Abundance of fluoride and its source in drinking water of Kheshki and surrounding area, district Nowshera, N.W.F.P., Pakistan

Authors

  • Shahab Danishwar Department of Geology, University of Peshawar
  • Mohammad Tahir Shah National Centre of Excellence in Geology, University of Peshawar, Pakistan
  • Mohammad Majid National Centre of Excellence in Geology, University of Peshawar, Pakistan

Abstract

Fluoride, if present in minute amount in human body, is beneficial for the growth of bones and teeth. Its excess is, however, very harmful and usually causes skeletal fluorosis. Few cases of skeletal fluorosis are reported in Kheshki and surrounding areas in N. W. F. P. The drinking water of study area has been, therefore, analyzed for the fluoride contents. It is noticed that this water has high concentration of fluoride. The source of fluoride enhancement in the drinking water of the area needs to be unraveled. For this purpose, the water of Kabul River, rocks of Nowshera Formation and the lacustrine and soil samples of the area have been analyzed for fluoride. These media show elevated amounts of fluoride. The study suggests that in the lacustrine and soil deposits of the Kheshki and surrounding area the detrital minerals which accommodate fluoride in their structure, are the main contributors of fluoride to the drinking water.

References

Adriano, D. C., 1986. Trace elements in the terrestrial environment. Springer-Verlag, New York.

American Public Health Association, 1985. Standard method for water and waste water analyses. Washington DC, 1266p.

Barnett, S. G., Kohut, J. J., Rust, C. C, & Sweet, W. C., 1966. Conodonts from Nowshera reef limestone (Upper Silurian or Lowermost Devonian) West Pakistan. Jour. Paleont., 40, 435-438.

Bernstein, D M., Sadowsky, N., Hegsted, D. Guri, C. D. & Stare, F. J., 1960. Prevalence of osteoporosis in high and low fluoride areas in North Dakota. Jour. Amer. Med. Assoc., 498, 499-504.

Burbank, D.W., 1983. Multiple episodes of catastrophic flooding in the Peshawar basin during the past 700,000 years. Geol. Bull. Univ. Peshawar, 16, 43-49.

Burbank, D. W. & Tahirkheli, R. A. K., 1985. The magnetostratigraphy, fission track dating and stratigraphic evolution of the Peshawar intermontaine basin, northern Pakistan. Geol. Soc. Am. Bull., 96, 539-552.

Danishwar, S., Majid, M., Shah, M. T. & Haq, N., 1994. Fluoride abundance in drinking water and related health hazards: a case study from Kheshki area, Nowshera district, N.W.F.P. Geol. Bull. Univ. Peshawar, 27, 113-116.

Danishwar, S., 1995. Geochemistry of water and soil samples from the Kheshki and surrounding area, Nowshera and Charsadda districts N.W.F.P., Pakistan. Unpubl. M. Phil. Thesis, Univ. Peshawar.

Malik, Y. M. & Riaz, M., 1990. Groundwater resources of Kheshki area, N.W.F.P., Pakistan. Hydrogeology Directorate WAPDA, Pakistan Technical Report No. V-4A.

Pindborg, J. J., 1970. Pathology of the dental hard tissues. Munskgaard, Copenhagen.

Steinberg, C. L., Gardner, D. E., Smith, F. A. & Hofge, H.C., 1955. Comparison of rheumatoid (ankylosing) spondylitis and crippling fluorosis. Ann. Rheum. Dis., 14, 378-384.

Weatheretl, J. A. & Wiedmann, S. M., 1959. The skeletal changes of chronic experimental fluorosis. Jour. Path. Bact., 78, 233-241.

World Health Organization (WHO) 1984. Guide line values for drinking water, Geneva, l.

Downloads

Published

1995-11-30

How to Cite

Danishwar, S., Shah, M. T., & Majid, M. (1995). Abundance of fluoride and its source in drinking water of Kheshki and surrounding area, district Nowshera, N.W.F.P., Pakistan. Journal of Himalayan Earth Sciences, 28(1), 31-37. Retrieved from http://ojs.uop.edu.pk/jhes/article/view/1473

Most read articles by the same author(s)

1 2 3 4 > >>