Abstract:

The sandy-Hüdai geothermal field is one of the geothermal fields in Afyonkarahisar. In the Sandy-Hüdai geothermal system, the reservoir is formed by the squares and shells, and the heat source is the old Sandy volcanism of Miyosen. The high values seen in the hydrogeochemical analysis data of underground samples indicate that these waters are heated by the geothermal system and/or geothermal water is mixed. The results of the hydrogeochemical analysis of the Geothermal Field of the Box-Hudai were processed into the database using the ArcGIS 10 program. The distribution within the pool of the T, pH, EC, Na+, K+, Ca2+, Mg2+, HCO3, Cl, SO42 values is determined by the IDW interpolation method. The geothermal waters in the Hüdai geothermal area are generally increasing towards the northeast according to the T, SO4, Cl, Ca and Mg thematic maps, while the work area has given higher values in the middle compared to the EC, Na, K and HCO3 thematic maps.

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