约旦浅层地温能资源
EnergyforSustainableDevelopment13(2009)124–128
ContentslistsavailableatScienceDirect
EnergyforSustainableDevelopment
StatusandoutlookofgeothermalenergyinJordan
EyadS.Hrayshat⁎
ElectricalEngineeringDepartment,FacultyofEngineering,TafilaTechnicalUniversity,P.O.Box66,Tafila66110,Jordan
articleinfoabstract
AnupdatedassessmentofgeothermalenergysourcesinJordanandtheprospectsfortheirfutureutilizationarepresented.Furthermore,adevelopmentstrategyforgeothermalenergyinthecountryisproposed.TheresultsshowthatJordanhasenormousundergroundenergyresourcesinmanypartsofthecountryintheformofthermalundergroundhotwater(wellsandthermalsprings),havingatemperaturerangingfrom20°Cto62°C.Itwasalsofoundthattheinstalledcapacityofgeothermalenergyis153.3MWtandtheannualenergysupplypotentialis1540TJ/yearintheformofdomestichotwaterforbathingandswimming,givinganoverallcapacityfactorof0.42.Possiblefutureapplicationsofgeothermalenergywerefoundtobeabsorptionrefrigerationtopreservefruitandvegetablesorfreezefishandmeat,aswellasfishfarmingandgreenhouseheating.
2009InternationalEnergyInitiative.PublishedbyElsevierInc.Allrightsreserved.
Articlehistory:
Received27April2009Revised18May2009Accepted18May2009Keywords:
GeothermalenergyJordan
Energysource
Introduction
Energyissuesandpolicieshavebeenconcernedmainlywithincreasingthesupplyofenergy.Countriesaroundtheworldhaveconsideredthesufficientproductionandconsumptionofenergyastobeoneoftheirmainchallenges.Moderneconomiesareenergydependent.Theprovisionofsufficientenergyhasbeenperceivedacentralproblem.Energyavailabilityandconsumptionhavebeensoimportantaconsiderationtoeconomiesworld-widethatthemagnitudeofenergyconsumedpercapitahasbecomeoneofthekeyindicatorsofmodernizationandprogressinagivencountry.Attentionhasbeguntoshifttowardamorebalancedperspective,includingconcernsrelatedbothtodemand-sideandenergycon-sumptionpatterns.Eitherway,thereisnoescapingthefactthattheuseofenergyisanecessaryandvitalcomponentofdevelopment(Reddyetal.,1997;Goldembergetal.,1987).
EnergyissuesposeacomplexsetofchallengesforJordan.Jordancurrentlyimportsmostofitscommercialenergyintheformofoilandthisisaburdenonthenationaleconomy.DespitethelimitationsofJordan'sconventionalenergyresources,thedemandforenergyiscontinuouslyrisingasaresultofincreasingpopulationandindus-trialization.Furthermore,utilizationoffossilenergyresourcesisbecomingasignificantenvironmentalconcerninthecountry.Inthisregard,thereisanurgentneedtodeploysustainableandenvir-onmentallycleanenergysources.Animportantcontributioncouldbemadebyrapidlyexpandingtheuseofrenewableenergysources,suchasgeothermalenergy,whichhasproventobereliable,cleanandsafe,andtherefore,itsuseforpowerproduction,andheatingandcoolingis
increasing.Itisapowersourcethatproduceselectricitywithminimalenvironmentalimpact(KömürcüandAkpinar,2009).
