Identifying sources of groundwater salinity and major hydrogeochemical processes in the Lower Kabul Basin aquifer, Afghanistan

Author(s):  
Abdulhalim Zaryab ◽  
Hamid Reza Nassery ◽  
Farshad Alijani

The origin of groundwater salinity and major hydrogeochemical processes in the LKB aquifer were investigated using hydrogeochemical and HCA methods. The results indicate that evaporitic lacustrine deposits are the major source of salinity in the aquifer.

2022 ◽  
Vol 174 ◽  
pp. 113264
Author(s):  
S. Selvakumar ◽  
N. Chandrasekar ◽  
Y. Srinivas ◽  
S. Selvam ◽  
S. Kaliraj ◽  
...  

2008 ◽  
Vol 23 (8) ◽  
pp. 2337-2349 ◽  
Author(s):  
Veronique de Montety ◽  
Olivier Radakovitch ◽  
Christine Vallet-Coulomb ◽  
Bernard Blavoux ◽  
Daniel Hermitte ◽  
...  

Waterlines ◽  
2007 ◽  
Vol 26 (1) ◽  
pp. 12-13 ◽  
Author(s):  
Suzanna Lipscombe

Author(s):  
М. I. Dzhalalova ◽  
P. А. Abdurashidova ◽  
R. М. Zagidova

The coastal strip of the northwestern Caspian is characterized by hydromorphism and salinization processes which depending on the Caspian piled-up water, groundwater salinity, seawater, and salt composition of the underlying rocks. The migrational salts capability in deltoic ecosystem components in dynamic over the main representatives of pasture plants occurring in the Western Caspian and playing an important role in developing the theoretical foundations of a system of measures to increase the productivity of cover crop have studied. Salts migration from soil layers into plants which taking place in synthesis of material-energy and material resource of environment is one of the chains of bio-substrat links. The research results confirm the data that the ash elements stock in the ephemeral-absinthial group varies from 21.5 to 64.5 kg per 1 ha. The organogens prevail in them – 944 kg / ha, K is dominant, then Ca and Mg. The amount of halogens is 7.05 kg / ha, of which Cl portion includes 3.31 and Na – 2.80 kg / ha. In the ephemeral-absinthial group cenoses rather high values of aboveground phytomass are up to 50 centners / ha and the supply of ash elements (halogens 32.14 and organogens 36.18 mg-eq) is much higher compared to their content in soil (7.05 and 6, 31 mg-eq). In roots difference in quantity of organogens and halogens is insignificant – 2.03 and 2.04 mg-eq. We associate such differences with a greater proportion of absinthial in the aboveground phytomass composition


1995 ◽  
Author(s):  
R.S. Thompson ◽  
Charles G. Oviatt ◽  
A.P. Roberts ◽  
J. Buchner ◽  
R. Kelsey ◽  
...  

2013 ◽  
Vol 32 (5) ◽  
pp. 123-129
Author(s):  
Hongliang ZHANG ◽  
Xianglin FANG ◽  
Qinglai FENG ◽  
Shengli ZOU

2016 ◽  
Author(s):  
Jonathan W. Pruiett ◽  
◽  
Melissa S. Rice ◽  
N.H. Warner ◽  
Sanjeev Gupta
Keyword(s):  

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