2016
DOI: 10.1007/s12517-015-2151-6
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Assessment of groundwater vulnerability and quality in coastal aquifers: a case study (Tipaza, North Algeria)

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Cited by 53 publications
(19 citation statements)
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“…The parameters used are the groundwater occurrence (G), aquifer hydraulic conductivity (A), height of the groundwater level above sea level (L), distance inland perpendicular from the shoreline (D), impact of existing seawater intrusion in the area (I), and thickness of the aquifer considered (T). Many studies have employed the GALDIT method to assess the overall vulnerability of coastal aquifers to SWI in coastal regions and islands of different countries in Europe, Asia, and Africa over very small (2 km 2 ) and large (2835 km 2 ) areas [4,[22][23][24][25][26][27].Lobo-Ferreira and Chachadi [21,22] used GALDIT to conduct vulnerability tests on an unconfined aquifer covering an area of approximately 10 km 2 at Monte Gordo, Portugal. They mapped the spatial distributions of the six GALDIT parameters and prepared SWI scenarios describing sea level rises of 0.25 and 0.5 m and applied them to the parameter G to calculate the vulnerability depending on individual scenarios.…”
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confidence: 99%
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“…The parameters used are the groundwater occurrence (G), aquifer hydraulic conductivity (A), height of the groundwater level above sea level (L), distance inland perpendicular from the shoreline (D), impact of existing seawater intrusion in the area (I), and thickness of the aquifer considered (T). Many studies have employed the GALDIT method to assess the overall vulnerability of coastal aquifers to SWI in coastal regions and islands of different countries in Europe, Asia, and Africa over very small (2 km 2 ) and large (2835 km 2 ) areas [4,[22][23][24][25][26][27].Lobo-Ferreira and Chachadi [21,22] used GALDIT to conduct vulnerability tests on an unconfined aquifer covering an area of approximately 10 km 2 at Monte Gordo, Portugal. They mapped the spatial distributions of the six GALDIT parameters and prepared SWI scenarios describing sea level rises of 0.25 and 0.5 m and applied them to the parameter G to calculate the vulnerability depending on individual scenarios.…”
mentioning
confidence: 99%
“…In a recent study, Kura et al [4] performed a GALDIT assessment on Kapas Island, a tropical island in northeastern Malaysia and concluded that the alluvial deposits west of the island were highly vulnerable to SWI. Recinos et al [26] carried out a GALDIT assessment on a Mediterranean alluvial aquifer, which is a representative pilot site for various case studies on SWI and reported that the intrinsic vulnerability shifted from moderate to high vulnerability in 15% of the regions between 1992 and 2004.Some studies have compared the GALDIT method to other index-based methods like DRASTIC, SINTACS, and AVI to evaluate the model performance [3,23,24,28]. Pedreira et al [25] applied two overlay and index techniques to one field; they assessed nitrate pollution using the DRASTIC model, while the SWI vulnerability was tested with the GALDIT method.…”
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“…Also, WQI is regarded as one of the most efficient technique to evaluate groundwater quality [1,13]. Among the main advantages of WQI is the ability to integrate data from multiple water quality parameters into a mathematical equation which determines the water quality level [14]. Therefore, the objective of this work is to assess the groundwater quality and to define its suitability for drinking based on hydrochemical analysis and WQI in the Quaternary Alluvial Basin.Thus, this serve as a background work to improve the evaluation of groundwater quality in the planning of water resources in the future.…”
Section: Introductionmentioning
confidence: 99%
“…The acronym GALDIT derived from the acronyms of the following six parameters: Groundwater occurrence (G), aquifer hydraulic conductivity (A), height of groundwater level above sea level (H), distance from the shore (distance inland perpendicular from shoreline) (D), impact of existing status of seawater intrusion in the area (I), and thickness of the aquifer (T) [5,6]. It has been applied in many Mediterranean countries, such as Portugal and Algeria [6,15,16]. It has been also used for the assessment of coastal aquifer vulnerability in Northern Greece, including a coastal plain part of Rhodope [16], a coastal aquifer system at River Nestos Eastern Delta [17] and a coastal area of the River Anthemountas basin [18].…”
Section: Introductionmentioning
confidence: 99%