Hydrogeological Modelling of Geothermal Waters in Cesme and Environs, Western Anatolia, Turkey

World Multidisciplinary Earth Sciences Symposium

Ozgur, Nevzat^1 ; Degirmenci, Saliha^2 ; Pala, Ebru Aras^2 ; Arici, Mehmet^1

Suleyman Demirel University, Faculty of Engineering, Department of Geological Engineering, Isparta, Turkey^1

Suleyman Demirel University, Institute of Natural and Applied Sciences, Isparta, Turkey^2

关键词: Basement rocks;    Deep reservoirs;    Geothermal water;    Hydrogeological;    Meteoric waters;    Number of samples;    Reservoir temperatures;    Western Anatolia;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/221/1/012026/pdf
DOI  :  10.1088/1755-1315/221/1/012026

来源: IOP

【 摘 要 】

The geothermal fields of Çeme are located in the western part of province capital of Izmir and can be considered as important tourist resorts with a great number of thermal hot springs which are used for thermal bathing since several years. Nowadays, the geothermal waters in the fields are used for district heating and greenhouses. In the area of Çeme, there are sedimentary and volcanic rocks predominantly. The basement rocks are of Devonian age and consists of intercalations of sandstones, greywackes and limestones overline by Upper to Middle Triassic carbonate rocks with intercalations of sandstones and claystones. These rocks are overlain by Neogene volcanic and terrestrial sedimentary rocks. In 1995, we have measured in-situ parameters in many locations of groundwaters and geothermal waters with collection of a great number of samples for these waters. The geothermal waters are of Na-Cl, Na-(Cl)-HCO3, Na-Ca-Cl, Na-Mg-(Cl)-HCO3, Na-Mg-Ca-(Cl)-HCO3 and Ca-Na-Mg-(Cl)-HCO3 type waters during the groundwaters display Na-Cl, Na-HCO3, Na-Mg-(Cl)-HCO3, Na-Mg-HCO3, Na-Mg-Ca-(Cl)-HCO3, Mg-Ca-Na-(Cl)-HCO3 and Mg-Ca-Na-(Cl)-HCO3 type waters. The Na-Cl type waters are originated from deep reservoir during the others can be considered as diluted Cl-HCO3 water type. The plot of δ18O versus δD shows that the geothermal waters are enriched in δ18O and δD and located on the mixing trend between groundwaters and seawaters indicating mixing of these both different waters. The proportion of seawaters in geothermal waters seems to be very higher than groundwaters. The shift in the δ18O values are related to δ18O exchange between the deeply circulating meteoric waters and reservoir rocks in the area. The increase of δD is related to the contribution of seawaters. The geothermal waters in the area fall into fields of immature to partially equilibrated waters. In general, the reservoir temperature of the area of Çeme is estimated to be 80 to 120 °C.