2017
DOI: 10.1016/j.apgeochem.2017.10.001
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Irrigation return flows in a mediterranean aquifer inferred from combined chloride and stable isotopes mass balances

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Cited by 18 publications
(12 citation statements)
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“…(2006) and Vallet‐Coulomb et al. (2017). Therefore, the planned increase in drip‐irrigated area in the Plana de Valencia Sur could further increase the region's vulnerability in terms of groundwater recharge.…”
Section: Discussionmentioning
confidence: 98%
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“…(2006) and Vallet‐Coulomb et al. (2017). Therefore, the planned increase in drip‐irrigated area in the Plana de Valencia Sur could further increase the region's vulnerability in terms of groundwater recharge.…”
Section: Discussionmentioning
confidence: 98%
“…The Mediterranean climate is characterized by few intense rainfall events concentrated in fall and winter. The occurrence or non‐occurrence of these events in a given year is of high importance for aquifer recharge as much of it can be generated by a few single rainfall events (Cheng et al., 2017; Poch‐Massegú et al., 2014; Vallet‐Coulomb et al., 2017). Our results confirmed this observation and additionally provided evidence that the sensitivity of annual recharge to single events was stronger in drip irrigation than in flood irrigation.…”
Section: Discussionmentioning
confidence: 99%
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“…Uncertainties in R predictions in semi‐arid regions are further intensified by the fact that much of the annual R can be generated by a few heavy precipitation events (Cheng et al., 2017; Poch‐Massegú et al., 2014; Vallet‐Coulomb et al., 2017). Uncertainties in the frequency and intensity of these (heavy) precipitation events can translate into considerable variability in R predictions (Smerdon, 2017).…”
Section: Discussionmentioning
confidence: 99%
“…Early studies in the Mediterranean area were developed in Israel [92,93], while since the year 2005, there has been a growing legacy of studies employing these techniques. Most of the studies used stable isotopes to distinguish between different GW origins [94][95][96][97][98][99][100][101][102][103][104][105][106][107][108][109][110][111][112][113], while some of them used radioactive isotopes to determine the residence time of GW [114][115][116], that is, one of the very few pieces of information allowing researchers to distinguish between actual and paleo SWI. These last elements have also been used to study surface water/groundwater interaction; for example, in a recent paper from Mayer et al [117], short-lived radioactive isotopes, such as radon-222, allowed not only for the determination of the amount of exchange between different water bodies, but also for the ability to precisely derive GW flow velocities and saturated hydraulic conductivities, which are vital parameters to constrain numerical simulations.…”
Section: Analytical Techniquesmentioning
confidence: 99%