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Öğe Current status and potentials of enhanced geothermal system in the Eastern Pontide Orogenic Belt, Turkey(Diponegoro Univ, 2024) Şener, Mehmet FurkanThe radioactive decay of isotopes is one of the most important sources of heat in the Earth's interior. The main radiogenic elements in the crust are U, Th, and K in granitoids. Radiogenic granites are becoming increasingly important as they support the development of the renewable energy sector. This study provides an in-depth review of the development of Enhanced Geothermal Systems (EGS) technology. Many countries, such as France and the UK, have initiated and contributed to energy production using EGS technology. In addition, this study calculates the potential production capacity of radiogenic granites in the Eastern Pontide Oraganic Belt (EPOB) and assesses their significant contribution to the Turkish economy in line with the Sustainable Development Goals (SDGs). The total area of radiogenic granites within the EBOP is 7116.35 km 2 and these granites contain average concentrations of U 3.25 ppm, Th 16.44 ppm, and K 3.7%. The plutons studied can generally be classified as medium to low heat producing granitoids. Ayeser, Camibo & gbreve;az & imath;, and Ayder (3.36-6.98 mu W/m 3 ), which are close to the average heat production value of the continental crust (5 mu W/m 3 ), may be suitable areas for EGS. Currently, EBOP granites have the capacity to produce 61 x 109 kWh of electricity. In addition to electricity, heat from granites can be used for other applications such as space heating and greenhouse cultivation.Öğe Geochemical proxies and formation mechanism of Hatay (Baslamis) travertine and relation with Dead Sea Fault Zone (S-Turkey)(Pergamon-Elsevier Science Ltd, 2021) Şener, Mehmet Furkan; Yiğit, Banu; Şener, MehmetThis study is the first investigation of the Baslamis(Hatay) travertines formed in the northern part of the left-lateral strike-slip Dead Sea Fault Zone. In this study, Baslamis travertines are examined in terms of structural, mineralogical and formation mechanism by conducting geochemical, hydrogeochemical and facies analysis. The Baslamis travertine occurrences are characterized by successions of terraces and pools developed in slope depositional system, mound depositional system and depression depositional system. The travertines have been classified into five lithotypes, namely: laminated, coated bubble, reed, intraclasts and micritic travertine. According to the thin section, XRD, SEM and EDX analysis, the Baslamis travertines are divided into two groups, the first group contains aragonite and secondary minerals such as silica and clay minerals, while the second group consists only of calcite minerals, therefore, the travertines are morphologically classified as aragonite-bearing travertines and massive calcite bearing travertines. The negative correlation between Ca and Sr abundances in travertine samples indicates that some Ca was replaced by Sr in the calcite lattice. Relatively rich trace element content in the Baslamis travertines is attributed to leaching of the underlying gabbro and limestone. Higher concentrations of some of the elements were probably the result of diagenetic processes and syngenetic mineralization. The Baslamis travertines are defined as meteogene travertine deposits and are fed with meteoric-origin waters along Dead Sea Fault Zone in terms of hydrogeochemical results. The conceptual model of the Baslamis travertine shows that the travertines are formed by precipitation of dissolving the limestone. The heat source of the geothermal fluid forming the travertines is of tectonic origin.Öğe Hydrogeochemical and rare earth element properties of geothermal waters and the use of abandoned oil wells in Diyarbakır(Springer, 2024) Şener, Mehmet FurkanT & uuml;rkiye is one of the most tectonically active regions in the world. Diyarbak & imath;r, which was chosen as the study area, is located in the south-eastern Anatolian region of T & uuml;rkiye and also in the south of the Bitlis-Zagros Suture Zone (BZSZ). Some of the geothermal resources in Diyarbak & imath;r are actively exploited. The temperature of & Ccedil;ermik geothermal waters was recorded at 40-51 degrees C by MTA (General Directorate of Mineral Research and Exploration) between 2010 and 2014. However, subsequent measurements conducted following the Kahramanmara & scedil; earthquake (Mw: 7.7 on 6 February 2023) revealed that the surface temperature of geothermal fluids had increased to between 52 and 56 degrees C. Previous studies have indicated that there are also many abandoned oil wells in the region where the wellhead temperatures are around 107 