Assessment of geochemistry and hydrogeochemical processes in groundwater of the Tefenni plain (Burdur/Turkey)

Varol, Simge; Davraz, Ayşen

doi:10.1007/s12665-013-2856-3

Cited by 58 publications

(23 citation statements)

References 33 publications

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“…1 Location, geological, and groundwater level (in May-2010) maps of the study area. (Varol 2011;Varol and Davraz 2014) Environ Earth Sci geology map was prepared using GIS-ArcView computer code. ArcGIS 9.3 software, Spatial Analyst extension, and inverse distance weight (IDW) interpolation methods were applied throughout research evaluations and the study area mapped to a UTM Zone 35, ED50 datum.…”

Section: Methodsmentioning

confidence: 99%

“…Generally, climate of the plain and its vicinity are affected from Mediterranean climate zone in the middle Anatolian climate zone. The mean rainfall is 465.03 mm and the mean evapotranspiration are 326.74 mm in the study area (Varol 2011;Varol and Davraz 2014). Eren (Boz) stream is the most important surface flow in the study area and discharged to Burdur Lake, which is located out of the Tefenni plain.…”

Section: Study Areamentioning

confidence: 97%

“…These springs have been discharged from overthrust zone, which are developed between allochthonous Kızılcadag ophiolite and Dutdere limestone. The discharge temperature of Barutlusu and Pınarbaşı springs are 17.6 and 27°C, respectively (Varol and Davraz 2014).…”

Section: Study Areamentioning

confidence: 99%

“…1) and it has a 1,527 km 2 watershed area (Varol and Davraz 2014). Generally, climate of the plain and its vicinity are affected from Mediterranean climate zone in the middle Anatolian climate zone.…”

Section: Study Areamentioning

confidence: 99%

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Evaluation of the groundwater quality with WQI (Water Quality Index) and multivariate analysis: a case study of the Tefenni plain (Burdur/Turkey)

2014

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Groundwater is a vital source of water for domestic and agricultural activities in the Tefenni plain. Therefore, groundwater quality, seasonal variations and its suitability for drinking, irrigation and industrial usage were evaluated. In this study, 56 water samples were collected from springs, wells, and lake in dry and wet seasons. CaMg-HCO 3 , Mg-Ca-HCO 3 , Na-CO 3 -Cl, and Na-HCO 3 -Cl water types are the dominant water types in the investigation area. Parameters, which are controlled to chemical variations of groundwater, were analyzed with R-mode factor and correlation analysis. According to R-mode factor analysis, total dissolved solids, Na, Cl, HCO 3 , and NH 3 are the most important parameters. In addition, Water Quality Index (WQI) was applied to suitability for drinking purpose and to investigation of groundwater quality. Quality of groundwaters are suitable for drinkable both dry and wet season in study area. In terms of the irrigation and industrial usage, generally groundwater is suitable in dry season but is not suitable in wet season. Groundwater chemistry is affected with water-rock interaction and densely agricultural activities.

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Section: Methodsmentioning

confidence: 99%

Section: Study Areamentioning

confidence: 97%

Section: Study Areamentioning

confidence: 99%

Section: Study Areamentioning

confidence: 99%

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Evaluation of the groundwater quality with WQI (Water Quality Index) and multivariate analysis: a case study of the Tefenni plain (Burdur/Turkey)

2014

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“…Firstly, special weights (w i ) in a scale of 1 (slightest consequence on water quality) to 5 (highest outcome on water quality) was allocated to every elemental parameter, on the basis of their supposed impact on primary health and their relative magnitude in the quality of drinking water (Sener & Davraz, 2013). The parameters having serious health impact and whose occurrence above the critical concentration amount could result in confined usage of the resource for household and drinking purposes were given the highest weight five (Varol & Davraz, 2014). The highest weight of 5 has been allocated to the parameters like nitrate, TDS, chloride, and fluoride because of their foremost significance in water excellence evaluation (Srinivasamoorthy et al, 2008).…”

Section: Residual Sodium Carbonatementioning

confidence: 99%

Geochemical assessment of groundwater quality for its suitability for drinking and irrigation purpose in rural areas of Sant Ravidas Nagar (Bhadohi), Uttar Pradesh

Madhav

Ahamad

Kumar

et al. 2018

Geology, Ecology, and Landscapes

107

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This study is aimed to assess the groundwater excellence within the rural areas of Sant Ravidas Nagar (Bhadohi), Uttar Pradesh, India. In the current work, estimation of groundwater excellence indices has been done to recognize the water quality for the appropriateness of groundwater resource for drinking and agricultural use. Twenty groundwater samples were collected and investigated for diverse geochemical parameters viz, pH, total dissolved solids (TDS), total hardness, cations and anions. The groundwater of the study region is neutral to slightly alkaline in nature. Piper's diagram classification shows that majority of the samples belong to CaMgHCO 3 hydrochemical facies. Gibbs plot specifies that majority of samples falls in rock dominance. The water quality index shows that the entire sample is under excellent water category. On the basis of TDS, all the samples are within the range of desirable to permissible for drinking and agriculture purpose. Forty percent samples of the study region are having nitrate content more than permissible limit (>50 mg/l) which is not fine for individual use. Poor drainage, domestic waste and use of N fertilization on farming land may be the main sources of nitrate in groundwater of the study region. On the basis of different water quality indices, groundwater of the study region is fit for agricultural use.

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澳大利亚昆士Tamborine山浅层和深层玄武岩含水层的水文地球化学演变

Catania

Reading

2023

Hydrogeol J

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Tamborine Mountain, Queensland (Australia), is a prime example of a basalt fractured-rock aquifer. Yet very little is known about the hydrochemistry of this groundwater system. Both analytical (major ions and stable isotopes) and multivariate (hierarchical cluster analysis, principal component analysis and factor analysis) analyses were used in this study to investigate the factors that interact within this aquifer system, in order to determine groundwater hydrogeochemistry. A new approach was applied to the data by classifying hydrographs by water type to clearly identify differing aquifer zones. Three distinct groundwater chemistry types were identified, and they were differentiated by variations in depth. Shallow bores were dominated by Na–Cl waters, deep bores were dominated by Na–HCO3 and Ca–HCO3 waters, and the two deepest bores were dominated by mixed water types. The evaluation of hydrogeochemical data has determined that both mineral weathering processes and groundwater/surface-water interaction had a strong influence on the hydrogeochemistry. Seasonal effects were minimal in the study area based on physicochemical parameters and ion chemistry. However, stable isotopic data show temporal trends. Increased rainfall events during the wet season produced a depletion in δ18O and increased d-excess values. The opposite is found during the dry season as a result of higher evaporation rates that are not hindered by intense rainfall events.

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Assessment of geochemistry and hydrogeochemical processes in groundwater of the Tefenni plain (Burdur/Turkey)

Cited by 58 publications

References 33 publications

Evaluation of the groundwater quality with WQI (Water Quality Index) and multivariate analysis: a case study of the Tefenni plain (Burdur/Turkey)

Evaluation of the groundwater quality with WQI (Water Quality Index) and multivariate analysis: a case study of the Tefenni plain (Burdur/Turkey)

Geochemical assessment of groundwater quality for its suitability for drinking and irrigation purpose in rural areas of Sant Ravidas Nagar (Bhadohi), Uttar Pradesh

澳大利亚昆士Tamborine山浅层和深层玄武岩含水层的水文地球化学演变

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