Abstract

Geothermal energy is becoming essential to deal with the catastrophic effect of climate change. Although the totality of the Earth’s crust allows the exploitation of shallow geothermal resources, it is important to identify those areas with higher thermal possibilities. In this sense, geophysical prospecting plays a vital role in the recognition and estimation of potential geothermal resources. This research evaluates the geothermal conditions of a certain area located in the center of Spain. The evaluation is mainly based on geological and geophysical studies and, in particular, the Time Domain Electromagnetic Method and the Electrical Resistivity Tomography. Once we analyzed the geology and the historical thermal evidence near the study area, our geophysical results were used to define the geothermal possibilities from a double perspective. In relation to anomalous heat gradient, the identification of a fault and the contact with impermeable granitic materials at the depth of 180 m denotes a potential location for the extraction of groundwater. Regarding the common ground-source heat-pump uses, the analysis has allowed the determination of the most appropriate area for the location of the geothermal well field. Finally, the importance of accurately defining the position of the drillings was confirmed by using software GES-CAL.

Highlights

  • The fight against climate change and its catastrophic effects is one of the main challenges that currently enrolls the whole world

  • Geophysical prospecting plays a vital role in the recognition and estimation of potential geothermal resources

  • This research has exposed the applicability of the geophysical techniques, Time Domain Electromagnetic Method (TDEM) and Electrical Resistivity Tomography (ERT), in the identification of potential areas for the exploitation of shallow geothermal resources

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Summary

Introduction

The fight against climate change and its catastrophic effects is one of the main challenges that currently enrolls the whole world. The origin of the Earth’s thermal energy is linked to the internal structure of the planet and the physical processes occurring there. The existence of this heat has been proved through the rocks’ temperature, which increases with depth (gradient commonly averages 3 ◦C/100 m of depth). Focusing on very low-enthalpy geothermal resources, they can be practically found at any point of the crust, thanks to the constant ground temperature from depths of 8–10 m. In these systems, heat can be extracted for heating and cooling applications, using geothermal heat pumps. Within the common exploitation of these resources, some areas, with specific geological and stratigraphic conditions, are especially appropriate for the implementation of these geothermal systems

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