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The use of Na/Cl ratios to trace solute sources in a semiarid zone
Year:
1981
Source of publication :
Water Resources Research
Authors :
Dan, Joel
;
.
Koyumdjisky, Hanna
;
.
Nadler, Arie
;
.
Volume :
17
Co-Authors:
Magaritz, M.
Nadler, A.
Koyumdjisky, H.
Dan, J.
Facilitators :
From page:
602
To page:
608
(
Total pages:
7
)
Abstract:
Rainwater interaction with soils is a major source of dissolved salts in groundwater. The transition zone between the humid and the arid area is characterized by a specific combination of reactions which do not exist elsewhere. This combination of CaCO3 dissolution and base exchange reactions affects the Na/Cl ratio, which is the quantitatively most important parameter used for tracing salinity sources of groundwater. The increase in the Na/Cl ratio in the coastal plain aquifer of Israel from north to south is related to local recharge of Na‐rich water after interaction with soils of loessial origin. Copyright 1981 by the American Geophysical Union.
Note:
Related Files :
Cl
Na
Semiarid zone
soil
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More details
DOI :
10.1029/WR017i003p00602
Article number:
0
Affiliations:
Database:
Scopus
Publication Type:
article
;
.
Language:
English
Editors' remarks:
ID:
29106
Last updated date:
02/03/2022 17:27
Creation date:
17/04/2018 00:44
Scientific Publication
The use of Na/Cl ratios to trace solute sources in a semiarid zone
17
Magaritz, M.
Nadler, A.
Koyumdjisky, H.
Dan, J.
The use of Na/Cl ratios to trace solute sources in a semiarid zone
Rainwater interaction with soils is a major source of dissolved salts in groundwater. The transition zone between the humid and the arid area is characterized by a specific combination of reactions which do not exist elsewhere. This combination of CaCO3 dissolution and base exchange reactions affects the Na/Cl ratio, which is the quantitatively most important parameter used for tracing salinity sources of groundwater. The increase in the Na/Cl ratio in the coastal plain aquifer of Israel from north to south is related to local recharge of Na‐rich water after interaction with soils of loessial origin. Copyright 1981 by the American Geophysical Union.
Scientific Publication
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