Metadata 1677
The map of “Switzerland during the Last Glacial Maximum (LGM), at a scale of 1:500,000” shows the maximum extent of glaciation in Switzerland at the height of the last Ice Age about 24,000 years BP. It incorporates the latest results of research on the Ice Age in Switzerland in a clearly legible format.
The WFS download service of the Shallow Geothermal Energy Potential Maps database contains the following information layers collected and produced within the framework of the Shallow Geothermal Energy Pottential Maps project:• 13 area-specific GIS information layers:o thermal conductivity maps λ [W/m*K] at depths of 40, 70, 100 and 130 m below ground level;o unit heat output maps qv [W/m] for 1800 h of heat pump operation per year at depths of 40, 70, 100 and 130 m below ground level;o unit heat output map...
The WMS viewing service of the Shallow Geothermal Energy Potential Maps database contains the following information layers collected and produced within the framework of the Shallow Geothermal Energy Pottential Maps project:• 13 area-specific GIS information layers:o thermal conductivity maps λ [W/m*K] at depths of 40, 70, 100 and 130 m below ground level;o unit heat output maps qv [W/m] for 1800 h of heat pump operation per year at depths of 40, 70, 100 and 130 m below ground level;o unit heat output maps...
Thermal conductivity of a geological unit relevant for shallow geothermal energy use (e.g. bedrock).
Maps showing average values of thermal conductivity of soils and rocks, expressed in units of W/(m*K), for the 0-100 m depth interval.Maps were created on the basis of a numerical, three-dimensional model of geological structure (base model), which was then filled with geological-thermal series with assigned values of thermal conductivity rate expressed in units [W/m*K] (parametric model). The parametric model was used to calculate the average value of thermal conductivity of soils and rocks at each point ...
Maps showing average values of thermal conductivity of soils and rocks, expressed in units of W/(m*K), for the 0-130 m depth interval.Maps were created on the basis of a numerical, three-dimensional model of geological structure (base model), which was then filled with geological-thermal series with assigned values of thermal conductivity rate expressed in units [W/m*K] (parametric model). The parametric model was used to calculate the average value of thermal conductivity of soils and rocks at each point ...
Maps showing average values of thermal conductivity of soils and rocks, expressed in units of W/(m*K), for the 0-40 m depth interval.Maps were created on the basis of a numerical, three-dimensional model of geological structure (base model), which was then filled with geological-thermal series with assigned values of thermal conductivity rate expressed in units [W/m*K] (parametric model). The parametric model was used to calculate the average value of thermal conductivity of soils and rocks at each point o...
Maps showing average values of thermal conductivity of soils and rocks, expressed in units of W/(m*K), for the 0-70 m depth interval.Maps were created on the basis of a numerical, three-dimensional model of geological structure (base model), which was then filled with geological-thermal series with assigned values of thermal conductivity rate expressed in units [W/m*K] (parametric model). The parametric model was used to calculate the average value of thermal conductivity of soils and rocks at each point o...
The intrinsic ability of hard rock samples to conduct heat.
The maximum temperature shift between the production and the injection well that is possible with regards to legal or ecological limitations.