Metadata 1672
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.
This is PSI data for Thessaly, Greece. It has been provided by GAMMA Remote Sensing as part of the ESA funded Terrafirma project.
Thickness of the Last Glacial Maximum (LGM) deposit. Contours are presented as depth (metres) below present seafloor or the base of the post LGM sedimentary cover. LGM is defined on average at 18,000 years BP. In glaciated regions the thickness of the Holocene is used. Confidence is defined as follows: 1. High: Sampled feature with good age and palaeoenvironmental control. 2. Sampled feature with poor or none age and palaeoenvironmental control. 3. Constructed by remote sensing data only, 4. Low: Reasonabl...
Iso-content maps of Thorium (Th), 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 squar...
