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Određivanje potencijala geotermalnih ležištas otopljenim ugljikovodičnim plinom

Marko Gaćina ; INA-Industrija nafte, d.d., Zagreb
Maja Gregurić-Malekoci ; INA-Industrija nafte, d.d., Zagreb
Adaleta Perković orcid id orcid.org/0009-0005-7301-2146 ; INA-Industrija nafte, d.d., Zagreb
Jasmina Jelić-Balta ; INA-Industrija nafte, d.d., Zagreb


Puni tekst: engleski pdf 1.709 Kb

str. 99-109

preuzimanja: 49

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Sažetak

S obzirom da je rast i razvoj geotermalne energije usko povezan i s naftnom industrijom, u radu je evaluirana mogućnost iskorištavanja geotermalnih ležišta gdje osim vode, u ležištu postoji i određena količina otopljenog plina koji u svom sastavu sadrži i ugljikovodike. Uloga takvog plina mogla bi biti značajna u podizanju rentabilnosti razvoja geotermalnog projekta, posebno u njegovom začetku. Glavni cilj rada je dati potrebne tehničke parametre kako bi se mogla izvršiti tehno-ekonomska analiza geotermalnog projekta koji se koristi već izbušenim bušotinama, rađenim za potrebe istraživanja ugljikovodika. U radu su korišteni seizmički podaci uz pomoć kojih je određena površina ležišta, bušotinski (karotažni) podaci za određivanje pojedinih litologija i debljina slojeva te njihove poroznosti. Također, korištena su i DST ispitivanja iz kojih je potvrđeno da su određeni slojevi zasićeni osim vode i s plinom u kojem udio ugljičnog dioksida i ugljikovodičnih komponenti varira ovisno o ispitivanom sloju. Obzirom da se radi o plinu otopljenom u vodi, potrebno je bilo upotrebom ležišne simulacije odrediti njegov iscrpak pri simultanoj proizvodnji plinom zasićene vode te utiskivanju degazirane. Provedeni su različiti simulacijski slučajevi koji pokrivaju MIN, MAX i MED petrofizikalne setove podataka te su uspoređeni s rezultatima prethodno kreiranog Monte Carlo modela. Osim ukupnog iscrpka plina, razmatrano je i ponašanje ležišnog tlaka i temperature u projektnom razdoblju od 30 godina.

Ključne riječi

ugljikovodični plin; geotermalna energija; ležišna simulacija; Monte Carlo metoda

Hrčak ID:

329301

URI

https://hrcak.srce.hr/329301

Datum izdavanja:

21.10.2019.

Podaci na drugim jezicima: engleski

Posjeta: 237 *




Introduction

Besides water, deeper geothermal reservoirs always contain some amount of dissolved gas. Usually, the gas composition is mostly carbon dioxide but sometimes it is enriched with lighter hydrocarbons, namely methane. Those hydrocarbons could potentially be of a great interest if their amount is significant which is mostly related to the pressure and temperature conditions in the reservoir and water production rates. In this work, we have considered a potential geothermal reservoir located in the Croatian part of the Pannonian basin for which data collected during a well DST performance was available as well as petrophysical data, gas and water analyses and geological and seismic studies. The prospect was explored during the 1980s in order to find oil and gas reserves. Data collected served for the initialization of the conceptual reservoir simulation models. Considering very high investment needs at the beginning of every geothermal project, namely drilling wells and building the power plant, additional income coming from the hydrocarbon gas could have a key role in project economics and investment return rate.

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References

1. 

Barylo A. , author. 2000."Assessment of the energy potential of the Beregovsky geothermal system, Ukraine.". United Nations University. ():

2. 

Blount C.W.; ; Price L.C. , authors. 1982."Solubility of Methane in Water Under Natural Conditions: A Laboratory Study". Final Report,DOE Contract No. DE-A508-78ET12145. ():

3. 

Dickson M.H.; ; Fanelli M. , authors. 2013."Geothermal energy: utilization and technology". Routledge. ():

4. 

DiPippo R. , author. 2016."Geothermal power generation: Developments and innovation.". Woodhead Publishing. ():

5. 

Duan Z.; ; Mao S. , authors. 2006."A thermodynamic model for calculating methane solubility, density and gas phase composition of methane-bearing aqueous fluids from 273 to 523 K and from 1 to 2000 bar". Geochimica et Cosmochimica Acta. 70(13):3369–3386

6. 

Ganjdanesh R.; ; Hosseini S.A. , authors. 2016.Potential assessment of methane and heat production from geopressured–geothermal aquifers. Geothermal Energy. 4(1):

7. 

Grant M.A. , author. 2015.Resource assessment, a review, with reference to the Australian code. Resource. ():

8. 

Li X.; ; Yang D. , authors. 2013.. Determination of Mutual Solubility between CO2 and Water by Using the Peng–Robinson Equation of State with Modified Alpha Function and Binary Interaction Parameter. Industrial and Engineering Chemistry Research. 52(38):13829–13838

9. 

Mao S.; ; Hu J.; ; Zhang D.; ; Li Y. , authors. 2013.Thermodynamic modeling of ternary CH4H2ONaCl fluid inclusions. Chemical Geology. (335):128–135

10. 

Ofwona C.O. , author. 2014.Geothermal resource assessment: case example. Olkaria I. 001374011. ():

11. 

Peng D.Y.; ; Robinson D.B. , authors. 1976. A new two-constant equation of state. Industrial and Engineering Chemistry Fundamentals. 15(1):59–64

12. 

Trota A.; ; Ferreira P.; ; Gomes L.; ; Cabral J.; ; Kallberg P. , authors. 2019.Power Production Estimates from Geothermal Resources by Means of Small-Size Compact Climeon Heat Power Converters: Case Studies from Portugal (Sete Cidades, Azores and Longroiva Spa, Mainland). Energies. 12(14):2838–

13. 

Ziabakhsh-Ganji Z.; ; Kooi H. , authors. 2012.An Equation of State for thermodynamic equilibrium of gas mixtures and brines to allow simulation of the effects of impurities in subsurface CO2 storage. International Journal of Greenhouse Gas Control. (11):


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