ThispaperpresentsanupdatedassessmentofgeothermalenergysourcesinJordan,inadditiontotheprospectsfortheirfutureutilization.Furthermore,adevelopmentstrategyforgeothermalenergyinthecountryisproposed.Jordan'senergysources
Jordanreliesalmostentirelyonimportedcrudeoilandoilproductstomeetitsneeds.Therefore,Jordanhasbeenstrivinghardtominimizedependenceonimportedenergythroughinvestinginthelocalsourcesofenergyinordertoreducetheoilbillwhichconstitutesaheavyburdenonitseconomy,particularlyinlightofveryhighworldoilpricesinrecentyears.Themostimportantsourcesoflocalenergysourcesarediscussedbelow,alongwiththeeffortsexertedtoincreasetheirutilization.Oilandgas
Table1representsJordan'sproductionofoilandgasandtheircontributiontotheoverallconsumptionofenergyduringtheperiod2003–2007(MEMR,2007).Itshowsthatcrudeoilandnaturalgasproductionwasnearly186.5thousandtonsofoilequivalent(toe),i.e.3.8%oftotalenergyneeds.Inviewofthislimitedproduction,Jordanhasdependedonimportstomeetitsenergyneeds.Oilshale
Jordanianoilshale–withaprovenamountofabout5×1010tons–isofquitegoodquality.Ithasrelativelylowashandmoisturecontent,grosscalorificvalueof7.5MJ/kg,andoilyieldof8–12%.Thereserves
⁎Tel.:+[1**********]0;fax:+[1**********].E-mailaddress:[email protected]
.
0973-0826/$–seefrontmatter2009InternationalEnergyInitiative.PublishedbyElsevierInc.Allrightsreserved.doi:
10.1016/j.esd.2009.05.004
E.S.Hrayshat/EnergyforSustainableDevelopment13(2009)124–128
125
Table1
Jordan'sproductionofcrudeoilandgasduringtheperiod2003–2007.YearCrudeoilNaturalgasContributiontotheoverall(1000tons)(billionCF)energyconsumption(%)20031.59.03.620041.410.23.720051.210.44.020061.18.53.72007
1.2
8.9
3.8
shouldbesufficienttosatisfythecountry'senergyrequirementsforcenturies(Hrayshat,2008a).Therefore,theGovernmentofJordanisconsideringoilshaleexplorationinacommercialperspective.Inthiscontext,internationalcompaniesinterestedinutilizingtheoilshalehavebeeninvitedtosubmittheirbidstoMEMRtoreachanacceptableagreementforconstructingaprivatepowerstationprojectusingthisoilshale,ortoproducefueloilfromit,usingretortingtechnologies(Hrayshat,2008b).TheroleofNationalElectricPowerCompany(NEPCO)inthisindependentpowerproducer(IPP)operationwillberestrictedtopurchasingelectricitythroughsomeappropriatelongtermorshorttermagreement.Renewableenergy
Jordanhasasubstantialpotentialofrenewableenergysources.However,renewableenergyprovidesapproximately1.5%ofthetotalcurrentprimaryenergydemandinJordan.TherenewableenergysourcesinJordanincludesolar,wind,geothermal,hydroelectricandbiomass.
Jordanisendowedwithahighpotentialofsolarenergy.Theaverageinsolationintensityonhorizontalsurfaceisabout5–7kWh/m2/daywhichisoneofthehighestintheworld(HrayshatandAl-Soud,2004).Theannualsunshinedurationisaround2900h,whichcanbeconsideredsufficienttoprovideenoughenergyforsolarheating/coolingapplications.Nevertheless,solarenergytechnologiesarenotextensivelyused,exceptforsolarwaterheaters(SWH),whichareusedforheatingofdomestic-waterforaboutaquarterofthehousingstock,therebyavoidingtheneedforabout1.5%ofthetotaloilimports.
Anotherinterestingapplicationofsolarenergyisforelectricitygenerationusingthephotovoltaic(PV)systems.Atpresent,JordandoesnothaveanorganizedcommercialPVprogram.However,therearesomeinstallations,withatotalpeakpowerofabout100kWp.Underthesolarconditions,eachkWpgivesanaverageof5kWh/day.ThusthetotalyearlyenergyoutputofPVsystemsinJordanisabout182.5MWh.
ThenorthernandsouthernpartsofJordanhavehighwindpotentialwithaveragewindspeedsof6.5m/sandmore.CurrentlysomeelectricityisproducedusingwindturbinesatAl-IbrahimyyaandAl-Hoffawindplants.Al-Ibrahimyyawindplantconsistsoffourhorizontalaxis80kWwindturbines,withahubheightof24mwhileAl-Hoffawindplantcontainsfivewindturbinesof225kWeach.Theirelectricityproductionduringtheyear2007wasnearly2.8MWh(CEGCO,2007).Thisisinsignificantcomparedtothetotal2007generationof13,001GWh.
