1997
DOI: 10.1007/s002540050140
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A graphic expression of salinization and pollution of groundwater The case of Israel's groundwater

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Cited by 8 publications
(2 citation statements)
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“…Measurements of flow taken from the different monitoring stations along the length of the stream in various seasons indicate that along the stream's first 60 km between 40% and 90% of the wastewater discharged (8000 -11,000 m 3 ) percolates into ground water before it reaches the green line and the Beer Sheva stream (Table 1). This is consistent with comparable hydrological research in Israel (Melloul and Azmon 1997) and in other regions (Triska et al 1989, Zaramella et al 2003, Ryan and Boufadel 2007.…”
Section: Flow and Infiltration To Groundwatersupporting
confidence: 92%
“…Measurements of flow taken from the different monitoring stations along the length of the stream in various seasons indicate that along the stream's first 60 km between 40% and 90% of the wastewater discharged (8000 -11,000 m 3 ) percolates into ground water before it reaches the green line and the Beer Sheva stream (Table 1). This is consistent with comparable hydrological research in Israel (Melloul and Azmon 1997) and in other regions (Triska et al 1989, Zaramella et al 2003, Ryan and Boufadel 2007.…”
Section: Flow and Infiltration To Groundwatersupporting
confidence: 92%
“…One of the first papers using major ions and trace elements for a geochemical assessment of GW salinization in the Mediterranean area is the paper by Mercado [58] that analyzed the chromatographic effect of Israel coastal aquifers during salinization and freshening due to their cation exchange capacity as a preliminary tool to delineate whether the aquifer is salinizing or freshening. A decade later, another simple approach was proposed by Melloul and Azmon [59], where groundwater quality trends of selected species were proposed as a qualitative indicator of aquifer salinization and aquifer pollution by anthropogenic sources. More recently, several papers have focused on the origin and distribution of GW salinization either in porous aquifers [60][61][62][63][64][65][66], especially in arid and semiarid regions of the Mediterranean basin [67][68][69][70][71][72][73], or in fractured aquifers [74][75][76][77][78][79], by means of a detailed geochemical study.…”
Section: Analytical Techniquesmentioning
confidence: 99%