they can

witness the testing.

2. Perform injection test as follows:

a. Before injecting any water, run a static pressure/temperature traverse from surface to5,000 ft. Verify data before proceeding to next step.

b. Kill well at 40 GPM with water until several wellbore volumes of water have beenpumped to slowly cool well and casing.

c. Increase pumping rate in 100 GPM steps holding each step for 2 hours until WHPreaches a maximum of 150 psi or until maximum available injection volume has beenreached. (Approximately 1200 GPM). -

d. Hold WHP constant at 150 psi for 12 hours. Vary injection rate to maintain a constant150 psi WHP.

e. Run a pressure/temperature tool with 12 hour clock to 5,000 ft.

f. Continue pumping into well for 1 hour. Shut in injection to well. Release Howco V-12.

g. Retrieve pressure/temperature tools when clocks expire.

h. Approximately 24 hours after shut-in, run a temperature traverse from surface to 5,000

KSIAINSP Page 1 November 21, 1991

PUNA GEOTHERMAL VENTURE

ft. to check for interformational flow behind casing. Minimum static time to be at lease12 hours.

3. Rig up to run casing inspection tools.

a. Rig up Howco TC4 to wing valve and water supply.

b. Check for casing leaks by killing well at 40 GPM with water and running aspinner/temperature survey during injection at a constant rate.

c. Install a 10-3/4" short lubricator with union connection, bleed off and wireline pack offon the 8" master valve. Use a 10" x 8" DSA crossover.

d. Move in crane to hang wireline sheave and handle lubricator (20 ton single line okay).

4. Run casing inspection logs as follows:

a. Keep well dead with at least 40 GPM water.

b. Run HLS 4 arm caliper as minimum 1.D. tool in 7" casing from the bottom of 7"cemented liner at 3,510 RKB (25" above G.L.) to surface.

c. Run HLS 60 arm Multi Finger Caliper from the bottom of the 7" cemented liner tosurface.

d. Shut in well and rig down. Interpret Logs.

5. Prepare to use well for injection service.

a. The well has four cemented casings below the last USDW.

b. The mechanical integrity of the casing will be ensured by the above testing to at least3,510' RKB.

c. We do not expect to find any mechanical problems with this well. If any of the testingindicates problems further diagnostic testing will be performed as per the CasingMonitoring Program.

d. The 20", 13-3/8", and 9-5/8" casings were installed by the previous operator.

KSIAINSP Page 2 November 21, 1991

PUNA GEOTHERMAL VENTURE

e. The 7" liner casing was tested during drilling to 600 psi surface pressure and test resultswere approved by the DLNR field representative before the casing shoe was drilled out.

f. All injection fluid will enter the geothermal zone in or below the aquitard which separatesthe geothermal fluids from the lower most USDW and will not migrate through thecemented annulus into the lowermost USDW.

g. This well will be used as a standby injector only. It will be used only in the event thatthe primary injector will not accept all of the injectate.

KSIAINSP Page 3 November 21, 1991

GROUND SURFACE

-----'-''----- Tl) 8505

PUNA GEOTHERMAL VENTURE

KS-1A CASINGSCHEMATIC AFTER REWORK

13-3/8" C-90 61# VNACEUENTED 0-2700'

2rt' 941 H-~ 8T&CCEMENTED 0-1376'

_-- 1376'

------- 40111'

,..~------- 9-5/8" C-90 47' H'rtlRIL SEU-GSCEUENTEO l>-406"

:.,.LJ._---- 2200'

1"'I~+ -1"-CEM-ENTED--UN-ER-3-/:-3-'/-:-9-1---'.,. .,. L-80 29# NEW VNA

0-3510'

PI~'+-------LINER twlGER3874'

.,. C-90 211' VNA SLOTlED,...il~-------- HUNG UNCEUENTED TO 11505'

CEUAR

26" HOLE----V

CE~ENT ----f'-/!V

36" HOLE ---<-1/

12-1/4" HOLE -------<-;'

17-1/'t' HOLE -----r

OBSTRUCTION, 8" 3' ---------t'-u;:~PARTEO LINER

8-1/2" HOLE ---------{

FISH, 5745'-6058' ---------'t<'OC'S, MIll. DP sruB

llIft 5/U/l' REV. 1

IrJ' w. 1'!PLDW GURE NO. 6

PUNA GEOTHERMAL VENTURE

PRODUCTION AND INJECTION WELLCASING MONITORING PROGRAM

1. INTRODUCTION

1.1 Background

November 21, 1991

Pursuant to Underground Injection Control (UIC) PermitNo. UH-1529, the Hawaii State Department of Health (DOH)requires Puna Geothermal Venture (PGV) to develop aCasing Monitoring Program (CMP) regarding production andinjection wells. This program is to be submitted to andapproved by DOH prior to start of operation of injectionwells drilled under permit UH-1529, for the PGV projectsite.

