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The natural seismic hazard and induced seismicity of the european HDR (hot dry rock) geothermal energy project at Soultz-sous-Forets (Bas-Rhin, France); Alea sismique naturel et sismicite induite du projet geothermique europeen RCS (roche chaude seche) de Soultz-sous-Forets (Bas-Rhin, France)

Abstract

Development of the Soultz-sous-Forets HDR (Hot Dry Rock) geothermal energy project will involve important fluid injections which will induce micro-seismic events. This thesis discusses the natural seismicity of the region and induced seismicity associated with fluid injections. A catalogue of all historical and instrument seismicity of the Soultz-sous-Forets (SSF) region has been compiled. This seismicity does not correspond to movements along the major tectonic features of the region. The area around SSF has been identified as being one where high heat flow corresponds to low seismicity. The largest well documented seismic event in the region which took place in 1952 had an epicentral intensity of VI. All important data pertaining to the series of seismic events which took place in the region from August to October 1952 have been collected and are presented. This work details the installation and operation of a permanent 3 station network of accelerometers and seismometers around the HDR site. Also the installation and operation of a mobile network of vertical seismometers during fluid injections. 167 micro-seismic events were recorded on the surface network, with magnitudes from -0.5 to 1.9. The preferential alignment of the micro-seismic cloud is N160 deg. Individual focal mechanisms of the larger  More>>
Authors:
Publication Date:
Jun 07, 1996
Product Type:
Thesis/Dissertation
Report Number:
FRNC-TH-4123
Reference Number:
SCA: 150600; 150301; 150906; PA: FRC-98:005217; EDB-98:105149; SN: 98002000032
Resource Relation:
Other Information: TH: These (D. es Sc.); PBD: 7 Jun 1996
Subject:
15 GEOTHERMAL ENERGY; HOT-DRY-ROCK SYSTEMS; FLUID INJECTION; SEISMICITY; HEAT FLUX; SEISMIC DETECTION; SEISMIC P WAVES; STRESS ANALYSIS; ENVIRONMENTAL EFFECTS; GRANITES; GEOLOGIC FAULTS; MICROEARTHQUAKES; GEOTHERMAL WELLS; SEISMIC SURVEYS; ACCELEROMETERS; HYDRAULIC FRACTURING; WELL STIMULATION; TECTONICS; GREEN FUNCTION; GROUND MOTION
OSTI ID:
655566
Research Organizations:
Universite Louis Pasteur, 67 - Strasbourg (France); Ecole et Observatoire de Physique du Globe de Strasbourg, 67 (France). Laboratoire de Sismologie
Country of Origin:
France
Language:
English;French
Other Identifying Numbers:
Other: ON: DE98775483; TRN: FR9805217
Availability:
OSTI as DE98775483
Submitting Site:
FR
Size:
197 p.
Announcement Date:
Oct 30, 1998

Citation Formats

Helm, J A. The natural seismic hazard and induced seismicity of the european HDR (hot dry rock) geothermal energy project at Soultz-sous-Forets (Bas-Rhin, France); Alea sismique naturel et sismicite induite du projet geothermique europeen RCS (roche chaude seche) de Soultz-sous-Forets (Bas-Rhin, France). France: N. p., 1996. Web.
Helm, J A. The natural seismic hazard and induced seismicity of the european HDR (hot dry rock) geothermal energy project at Soultz-sous-Forets (Bas-Rhin, France); Alea sismique naturel et sismicite induite du projet geothermique europeen RCS (roche chaude seche) de Soultz-sous-Forets (Bas-Rhin, France). France.
Helm, J A. 1996. "The natural seismic hazard and induced seismicity of the european HDR (hot dry rock) geothermal energy project at Soultz-sous-Forets (Bas-Rhin, France); Alea sismique naturel et sismicite induite du projet geothermique europeen RCS (roche chaude seche) de Soultz-sous-Forets (Bas-Rhin, France)." France.
@misc{etde_655566,
title = {The natural seismic hazard and induced seismicity of the european HDR (hot dry rock) geothermal energy project at Soultz-sous-Forets (Bas-Rhin, France); Alea sismique naturel et sismicite induite du projet geothermique europeen RCS (roche chaude seche) de Soultz-sous-Forets (Bas-Rhin, France)}
author = {Helm, J A}
abstractNote = {Development of the Soultz-sous-Forets HDR (Hot Dry Rock) geothermal energy project will involve important fluid injections which will induce micro-seismic events. This thesis discusses the natural seismicity of the region and induced seismicity associated with fluid injections. A catalogue of all historical and instrument seismicity of the Soultz-sous-Forets (SSF) region has been compiled. This seismicity does not correspond to movements along the major tectonic features of the region. The area around SSF has been identified as being one where high heat flow corresponds to low seismicity. The largest well documented seismic event in the region which took place in 1952 had an epicentral intensity of VI. All important data pertaining to the series of seismic events which took place in the region from August to October 1952 have been collected and are presented. This work details the installation and operation of a permanent 3 station network of accelerometers and seismometers around the HDR site. Also the installation and operation of a mobile network of vertical seismometers during fluid injections. 167 micro-seismic events were recorded on the surface network, with magnitudes from -0.5 to 1.9. The preferential alignment of the micro-seismic cloud is N160 deg. Individual focal mechanisms of the larger seismic events correspond to an extensional tectonic regime. Stress inversion of P wave polarities indicates that the maximum stress is vertical and the intermediate and minimum stress axes horizontal. The largest of the horizontal stresses is orientated N124 deg and the smallest N34 deg. Induced seismic movement is taking place on pre-existing fractures controlled by the in situ stress seismic movement is taking place on pre-existing tectonic fractures controlled by the in situ stress field, and the largest of the induced events had a magnitude 1.9. This level of seismicity does not pose any environmental hazard to the region around Soultz-sous-Forets. (author) 151 refs.}
place = {France}
year = {1996}
month = {Jun}
}