2002
DOI: 10.1016/s0377-0273(02)00217-2
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Hydrogeochemistry of the Simav geothermal field, western Anatolia, Turkey

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Cited by 60 publications
(22 citation statements)
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“…As in the case of EC, this situation is also attributed to the hot geothermal water intrusion to the surfacial aquifer. The results of a previous study also verify this finding and reports that sodium is one of the main elements in the waters of the geothermal fields in Simav Plain (Gemici & Tarcan, 2002). When EC and SAR are combined to assess the infiltration hazard, it has been found out that these areas where groundwater is affected from the intrusion of geothermal fluid demonstrate moderately suitable areas for irrigation water extraction as high SAR and EC values counter balance the negative effects of each other.…”
Section: Infiltration Hazardsupporting
confidence: 73%
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“…As in the case of EC, this situation is also attributed to the hot geothermal water intrusion to the surfacial aquifer. The results of a previous study also verify this finding and reports that sodium is one of the main elements in the waters of the geothermal fields in Simav Plain (Gemici & Tarcan, 2002). When EC and SAR are combined to assess the infiltration hazard, it has been found out that these areas where groundwater is affected from the intrusion of geothermal fluid demonstrate moderately suitable areas for irrigation water extraction as high SAR and EC values counter balance the negative effects of each other.…”
Section: Infiltration Hazardsupporting
confidence: 73%
“…In addition, it is also believed that a secondary reservoir system has developed in the young volcanic system located underneath Simav Plain as a result of basalt intrusion and lava flow. The bore log data obtained from a geothermal well indicates that the thickness of these Neogene-aged and volcanic reservoir rocks reach a total of about 400 m (Gemici & Tarcan, 2002).…”
Section: Hydrogeologymentioning
confidence: 99%
“…Peloids P-11 and P-12 are formed from the units. Paleozoic to Early Mesozoic metamorphic rocks, e.g., gneiss, schist, marble, and ophiolites, and Late Eocene to Middle Miocene basaltic, andesitic, dacitic, and rhyolitic lavas and pyroclastic rocks are overlain by Upper Miocene to Pliocene lacustrine and fluvial deposits (Gemici and Tarcan, 2002;Mutlu, 2007). The samples numbered P-13 to P-15 have been used as peloids, which were taken from the deposits.…”
Section: Geologymentioning
confidence: 99%
“…The many geothermal water sources were formed in the region as a result of the formation of the Büyük Menderes graben and high concentration of boron (B) in some water resources was reported [9]. The contamination of the hot-water resources with high boron consantration is one of the most important source the high concentration of B in irrigation water resources like well and surface water especially Büyük Menderes River.…”
Section: Boron Toxicitymentioning
confidence: 99%
“…Recent studies [17,18,24] have shown that boron toxicity is a major problem at Büyük Menderes valley because of activity of geothermal power plants and their discharge of geothermal waste water due to drilling well to have effiancy and take it under control and into next stage due to holding electrical energy by using flash methode. Fluids emerging from some of these areas contain high boron concentrations and cause environmental problems for irrigation waters in agricultural areas where boron contaminates aquifers and soils [9]. Boron has accumulated in the plants more than required in the area [19].…”
Section: Boron Toxicitymentioning
confidence: 99%