Reservoir and hydrogeochemical characterizations of geothermal fields in Salihli, Turkey

Ozen T., BÜLBÜL A., TARCAN G.

JOURNAL OF ASIAN EARTH SCIENCES, cilt.60, ss.1-17, 2012 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 60
  • Basım Tarihi: 2012
  • Doi Numarası: 10.1016/j.jseaes.2012.07.016
  • Dergi Adı: JOURNAL OF ASIAN EARTH SCIENCES
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.1-17
  • Anahtar Kelimeler: Hydrochemistry, Salihli thermal waters, Isotope chemistry, Geothermometer, Mineral saturation, Scaling, WESTERN TURKEY, GEDIZ GRABEN, TECTONIC EVOLUTION, 2-STAGE EXTENSION, ALASEHIR GRABEN, ANATOLIA, WATERS, PRESSURES, GEOMETRY, SYSTEMS
  • Dokuz Eylül Üniversitesi Adresli: Evet

Özet

Geothermal and hydrochemical characteristics of thermal waters in the Salihli geothermal area are described in this study. This geothermal area is geographically divided into five main groups; Kursunlu, Caferbey, Greenhouse, Ufuruk and Sart geothermal fields. In the study area, the outlet temperatures of the thermal waters are between 30 and 90 degrees C. their discharges are between 2 and 80 l/s in springs and the depths of wells vary between 200 and 1189 m. Hydrochemical analysis results suggest four different water types of Na-HCO3, Ca-Mg-HCO3, Ca-Na-HCO3 and Ca-Mg-SO4 in Kursunlu, Caferbey-Greenhouse, Sart, and Ufuruk, respectively. Cold waters are mainly dominated by the HCO3 and SO4 anions and Na, Ca, and Mg cations.