Physiochemical Analysis of Fresh Water Sources in District Bhimber, Azad Jammu Kashmir

Authors

  • Iftikhar Alam Pakistan Atomic Energy Commission (PAEC), Islamabad, Pakistan
  • Salim Shehzad Pakistan Atomic Energy Commission (PAEC), Islamabad, Pakistan
  • Saqib Mehmood Department of Earth & Environmental Sciences, Bahria University, E-8, Islamabad, Pakistan

DOI:

https://doi.org/10.46660/ijeeg.v9i2.682

Abstract

The present study investigates the physiochemical parameters of drinking water quality in district Bhimber of
Azad Jammu and Kashmir. The drinking water supplies in the area come from four main sources, streams, springs, hand
pumps and boreholes. A total of seventy one (71) samples from all four water sources were taken for determination of
physiochemical parameters. The results show considerable variation in water quality parameters of different water
sources. However, the data analyses indicate that physiochemical parameters of water samples are well within the
permissible limits of drinking water quality. Stream water samples show slightly higher pH values, while two samples
from hand-pump have shown marginally higher content of TDS. The mean values of dissolved oxygen in borehole and
hand-pump water samples are also slightly below the water quality standard limits. The correlation studies show that pH
has a strong negative correlation with calcium and positive relation with sodium in water samples of all four sources.
Similarly, the dissolved oxygen has shown negative relationship with temperature and a weak to moderate positive
relationship with pH of water. No evidence of pollution and industrial contamination of water was found. The study
found that water from all four sources is safe for drinking purpose. 

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Published

2018-06-20

How to Cite

Iftikhar Alam, Salim Shehzad, & Saqib Mehmood. (2018). Physiochemical Analysis of Fresh Water Sources in District Bhimber, Azad Jammu Kashmir. International Journal of Economic and Environmental Geology, 9(2), 54–60. https://doi.org/10.46660/ijeeg.v9i2.682

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