1.2 Purpose

The purpose of this CMP is to specify the observations,tests, drilling operations and, if necessary, remedialactions required to insure that the mechanical integrityof production and injection casing and cement ismaintained throughout the drilling I testing and operationof PGV wells. The cemented and hung casing strings thatare used in the PGV wells are designed to preventcontamination of any underground sources of drinkingwater (USDW) by either reservoir fluid in productionwells or power plant effluent in injection wells.contamination of the USDW's might occur if the casingstrings are breached due to corrosion or mechanicalfailure or if there is a failure of the cement to sealthe casing/borehole annulus above the zone of injectionor production. The casing monitoring program describedbelow is designed to detect and diagnose a loss ofmechanical integrity in the cas~ng or cement. Remedialactions required to restore mechanical integrity are alsodescribed.

pgv\casinteg Page 1

PUNA GEOTHERMAL VENTURE

1.3 Scope

November 21, 1991

This CMP covers all production and injection wellsdrilled by PGV and all existing wells that were drilledby previous operators on the 500 acre PGV site which todate have not been plugged and abandoned.

1.4 Hydrogeologic Basis for the Casing Monitoring Program

The hydrogeologic basis for the CMP is derived fromdata available from the drilling of five productionwells to depths ranging from 6500' to 8000' and by twoshallow monitoring wells drilled to depths of 640' and720' (F igure 1).

1.4.1.

1. 4.2

pgv\casinteg

The shallowest zone extending from surface(approximately 620' above sea level) to about7' above mean sea level is unsaturated andconsists of a highly permeable sequence ofsubareal basalt flows and interflow breccias.Within the project area this zone varies inthickness from 600' to 720' depending on thesurface elevation. Numerous cracks withwidths of up to 2' traverse the area. Thesecracks are vertical or very steeply dippingand reach from the surface to at least the topof the warm unconfined aquifer describedbelow. This is evidenced by the discharge ofwarm moist air from many of these cracks. Thecracks trend parallel to the major structuresand lineaments of the Lower East Rift Zone.

The zone below the unsaturated surface rockconsists of an unconfined aquifer whichcontains ground water with varying degrees ofnatural contamination from the underlyinggeothermal system. This zone is approximately1400' thick with the water surface elevationcontrolled by sea level according to theGhyben-Herzberg model~ The unconfined aquifersurface in the project area is approximately7' above mean sea level. Based on the model,the thickness of the low salinity lens istherefore about 280'. This constitutes theUSDW. The salinity of the underlying water

Page 2

PUNA GEOTHERMAL VENTURE

1.4.3.

1. 4.4

1.4.5

pgvlcasinteg

November 21, 1991

will probably approach that of sea water. Thetemperature of the unconfined aquifer zoneranges from 95 0 to 192 0 F. in the project areaand tends to be nearly isothermal throughoutthe entire interval, indicating good verticalmixing. A detailed description of thisaquifer is given in the Puna GeothermalVenture Hydrologic Monitoring Programsubmitted to DOH in April 1990.

The interval from 1400' below sea level to2400' below sea level (2000' to 3000' GL inFigure 2) is characterized by an extremelysteep thermal gradient in the range of 30F/100' or more. The steep temperaturegradient is characteristic of conductive heattransfer and indicates the zone hasessentially zero vertical permeability. Thus,the zone appears to be an effective aquitardseparating the high temperature geothermalfluid below from the low temperatureunconfined aquifer overlying it. Locally theaqui tard exhibits natural leakage as in thearea of MW-2 and GTW-III where anomalouslyhigh shallow ground water temperatures andsalinities are observed.

Between the depths 2400' and 4300' below sealevel (3000' to4900' GL in Figure 2) thetemperature profile indicates the existence ofa transition zone which consists ofalternating permeable and impermeable strata.Within this zone are two or more alternatingzones of high thermal gradients and isothermalintervals. The high average thermal gradientthrough this zone indicates that verticalfluid circulation is very limited.

