Active seismic characterization experiments of the Hontomin research facility for geological storage of CO2, Spain

J. Alcalde*, D. Marti, A. Calahorrano, I. Marzan, P. Ayarza, R. Carbonell, C. Juhlin, A. Perez-Estaun

*Corresponding author for this work

Research output: Contribution to journalArticle

22 Citations (Scopus)

Abstract

An active source seismic experiment was carried out as part of the subsurface characterization study of the first Spanish Underground Research Facility for Geological Storage of CO2 in Hontomin (Burgos, Spain). The characterization experiment included a 36 km(2) 3D seismic reflection survey and two three-component seismic profiles. The target reservoir is a saline aquifer located at 1450 m depth within Lower Jurassic carbonates (Lias). The main seal is formed by interlayered marlstones and marly limestones of Early to Middle Jurassic age (Dogger and Lias). The seismic images obtained allow defining the 3D underground architecture of the reservoir site. The structure consists of an asymmetric dome crosscut by a relatively complex fault system. The detailed characterization of the fracture system is currently under study to unravel the geometric distribution of the faults and their extent within the different formations that form the structure. The constrained model has guided the design of the injection and monitoring boreholes and provided the data for the baseline study. The resultant high resolution seismic model will be used as a reference in future monitoring stages. (C) 2013 Elsevier Ltd. All rights reserved.

Original languageEnglish
Pages (from-to)785-795
Number of pages11
JournalInternational journal of greenhouse gas control
Volume19
Early online date1 Mar 2013
DOIs
Publication statusPublished - Nov 2013

Keywords

  • 3D seismic reflection
  • Reservoir characterization
  • CO2 storage
  • High resolution
  • Three-component seismic

Cite this

Active seismic characterization experiments of the Hontomin research facility for geological storage of CO2, Spain. / Alcalde, J.; Marti, D.; Calahorrano, A.; Marzan, I.; Ayarza, P.; Carbonell, R.; Juhlin, C.; Perez-Estaun, A.

In: International journal of greenhouse gas control, Vol. 19, 11.2013, p. 785-795.

Research output: Contribution to journalArticle

Alcalde, J, Marti, D, Calahorrano, A, Marzan, I, Ayarza, P, Carbonell, R, Juhlin, C & Perez-Estaun, A 2013, 'Active seismic characterization experiments of the Hontomin research facility for geological storage of CO2, Spain', International journal of greenhouse gas control, vol. 19, pp. 785-795. https://doi.org/10.1016/j.ijggc.2013.01.039
Alcalde, J. ; Marti, D. ; Calahorrano, A. ; Marzan, I. ; Ayarza, P. ; Carbonell, R. ; Juhlin, C. ; Perez-Estaun, A. / Active seismic characterization experiments of the Hontomin research facility for geological storage of CO2, Spain. In: International journal of greenhouse gas control. 2013 ; Vol. 19. pp. 785-795.
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abstract = "An active source seismic experiment was carried out as part of the subsurface characterization study of the first Spanish Underground Research Facility for Geological Storage of CO2 in Hontomin (Burgos, Spain). The characterization experiment included a 36 km(2) 3D seismic reflection survey and two three-component seismic profiles. The target reservoir is a saline aquifer located at 1450 m depth within Lower Jurassic carbonates (Lias). The main seal is formed by interlayered marlstones and marly limestones of Early to Middle Jurassic age (Dogger and Lias). The seismic images obtained allow defining the 3D underground architecture of the reservoir site. The structure consists of an asymmetric dome crosscut by a relatively complex fault system. The detailed characterization of the fracture system is currently under study to unravel the geometric distribution of the faults and their extent within the different formations that form the structure. The constrained model has guided the design of the injection and monitoring boreholes and provided the data for the baseline study. The resultant high resolution seismic model will be used as a reference in future monitoring stages. (C) 2013 Elsevier Ltd. All rights reserved.",
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author = "J. Alcalde and D. Marti and A. Calahorrano and I. Marzan and P. Ayarza and R. Carbonell and C. Juhlin and A. Perez-Estaun",
note = "The authors sincerely thank the Managing Guest Editor Michael K{\"u}hn, Guest Editor Stefan Lueth and the anonymous reviewers for their useful comments. Funding for this Project has been partially provided by the Spanish Ministry of Industry, Tourism and Trade, through the CIUDEN-CSIC-Inst. Jaume Almera agreement (Characterization, Development and Validation of Seismic Techniques applied to CO2 Geological Storage Sites) and by the European Union through the Technology Demonstration Plant of Compostilla OXYCFB300 Project (European Energy Programme for Recovery). Additional support has been provided by Spanish Ministry of Education and Science and Generalitat de Catalunya through grants: CSD2006-00041 and 2009SGR006, respectively. The sole responsibility of this publication lies with the author. The European Union is not responsible for any use that may be made of the information contained herein. Juan Alcalde is being currently supported by the Fundaci{\'o}n Ciudad de la Energ{\'i}a (CIUDEN) Research training program. We sincerely thank CGGVeritas for their assistance during the acquisition. Processing has been carried out using GLOBE Claritas™, under license from the Institute of Geological and Nuclear Sciences Limited, Lowre Hutt, New Zealand and SeismicUnix from CWP (Center for the Wave phenomena, Colorado School of Mines). We thank all the people involved directly or indirectly in the elaboration of this work.",
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AU - Ayarza, P.

