2015
DOI: 10.1016/j.renene.2014.09.033
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A pan-European planning basis for estimating the very shallow geothermal energy potentials

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Cited by 61 publications
(34 citation statements)
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“…Another potential data set dealing with thermal conductivities of the underground would have been the outcomes of the European ThermoMap project [8]. Within this project, a pan-European outline map providing the very shallow geothermal potential (vSGP) was developed and expressed within ThermoMap-MapViewer [9]. The pedological data set for creating the pan-European outline map was provided by the ESDAC's (European Soil Data Centre) TXSRFDO (Dominant surface textural class) for STU (soil typological unit) or by national datasets for different test areas on a small-scale level.…”
Section: Data Acquisitionmentioning
confidence: 99%
“…Another potential data set dealing with thermal conductivities of the underground would have been the outcomes of the European ThermoMap project [8]. Within this project, a pan-European outline map providing the very shallow geothermal potential (vSGP) was developed and expressed within ThermoMap-MapViewer [9]. The pedological data set for creating the pan-European outline map was provided by the ESDAC's (European Soil Data Centre) TXSRFDO (Dominant surface textural class) for STU (soil typological unit) or by national datasets for different test areas on a small-scale level.…”
Section: Data Acquisitionmentioning
confidence: 99%
“…Bertermann [17,18] made a detailed study of the very first shallow layers (down to 10 m depth, very shallow geothermal potential vSGP), and created a WebGIS dynamic tool within the framework of the Thermomap Project. The method did not, however, consider seasonal changes in subsoil temperature due to heat flux variations.…”
Section: Introductionmentioning
confidence: 99%
“…However, their results were obtained for a short period (200 h) during which the soil condition did not vary significantly. Bertermann et al [14] analyzed very shallow geothermal energy potentials for Europe based on the annual mean air temperature and constant thermal properties derived from relatively simplified data sets. Finally, as noted by Spitler and Bernier [15], most models of GHEs rely on extreme simplifications of the surface boundary conditions and they identified the study of near-surface effects as one of the future research needs on GSHP systems.…”
Section: Introductionmentioning
confidence: 99%