Metadata 1651
Měsíční soubory čtení časů příchodu seismických jevů z celého světa ze stanic JAVC (od r. 1997), KRUC (od r. 1997), MORC (od r. 1995) a VRAC (od r. 1993), provozovaných Ústavem fyziky Země PřF Masarykovy univerzity Brno.
Created using karst information for Rockingham Catchment Region in the West of Ireland. The catchment for each swallow hole was delineated and distance from each swallow hole was calculated within the catchment. These were assigned the appropriate value according to COP methodology. The slope and vegetation types within and outside that catchments were also assigned appropriate values.
C layer represents hydraulic conductivity of hydrological units and direct assignment of C index to each aquifer.
The Hydraulic conductivity layer is taken as a direct assignment of the hydraulic conductivities from the aquifer parameter database to the C index values according to DRASTIC, ranging from 1 to 10
C layer represents hydraulic conductivity of hydrological units (from cp map Kennesey) and direct assignment of C index to each aquifer. Higher values of C correspond to alluvial aquifers, and smaller values to metamorphic and igneous rocks.
The Hydraulic conductivity layer is taken as a direct assignment of the hydraulic conductivities from the aquifer parameter database to the C index values according to DRASTIC, ranging from 1 to 10.
C map in Slovenia represents one layer of vulnerability map COP in Slovenia that has been applied on the area covered by karstic rocks. The map is constituated from calcualation of distance to swallow holes and sinkihg streams, slope, high and low vegetation cover. Vulnerability classes are: 0-0.2 Very High,0.2-0.4 High, 0.4-0.6 Moderate, 0.6-0.8 Low, 0.8-1.0 Very low.
factor C of DRASTIC groundwater vulnerability of Traun-Enns-Platte/AUSTRIA
Hydraulic conductivity, for Sarmatian aquifer in Dobrogea de Sud, Romania
The Cadastre of Mineral, Thermal, and Thermomineral Waters is a register containing data on all known sources of these waters. Mineral waters have a high content of minerals and other dissolved substances. The cadastre records their geographical location, chemical composition, flow rate, and other characteristics. Thermal waters are those that emerge from deep layers of the Earth and have a higher temperature than the average ambient temperature. The cadastre for thermal waters documents their temperature ...
