2015
DOI: 10.1016/j.scitotenv.2014.09.041
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Geochemical processes controlling water salinization in an irrigated basin in Spain: Identification of natural and anthropogenic influence

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Cited by 47 publications
(30 citation statements)
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“…The clearing of natural vegetation for rainfed crop production, especially in arid to semiarid areas, is reported to increase mobilization of salts stored in the vadose zone over millennia due to an increases in soil water leaching (Scanlon et al, 2007). The shift to irrigated agriculture normally enhances this process due to an increase in available water for leaching (Merchán et al, 2015a). The rate at which salts are washed out depends mainly on the available amount of salts and the water leached.…”
Section: Agricultural Pollution Dynamics In Irrigated Areas In Contramentioning
confidence: 99%
“…The clearing of natural vegetation for rainfed crop production, especially in arid to semiarid areas, is reported to increase mobilization of salts stored in the vadose zone over millennia due to an increases in soil water leaching (Scanlon et al, 2007). The shift to irrigated agriculture normally enhances this process due to an increase in available water for leaching (Merchán et al, 2015a). The rate at which salts are washed out depends mainly on the available amount of salts and the water leached.…”
Section: Agricultural Pollution Dynamics In Irrigated Areas In Contramentioning
confidence: 99%
“…The deterioration of coastal aquifers due to salinization may endanger future water exploitation . There are a number of mechanisms that have the potential to lead to salinity in coastal regions: (i) agricultural return flows from local groundwater extraction (Bouchaou et al, 2008;Cruz-Fuentes et al, 2014); (ii) a high degree of evaporation in residual saline water (McCaffrey et al, 1987;Han et al, 2014); (iii) recharge/leakage of imported salt water from the sea for fishing industries (Chang and Li, 2011); (iv) seawater intrusion/tidal flat/sea level rising (Werner et al, 2013); (v) saltwater upconing from underlying aquifers (Barlow, 2003;Szynkiewicz et al, 2008) or downward movement of shallow saline groundwater from upper aquifers under extensive pumping (Vengosh and Ben-Zvi, 1994;Guo et al, 1995;Cary et al, 2015); (vi) mixing modern recharged water with the palaeo-seawater (brines) (Yechieli et al, 1992;Han et al, 2011Han et al, , 2012; (vii) sewage effluents (Vengosh et al, 1998);and (viii) water-rock interaction (Jones et al, 1999;Vengosh et al, 2007;de Montety et al, 2008;Mongelli et al, 2013;Merchán et al, 2015). For a reliable water management/protection plan and to prevent further deterioration, it is essential to study the major geochemical processes that modify hydrochemical compositions of waters salinized by seawater intrusion and to elucidate the salinity sources and flow paths that exist in the coastal aquifer.…”
Section: Introductionmentioning
confidence: 99%
“…Other factors controlling the salinity level of IRFs include quality, volume and rate of applied water, climate, soils, water table depth, type of aquifer, and the specific agricultural, drainage and irrigation management practices (Tanji and Kielen 2002;Aragues and Tanji 2003;Kass et al 2005;Scanlon et al 2007Scanlon et al , 2010Garcia-Garizabal and Causape 2010;Merchan et al 2015). Irrigation water quality will substantially influence the extent of the groundwater salinization process, ranging from fresh water to saline water depending on the source.…”
Section: Direct Impactsmentioning
confidence: 99%