AU - Carbonell, R.

AU - Juhlin, C.

AU - Perez-Estaun, A.

N1 - The authors sincerely thank the Managing Guest Editor Michael Kühn, Guest Editor Stefan Lueth and the anonymous reviewers for their useful comments. Funding for this Project has been partially provided by the Spanish Ministry of Industry, Tourism and Trade, through the CIUDEN-CSIC-Inst. Jaume Almera agreement (Characterization, Development and Validation of Seismic Techniques applied to CO2 Geological Storage Sites) and by the European Union through the Technology Demonstration Plant of Compostilla OXYCFB300 Project (European Energy Programme for Recovery). Additional support has been provided by Spanish Ministry of Education and Science and Generalitat de Catalunya through grants: CSD2006-00041 and 2009SGR006, respectively. The sole responsibility of this publication lies with the author. The European Union is not responsible for any use that may be made of the information contained herein. Juan Alcalde is being currently supported by the Fundación Ciudad de la Energía (CIUDEN) Research training program. We sincerely thank CGGVeritas for their assistance during the acquisition. Processing has been carried out using GLOBE Claritas™, under license from the Institute of Geological and Nuclear Sciences Limited, Lowre Hutt, New Zealand and SeismicUnix from CWP (Center for the Wave phenomena, Colorado School of Mines). We thank all the people involved directly or indirectly in the elaboration of this work.

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N2 - An active source seismic experiment was carried out as part of the subsurface characterization study of the first Spanish Underground Research Facility for Geological Storage of CO2 in Hontomin (Burgos, Spain). The characterization experiment included a 36 km(2) 3D seismic reflection survey and two three-component seismic profiles. The target reservoir is a saline aquifer located at 1450 m depth within Lower Jurassic carbonates (Lias). The main seal is formed by interlayered marlstones and marly limestones of Early to Middle Jurassic age (Dogger and Lias). The seismic images obtained allow defining the 3D underground architecture of the reservoir site. The structure consists of an asymmetric dome crosscut by a relatively complex fault system. The detailed characterization of the fracture system is currently under study to unravel the geometric distribution of the faults and their extent within the different formations that form the structure. The constrained model has guided the design of the injection and monitoring boreholes and provided the data for the baseline study. The resultant high resolution seismic model will be used as a reference in future monitoring stages. (C) 2013 Elsevier Ltd. All rights reserved.

AB - An active source seismic experiment was carried out as part of the subsurface characterization study of the first Spanish Underground Research Facility for Geological Storage of CO2 in Hontomin (Burgos, Spain). The characterization experiment included a 36 km(2) 3D seismic reflection survey and two three-component seismic profiles. The target reservoir is a saline aquifer located at 1450 m depth within Lower Jurassic carbonates (Lias). The main seal is formed by interlayered marlstones and marly limestones of Early to Middle Jurassic age (Dogger and Lias). The seismic images obtained allow defining the 3D underground architecture of the reservoir site. The structure consists of an asymmetric dome crosscut by a relatively complex fault system. The detailed characterization of the fracture system is currently under study to unravel the geometric distribution of the faults and their extent within the different formations that form the structure. The constrained model has guided the design of the injection and monitoring boreholes and provided the data for the baseline study. The resultant high resolution seismic model will be used as a reference in future monitoring stages. (C) 2013 Elsevier Ltd. All rights reserved.

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KW - High resolution

KW - Three-component seismic

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JO - International journal of greenhouse gas control

JF - International journal of greenhouse gas control

SN - 1750-5836

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