Table2
Primaryenergyconsumption(thousandtoe),2003–2007.Year
TypeofprimaryenergyTotal
Crudeoil
NaturalgasRenewableElectricityenergy[***********]920045030.743277234.[1**********]12.41194.982199.[**************]82.382238.270282007
4953
1995.9
111
127.1
7187Table3
Sectorialdistributionoffinalenergyconsumption(thousandtoe),2003–2007.YearSectorTotalTransportIndustryHouseholdOthersa
[***********][***********][***********][***********][***********]07
1822
1182
1064
821
4889
a
Includingthetradeandagriculturalsectorsalongwithstreet
lightings.
HydropowersourcesareverylimitedinJordan.Currently,therearetwosmallhydropowersystems:KingTalaldamspanningtheriverZarqanearJerashwitharatedelectricitygenerationcapacityofabout5MWandthehydroturbine,utilizingtheavailableheadofcoolingseawaterattheAqabathermalpowerstationwithacapacityofabout5MW(JordanValleyAuthority,2007).Thetotalelectricitygeneratedin2007was45GWh,i.e.0.58%oftotalnationalelectricgeneration.Thisrepresents,atpresent,thetotaleconomicallyfeasiblecapacityforhydropowerinJordan.However,thereisagreatpossibilitytogenerateelectricity,usinghydropowerstations,byexploitingtheelevationdifferencebetweentheRedandDeadSeas.
ThebiogasplantattheAmmanmunicipalwastedisposalsitewasfoundedtoextractgasesfromthelandfillsiteinordertofuelthe1-MWgenerationunitandtosupplythenetworkwithgeneratedelectricity.Thevolumeofthesolidandliquidwastes–treatedin2007–reachedaround4812tons,andtheamountofelectricitygeneratedwas6240MW.Byburningthemethanegascontainedinthelandfillgasinsteadofreleasingitintotheatmosphere,theplantprevented–since2002–theemissionof13thousandtonsofmethanegas,i.e.equivalentto275thousandtonsofcarbondioxide.Totheextentthatelectricitygeneratedfromrenewablesourcesoffsetsgenerationusingfossilfuels,allrenewableelectricitygenerationalsoreducesCO2emissions.
Jordan'sgenerationandconsumptionofenergyandelectricity
Primaryandfinalenergyconsumption
Jordan'sprimaryenergyconsumptionbetween2003and2007isshowninTable2.In2007,theoverallconsumptionofprimaryenergywasabout7187thousandtoe,yieldingagrowthof2.3%against2006,whilethetotalconsumptionoffinalenergy(seeTable3)–whichistheenergyavailabletoconsumers–wasnearly4889thousandtoewithagrowthrateof1.8%comparedtothe2006consumptionlevels.Ontheotherhand,theyear2007haswitnessedasignificantdeclineintheconsumptionofoilproducts(seeFig.1),withaconsumptionofnearly4842thousandtonscomparedtoaround5081thousandtonsin
Fig.1.OilconsumptioninJordan,2003–2007.
126
E.S.Hrayshat/EnergyforSustainableDevelopment13(2009)124–128
Table4
Availablecapacity(inMW)ofelectricpowerplants.YearSteamDieselGasturbinesCombinedRenewableTotalenginesDieselNaturalgascycleenergy[**************]0–14.[***********]15030014.[***********]21060017.420762007
1013
43
193
310
600
17.4
2176
2006,therebypostingageneraldropinconsumptionto4.7%.Apparentlyalltheoilproductshavewitnesseddeclineintermsofthevolumeofconsumptionwiththeexceptionofliquefiedpetroleumgasandgasolinewhosegrowthwere4.7%and6.3%respectively(JordanRefinery,2007).Themostimportantreasonsthatledtoasmallreductioninconsumingoilproductsare:i)increaseduseofthenaturalgasforgeneratingelectricityinsteadofthefueloilandii)usingelectricityforheatinginthehouseholdandtradesectorsinsteadofthekeroseneanddieselasaresultoftherelativelyhigherpricesofthesetwofuels.
