WP 2 Romanian Report. Romanian Storage Capacity
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1 WP 2 Romanian Report Romanian Storage Capacity EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
2 Content 1. Romanian Sedimentary Basins 2. CO 2 Storage Possibilities in Deep Saline Aquifers 3. CO 2 Storage Possibilities in Hydrocarbon Fields 4. Romanian Case Studies EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
3 1. Romanian Sedimentary Basins EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
4 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
5 The major sedimetary structures within Romanian territory are: Pannonian Depression: Transylvanian Depression (TD) Pannonian Depression North (PDN) Pannonian Depression South (PDS) Moesian Platform: Moesian Platform West (MPW) Moesian Platform East (MPE) East Carpathians Paleogene Flysh (ECPF) Carpathians Foredeep: East Carpathians Foredeep (ECF) Diapir Fold Zone (DFZ) Getic Depresssion (GD) Moldavian Platform (MP) North Dobrogea & Predobrogean Depression (NDPD) EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
6 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
7 2. CO 2 Storage Possibilities in Deep Saline Aquifers EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
8 Structure Stratigraphic unit Formation Lithology Top depth (m) Permeabilit y (md) Moesian Platform and South Carpathians Foredeep Sarmatian Sarmatian Limestones and arenitic rocks Moesian Platform and South Carpathians Foredeep Cretaceous Cretaceous Sandstones and sandy limestones Moesian Platform and South Carpathians Foredeep Triasic Triasic Siliceous sands and sandstones Moldavian Platform and East Carpathians Foredeep Sarmatian Valea Seaca Limy sandstones Moldavian Platform and East Carpathians Foredeep Lower Bademian Bademian Limestones 1000 Transilvanian Depression Sarmatian Sarmatian Sands 1000 Pannonian Depression Pannonian Pannonian Silty sands 1200 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
9 Structure/Zone Area (10 6 m 2 ) Thickness of aquifer (m) Net/gross ratio Effective Porosity CO 2 density (t/ m 3 ) Storage efficiency factor Total estimated CO 2 storage Capacity (Mt) Moesian Platform and South Carpathians Foredeep Moldavian Platform and East Carpathians Foredeep Transilvanian Depression Pannonian Depression Total estimated CO 2 storage capacity in deep saline aquifers (Mt) 18.6 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
10 3. CO 2 Storage Possibilities in Hydrocarbon Fields EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
11 Geological Units Produced Mt oil Gm3gas Produced estimated % oil % gas Total Mt oil Gm3 gas Gt CO2 capacity Oil d. Gas d. Pannonian depr ,03 0,07 Transilvanian depr ,27 Barlad Depression N. Dobrogean Pro East. Carpathians ,34 0,25 Getic Deprssion ,09 0,48 Moesian Platform ,13 0,34 Total ,59 3,41 Formation volume factor : Oil 1,5 Gas 0,005 CO2 density 0,5 Total 4,00 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
12 4. Romanian Case Studies EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
13 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
14 Tataru Hydrocarbon Field EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
15 Location the MioPliocene Subzone in Muntenia on the internal flank of the Carpathian Foredeep Storage formation Miocene sands Structure faulted anticline oriented W E system of longitudinal and transversal faults several tectonic blocks Moetian divided in three sandy complexes Me II ( m thick ) hydrocarbons Me int ( m thick ) Me I ( m thick) Pontian maximum thickness of 500 m Marls End of exploitation 2006 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
16 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
17 Field X coordinates Z coordinates WOC [mbsl] Etage [m] Porosity [%] Avg water saturation [%] Avg permeability Tataru Initial pressure [atm] Initial temperature [º C] Boi [m 3 /m 3 ] Bgi [m 3 /m 3 ] O.O.I.P [kt] O.G.i.P (solved) [Mm 3 ] Producible oil [kt] Producible solved gases [Mm 3 ] CO 2 storage capacity [Mt] EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
18 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
19 No. Powerplant Location Longitudes Latitudes Annual emission [Mt] 1 S.C. Termoelectrica S.A. SE Doicesti SE Doicesti 25º23' º59' S.C. Petrotel Lukoil S.A. Teleajen 26º03' º57' S.C. Dalkia Thermo River SRL Point of Brazi Brazi 25º59' º53' S.C. Electrocentrale Bucharest SA SE Bucharest Bucharest West PP Bucharest 28º58' º25' S.C. Electrocentrale Bucharest SA SE Bucharest Grozavesti PP Bucharest 26º03' º26' S.C. Electrocentrale Bucharest SASE Bucharest Bucharest South PP Bucharest 26º09' º24' S.C. Electrocentrale Bucharest SA SE Bucharest Progresu PP Bucharest 25º53' º53' EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
20 Ghercesti Malu Mare Hydrocarbon Field EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
21 Location near the city of Craiova western part of Moesian Platform Structure anticlines oriented N S and W E Reservoir formation Middle Jurasic Formation (Dogger) Dogger I sands, limy sandstones, siliceous sandstones, limestones, dolomites, marls, shales and siderites width of 130 m at Simnic and m at Malu Mare Dogger II mixed character breccias, micro conglomerates, siliceous sandstones, marls, limy sandstones The Pontian marly deposits of meters thickness meters of marly sands meters of greyyellowish marls EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
22 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
23 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
24 Hydrocarbons Dogger complexes I and II Dogger I has a narrow oil band situated around the big gas cap throughout the three structures Free gas deposits are known in both complexes. Ghercesti structure four gas cap oil deposits and an oil deposit in Dogger I Carcea structure five gas cap oil deposits in Dogger I Malu Mare structure three free gas deposits and a cap gas deposit in Dogger I six free gas deposits in Dogger II Pontian formation five faults: Ghercesti, Carcea, Malu Mare and Urechesti sand bed (230 m thick) free gases in sands EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
25 Field Ghercesti, Dg I Carcea, Dg I Malu Mare, Dg I Malu Mare, Dg II X coordinates Z coordinates WOC [m] GWC[m] GOC[m] Etage [m] Porosity [%] Initial pressure [atm] Initial temperature [ºC] Boi [m 3 /m 3 ] Bgi [m 3 /m 3 ] O.O.I.P [kt] O.G.i.P (cap) [Mm 3 ] O.G.i.P (solved) [Mm 3 ] Producible oil [kt] Producible cap gas [Mm 3 ]] Producible solved gases [Mm 3 ] CO 2 storage capacity [Mt] EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
26 EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
27 No Powerplant Location Longitudes Latitudes Annual emission [Mt] 1 S.C. Energy Complex Rovinari S.A. Rovinari 23º09' º55' S.C Govora Power Plant SA Ramnicu Valcea 24º17' º03' S.C. Energy Complex Turceni S.A. Filiasi 23º24' º40' S.C. Energy Complex Craiova S.A. SE Isalnita Isalnita 23º24' º24' S.C. Energy Complex Craiova S.A. SE Craiova II Craiova 23º48' º20' EU GeoCapacity Final Conference, Copenhagen, 2122 October 2009
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