Hydrogeochemical evolution and groundwater recharge processes in arsenic enriched area in central Gangetic plain, India

2021 ◽  
pp. 105044
Author(s):  
Sumant Kumar ◽  
Suneel Kumar Joshi ◽  
Neeraj Pant ◽  
Surjeet Singh ◽  
Biswajit Chakraborty ◽  
...  
Keyword(s):  
Groundwater Recharge ◽  
Gangetic Plain ◽  
Hydrogeochemical Evolution

Groundwater recharge environments and hydrogeochemical evolution in the Jiuquan Basin, Northwest China

2012 ◽  
Vol 27 (4) ◽  
pp. 866-878 ◽  
Author(s):  
Jianhua He ◽  
Jinzhu Ma ◽  
Peng Zhang ◽  
Liming Tian ◽  
Gaofeng Zhu ◽  
...  
Keyword(s):  
Groundwater Recharge ◽  
Northwest China ◽  
Hydrogeochemical Evolution

Groundwater recharge history and hydrogeochemical evolution in the Minqin Basin, North West China

2006 ◽  
Vol 21 (12) ◽  
pp. 2148-2170 ◽  
Author(s):  
W.M. Edmunds ◽  
Jinzhu Ma ◽  
W. Aeschbach-Hertig ◽  
R. Kipfer ◽  
D.P.F. Darbyshire
Keyword(s):  
Groundwater Recharge ◽  
West China ◽  
North West ◽  
Hydrogeochemical Evolution ◽  
Minqin Basin

Groundwater Recharge Environments and Hydrogeochemical Evolution in Beijing, China: Multi-Tracer Approach

2012 ◽  
Vol 518-523 ◽  
pp. 3647-3651
Author(s):  
Ji Lai Liu ◽  
Tian Ming Huang ◽  
Jie Li
Keyword(s):  
Stable Isotopes ◽  
Water Chemistry ◽  
Groundwater Recharge ◽  
Radiocarbon Dating ◽  
Cold Climate ◽  
Hydrogeochemical Evolution ◽  
Chemical Indicators ◽  
Groundwater Samples ◽  
Δ13c Value ◽  
Beijing China

The groundwater recharge environments and hydrogeochemical characteristics in Beijing were investigated using a combination of chemical indicators, stable isotopes, and radiocarbon dating. There are two distinct zones for those groundwaters: modern water (1000 a) are depleted, which implies that the palaeowaters were recharged in relatively cold climate. The TDS for all groundwater samples range from 312 to 914 mg/L. Groundwaters are supersaturated with respect to calcite and the δ13C value is stable (around -13‰), which suggests dissolution of calcite is limited. Dissolution of halite, sulfate and carbonate and exchange of cations are main processes of water chemistry. The results have important implications for groundwater management in Beijing, where a certain proportion of the unrenewable water has been mined.

Groundwater recharge and hydrogeochemical evolution in the Ejina Basin, northwest China

2013 ◽  
Vol 476 ◽  
pp. 72-86 ◽  
Author(s):  
Ping Wang ◽  
Jingjie Yu ◽  
Yichi Zhang ◽  
Changming Liu
Keyword(s):  
Groundwater Recharge ◽  
Northwest China ◽  
Hydrogeochemical Evolution ◽  
Ejina Basin
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