Electricitygenerationandconsumption
Table4showstheavailablecapacityofpowerplantsinJordan.Thedominantplantsaresteamturbinesanddiesel-fuelfiredgasturbines.
Theelectricitygeneratedin2007–asexhibitedinTable5–reachednearly13,001GWh,16.9%highercomparedto2006.However,theelectricityconsumedin2007wasabout9579GWh,only9.6%highercomparedto2006(NEPCO,2007).ThisledtomoreexportofexcesselectricitytoEgyptandSyria.Thepeakelectricloadin2007reachedaround1901MW,8.6%highercomparedto2007.GeothermalenergyinJordanGeothermalinvestigations
GeothermalenergyexplorationsinJordanhavebeencarriedoutbytheNaturalResourcesAuthority(NRA)withtheassistanceofforeigninstitutionsandcompanies.TheseinvestigationswerereviewedbySaudiandSwarieh(2005)andaresummarizedbelow.
Thefirststudywascarriedoutin1965,andcomprisedchemicalanalysisofsamplesfromZarqaMa'in(MacDonald,1965).Bender(1974)describedthemajorandminorspringareasandprovidedchemicalanalysisoftheZarqaMa'inthermalsprings.McNitt(1976)reviewedexistingchemicaldatafortheZarqaMa'insystemandrecommendedfurtherwork(aresistivitysurveyanddrilling)toinvestigatethearea.Onthebasisoftemperatureandfluidchemistry,Marinelli(1977)concludedthattheeastescarpmentoftheDeadSeaRiftandparticularlytheZarqaMa'inandZarqaareaspossessedthemostfavorablegeothermalpotential.Truesdell(1979)foundthattheZarqaMa'inandZaraSpringsarefedbywatercirculatingdeepwithinthePalaeozoicSandstoneaquifersandreceivingheatfromanormalgeothermalgradient.Hesuggestedthatthesewatersexistatamaximumtemperatureof110°Catdepthandarecooledduringtheirascentbymixing.Abu-Ajamieh(1980)reportedonmajorexploration
Table5
Electricalenergyproduction(inGWh)bytypeofgeneration.Typeofgeneration[**************]7Growth2006/2007(%)Steamunits
[***********].2Gasturbines/diesel
4643416732−52.2Gasturbines/naturalgas[1**********]6−2.9Dieselengines/HFO75733214−56.2Combinedcycle–[1**********]31.8Renewableenergy6265607423.3Total
8967
9654
11,120
13,001
16.9
exercise–usingavarietyofexploratorytechniques–carriedoutbyNRAin1977and1978intheZarqaMa'in–Zarathermalarea.Themainoutcomeofthisreportwasthatanimportantgeothermalreservoirisindicatedintheareaofthesprings,mostprobablyheatedbytheHammamatUmmHasanbasaltplug.Themoderateradioactivityofthewaterswasalsonoted.Mabey(1980)studiedpreviousdataoftheZarqaMa'in–Zaraarea.HakkiandTeimeh(1981)carriedoutadetailedgeologicalstudyoftheZarqaMa'in–Zaraarea.Theirworkrelatedthehottestspringstothehighestintensityofshearinginthearea.DiPaola(1981)foundthattheexistinggeochemicalandisotopicresultsoftheZarqaMa'inareaindicatethatthetemperatureofthespringswasmostprobablyduetotheuprisingofdeeplycirculationwatersinanormalgeothermalgradient.McEwenandHolconmbe(1982)appliedterraincorrectiontotheresistivitydatareportedbyAbu-Ajamieh(1980).ThecorrecteddatasuggestedthatfourareasoflowresistivityexistintheZarqaMa'in–Zaraarea,butnoneofthemhadlateralextent.FlaniganandElKaysi(1984)reportedonpre-liminaryaudio-magnetotelluricstudiesintheZarqaMa'in–Zaraarea.Theyfoundthatrocksinthisarearangedfrommoderatelyconductivetoveryconductive.Galanisetal.