Metadata 1660
Map showing the geographical distribution of ground movements classified into four main groups: horizontal component in continental areas, vertical component in continental areas, unstable areas linked to coastal areas and movements related to mining operations. Also included are continental areas with important erosive processes.
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.
Thermal response test (TRT) is the customary method to determine ground thermal conductivity in situ.
Numerous thermal, mineral and thermomineral waters and the variety of their hydrochemical types represent the most interesting geological issue and signifcant economic potential of the territory of the Republic of Srpska. The proper interpretation of the genesis, hydrogeologic mechanism, chemical content and the regime of some occurrences of these waters provide the consideration of their economic importance and possibilities of utilization.
