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GEOTHERMAL SYSTEMSin TRANSENERGY region
Vienna,27. 5. 2010
Andrej Lapanje, MSc. Geological Survey of Slovenia
• Geothermal systems characteristics
• Transboundary aquifers and geothermal conditions
– that is why we are here
• Overview of geothermal systems in TRANSENERGY project areaSLOVENIA AUSTRIAHUNGARY SLOVAKIA
• Final remarks
PRESENTATION TOPICS
• heat source: normal or elevated heat flow• geothermal reservoir • fluid: liquid and/or gas
• impermeable low conductive overburden• recharge
GEOTHERMAL SYSTEMS
Modified from http://iga.igg.cnr.it/geo/geoenergy.php
CLASSIFICATION OF GEOTHERMAL SYSTEMS
(Hochstein, 1988)
Low enthalpy resources < 90°C < 125°C
Intermediate enthalpy resources
90°-150°C 125°-225°C
High enthalpy resources >150°C >225°C
Geological and structural properties• depth• position• wideness• thickness• shape
Hydrogeological properties• porosity• permeability• transmissivity• static reservoir pressure• fluid mineralization• dissolved gas content
Geothermal properties• heat flow• fluid temperature
GEOTHERMAL RESERVOIRS
Muffler & Cataldi (1978); Hochstein (1990)
TRANSBOUNDARY AQUIFERS
Economic Commission for Europe: Inventory of Transboundary Ground Water in EuropeG.E. Arnold, Zs. Buzas GROUND WATER 2001. 43, no. 5: 669–678
HEAT FLOW IN TRANSENERGY REGION
Lenkey et al., 2002
Geotermalni sistemi v Sloveniji
GEOTHERMAL SYSTEMS in SLOVENIARelevant basin1. Mura-Zala basin
Maximum basin depths ~5.500m
Maximum reservoir temperatures ~200°C
Heat flow 60 -150 mW/m²Reservoir Systems: Basement, Sedimentary
Aquifers in sedimentary basins Basement aquifers beneath sedimentary basins
Tertiary sands, gravels and sandstones Fissured metamorphic Paleozoic rocks, fissured and karstified carbonate Mesozoic rocks
I II I II
25 – 60 °C < 80 °C 40 – 100 °C < 200 °C
Na-HCO3 Na-HCO3-Cl, Na-Cl Ca-Mg-HCO3, Na-HCO3-Cl, Na-Cl
Na-Cl
Low mineralization
High mineralization Low to moderate mineralization (0,5 -10g/l)
High mineralization (10-25 g/l)
Active recharge Connate water /minor recharge
Active to minor recharge
Connate water
Low gas content CO2, CH4 gas CO2 gas CO2, CH4 gas
Geothermal characteristics of Slovenia
SURFACE HEAT FLOW DENSITY - AUSTRIA
2. Vienna BasinMaximum basin depths ~7.000mMaximum reservoir temperatures ~200°CHeat flow 40-90 mW/m²Reservoir Systems: Bedrock, Sedimentary
3. Pannonian Basin (western margin)Maximum basin depths ~2.000mMaximum reservoir temperatures ~70°CHeat flow 70-110 mW/m²Reservoir Systems: Sedimentary
TRANSENERGY REGION - AUSTRIA1. Styrian Basin
Maximum basin depths ~3.500mMaximum reservoir temperatures ~130°CHeat flow 70-130 mW/m²Reservoir Systems: Bedrock, Sedimentary
Styrian Basin – hydrogeothermal overview
Goldbrunner J., 2005: Hydrogeological cross-section
Cross - section
Sedimentary reservoirs High mineralization low / no recharge Locally confined reservoirs
Bedrock reservoirs Low to moderate mineralization recharge High productivity
Preneogene Basement rocks (Styrian Basin & Mura - Zala Basin)
Moedling Block
cross - section
a)
b)
TRANSENERGY REGION - AUSTRIA2. Vienna Basin
Maximum basin depths ~7.000mMaximum reservoir temperatures ~200°CHeat flow 40-90 mW/m²Reservoir Systems: Bedrock, Sedimentary
Hydraulic barrier
Recharge area
High mineralization Connate Overpressured
Low mineralization Active recharge Temperature anomalies
Leopoldsdorf fault system