(1986)concludedthattheheatflowinZarqaMa'in–Zaraareaishigh—upto472mW/m2,andthattheareaofhighestheatflowisassociatedwiththeZarqaMa'infaultzoneratherthanthelocalbasalticeruptions.Myslil(1988)re-evaluatedtheheatflowdatapresentedbyGalanisetal.(1986),includedotherrecentdata,presentedtemperaturegradientmapandidentifiedtwofavorablezonesforfutureexploration:i)theeastescarpmentoftheDeadSeaRift–northofEl-Lisan–wheregradientsof50°C/kmcouldbeexpected,andii)theregionneartheborderswithSyriaandIraq,wherethetemperaturegradientsareintheorderof40°C/km.Allen(1988)reviewedandsummarizedallthepreviousgeothermalinvestigationsinJordanandintroducedaproposalforfuturegeothermalstudies.Swarieh(1992)statedthatthepresenceofthermalwaterintheshallowboreholesnearQueenAliaairportisduetothewatermixingbetweenthethermalwateroftheloweraquifer(LowerCretaceousSandstone)andthefreshcoldwateroftheupperaquifer(UpperCretaceousLimestone).HealsorelatedtheheatsourcesinZarqaMa'intothedeepcirculationprocessalongtheZarqaMa'infault.SwariehandMassarweh(1993)studiedthethermal
Table6
ThermalspringsandwellsinJordan.Location
FlowrateTemperature(m3/h)range(°C)1.Thermalsprings
Himmehthermalsprings2828–43AbuThablehthermalspring1737DeirAllathermalspring1735WadiHisbanthermalspring–32Jerashthermalspring1028AinElHammam
–36ElDachruk(ZarqaRiver)–34Suweimeh–27AinEzZarqa
–20–34ZarqaMa'in(60thermalsprings)–63Burbeita–
38Afrasprings
50–10044–48Zara(45thermalsprings)–53Zara180054Zara2
6759WadiIbnHammadsprings–35Weida'athermalspring–32NorthShaunawell35057Kafrainwells
–
33–36
2.Wells
ZaraandZarqaMa'inexplorationwellsA—GTZ2D–68.5B—GTZ3D
–57TSD1well—GhorElHadithaarea
40050
E.S.Hrayshat/EnergyforSustainableDevelopment13(2009)124–128
127
Table7
2008utilizationofgeothermalenergyinJordan.Location
Capacity(MWt)Annualutilization(TJ)CapacityfactorNorthShunehwell22.0197.70.29Himmeh52.3274.80.17ZarqaMa'in58.67390.40Zarqa8.40790.30Burbeita5.121110.68Afra6.54138.50.67Total
153.5
1540
0.42
springsinWadiIbenHammad,Karakregion.Theyfoundthattheheatsourcethereis–morelikely–duetotheheatstorageinthesaturatedsandstonecomplex,resultinginhighergeothermalgradient.SwariehandMassarweh(1995)studiedthemajorgeothermalfieldinJordan(ZaraandZarqaMa'in).Theydescribedthereservoirandtheoptimumuseofthissourceofenergy.StudyofthethermalwaterinMukhiebehandShunehthermalwellfieldswasconducted(SwariehandMassarweh,1997).Theresultsrevealedthatthethermalwaterismixingwaterbetweenthehotwaterofthedeepaquiferandthecoldfreshwateroftheupperaquifer.Saudi(1999)studiedthethermalwaterwellsnearQueenAliaAirport.HefoundthatthemaximumreservoirtemperaturefortheJordanianwells–predictedbycalculationofvariousgeo-thermometers–exceeds100°C,andthatthethermalfluidsarewellmixedwithcoldgroundwaterinthestudiedarea.Saudietal.(2004)conductedseveralstudiesaboutthechemicalcompositionandpropertiesofgeothermalwaterfromcentralJordaninordertoevaluatetheirpossibleusefordesalinationofbrackishwater.Theyfoundthatthehighesttemperaturepredictedbyusingmineralsaturationindexforthereservoirisabout115°Candhighradonconcentrationisfoundonthefault'sintersections.Radonisaradioactivegas,anditspresencewouldlimitpossibleapplicationsofthiswater.
