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Active seismic characterization experiments of the Hontomin research facility for geological storage of CO2, Spain
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2013 (English)In: International Journal of Greenhouse Gas Control, ISSN 1750-5836, E-ISSN 1878-0148, Vol. 19, no 0, 785-795 p.Article in journal (Refereed) Published
Abstract [en]

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 Hontomín (Burgos, Spain). The characterization experiment included a 36 km2 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.

Place, publisher, year, edition, pages
2013. Vol. 19, no 0, 785-795 p.
Keyword [en]
3D seismic reflection, Reservoir characterization, CO2 storage, High resolution, Three-component seismic
National Category
Geophysics
Identifiers
URN: urn:nbn:se:uu:diva-213791DOI: 10.1016/j.ijggc.2013.01.039ISI: 000332396700015OAI: oai:DiVA.org:uu-213791DiVA: diva2:683485
Available from: 2014-01-03 Created: 2014-01-03 Last updated: 2017-12-06Bibliographically approved

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Publisher's full texthttp://www.sciencedirect.com/science/article/pii/S1750583613000704

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Juhlin, Christopher

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