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Geophysical Prospecting for Geothermal Resources in the South of the Duero Basin (Spain)

Author

Listed:
  • Ignacio Martín Nieto

    (Department of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, Spain)

  • Pedro Carrasco García

    (Department of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, Spain)

  • Cristina Sáez Blázquez

    (Department of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, Spain)

  • Arturo Farfán Martín

    (Department of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, Spain)

  • Diego González-Aguilera

    (Department of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, Spain)

  • Javier Carrasco García

    (Department of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, Spain)

Abstract

The geothermal resources in Spain have been a source of deep research in recent years and are, in general, well-defined. However, there are some areas where the records from the National Institute for Geology and Mining show thermal activity from different sources despite no geothermal resources being registered there. This is the case of the area in the south of the Duero basin where this research was carried out. Seizing the opportunity of a deep borehole being drilled in the location, some geophysical resources were used to gather information about the geothermal properties of the area. The employed geophysical methods were time-domain electromagnetics (TDEM) and borehole logging; the first provided information about the depth of the bedrock and the general geological structure, whereas the second one gave more detail on the geological composition of the different layers and a temperature record across the whole sounding. The results allowed us to establish the geothermal gradient of the area and to discern the depth of the bedrock. Using the first 200 m of the borehole logging, the thermal conductivity of the ground for shallow geothermal systems was estimated.

Suggested Citation

  • Ignacio Martín Nieto & Pedro Carrasco García & Cristina Sáez Blázquez & Arturo Farfán Martín & Diego González-Aguilera & Javier Carrasco García, 2020. "Geophysical Prospecting for Geothermal Resources in the South of the Duero Basin (Spain)," Energies, MDPI, vol. 13(20), pages 1-22, October.
    • Handle: RePEc:gam:jeners:v:13:y:2020:i:20:p:5397-:d:428864
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    References listed on IDEAS

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    1. Chamorro, César R. & García-Cuesta, José L. & Mondéjar, María E. & Linares, María M., 2014. "An estimation of the enhanced geothermal systems potential for the Iberian Peninsula," Renewable Energy, Elsevier, vol. 66(C), pages 1-14.
    2. Colmenar-Santos, Antonio & Folch-Calvo, Martin & Rosales-Asensio, Enrique & Borge-Diez, David, 2016. "The geothermal potential in Spain," Renewable and Sustainable Energy Reviews, Elsevier, vol. 56(C), pages 865-886.
    3. Cristina Sáez Blázquez & Ignacio Martín Nieto & Arturo Farfán Martín & Diego González-Aguilera & Pedro Carrasco García, 2019. "Comparative Analysis of Different Methodologies Used to Estimate the Ground Thermal Conductivity in Low Enthalpy Geothermal Systems," Energies, MDPI, vol. 12(9), pages 1-14, May.
    4. Cristina Sáez Blázquez & Arturo Farfán Martín & Ignacio Martín Nieto & Diego González-Aguilera, 2018. "Economic and Environmental Analysis of Different District Heating Systems Aided by Geothermal Energy," Energies, MDPI, vol. 11(5), pages 1-17, May.
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