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A plot of Gibbs diagram reveals that rock weathering and precipitation are the major hydrogeochemical processes regulating the water chemistry of the study area.
The Gibbs plot suggests that rock weathering and precipitation are the major hydrogeochemical processes regulating the water chemistry of the study area.
In the study area, rock weathering and evaporation processes are the major hydrogeochemical processes responsible for the concentration of major ions in groundwater.
This work aims to investigate the origin of groundwater salinity and the major hydrogeochemical processes controlling the groundwater evolution in the confined basal aquifer of the PRD.
Thus main objectives of the present study is (1) to identify the major hydrogeochemical processes (2) to determine the groundwater quality and (3) to delineate regions where groundwater is suitable or unsuitable for drinking, irrigation and industrial purpose.
The objective was to characterize the physico-chemical properties of groundwaters in TCP, assess the impact of anthropogenic activities on the groundwater hydrology and chemistry, and identify the major hydrogeochemical processes occurring in the area.
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However, hyporheic zone exchange can be a major hydrogeochemical process in these streams.
This reveals that rock weathering and rainfall are the major possible hydrogeochemical processes regulating the water chemistry of the study area.
Hydrogeochemical processes are the major responsible for the alteration of groundwater in their chemical composition.
With the above background, the main objectives of this study are: (1) to assess the major ion chemistry of groundwater; (2) to identify the hydrogeochemical processes affecting the groundwater chemistry.
Increase in population and rapid urbanization have made groundwater the major source of water supply; hence, it is very essential to understand the hydrogeochemical processes that take place in the aquifer system.
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