Geothermal gradient: ~5°C/100 m due to the thin litosphere → Middle Miocene back-arc style basin formation (rifting)
(Dövényi et al., 2002)
TRANSENERGY REGION - HUNGARYTemperature at a depth of 1000 m
Temperature at a depth of 2000 m
Heat flow density: 50 to 130 mW/m2
Thermal wells (T>30°C) of Hungary
high potential for intermediate and high-enthalpy resources below 1000 -1500 m
Energy content of the Upper-Pannonian-Quaternary reservoirs
(Dövényi et al., 2002)
Transenergy areas: Danube basin
Zala basin
main reservoirs
Mura-Zala basin geology
Major geothermal reservoirs: Late Miocene porous sediments
Energy content of the Mesozoic reservoirs
(Dövényi et al., 2002)
Transenergy areasKomarno Block (NE-Transdanubian Mts)
Zala basin
Major mesozoic hydrogeogical blocks of the Transdanubian Central range (after Jocha-Edelényi, 2004)
Major geothermal reservoirs: fractured-karstified mesozoic basement carbonates
SLOVAKIAGeothermal activity of selected areas expressed by surface heat flow densities
20 - Vienna Basin, 2 - Danube Basin (Central Depression), 1 - Komarno High Block, 19 - Komarno Marginal Block
Transenergy Region
Hydrogeological overview TE- SK1. Vienna Basin (Serial number of area 20)
Maximum basin depths ~6.000mMaximum reservoir temperatures ~170°CHeat flow 50-70 mW/m²Reservoir Systems: Bedrock, Sedimentary
2. Danube Basin (Central Depression) (2)Maximum basin depths ~6.000mMaximum reservoir temperatures ~200°CHeat flow 70-90 mW/m²Reservoir Systems: Sedimentary
3. Komarno High Block (1)Maximum basin depths ~3.000mMaximum reservoir temperatures ~100°CHeat flow 50-65 mW/m²Reservoir Systems: Bedrock
1.
2.
3.
4.
4. Komarno Marginal Block (19)Maximum basin depths ~2.000mMaximum reservoir temperatures ~50°CHeat flow 60-75 mW/m²Reservoir Systems: Bedrock , Sedimentary
Vienna Basin – geothermal overview
Danube Basin (Central Depression) – geothermal overview
Komarno High Block and Komarno Marginal Block – geothermal overview
Hydrogeothermal overviewVienna Basin Sedimentary BedrockTDS (g.l-1): 5 – 15 14 - 129Chemical Water Type: Na-Cl Na-ClAge of aquifer: Egenburgian TriassicAquifer lithology: clastics limestones
Danube Basin (Central Depression) Sedimentary TDS (g.l-1): 0,5 – 5 2,5 – 10 11- 125 Chemical Water Type: Na-HCO3, Na-Cl Na-ClAge of aquifer: Dacian-Pontian Pontian-Pannonian BadenianAquifer lithology: sands sands and sandstones andesites and base clastics
Komarno High Block BedrockTDS (g.l-1): 0,6 – 0,7Chemical Water Type: Ca-(Mg)-HCO3Age of aquifer: TriassicAquifer lithology: limestones, dolomites
Komarno Marginal Block Sedimentary BedrockTDS (g.l-1): 0,8 - 90 0,75 - 3,0Chemical Water Type: Ca-(Mg)-Na-HCO3-Cl, Na-Cl Ca-(Mg)-Na-SO4-Cl-HCO3Age of aquifer: Neogene Jurassic-Triassic Aquifer lithology: conglomerates and sands limestones
FINAL REMARKS
PRESENT SITUATIONVast pool of particular geognostic data in each partner stateDifferent approaches of the description of the same natural phenomena‘’White zones or border faults’’ – missing or misinterpreted geological models
of the border regionsThe transboundary character of geothermal systems is recognized –geological structures
do not stop at bordersTRANSENERGY Transboundary approach (homogenization and unification of knowledge about
geothermal systems in the region)Preparation of geognostic models (delineation and main parameter description of all
common geothermal systems)Exposition of promising areas for researchExposition of missing data to be research for
INPUT FOR THE IMPLEMENTATION TOOL