An updated geothermal model of the Dutch subsurface based on inversion of temperature data
The subsurface temperature is one of the most crucial parameters for the development of geothermal energy. Physics-based temperature models calibrated with temperature data are especially relevant for deep geothermal exploration. We present an updated high-resolution 3D thermal model of the onshore Netherlands. We constructed the model in 7 steps, starting from a lithospheric-scale, physics-based forward model and progressively detailing and updating it using temperature data. The model is built up from 14 sedimentary layers and layers for the upper crust, lower crust, and lithospheric mantle.... Mehr ...
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Dokumenttyp: | Artikel |
Erscheinungsdatum: | 2020 |
Schlagwörter: | 3D thermal field / Regional-scale conductive modelPseudo-convectionData assimilationthe Netherlands / Pseudo-convection / Data assimilation / the Netherlands |
Sprache: | Englisch |
Permalink: | https://search.fid-benelux.de/Record/base-29202788 |
Datenquelle: | BASE; Originalkatalog |
Powered By: | BASE |
Link(s) : | https://dspace.library.uu.nl/handle/1874/408460 |