2017
DOI: 10.1007/s12665-017-6514-z
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Investigation of seawater intrusion using stable and radioisotopes at coastal area south of Beirut, the Capital of Lebanon

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Cited by 6 publications
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“…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%
“…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%