Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection

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Access type: Metadata onlySubject: search.filters.subject.geothermal energy

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  • Book Part
    Citation - Scopus: 3
    Renewable Energy Sources Utilized for Membrane Desalination Processes
    (Elsevier, 2023) Tomaszewska, B.; Akkurt, G.G.; Kaczmarczyk, M.; Kasztelewicz, A.; Mukti, M.; Gural, H.B.; Jarma, Y.A.
    Desalination has mostly been used to produce drinkable water due to the rapid increase in water scarcity. On the other hand, desalination processes require more energy than that of conventional water treatment methods. To decrease the consumption of fossil fuel and the cost of freshwater production, renewable energy sources (RESs) to power the desalination processes have been introduced. The RES used in desalination has a broad spectrum from photovoltaics, concentrated solar power, and wind energy to integrated RESs. In this chapter, desalination processes that are powered by RESs are discussed. Also, new generations of RESs in membrane desalination systems are introduced. © 2023 Elsevier Inc. All rights reserved.
  • Article
    Citation - WoS: 2
    Citation - Scopus: 1
    A Review of the Geothermal System Evolution and Distribution in the Central Anatolian Crystalline Complex (türkiye)
    (TUBITAK, 2023) Şener, M.F.; Öztürk, M.Z.; Baba, A.
    Türkiye is located in the Mediterranean sector of the Alpine–Himalayan tectonic belt and is among the foremost seven countries in the world having an abundance of geothermal resources. The Central Anatolian Crystalline Complex (CACC) is one of the most important geothermal regions in Türkiye. This study aims to evaluate the geothermal system of CACC using the geological, structural, and hydrogeochemical properties that were obtained from previous studies. The present study investigated and evaluated the hydrogeochemical and isotopic properties of 762 water samples belonging to 45 different localities from 41 scientific studies. The result shows that CACC has different heat sources and different hydrogeochemical processes. Major element chemistry of the water reveals that the geothermal fluids are mostly of the Ca-Mg-HCO3, Na-Cl-HCO3, and Ca-Cl water types. Silica geothermometers suggest that the reservoir temperature ranges from 48 to 180 °C. Based on the δ18O-δD relationship, water samples have a high-altitude meteoric origin. Stable isotopic data indicate that the geothermal fluids are formed by local recharge and deep circulation of meteoric waters. © TÜBİTAK.