2012
DOI: 10.1007/s12665-012-2138-5
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A preliminary assessment of hydrogeological features and selected anthropogenic impacts on an alluvial fan aquifer system in Greece

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Cited by 11 publications
(5 citation statements)
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“…Channelization has been particularly common within portions of a river network that naturally store sediment, such as alluvial fans (Petalas, 2013), deltas (Arnaud-Fassetta, 2003), braided or anastomosing channel segments (Surian and Rinaldi, 2004), and floodplains (Kroes and Hupp, 2010) (Fig. 6), as well as within urban areas (Martín-Vide and Andreatta, 2009).…”
Section: Increased River Transport Capacitymentioning
confidence: 99%
“…Channelization has been particularly common within portions of a river network that naturally store sediment, such as alluvial fans (Petalas, 2013), deltas (Arnaud-Fassetta, 2003), braided or anastomosing channel segments (Surian and Rinaldi, 2004), and floodplains (Kroes and Hupp, 2010) (Fig. 6), as well as within urban areas (Martín-Vide and Andreatta, 2009).…”
Section: Increased River Transport Capacitymentioning
confidence: 99%
“…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. Together with major ions trend, selected trace elements were used to better characterize GW flow and thus salt transport [80].…”
Section: Analytical Techniquesmentioning
confidence: 99%
“…140 km 2 , has a combined thickness of 80 to more than 150 m, while a sequence of alternations of fine-grained sediments of low permeability and coarse grained sedimentary deposits of various permeability constitutes the base of it (Petalas, 2013) and the hydraulic conductivity ranges from 0.4 to 2,870 m/day, averaging about 841 m/day.…”
Section: Granular Aquifers Of Rhodopementioning
confidence: 99%