Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
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Book Part Citation - Scopus: 3An Introduction To Geothermal Energy(Elsevier, 2024) Uzelli, T.; Ayzit, T.; Baba, A.Geothermal energy is one of the most important renewable sources, generally recognized as an environmentally friendly resource. The general distribution of geothermal systems is controlled by the different types of fault systems, active volcanism, and hydrothermally altered areas. These diverse resources occur in different parts of the Earth and different geologic settings. In addition, geothermal resources may have different physical and chemical properties depending on temperature and depth variations, geology, geochemistry, and hydrogeological characteristics. These resources are used for direct (heating, cooling, greenhouse, thermal bath, and others) and indirect (electricity generation) applications. Today, geothermal heat base applications continue to develop in an integrated manner with the processes of combating global warming and adaptation to climate change. This chapter provides information on the source of geothermal energy, the current status of the geothermal energy sector, the importance of geothermal energy, the history of geothermal energy applications, and the classification of geothermal systems. © 2024 Elsevier Inc. All rights are reserved, including those for text and data mining, AI training, and similar technologies.Book Part Geothermal Fluids: Physicochemical Properties, Compositions, and Treatment(Elsevier, 2024) Jarma, Y.A.; Cihanoğlu, A.; Kabay, N.; Baba, A.; Tomaszewska, B.; Kasztelewicz, A.; Bryjak, M.Geothermal energy is known as an environmentally friendly, reliable, and safe source of energy produced from renewable sources. In order to ensure the sustainable operation of geothermal power plants, it is necessary to recharge geothermal fluids back into the reservoirs. It is worth mentioning that the accidental release of geothermal brines or the accumulation of salts and silica from geothermal power facilities can lead to significant environmental issues. Geothermal fluids brought to the surface for any application must be treated in the most practical and feasible way before discharge to the any receiving body or back to the reservoirs. The objective of this chapter was therefore to study the hydrogeochemical properties of geothermal fluids in different regions and propose some scientific approached for the treatment of spent geothermal fluid prior to its use as an alternative water source, especially in agriculture applications. © 2024 Elsevier Inc. All rights are reserved, including those for text and data mining, AI training, and similar technologies.Article Effect of Degassing on Scaling in Hypersaline System: Tuzla Geothermal Field, Turkey(Springer Science and Business Media Deutschland GmbH, 2025) Tonkul, S.; André, L.; Baba, A.; Demir, M.M.; Regenspurg, S.; Kieling, K.A serious issue with geothermal power plants is the loss of production and decline in power plant efficiency. Scaling, also known as mineral precipitation, is one of the frequently-observed issue that causes this loss and decreasing efficiency. It is heavily observed in the production wells when the geothermal fluid rises from the depths due to a change in the fluid’s physical and chemical properties. Scaling issue in geothermal power plants result in significant output losses and lower plant effectiveness. In rare instances, it might even result in the power plant being shut down. The chemistry of the geothermal fluid, non-condensable gases, pH, temperature and pressure changes in the process from production to reinjection, power plant type and design, and sometimes the materials used can also play an active role in the scaling that will occur in a geothermal system. ICP–MS was used to evaluate the chemical properties of the fluids. On the other hand, XRD, XRF and SEM were used to investigate the chemical and mineralogical compositions of the scale samples in analytical methods. For the numerical approach, PhreeqC and GWELL codes were used to follow the chemical reactivity of the geothermal fluid in Tuzla production well. The novelty of this study is to determine potential degassing point and to characterize the mineralogical assemblage formed in the well because of the fluid composition, temperature and pressure variations. During production, geothermal fluids degas in the wellbore. This causes a drastic modification of the chemistry of the Tuzla fluids. This is why it is focused the calculations on the nature of the minerals that are able to precipitate inside the well. According to simulation results, the degassing point is estimated to be about 105 m depth, consistent with the field observations. If a small quantity of precipitated minerals is predicted before the boiling point, degassing significantly changes the fluid chemistry, and the model predicts the deposition of calcite along with smaller elements including galena, barite, and quartz. The simulation results are consistent with the mineral composition of scaling collected in the well. © The Author(s) 2024.