TY  - JOUR
AU  - Gat, J. R.
PY  - 1980//
TI  - 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 propriétés caractéristiques de l’eau dans les zones à précipitation faible
JO  - Hydrological Sciences Bulletin
SP  - 257
EP  - 267
VL  - 25
IS  - 3
N2  - 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.
SN  - 0303-6936
UR  - http://www.tandfonline.com/doi/abs/10.1080/02626668009491933
UR  - http://dx.doi.org/10.1080/02626668009491933
N1  - exported from refbase (http://www.uhydro.de/refbase/show.php?record=22), last updated on Tue, 17 Mar 2020 13:48:25 +0100
ID  - Gat1980
ER  -