Below a depth of about 4300' below sea level(4900' GL in Figure 2) the temperature profilebecomes nearly isothermal. This interval iswithin the geothermal reservoir in whichsignificant vertical movement of fluid istaking place at temperatures above 620 degreesF.

Page 3

PUNA GEOTHERMAL VENTURE November 21, 1991

The casing program planned for the production andinjection wells calls for cemented casing to reach fromground surface to a depth of about 3400' below sea level(Figures 3 and 4). This allows the casing to be anchoredsecurely within the transition zone described in 1.4.4and to fully isolate the geothermal reservoir from theshallow aquifer (lowermost USDW) with a cemented intervalthrough the aquitard (1400'-2400' below sea level).Within the shallow aquifer zone, two cemented casingstr ings are insta lied. Three cemented cas ing str ingspass through the top of the shallow aquifer and theunsaturated zone. The production and injection casingprograms are designed to prevent leakage of geothermalfluid from the wellbore into the shallow aquifer above adepth of 1400' below sea level. The CMP discussed belowprovides the methods and procedures necessary to detectany leakage and to repair those leaks if detected.

2. PRODUCTION WELL CASING MONITORING PROGRAM

2.1 Pressure Testing During Drilling

Each production well is completed with three casingstrings (not including the 30-inch conductor pipe)cemented to the surface (Figure 3). Immediately uponcompletion of cementing each casing string and prior todrilling out the cement shoe, the casing will be pressuretested. The test will consist of pressurizing the casingto a specified test pressure and holding for 30 minutes.The specified test pressure shall be the lesser of: (a)2000 psig surface pressure or (b) 70% of the casinginternal yield pressure less 250 psi at the shoe. (2000psig is the maximum expected surface pressure on the 9­5/8" casing during production operations.) The pressurechange during the 30 minute period shall not exceed 8%.The effect of the fluid expansion due to thermal recoveryin the wellbore during the test period will be negligiblethroughout the test period.

In the event that excessive bleed-off occurs, one ormore of the following diagnostic methods will be used tolocate the leak:

Temperature log while injectingstatic temperature survey

pgv\casinteg Page 4

PUNA GEOTHERMAL VENTURE November 21, 1991

Casing inspection logs with multi-armcaliper and/or magnetic inspection toolsPressure testing with a packer(s) on

drillpipeother applicable methods

After identification of the point of leakage, a cementsqueeze job will be performed and the casing retested.Results of each pressure test will be reported to theDepartment of Land and Natural Resources (DLNR) and theDepartment of Health (DOH),

After a successful pressure test of each casing string,drilling will proceed to a point at least one foot belowthe cement shoe, and a pressure leak-off test will beperformed to test the integrity of the annular cement.Each test will be performed at a pressure approaching thefracturing pressure of the exposed formation. If thereis excessive leak-off, a squeeze cement job will beperformed, the cement will be drilled out and the testwill be repeated. Drilling will not proceed until aneffective cement seal is established in thecasing/borehole annulus above the shoe. In somesituations, such as the case where there is naturalformation permeability immediately below the casing shoe,it may not be practical to prove cement integrity withthe pressure test described above. As an alternative, astandard water shutoff test (WSO) may be done above theshoe, or shut-in temperature surveys may be run.

If there have been indications of problems with the 9­5/8" cement job, a cement bond log (CBL) will be run inthe 9-5/8" casing. Adequate cement curing time will beallowed before running the CBL.

Although CBL's may be of interest on the surface andintermediate casing strings, they are not planned becausethe necessary logging tools are not available from PGV'slogging contractor to obtain meaningful results in thelarge diameter, 20" and 13-3/8" casing strings. CBL'sare not commonly run in geothermal production andinjection wells on the mainland, and they are virtuallynever run on the surface and intermediate casings. Thelarge surface and intermediate casing sizes common togeothermal wells cannot be bond logged with usefulresults using conventional logging tools.

pgv\casinteg Page 5

PUNA GEOTHERMAL VENTURE November 21, 1991

with regard to the surface and intermediate casingstrings, if any problems are suspected from the resultsof the cement job or pressure testing, a statictemperature survey will be run to check forinterformational flows behind the casing. The shut-intime before logging will be sufficient to obtain usefulresults.

