Determining Geothermal Resource Areas with Vector Data
The ideal combination of certain features maximizes the geothermal potential. In general, high potential locations can be determin by considering the thermal conductivity of the main rock layers, underground water flow, proximity to fault lines, and surface cover thickness. Apart from these, many other details are important in the correct assessment of thermal potential. In the sample study in this article, an evaluation was made on fault lines and geological information.
lass=”yoast-text-mark” />>First, the porosity and permeability of the main rock were taken as reference using the information from the geological map in vector data type. For this, the age and lithology information we have in the geological layer was us.
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Lithology Information
Geological Age Information
Grouping by Geological Age and Lithology
Considering the effect of geological data on the formation of thermal resources, age and lithology grouping was perform. Age information was divid into five different levels and each age unit was rank according to its contribution to the geothermal potential. Lithology layers were also evaluat according to their properties such as permeability and porosity according to the main rock types.
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In the first part of the three-part blog post, we aim to determine areas with high geothermal resource potential in a specific region using vector data. In the second part of the series, we will evaluate potential areas using raster data and use the information we obtain with vector data together with these analyses. In the last part, we will discuss drilling management for geothermal resources and a greenhouse project scenario where the obtain geothermal energy is us.
