@Article{Gat1980,
author="Gat, J. R.",
title="The relationship between surface and subsurface waters: water quality aspects in areas of low precipitation / Rapport entre les eaux de surface et les eaux souterraines: aspects des propri{\'e}t{\'e}s caract{\'e}ristiques de l{\textquoteright}eau dans les zones {\`a} pr{\'e}cipitation faible",
journal="Hydrological Sciences Bulletin",
year="1980",
volume="25",
number="3",
pages="257--267",
abstract="In the temperate and semiarid environment the salinity of both surface and subsurface(meteoric) waters is dominated by the weathering products of soil and aquifer minerals, since even surface waters have a history of subsurface flow. In the desert environment, in contrast, surface flows are more superficial and their chemistry dominated by the aeolian salinity. This has both a marine input anda contribution from recycled salinity from surface accumulation of evaporitic minerals. Both these sources have chloride (and to a lesser extent sulphate) as the dominant anion.",
optnote="exported from refbase (http://www.uhydro.de/refbase/show.php?record=22), last updated on Tue, 17 Mar 2020 13:48:25 +0100",
issn="0303-6936",
doi="10.1080/02626668009491933",
opturl="http://www.tandfonline.com/doi/abs/10.1080/02626668009491933"
}