If the eBL is run in the 9-5/8" production casing it willbe used only to determine cement tops or as a diagnostictool. The logging results will not meet oil and gasstandards for cement bond or cement compressive strength.This is due to two factors:

pgv\casinteg

2.1.1

2.1.2

Because of the temperature limitations onlogging tools, a well must be cooled by waterinjection during the logging operation. Theresul ting thermal contraction of the casingcreates a temporary micro annulus between thecasing and cement. Therefore, the log showsthat no bond exists. This micro annulus isbelieved to seal after the well heats back upto the usual temperature. The micro annulusis usually so small that it would only be aproblem with high pressure gas and would notprovide a flow path for geothermal fluids.

The cement used in geothermal wells isrelatively light weight, low compressivestrength cement. Geothermal casing is usuallycemented in place over its entire length andthe cement used must be lightweight or theformation will fracture due to thehydrostatic pressure from the cement column.Fracturing and the resultant loss ofcirculation cause an incomplete primary cementjob. Any secondary cementing procedureusually never approaches the quality of asuccessful primary cement job. All of thelight weight cements available on the marketproduce relatively low compressive strengthswhen set. High compressive strengths are notrequired for geothermal wells because thecasing is cemented over its entire length.This supports and protects the casing andseals off any possible flow in the annulus.This is unlike the common practice in oil and

Page 6

PUNA GEOTHERMAL VENTURE November 21, 1991

gas wells where casing is cemented only toseal off the zones of interest or fresh waterzones. The main method of determining thecompetency of the casing cement job whiledrilling will be the surface indications ofpressure and circulation returns during thecement job and the shoe leak-off test. Ifboth of these are positive, the cement job hasan extremely high probability of providing agood seal against the migration of productionfluids.

2.2 Monitoring During Injection Testing

Upon completion of each production well aninjection test may be performed to give an initialindication of reservoir permeability. Theinjection test consists of pumping relatively cool,fresh water into the wellbore at several controlledrates while monitoring downhole and wellheadpressure. Temperature-pressure-spinner (TPS) logswill normally be run during the test. These logscan be used to locate leaks in the casing by notinga sudden change in temperature with depth or a dropin flow velocity within the casing string. In theevent that a loss of mechanical integrity isindicated during or after injection, one or more ofthe following diagnostic methods will be used toconfirm the leak:

Temperature log while injectingstatic temperature surveyCasing inspection logs with multi-armcaliper and/or magnetic inspection toolsOther applicable methods as determined byPGV.

2.3 Monitoring During Flow Testing

During flow testing of each production well, wellheadtemperature and pressure along with steam and brine flowrate and chemistry are continuously monitored. After theinitial 24 hours of flow, flow characteristics tend to bestable. Sudden changes in the wellhead pressure,temperature, br ine/ steam ratio, or brine chemistry duringstabilized flow can be indicative of a loss of mechanical

pgv\casinteg Page 7

PUNA GEOTHERMAL VENTURE November 21, 1991

integrity which is allowing cool water leakage into thewellbore.

Also during flow testing, TPS logs are periodically run.Leakage of cool water into the wellbore or loss of fluid

to zones behind casing may be seen in the TPS logs runduring or after shut-in. In the event that wellhead orlogging data indicate a loss of mechanical integrityduring the flow test, the well will be shut in and one ormore of the following diagnostic methods will be used toconfirm the leaks and locate it more precisely:

Temperature log while injectingstatic temperature surveyCasing inspection logs with multi-arm caliperand/or magnetic inspection toolsother applicable methods as determined by PGV

2.4 Monitoring During Production

Wellhead pressure and temperature will be monitoreddaily during normal production. Brine and steamchemistry will also be analyzed for each production well.Initially, samples will be taken weekly to establish abaseline geothermal fluid chemistry. The samplingfrequency will then be reduced to monthly and quarterlyas stabilization of the fluid chemistry is confirmed.

Casing failure causing leakage of cool ground water intothe wellbore or loss of geothermal fluid to the formationmay be manifested as a pressure and temperature drop atthe wellhead. Fluid chemistry changes may also indicateground water leakage. Wellhead pressure, temperature,and chemistry data will be reported to the DOH quarterlyon a routine basis.

