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Authors
Info
K. Ravindra1*, Suman Mor2,
A. Singh3, V.J. Singh3,
N. Dhanda3,? P. Rani3
and
S. Mor4
1School of Public
Health, Department of Community Medicine, Post Graduate Institute of Medical
Education and Research, Chandigarh-160 012, India
2Department of
Environment Studies, Panjab University, Chandigarh-160 014, India
3Department of
Energy and Environmental Science,? Chaudhary Devi Lal University, Sirsa-125
055, India
4Centre for Public
Health, Panjab University,
Chandigarh-160
025, India
*Corresponding
Author Email :
khaiwal@yahoo.com
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Abstract
Aim: The current study
aimed to identify the hydro-geological processes that control the groundwater
chemistry. Further, groundwater quality was also evaluated for drinking and
irrigation purposes.
Methodology: Groundwater
samples were collected from a semi-arid region of North India i.e.,
Ellenabad, Sirsa, Haryana. The samples were analyzed following the American
Public Health Association standard methods for the examination of water and
wastewater.
Results: Most of the
groundwater samples of study area fall under hard category. The saline nature
of groundwater can be attributed to high concentration of total dissolved
salts (340?104 mg l-1). Majority of the groundwater samples showed
fluoride concentration below the permissible limit of WHO and BIS (1.0 mg l-1).
Multivariate analysis including sodium absorption ratio was calculated to
assess the water quality for irrigation purpose and it was found appropriate
for majority of crops, except for sensitive plant species.
Interpretation: Potability
assessment of groundwater showed that more than 40% samples were unacceptable
for drinking purpose without any prior treatment, hence, it is essential to
conduct a routine monitoring of groundwater to determine its aptness for
drinking, domestic and agriculture purposes.
Key words: Gibb's plot, Groundwater quality, Hydro-geochemistry,
Piper trilinear plot, Wilcox diagram
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