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21 May 2008 SPE ATW Dubrovnik 1 Assessing European Capacity for Geological Storage of Carbon Dioxide www.geocapacity.eu Bruno Saftić, Domagoj Vulin & Iva Kolenković PERSPECTIVES FOR GEOLOGICAL PERSPECTIVES FOR GEOLOGICAL STORAGE STORAGE OF CARBON DIOXIDE IN CROATIA OF CARBON DIOXIDE IN CROATIA

Bruno Saftić, Domagoj Vulin & Iva Kolenković

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Bruno Saftić, Domagoj Vulin & Iva Kolenković. PERSPECTIVES FOR GEOLOGICAL STORAGE OF CARBON DIOXIDE IN CROATIA. Sources 7 TPP NGPP Molve CO 2 emmissions 23 M t/yr (2003) Reported from these point sources 6 M t/yr (2003) 5 Mt/yr (2005). Conclusions - PowerPoint PPT Presentation

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Page 1: Bruno Saftić, Domagoj Vulin & Iva Kolenković

21 May 2008 SPE ATW Dubrovnik 1

Assessing European Capacity for Geological Storage of Carbon Dioxide    

www.geocapacity.eu

Bruno Saftić, Domagoj Vulin & Iva Kolenković

PERSPECTIVES FOR PERSPECTIVES FOR GEOLOGICAL STORAGE GEOLOGICAL STORAGE

OF CARBON DIOXIDE IN CROATIAOF CARBON DIOXIDE IN CROATIA

Page 2: Bruno Saftić, Domagoj Vulin & Iva Kolenković

21 May 2008 SPE ATW Dubrovnik 2

Assessing European Capacity for Geological Storage of Carbon Dioxide    

www.geocapacity.eu

Page 3: Bruno Saftić, Domagoj Vulin & Iva Kolenković

21 May 2008 SPE ATW Dubrovnik

Assessing European Capacity for Geological Storage of Carbon Dioxide    

www.geocapacity.eu

Page 4: Bruno Saftić, Domagoj Vulin & Iva Kolenković

21 May 2008 SPE ATW Dubrovnik 4

Assessing European Capacity for Geological Storage of Carbon Dioxide    

www.geocapacity.eu

Sources- 7 TPP- NGPP Molve

CO2 emmissions

23 Mt/yr (2003)Reported from these point sources

- 6 Mt/yr (2003)- 5 Mt/yr (2005)

Page 5: Bruno Saftić, Domagoj Vulin & Iva Kolenković

21 May 2008 SPE ATW Dubrovnik 5

Assessing European Capacity for Geological Storage of Carbon Dioxide    

www.geocapacity.eu

Page 6: Bruno Saftić, Domagoj Vulin & Iva Kolenković

21 May 2008 SPE ATW Dubrovnik 6

Assessing European Capacity for Geological Storage of Carbon Dioxide    

www.geocapacity.eu

ConclusionsThere are favourable natural conditions for geological storage of CO2 in deep structural depressions of the southern Pannonian basin and in the Adriatic offshore.

The most prospective objects in the near future are the depleted hydrocarbon fields.

Significantly larger capacity is estimated in the deep saline aquifers, but it is necessary to develop research projects targeted specifically to the better definition of their geological composition and reservoir properties.