In the event that anomalous production parameters areobserved, TPS survey(s) will be run with the wellflowing. The TPS profiles will be used to determinewhether the observed changes are due to changes inreservoir characteristics or are caused by a loss ofmechanical integrity. In the event of a suspected lossof mechanical integrity, one or more of the followingdiagnostic methods will be used to confirm the leak andlocate it more precisely:

pgv\casinteg Page 8

PUNA GEOTHERMAL VENTURE November 21, 1991

Temperature log while injectingStatic temperature surveyCasing inspection logs with multi-arm caliperand/or magnetic inspection toolsother applicable methods as determined by PGV

2.5 Casing Repair

Once a loss of mechanical integrity is identified andapproximately located, casing repair procedures will beinitiated. These procedures may include any or all ofthe following activities:

pgv\casinteg

2.5.1

2.5.2

2.5.3

2.5.4

2.5.5

2.5.6

2.5.7

Shut in well and run magnetic and multi­arm casing inspection logging tools toprecisely locate leak and to evaluatecasing condition.

Rig up workover rig on well. Runpacker(s) on drillpipe and pressure testto confirm suspected leaking interval.

Execute cement squeeze job to seal casingleak or stop interformational flowsbehind casing.

Perform casing pressure test and otherdiagnostic tests as necessary to confirmsuccess of the remedial work. If good,move rig off well and return well toproduction.

In the event of major casing failure, acemented liner may be installed throughthe damaged interval.

Prior to drilling out the liner shoe, theliner will be pressure tested asdescribed in Section 2.1.

If mechanical integrity cannot berestored satisfactorily, the well will beplugged and abandoned.

Page 9

PUNA GEOTHERMAL VENTURE

3. INJECTION WELL CASING MONITORING PROGRAM

3.1 Pressure Testing During Drilling

November 21, 1991

The cemented casing string design in PGV injection wells(Figure 4) is similar to that of production wells.Testing of each string will proceed as described in 2.1above.

3.2 Monitoring During Injection Testing

Prior to installation of the hangdown liner, aninjection test will be performed to measure injectivityof the open formation below the cemented 9-5/8" casing.During the test, one or more of the following logs orsurveys will be run:

TPS through the open hole and cased intervalswith the well on injection.

Static temperature surveysevidence of interformationalcasing.

to check forflows behind

Other logs or surveys, as determined by PGV,to check for mechanical integrity of thecasing and cement.

If the results of the logs and surveys confirmmechanical integrity, then the 7" hangdown liner may beinstalled. If leakage is found, repair procedures asdescribed in 2.5 will be performed.

3.3 Monitoring During Routine Injection

During routine injection, the 7" x 9-5/8" annulus willbe purged with nitrogen. Purge pressure and flow ratewill be monitored for any changes indicative of a casingleak. Purge will be repeated as necessary to maintainthe fluid level more than 1/2 way down the annulus. Onceannually, tests and surveys will be conducted to verifymechanical integrity of the hangdown liner. The casingand hangdown liner will be tested for leaks by one of thefollowing procedures, or a combination thereof:

pgv\casinteg

3.3.1 Perform a pump-down test on the 7" x 9-5/8"

Page 10

PUNA GEOTHERMAL VENTURE

3.3.2

November 21, 1991

annulus. Nitrogen will be injected into theannulus to a pressure sufficient to displacethe water level to the 9-5/8" casing shoe andshut in. Surface pressure on the annulus andhangdown liner will be monitored and recorded.Annulus pressure bleed-off exceeding 8% in 30minutes will be considered indicative of aleak. If necessary, the pressure test will beextended beyond 30 minutes to preclude thermaleffects on the surface pressure. In thatcase, the final 30 minutes will constitute thetest period.

If the hangdown liner is pulled, the casingmay be pressure tested above a bridge plug orpacker set near the shoe following the basicprocedure outlined in Section 2.1. Integrityof the hangdown liner may be verified byinspection on the surface, by a pressure testafter it is run in the hole, or by a TPS logwith the well on injection.

Integrity of the cement will be checked during eachworkover by one or more of the following procedures:

3.3.3 One or more shut-in static temperature surveyswill be run. Shut-in time will be at least 12hours, or longer if necessary to obtainmeaningful results.

