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Environmental Earth Sciences

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01.02.2011 | Original Article

Hydrogeochemical and isotopic composition of a low-temperature geothermal source in northwest Turkey: case study of Kirkgecit geothermal area

verfasst von: Deniz Sanliyuksel, Alper Baba

Erschienen in: Environmental Earth Sciences | Ausgabe 3/2011

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Abstract

Chemical and isotopic compositions of three hot springs and one cold spring in the Kirkgecit geothermal field, located 15 km southwest of Canakkale-Biga in the northwest of Turkey, were monitored five times during 2005 and 2007. The physico-chemical characteristics of the hot springs are average discharge 3–3.5 L/s, surface temperature 45–52°C, pH 8.9–9.3, and electrical conductivity (EC) 620–698 μS/cm. The cold spring has a temperature of 12–13°C, pH 7.5–8.3, and EC 653–675 μS/cm. The hot waters are Na-SO₄ type, whereas the cold water is Ca-HCO₃ type. Chemical geothermometers suggest that the reservoir temperature is around 80–100°C. The isotopic data (oxygen-18, deuterium and tritium) indicate that the thermal waters are formed by local recharge and deep circulation of meteoric waters.

Vorheriger Artikel Competitive heavy metals adsorption on natural bed sediments of Jajrood River, Iran

Nächster Artikel Diffuse and concentrated recharge evaluation using physical and tracer techniques: results from a semiarid carbonate massif aquifer in southeastern Spain

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Titel: Hydrogeochemical and isotopic composition of a low-temperature geothermal source in northwest Turkey: case study of Kirkgecit geothermal area
verfasst von: Deniz Sanliyuksel
Alper Baba
Publikationsdatum: 01.02.2011
Verlag: Springer-Verlag
Erschienen in: Environmental Earth Sciences / Ausgabe 3/2011
Print ISSN: 1866-6280
Elektronische ISSN: 1866-6299
DOI: https://doi.org/10.1007/s12665-010-0545-z

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