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

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 bei...

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Main Authors: Ignacio Martín Nieto, Pedro Carrasco García, Cristina Sáez Blázquez, Arturo Farfán Martín, Diego González-Aguilera, Javier Carrasco García
Format: Article
Language:English
Published: MDPI AG 2020-10-01
Series:Energies
Subjects:
Online Access:https://www.mdpi.com/1996-1073/13/20/5397
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author Ignacio Martín Nieto
Pedro Carrasco García
Cristina Sáez Blázquez
Arturo Farfán Martín
Diego González-Aguilera
Javier Carrasco García
author_facet Ignacio Martín Nieto
Pedro Carrasco García
Cristina Sáez Blázquez
Arturo Farfán Martín
Diego González-Aguilera
Javier Carrasco García
author_sort Ignacio Martín Nieto
collection DOAJ
description 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.
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spelling doaj.art-69656e8d17314af2a6fe0812aa41d4342023-11-20T17:17:57ZengMDPI AGEnergies1996-10732020-10-011320539710.3390/en13205397Geophysical Prospecting for Geothermal Resources in the South of the Duero Basin (Spain)Ignacio Martín Nieto0Pedro Carrasco García1Cristina Sáez Blázquez2Arturo Farfán Martín3Diego González-Aguilera4Javier Carrasco García5Department of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, SpainDepartment of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, SpainDepartment of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, SpainDepartment of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, SpainDepartment of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, SpainDepartment of Cartographic and Land Engineering, University of Salamanca, Higher Polytechnic School of Avila, Hornos Caleros 50, 05003 Avila, SpainThe 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.https://www.mdpi.com/1996-1073/13/20/5397geothermal resourcesgeophysical prospectingtime-domain electromagneticsborehole logginggeothermal gradientthermal conductivity
spellingShingle Ignacio Martín Nieto
Pedro Carrasco García
Cristina Sáez Blázquez
Arturo Farfán Martín
Diego González-Aguilera
Javier Carrasco García
Geophysical Prospecting for Geothermal Resources in the South of the Duero Basin (Spain)
Energies
geothermal resources
geophysical prospecting
time-domain electromagnetics
borehole logging
geothermal gradient
thermal conductivity
title Geophysical Prospecting for Geothermal Resources in the South of the Duero Basin (Spain)
title_full Geophysical Prospecting for Geothermal Resources in the South of the Duero Basin (Spain)
title_fullStr Geophysical Prospecting for Geothermal Resources in the South of the Duero Basin (Spain)
title_full_unstemmed Geophysical Prospecting for Geothermal Resources in the South of the Duero Basin (Spain)
title_short Geophysical Prospecting for Geothermal Resources in the South of the Duero Basin (Spain)
title_sort geophysical prospecting for geothermal resources in the south of the duero basin spain
topic geothermal resources
geophysical prospecting
time-domain electromagnetics
borehole logging
geothermal gradient
thermal conductivity
url https://www.mdpi.com/1996-1073/13/20/5397
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