Metadata 1798
The underground geothermal conditions can be presented, irrespective of the aquifers' position, with the appropriate geothermal maps. This map represents the expected temperatures at a depth of 3000 m and is made with data from 214 boreholes. It is made on the basis of measured temperatures in accessible boreholes throughout the country. However, since the temperature field depends on the geological structure in the depths and tectonic characteristics, the course of the isotherms is a result of many influe...
The underground geothermal conditions can be presented, irrespective of the aquifers' position, with the appropriate geothermal maps. This map represents the expected temperatures at a depth of 500 m and is made with data from 354 boreholes. It is made on the basis of measured temperatures in accessible boreholes throughout the country. However, since the temperature field depends on the geological structure in the depths and tectonic characteristics, the course of the isotherms is a result of many influen...
The underground geothermal conditions can be presented, irrespective of the aquifers' position, with the appropriate geothermal maps. This map represents the expected temperatures at a depth of 5000 m and is made with data from 192 boreholes. It is made on the basis of measured temperatures in accessible boreholes throughout the country. However, since the temperature field depends on the geological structure in the depths and tectonic characteristics, the course of the isotherms is a result of many influe...
The underground geothermal conditions can be presented, irrespective of the aquifers' position, with the appropriate geothermal maps. It is made on the basis of measured temperatures in accessible boreholes throughout the country. However, since the temperature field depends on the geological structure in the depths and tectonic characteristics, the course of the isotherms is a result of many influences, such as thermal conductivity of rocks, permeability and fracturing of rocks, all of which are reflected...
The underground geothermal conditions can be presented, irrespective of the aquifers' position, with the appropriate geothermal maps. It is made on the basis of measured temperatures in accessible boreholes throughout the country. However, since the temperature field depends on the geological structure in the depths and tectonic characteristics, the course of the isotherms is a result of many influences, such as thermal conductivity of rocks, permeability and fracturing of rocks, all of which are reflected...
Geothermal plants are often exposed to problems that affect the performance of the plant. Typical problems are mineral scaling, particles clogging, corrosion and temperature/stress related effects of geothermal flow and injectivity. In the PERFORM project contains data about the properties and geology of the reservoirs, the chemistry of the water and precipitates and the construction of the plants. The goal is to give recommendations that can help the operators to avoid or mitigate the problems The PERFORM...
ArcGIS Server service displays .....
GeoMol Pilot Area Upper Austria - Upper Bavaria: Map of temperature distribution at the top of Upper Jurassic as the principal geothermal aquifer, arranged in six use-specific temperature ranges. Map derived from the 3D geological model and temperature model as prepared in the GeoMol Project. Details in the Project Report http://www.geomol.eu/report/
The map shows the location and main data of geothermal district heating, thermal water town-heating and geothermal power production projects.
Dataset contains locations and obligatory metadata properties of geothermal wells that were identified and catalogued in the Danube Region Leading Geothermal Energy (DARLINGe) project in 2017-2019. For more information visit the project website at https://www.darlinge.eu/