degrees C. As a result of hydrogeochemical analyses, deep circulating geothermal waters such as & Ccedil;ermik have Na-HCO3 composition, while shallow circulating and mixed cold surface waters such as & Ccedil;& imath;nar, Bismil and Sur have Na-Ca-Cl-HCO3 composition. According to the chalcedony geothermometer results, the reservoir temperatures in the study area vary between 90 degrees C and 173 degrees C. REY (Rare Earth Elements and Yttrium) results show that geothermal fluids in the study area have negative cerium (Ce), europium (Eu) and yttrium (Y) anomalies. The negative Ce anomaly indicates that the colder aquifers are close to oxygen-rich surface waters and thermal fluids interact with Karacada & gbreve; volcanic rocks. Eu anomalies in groundwater are controlled by preferential mobilisation of Eu2+ during water-rock interaction compared to Eu3+, and negative Eu anomalies indicate leakage of geothermal fluids from granites. The Y/Ho values of the thermal fluids in the study area are between 30 and 40. This value is due to the active contribution of fluorine during the mobilisation of REY as a fluoride or fluorocarbonate ligand complex, causing Y to behave as a heavy pseudolanthanide. delta 18O and delta 2H isotope values show that the geothermal waters in the study area are of meteoric origin. The obtained results reveal that Diyarbakir province has a geothermal potential and usage potential can be increased by using the abandoned oil wells.Öğe Lithium: An energy transition element, its role in the future energy demand and carbon emissions mitigation strategy(Elsevier Ltd, 2024) Chandrasekharam D.; Şener, Mehmet Furkan; Recepoğlu Y.K.; Isık T.; Demir M.M.; Baba A.Energy transition elements (Li, Ni, Co, Fe, Cu) are gaining importance due to their ability to provide energy and play an important role as primary energy sources. Because of the energy density and power density, Li-ion batteries have the edge over other batteries. Li is distributed in various rock-forming minerals and brines, and geothermal waters. Though lithium-bearing minerals are spread over a broad geographic region, these minerals are confined to certain countries with substantial economic potential. Li is extensively used in batteries, and battery-driven vehicles are growing exponentially to meet the carbon reduction goal of the Paris agreement in 2015 and signed by more than 50 percent of the countries. Nearly 55 million cars supported by Li batteries are expected to roll out by 2030. While this is the demand, its occurrence and concentration/extraction processes are not keeping pace with this demand. The extraction of Li from its ore is an energy-intensive process involving many fossil fuel-based energies. To recover one ton of Li metal, nearly 5 to 6 tons of CO2 is emitted. The CO2 emissions of 28 kWh LFP, NMC, and LMO batteries vary from 5600 to 2705 kg CO2-eq. The end-of-life emissions of an internal combustion engine (ICE) vehicle are 400 kg CO2/vehicle, while Li Battery supports 500 kg/vehicle. The quantity of Li required for a 24 kWh average capacity leaf battery is about 137 g/kWh. While emissions are associated with the manufacturing of the batteries, emissions are also associated with a way that while they are recharged as the recharging source is fossil fuel-based energy. The best option to meet zero net carbon emissions by 2050, as envisaged by International Energy Agency (IEA), is to recover Li from geothermal brines and use geothermal energy for recharging. While hydrothermal energy sources are site-specific, enhanced geothermal system (EGS) based geothermal energy is not site-specific and is found wherever high radiogenic granites are available. High radiogenic granites are widely distributed, and heat recovered from EGS sources can provide clean energy and heat. Extraction of lithium from geothermal waters and using geothermal energy for recharging the batteries will drastically reduce CO2 emissions. It will drive the world towards Net Zero Emissions (NZE) scenario in the future. This is being practiced in Turkey. Future research should develop technology to recover Li from geothermal fluids with low concentration and support EGS development. © 2024 Elsevier LtdÖğe Mapping investigation based on engineering geology of a developing urban area (Nigde, Turkey)(Springer Heidelberg, 2021) Çelik, Fatih; Öztürk, Muhammed Zeynel; Şener, Mehmet Furkan; Arioz, Ömer; Erbil, MerveDefinitions of urban geological environments are usually required to provide information about an engineering basis for planners and design engineers to prepare a rational land use planning and developing urban areas. Therefore, the geological mapping investigation method can be a beneficial way of