In marginal and
central alluvial plains (Ganga Plain) of India, the inland salinity is
continuously increasing, canal network and arid to semi-aridclimatic conditions
that led to excessive evapotranspiration concentrates the salt in soil and
thereby escalating the groundwater salinity. In MatTahsil, Mathura district
(Ganga Plain) study on shallow and deep aquifer salinity and fluoride was
carried out in August 2001 and 2004.Groundwater salinity in some parts is more
then 4000−1/cm. This region is severely affected by endemic fluorosis due to
consumption offluoride-contaminated water. Analysis of F−, Na+, K+, Cl− and
HCO3− was carried out at 30 sites of dugwells and borewells. Result shows thatthere
is a variation and continuous escalation in the groundwater salinity and fluoride
concentration in deep and shallow aquifers on the basis ofanalysis.
Classification of salinity levels was carried out in 2001 and 2004. The deep
aquifers (borewells) are found more saline as compare tothe shallow aquifers
(dugwells) while F−, Na+, K+, Cl− and HCO3− shows high concentration in shallow
aquifers. The fluoride concentration inthe groundwater of these villages showed
values from 0.1 to 2.5 mg/l, severe enough to cause dental and skeletal
fluorosis among the inhabitants,especially children of these villages. One of
the major effects of inland salinity in this region is from saline groundwater,
which is reaching theland surface and causing soil salinisations and water
logging in the NE and SE parts of Mat block.
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