Soultz-sous-Forets

General information about the site
Description of the geothermal plant

The Soultz-sous-Forêts geothermal project started in 1987, and is the cradle of the geothermal energy European research in granitic and fractured systems. After almost 30 years of research, the geothermal site is exploiting the fractured basement at 5 km depth, under commercial conditions, for the EEIG Heat Mining. The installed gross capacity of the plant is about 1.7 MWe.

The actual geothermal system is made of three wells: one production well named GPK-2 and two injection wells named GPK-3 and GPK-4. The geothermal brine is produced at a temperature of 150°C, reaching the wellhead with a nominal flow rate of 30 kg/s provided by a Downhole production Line Shaft Pump.

The geothermal brine is then flowing through a system of three consecutive double-pass tubular heat exchangers supplying heat to an. Organic Ranking Cycle (ORC), in order to produce electricity. The geothermal brine is then fully reinjected at around 70°C, and the volume of reinjected brine is shared between the two injection wells, one third in GPK-4 and two third in GPK-3 without using reinjection pumps. The reinjection temperature is linked to the conversion process. The geothermal plant has been successfully producing electricity since September 2016 under commercial conditions.

Presentation of the site
Soultz-sous-Forêts geothermal power plant
General documentation and bibliography

Genter A., Baujard C., Cuenot N., Hehn R., Maurer V., Mouchot J., Seibel O., Vidal J., Exploiting fractured granites for producing heat or electricity: dream or reality? 80th EAGE Conference & Exhibition, Copenhagen, Denmark, (2018)

Mouchot, J., Ravier, G., Seibel, O., Pratiwi, A.: Deep Geothermal Plants Operation in Upper Rhine Graben: Lessons Learned, European Geothermal Congress 2019, The Hague, Netherlands (2019)

https://geothermie.es.fr/references/projet-geie-emc/

Genter, A., Evans, K., Cuenot, N.,  Fritsch, D., Sanjuan, B., Contribution of the exploration of deep crystalline fractured reservoir of Soultz to the knowledge of enhanced geothermal systems (EGS), Comptes Rendus Geoscience, 342, Issues 7–8, 502-516, 2010, https://www.sciencedirect.com/science/article/pii/S1631071310000179

Country
Location
Grand Est, Soultz-sous-Forest
Exploitation starting date
2016
Current status of the operation
Type of exploitation
Geographic coordinate system and map projection
WGS 84
X coordinate
48.93
Y coordinate
7.88
Site operator
GEIE EMC
Privacy
Information filling date
Surface operation
Electricity energy produced (MW)
1.70
Power generation unit
Fluid cooling system
Gas control system
Reservoir / geothermal operations
Use of inhibitors
Y
Use of stimulation
Y
Exploitation flow rate (m3/h)
125.00
Surface discharge of geothermal fluids
N
Discharge temperature (°C)
70.00
Environmental related documents
Life cycle analysis
Life cycle analysis files
Document on LCA

Lacirignola, M., Meany, B. H., Padey, P. & Blanc, I. A simplified model for the estimation of life-cycle greenhouse gas emissions of enhanced geothermal systems. Geotherm. Energy 2, 1–19 (2014).

Lacirignola, M. & Blanc, I. Environmental analysis of practical design options for enhanced geothermal systems (EGS) through life-cycle assessment. Renew. Energy 50, 901–914 (2013).

Environment impact assessments
Document on environment impact assessment
Reservoir characteristics
Depth of top reservoir formation (m b.g.l.)
1500
Average reservoir thickness (m)
2500.00
Reservoir temperature (°C)
160.00
Reservoir pressure at datum (bars)
358.00
Reference depth for pressure (m b.g.l.)
3500.00
Productivity index (m3/h/bar)
2.90000
Injectivity index (m3/h/bar)
1.80000
Mineralisation (TDS mg/L)
100000.00
Dominant phase of the geothermal resource
Gas water ratio (val/vol)
1.10
Presence of hydrocarbons
No
Geothermal fluid composition
Na-Ca-K-Cl
Gas composition
90% CO2
Geological context
Geological setting
Geological plays
Geological control
Geological period
Lithology
Stratigraphy
Basement
Natural seismicity