defining urban geological environments visually. In this study, the Engineering Geological Mapping Method (EGMM) was used to investigate and present the geotechnical and geological data obtained from Nigde city of Turkey. Around forty-five unpublished reports that were obtained from the construction work done around the study area were evaluated as detail. Then, the study area was divided into five different regions which were considered their geological characteristics. In each region, nine unpublished reports were selected and analyzed for interpreting the data and plotting the geotechnical and geological maps. The main indispensable parameters for geotechnical design engineers were drawn by using the data obtained from the different boreholes for Nigde city. These drawn maps by GIS technic: (1) groundwater table, (2) liquefaction zone, (3) plasticity index, (4) bearing capacity, (5) soil classification, and (6) SPT results. For preparing the maps, two types of interpolation methods were used (minimum curvature and Voronoi polygons methods). The Geographic Information System (GIS) was used to rearrange and control all this information and to prepare engineering geotechnical and geological maps. As a result, the Engineering Geological Mapping Method applied for this study is to show more crucial for preventing mistakes making in practical works during preparing urban extension planning for developing cities in the future.Öğe Morphotectonic development of dolines on Mt. Bozdag (Karaburun Peninsula)(Tmmob Jeoloji Muhendisleri Odasi, 2024) Şener, Mehmet FurkanThis study investigated the morphometric and morphogenetic characteristics of dolines in the Bozda & gbreve; Massif, located in the north of Karaburun Peninsula. Dissolution dolines are one of the characteristic surface features of mid-latitude high karst plateaus, and doline morphometry is one of the methods commonly used to study the morphotectonic evolution characteristics of karst plateaus. In this study, an automatic extraction technique was used with a high-resolution digital elevation model to determine the areal distribution, density and morphometric characteristics of dolines. After the dolines were identified, several morphometric parameters such as area, perimeter, circularity index, length, width and elongation rates were calculated. According to the analyses and results obtained, a total of 564 dolines were detected in the area, with a maximum density of 74 dolines/km 2 . All the dolines, with an average elevation of 1,080 metres, are located on limestone from the Camibo & gbreve;az & imath; Formation. The dolines extend in roughly NW-SE direction, parallel to lineaments in the area, which formed in relation to tectonic processes that started with palaeotectonic evolution and influenced the Karaburun platform in the Izmir-Ankara zone during the Cretaceous period.Öğe Structural controls and hydrogeochemical properties of geothermal fields in the Varto(Scientific Technical Research Council Turkey-Tubitak, 2021) Uzelli, Taygun; Şener, Mehmet Furkan; Dölek, İskender; Baba, Alper; Sözbilir, Hasan; Dirik, Ramazan KadirVarto and the surrounding region have important geothermal fields, developing in strike-slip tectonic setting in East Anatolia, which resulted from the collision of the Arabian and Eurasian plates. The main structural elements in the area are the NE-trending sinistral and NW-trending dextral strike-slip fault segments and N-S trending extension zones. In order to determine fault-controlled geothermal circulation, it is very important to fully characterize the structural elements in these complex environments. The widely distributed volcanic rocks have fracture and crack systems that play an important role in surface infiltration, geothermal fluid, and groundwater circulation. Especially in areas where the fault segments intersect, hot springs outlets and natural resources easily come to the surface. In order to understand the flow paths of geothermal fluid along the faults in these geothermal systems, it is necessary to determine the stress state of the faults and to map the distribution of the structural elements. For this reason, we conducted a detailed study on the Varto Fault Zone, which has important geothermal fields in Eastern Anatolia. We present conceptual models of the geothermal fields in the Varto region that show favorable geothermal activity on the intersecting fault segments, fault bends, step-overs, and accompanying fracture-crack sets. As a result, we emphasize that the planes of strike-slip faults in transtensional areas are more favorable for secondary permeability and enhances the geothermal fluid circulation, and this can be supported by hydrogeochemical data.
