CO₂ storage potential of sedimentary basins of Slovakia, the Czech Republic, Poland and the Baltic States

• Autorzy: Šliaupa S. , Lojka R. , Tasáryová Z. , Kolejka V. , Hladík V. , Kotulová J. , Kucharič L. , Fejdi V. , Wójcicki V. , Tarkowski R. , Uliasz-Misiak B. , Šliaupienė R. , Nulle I. , Pomeranceva R. , Ivanova O. , Shogenova A. , Shogenov K.
• Języki publikacji: EN

Abstrakty

EN

It has been increasingly realised that geological storage of CO₂ is a prospective option for reduction of CO₂ emissions. The CO₂ geological storage potential of sedimentary basins with the territory of Slovakia, the Czech Republic, Poland, and the Baltic States is here assessed, and different storage options have been considered. The most prospective technology is hydrodynamic trapping in the deep saline aquifers. The utilisation of hydrocarbon (HC) fields is considered as a mature technology; however storage capacities are limited in the region and are mainly related to enhanced oil (gas) recovery. Prospective reservoirs and traps have been identified in the Danube, Vienna and East Slovakian Neogene basins, the Neogene Carpathian Foredeep, the Bohemian and Fore-Sudetic Upper Paleozoic basins, the Mesozoic Mid-Polish Basin and the pericratonic Paleozoic Baltic Basin. The total storage capacity of the sedimentary basins is estimated to be as much as 10170 Mt of CO₂ in deep saline aquifer structures, and 938 Mt CO₂ in the depleted HC fields. The utilisation of coal seams for CO₂ storage is related to the Upper Silesian Basin where CO₂ storage could be combined with enhanced recovery of coal-bed methane.

Słowa kluczowe

EN

CO2 geological storage; saline aquifer; coal bed; EOR; ECBM

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2013
• Tom: Vol. 57, No. 2
• Strony: 219–--232
• Opis fizyczny: Bibliogr. 67 poz., rys., wykr.

Twórcy

autor

Šliaupa S.

• Institute of Geology and Geography, Nature Research Centre, Ševèenkos 13, 03223 Vilnius, Lithuania

autor

Lojka R.

• Czech Geological Survey, Klárov 3, 118 21 Praha 1, Czech Republic

autor

Tasáryová Z.

• Institute of Geology and Geography, Nature Research Centre, Ševèenkos 13, 03223 Vilnius, Lithuania

autor

Kolejka V.

• Institute of Geology and Geography, Nature Research Centre, Ševèenkos 13, 03223 Vilnius, Lithuania

autor

Hladík V.

• Institute of Geology and Geography, Nature Research Centre, Ševèenkos 13, 03223 Vilnius, Lithuania

autor

Kotulová J.

• Dionýz Štúr State Geological Institute, Mlynská dolina 1, 817 04 Bratislava 11, Slovak Republic

autor

Kucharič L.

• Dionýz Štúr State Geological Institute, Mlynská dolina 1, 817 04 Bratislava 11, Slovak Republic

autor

Fejdi V.

• Dionýz Štúr State Geological Institute, Mlynská dolina 1, 817 04 Bratislava 11, Slovak Republic

autor

Wójcicki V.

• Polish Geological Institute – National Research Institute, Rakowiecka 4, 00-975 Warszawa, Poland

autor

Tarkowski R.

• Min eral and En ergy Econ omy Research Institute, Polish Academy of Sciences, Wybickiego 7, 31-261 Kraków, Poland

autor

Uliasz-Misiak B.

• AGH University of Science and Technology, Faculty of Drilling, Oil and Gas, A. Mickiewicza 30, 30-059 Kraków, Poland

autor

Šliaupienė R.

• Institute of Geology and Geography, Nature Research Centre, Ševèenkos 13, 03223 Vilnius, Lithuania

autor

Nulle I.

• State Ltd “Latvian Environment, Geology and Meteorology Centre”, Maskavas 165, 1019 Riga, Latvia

autor

Pomeranceva R.

• State Ltd “Latvian Environment, Geology and Meteorology Centre”, Maskavas 165, 1019 Riga, Latvia

autor

Ivanova O.

• State Ltd “Latvian Environment, Geology and Meteorology Centre”, Maskavas 165, 1019 Riga, Latvia

autor

Shogenova A.

• Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia

autor

Shogenov K.

• Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia

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