Metadata 1641
Simulated change in mean groundwater head between the future (3 degree warming, minimum precipitation change) and past (1989-2018) for Denmark. Simulated by a 500 m by 500 m grid. Unit: Meters.
Simulated change in mean groundwater head between the future (3 degree warming, minimum precipitation change) and past (1989-2018) for Denmark. Simulated by a 500 m by 500 m grid. Unit: Meters.
Simulated change in mean groundwater head between the future (3 degree warming, minimum precipitation change) and past (1998-2018) for Drava-Mura aquifer, Croatia. Simulated by a 100 m by 100 m grid. Unit: Meters.
Simulated change in mean groundwater head between the future (3 degree warming, minimum precipitation change) and past (1989-2018) for Sunds, Denmark. Simulated by a 25 m by 25 m grid. Unit: Meters.
Simulated change in mean groundwater head between the future (3 degree warming, minimum precipitation change) and past (2011-2018) for The Netherlands. Simulated by a 250 m by 250 m grid. Unit: Meters.
Simulated change in mean groundwater head between the future (3 degree warming, minimum precipitation change) and past (2015) for the Upper Guadiana Basin, Spain. Simulated by a 1000 m by 1000 m grid. Unit: Meters.
Zones inside groundwater bodies or groundwater bodies potentially leading to operational problems for shallow geothermal use due to a critical chemical composition.
Zoltán Püspöki, Gábor Markos 2024:
During the modelling, a total of 593 deep boreholes were stratigraphically evaluated along correlation sections. During the evaluation, the Quaternary sequence, which is usually treated as a single (model) layer in regional geological modelling, was subdivided into 11 layers. The settlement depths of the identified layer boundaries were determined per borehole (593*11=6523 data points), and the resulting layer data table was converted into a format that can be imported ...
A Talajvíztükör NATéR témakörhöz tartozó térképsorozat.
Areas dedicated to drinking water or curative water supply, which might limit the use of shallow geothermal energy.