Inadditiontotheaforementionedstudies,geothermalresearchhasbeencarriedoutbyNRAincooperationwithsomeoftheJordanianuniversities(NRA,2007).Theresultsofthesestudies–basedonhydro-chemicalandhydro-geologicaldata–showthatthethermalwateroftheZarqaMa'in–Zarasystemistheresultofdeepcirculationinarelativelynormalgeothermalgradient.Geothermalresources
Jordanhasenormousundergroundenergyresourcesinmanypartsofthecountryintheformofthermalundergroundhotwater(wellsandthermalsprings).Thermalspringsformthemainsurfacemani-festationofgeothermalenergyinJordan,havingatemperaturerangingfrom20°Cto62°C(Swarieh,2000).ThesespringsaredistributedalongtheeasternescarpmentoftheJordanandDeadSeagraben(200km).About100thermalwellsdrilledforwaterintheDeadSeaRiftValley,theareaoftheAzraqBasinandRisha(NortheastJordan)andtheareasouthofQueenAliaAirporthavelowtointermediatewatertemperature.Asummaryofthesethermalwellsandspringswasreported(Sunna,2004).TheyarepresentedinTable6.CurrentandfutureutilizationofgeothermalenergyinJordan
TheInternationalGeothermalAssociation(IGA,2008)reportsnofurtherdevelopmentofdirectusesofgeothermalfluidswithrespecttothesituationdescribedbySaudiandSwarieh(2005).Inthelatterpublicationitwasreportedthattheinstalledcapacityatsixsitesis153.3MWtandtheannualenergysupplypotentialis1540TJ/yearintheformofdomestichotwaterforbathingandswimming,givinganoverallcapacityfactorof0.42(seeTable7).Possiblefutureapplica-tionsofgeothermalenergyincludeabsorptionrefrigerationtopreservefruitandvegetablesorfreezefishandmeat,aswellasfishfarmingandgreenhouseheating.
DevelopmentstrategyforgeothermalenergyinJordan
Beinganoilimportingcountry,Jordanshouldadoptthefollowingstrategiesforthedevelopmentandutilizationofgeothermalenergy:•Pursuinggeothermalenergyexplorationanddevelopment
•Conductingresearch,development,anddemonstrationstudiesfortheutilizationofgeothermalenergy
•Invitingprivatesectorparticipationinthegeothermalenergyindustry
•Formulatingregulationsandsupportingpoliciesongeothermalenergytoattractinvestorsingeothermalindustrialdevelopment•Heighteninginternationalcooperationparticularlyintheareasofinformationexchange,training,andlocalmanufacturing.Conclusions
Themainconclusionsderivedfromthepresentinvestigationmaybesummarizedasfollows:
•SinceJordanisanenergyimportingcountry,geothermalenergyhasthepotentialtoplayanimportantroleinitsfutureenergysupplynotonlyfromeconomicbutalsofromenvironmentpointofview.•Jordanhasenormousundergroundenergyresourcesinmanypartsofthecountryintheformofthermalundergroundhotwater(wellsandthermalsprings),havingatemperaturerangingfrom20°Cto62°C.
•Theinstalledcapacityofgeothermalenergyis153.3MWtandtheannualenergysupplypotentialis1540TJ/yearintheformofdomestichotwaterforbathingandswimming,givinganoverallcapacityfactorof0.42
•Possiblefutureapplicationsofgeothermalenergyincludeabsorp-tionrefrigerationtopreservefruitandvegetablesorfreezefishandmeat,aswellasfishfarmingandgreenhouseheating.References
Abu-AjamiehM.ThegeothermalresourcesofZarqaMa'inandZara.Amman:NRA;1980.AllenD.PreliminaryevaluationofthegeothermalpotentialofJordanrecommendations
forfuturestudies.Keyworh:BGS;1988.
BenderF.GeologyofJordan.Berlin:ContributionoftheRegionalGeologyoftheEarth.
GebruderBorntraeger;1974.
CEGCO,2007.Annualreport.CEGCO,Amman.
DiPaolaG.MissionreportonvisittothegeothermalprojectJOR/76/004inthe
HashemiteKingdomofJordanfrom30Novemberto4December1981.NewYork:UN/DTCD;1981.
FlaniganF,ElKaysiQ.Preliminaryinterpretationofaudio-magnetotelluric(ATM)
soundingintheZara–ZarqaMa'ingeothermalareas.Amman:USGS;1984.
