Environmental Engineering Reference
In-Depth Information
Base Exchange Indices ( r 1 ) and Meteoric Genesis Indices ( r 2 )
The changes in the chemical composition of groundwater during its travel in the
subsurface must be understood (Sarin et al. 1989 ). Base Exchange Indices ( r 1 ) and
MeteoricGenesisIndices( r 2 ) are proposed to indicate the ion exchange between the
groundwater and its host environment. Base Exchange Indices ( r 1 ) is determined by
using the equation which could be applied for the further classification of ground-
water given as follows:
(
)
)
(
r 1
=
Na
+
Cl
/
SO
2
where
allions in meql
/
4
The groundwater can be grouped as Na + -HCO 3 type if r 1 > 1 and Na + -SO 4 2− type if
r 1 < 1 (Soltan 1998 ). Majority of samples in both the seasons are of Na + -HCO 3 type.
Based on Base Exchange Indices, 89 % and 11 % of samples are Na + -HCO 3 type and
Na + -SO 4 2− type waters in both the seasons, respectively (Fig. 4 ). The dissolution of
gasesandminerals,particularlyCO 2 andCO 3 2− related compounds in the atmosphere
and in the unsaturated zone during precipitation and infiltration, would impart the
observedHCO 3 water type (Shanyengana et al. 2004 ; Singh et al. 2006 ).
ThegroundwatersourcescanalsobeclassiiedbasedonMeteoricGenesisIndex
and can be computed using following equation (Soltan 1999 ):
{
(
)
}
)
(
r 2
=
K
+
+
Na
+
Cl
/
SOwhere
2
allions in meql
/
4
The groundwater source is of deep meteoric water percolation type, if r 2 < 1
while r 2 > 1 indicates that it is of shallow meteoric water percolation type. No sig-
nificant variations were noticed within this category. Based on r 2 indices, 89 % and
11 % of samples are shallow meteoric water and deep meteoric water type in both
the seasons, respectively (Fig. 5 ). The groundwater samples are showing shallow
meteoricwatersduetolessutilizationofborewellwatersaswellashardbasement
rock in the study area.
Pre-monsoon
Post-monsoon
4
3
2
1
0
0
2
4
6
8
10
1
2
3
4
Sample Numbers
Fig. 4 Scatter plot of base-exchange indices
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