3.3.4 Other logs or surveys may bediscretion of PGV, if staticsurveys are not definitive.

run, at thetemperature

3.4 Restoration of Mechanical Integrity or Abandonment

In the event that the diagnostic procedures indicate aloss of mechanical integrity, remedial or abandonmentprocedures will be carried out as specified in section2.5.

pgv\casinteg Page 11

WELL LOCATION MAP

."

...lANlPUI

o

,.'.'

,./'.'

".",.,;,-',.

A,,·'

~

DO

\

\ 0l\l\,

~ 0\ ~._-.., ,

,......... J-.........__.-

IoIONITORING WEll. ,

....I>- IoIW-2 ""-y , •.'",..'

",....,..,........-.­

,. ........-",. ........­.....................................

\)~IGURE 1

o .:r 1000 FEET.... I

SCALE

EXPLANATION '·V/ 00-+ PRODUCTION WEll (PROPOSED)-+ PRooucnDN WEll (EXlS1lNG)

..- IHJECTlDH WEll (PROPOSED)

.~ 0,." GEOlH£RlolAl lEASE BOUNlWlY 0

... llDNITORING STATION 0o RESlOENCE

"' ..-g,..lI:~J.I~1

PUNA GEOTHERMAL VENTURE

PL GEOTHERMAL VENTUKS-J STATIC AND FLOWINuTEMPERATURE PROFILES

O-,---"""JIii:::r------.----r----,---_~--..._---

UNSATURATED ZONE

1000 --t----++-~-_+---_+---++---_1---_+_---

UNCONFINED AQUIFER

2000 T---r~~9F===+===!==~t~_=_}~_=_-IMPERMEABLE ZONE

3000 -t-----+-------i----+---~~--l__--___+_---

~ 4000 -;-----+-------i------.,Lt-----+-:~--l__.......-___+_---TRANSITION ZONE

:cI­a..wo 5000 -;----+-----t----+---+-----dr----'f---=--~~--

GEOTHERMAL RESERVOIR

6000 -;-----+----I-----t--~--+--~~+-----+---*--

7000 -i----+----f-----t---.----+-----I-----+---~ KS J, STATICAfiI!'M KS J, FlOWING

o 100 200 300 400 500TEMPERATURE (deg.F)

600

FIGURE

CROUNO SURFACE APPROX. 600' ABOVE I.lSL

CELlAR,r

------- 4000'

1000'

2000'

20" 9~ K-5S BT&CCEMENTED 0-1000'

13-3/a" 611K-55 NEW VAI.lCEI.lENTEO 0-2200'

PUNA GEOTHERMAL VENTURE

~~.......__ 30" CONDUCTOR CEMENTmTO SURFACE

9-5/a" 471 C-90 NEW V~

P"'!"""":T------- CEI.lENTEO 0-3900'

_ ........,..------- 9-5/a" 471 X T 291 L-80UNER HANCER

I; I;IIIIIIIIIIIII I I,~~ T 291 L-80 BT&C SLOTTED UNERI I I HUNC UNCEI.lENTEll 3780'-7400'

IIIIIIIIIIIIIII

1'11__.0'_--- TO 7400' PRODUCTION WELL

CASING DESIGN

CE/olE.NT ----4'-/

26" HOLE ----v:

36" HOLE ---<./

8-1/t' HOLE ---------{

17-1/t' HOLE ----__.('

12-1/4" roOLE -------JV

lW! 5/28/11 REV. 2

III' •. l'IPUllI P'l1Z:l'<:V\1'lIOIlCAS.DWC FIGURE NO. J

CROUNO SURFACE

J6" HOLE ---1/

26" HOLE ----V

CEJ,jENT ----40--/

'7-,/2" HOLE ----.-.1'

,2-'/4" HOLE -------1/

a-,/2' HOLE ---------(

APPROX. 600' ABOVE I.ISl

CELlARIF

20" 9~ K-55 8T&:CCEI.IENTED 0-1000'

,000'

1J-J/8" 6'# K-55 NEW VAllCEJ,jENTEO 0-2000'

2000'

9-5/8" .7# C-90 NEW VAll

CEJ,jENTED TO SURFACE

I .....~'f-------- r SI.I22 Cr-65 23# VAM ACEHANG DOWN UNER

------- .000'

PUNA GEOTHERMAL VENTURE

"----/----- Ttl 7.00' INJECTION WELLCASING DESIGN

~ 4/1/11

IIr w. MI"I..OW FIGURE NO.4


Recommended