Supercritical Geothermal Systems - A Review of Past Studies and Ongoing Research Activities

International audience Supercritical geothermal systems are very high temperature geothermal systems that are located at depths near or below the brittle-ductile transition zone in the crust where the reservoir fluid is assumed to be in the supercritical state, e.g., for pure water temperature and p...

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Bibliographic Details
Main Authors: Dobson, Patrick, Asanuma, Hiroshi, Huenges, Ernst, Poletto, Flavio, Reinsch, Thomas, Sanjuan, Bernard
Other Authors: Lawrence Berkeley National Laboratory Berkeley (LBNL), Fukushima Renewable Energy Institute, German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ), Istituto Nazionale di Oceanografica e di Geofisica Sperimentale Trieste, Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)
Format: Conference Object
Language:English
Published: HAL CCSD 2017
Subjects:
supercritical geothermal systems
brittle-ductile transition
international collaboration
[SPI.NRJ]Engineering Sciences [physics]/Electric power
New Zealand
Reykjanes
Krafla
Iceland
Online Access:https://hal.science/hal-01497951
https://hal.science/hal-01497951/document
https://hal.science/hal-01497951/file/Dobson_etal_2017_final.pdf
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Summary:International audience Supercritical geothermal systems are very high temperature geothermal systems that are located at depths near or below the brittle-ductile transition zone in the crust where the reservoir fluid is assumed to be in the supercritical state, e.g., for pure water temperature and pressure are respectively in excess of 374°C and 221 bar. These systems have garnered attention in recent years as a possible type of unconventional geothermal resource that could yield much higher well productivities due to their very high enthalpy fluids. Supercritical conditions are often found at the roots of volcanic-hosted hydrothermal systems. Deep wells drilled in geothermal fields such as The Geysers and Salton Sea, USA, Kakkonda, Japan, Larderello, Italy, Krafla, Iceland and Los Humeros, Mexico, have encountered temperatures in excess of 374°C, and in some cases have encountered fluid entries. The IDDP-1 well at Krafla encountered magma, and ended up producing very high enthalpy fluids; however these fluids were very corrosive and abrasive. Innovative drilling and well completion techniques may be needed to deal with the extreme temperatures and aggressive fluid chemistry compositions of these systems. New efforts are underway in Japan (northern Honshu), Italy (Larderello), Iceland (Reykjanes peninsula), Mexico (Los Humeros), and New Zealand (Taupo Volcanic Zone) to investigate supercritical systems. The Japan Beyond Brittle Project (JBBP), the New Zealand Hotter and Deeper Project (HADES), the FP7 project IMAGE as well as the Horizon 2020 projects DEEPEGS, DESCRAMBLE, GeoWell and GEMex, funded by the European Commission, provide an unprecedented opportunity for international collaboration to help solve the technical challenges associated with characterizing, drilling, and developing these high temperature systems. To facilitate interaction, METI Japan organized a meeting with invited representatives from selected G7 countries to discuss international collaboration for supercritical geothermal development ...

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