GalanisS,SassJ,MunroeR,AjamiehAbu.HeatflowatZarqaMa'inandZaraanda
geothermalreconnaissanceofJordan.California:U.S.Geol.Survey;,1986.
GoldembergJ,JohanssonT,ReddyA,WilliamsR.Energyforasustainableworld.New
Delhi:WileyEastern;1987.
HakkiW,TeimehM.ThegeologyofZarqaMa'inandZaraareas.Amman:NRA;1981.HrayshatE.Oilshale—analternativeenergysourceforJordan.EnergySources,PartA
2008a;30:1915–20.
HrayshatE.AnalysisofrenewableenergysituationinJordan.EnergySources,PartB
2008b;3:89-102.
HrayshatE,Al-SoudM.SolarenergyinJordan:currentstateandprospects.Renewable
andSustainableEnergyReviews2004;8:193–200.
InternationalGeothermalAssociation,2008.http://iga.igg.cnr.it.Accessed25march
2009.
JordanRefinery,2007.Annualreport.JRpress,Amman.
JordanValleyAuthority,2007.Annualreport.JordanValleyAuthoritypress,Amman.KömürcüM,AkpinarA.Importanceofgeothermalenergyanditsenvironmentaleffects
inTurkey.RenewableEnergy2009;34:1611–5.
MabeyR.RecommendedprogramfortheZarqaMa'inandZaraarea.California:U.S.
Geol.Survey;1980.
MacDonaldM.EastBankJordanwaterresources.Amman:CentralWaterAuthority;
1965.
MarinelliG.ReportonthepossibilityofdevelopinggeothermalresourcesinJordan.
Rome:UniversityofPiza;1977.
McEwenR,HolconmbeH.InterpretationofresistivitydatainZarqaMa'inandZarahot
springs.Santiago:ExplorationGeothermics;1982.
McNittS.GeothermalresourcesinJordan—interpretationofdatasubmittedbythe
government.NewYork:UNDP;1976.MEMR,2007.Annualreport.MEMR,Amman.
128E.S.Hrayshat/EnergyforSustainableDevelopment13(2009)124–128
SunnaB.Recommendedapproachestodevelopthedirectutilizationofgeothermal
energy(hotwater).JordanInternationalWaterDemandManagementConference.Jordan:DeadSea;2004.
SwariehA.ThermalboreholesnearQueenAliaairport.Amman:NRA;1992.
SwariehA,MassarwehR.ThermalspringsinWadiIbnHammad.Amman:NRA;1993.SwariehA,MassarwehR.GeothermalwaterinZaraandZarqaMa'inarea.Amman:
NRA;1995.
SwariehA,MassarwehR.GeothermalwaterinMukhiebehandNorthShunehareas.
Amman:NRA;1997.
SwariehA.GeothermalenergyresourcesinJordan,countryupdate.ProceedingsWorld
GeothermalCongress.Tokyo:Kyushu;2000.
TruesdellA.Finalreportonthechemistryandgeothermalenergypossibilitiesofthe
Zara–ZarqaMa'insprings.California:Jordan.U.S.Geol.Survey;1979.
MyslilV.ReportonevaluationofgeothermalpotentialofJordan.Strojexportprague,
Gzechoslovakia.Prague:GeologicalSurvey;1988.NEPCO,2007.Annualreport.NEPCO,Amman.NRA,2007.Annualreport.NRA,Amman.
ReddyA,WilliamsR,JohanssonT.EnergyafterRio:prospectsandchallenges.NewYork:
UNDP;1997.
SaudiA.ThegeochemistryofthermalfluidinthegeothermalfieldnearAliaairportin
JordanandSelfossgeothermalfield.S-Iceland:UnitedNationsUniversity;1999.Saudi,A.,Swarieh,A.,2005.GeothermalenergyresourcesinJordan,countryupdate
report.InProceedingsofWorldGeothermalCongress,24–29AprilAntalya,Turkey:1–8.
SaudiA,SwariehA,DiabatA,MasriA,MasarwihR.ThermalfluidsincentralJordan.
Amman:NRA;2004.