Metadata 1639
Maps showing average values of specific heat extraction rate for 2100 h of heat pump operation per year, expressed in units of W/m, for a depth interval of 0-100 m.Maps were developed based on empirical linear calculation formulas according to Sanner, 1999, in accordance with guidelines for ground source heat pumps design, execution and acceptance of installations, published by The Polish Organisation for the Development of Heat Pump Technology (PORT PC), “PORT PC. Wytyczne projektowania, wykonania i odbio...
Maps showing average values of specific heat extraction rate for 2100 h of heat pump operation per year, expressed in units of W/m, for a depth interval of 0-130 m.Maps were developed based on empirical linear calculation formulas according to Sanner, 1999, in accordance with guidelines for ground source heat pumps design, execution and acceptance of installations, published by The Polish Organisation for the Development of Heat Pump Technology (PORT PC), “PORT PC. Wytyczne projektowania, wykonania i odbio...
Maps showing average values of specific heat extraction rate for 2100 h of heat pump operation per year, expressed in units of W/m, for a depth interval of 0-40 m.Maps were developed based on empirical linear calculation formulas according to Sanner, 1999, in accordance with guidelines for ground source heat pumps design, execution and acceptance of installations, published by The Polish Organisation for the Development of Heat Pump Technology (PORT PC), “PORT PC. Wytyczne projektowania, wykonania i odbior...
Maps showing average values of specific heat extraction rate for 2100 h of heat pump operation per year, expressed in units of W/m, for a depth interval of 0-70 m.Maps were developed based on empirical linear calculation formulas according to Sanner, 1999, in accordance with guidelines for ground source heat pumps design, execution and acceptance of installations, published by The Polish Organisation for the Development of Heat Pump Technology (PORT PC), “PORT PC. Wytyczne projektowania, wykonania i odbior...
The updated 3D structural geological model of the Březový potok locality was created in the MOVE software, primarily for a user-friendly access to the geological interpretations of an extensive geophysical and geological research conducted at this site in the recent years. The possibility of using the model in subsequent hydrogeological and transport models was taken into account during its creation. For the purposes of 3D models of potential localities for deep repository of HLW, faults of categories I, I...
The updated 3D structural geological model of the Hrádek locality was created in the MOVE software, primarily to provide a user-friendly access to the geological interpretations of an extensive geophysical and geological research conducted at this site in the recent years. The possibility of using the model in subsequent hydrogeological and transport models was taken into account during its creation. For the purposes of 3D models of potential localities for deep repository of HLW, faults of categories I, I...
The updated 3D structural geological model of the ETE-Jih locality was created in the MOVE software, primarily to provide a user-friendly access to the geological interpretations of an extensive geophysical and geological research conducted at this site in the recent years. The possibility of using the model in subsequent hydrogeological and transport models was taken into account during its creation. For the purposes of 3D models of potential localities for a deep repository of HLW, faults of categories I...
The updated 3D structural geological model of the Horka locality was created in the MOVE software, primarily for a user-friendly access to the geological interpretations of an extensive geophysical and geological research conducted at this site in the recent years. The possibility of using the model in subsequent hydrogeological and transport models was taken into account during its creation. For the purposes of 3D models of potential localities for deep repository of HLW, faults of categories I, II and II...
Iso-content maps of Uranium (U), one of the chemical elements.obtained in the Geochemical Atlas of Spain Project, distributed in stream sediments (14,864 samples), superficial soils (0-20 cm.) (13,505 samples) and deeper soils (20-40 cm.) (7,682 samples). The results of the chemical analysis are shown in two types: total dissolution of the sample with 4 acids and partial dissolution with aqua regia. With the analytical results of all the sampled points, an isocontent map is made with adjustment to a square...
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