Abstract:
The Walawe River basin is the fourth largest river basin in Sri Lanka which is
undergoing rapid industrial and agricultural development. Hence groundwater has
become an important freshwater source for consumption and become vulnerable due
to over-exploitation and predicted climate change scenarios. A detailed
hydrogeochemical study was carried out in the Walawe river basin to investigate the
groundwater suitability for drinking and irrigation purposes. A total of sixty-four
groundwater samples were collected from thirty-two locations of the study area
during the pre- (May - June) and post-monsoon (February –March) periods and
analyzed for their major and trace elements, and also for water isotopes (δ18OH2O and
δ
2HH2O). The solute compositions in groundwater in the region were dominated by
HCO3
-
, Cl-
, and SO4
2-
, which were mostly balanced by Na+
, Ca2+, and Mg2+. The
Piper classification indicated that the groundwater in the region was dominated by
Ca2+
-HCO3
-
type of water with subordinate contributions of Ca2+
-Na+
-HCO3
-
, Ca2+
-
Mg2+
-Cl-
, Na+
-Cl-
, and Ca2+
-SO4
2-
rich waters. Groundwater in the region exceeded
the levels in terms of EC, hardness, and fluoride. A greater percentage (82%) of postmonsoon samples was poor in quality for drinking purposes when compared to premonsoon (47%) samples. According to the US salinity laboratory and Wilcox’s
classification, two-thirds of investigated groundwater samples were suitable for
irrigation purposes. The isotope data suggested that the groundwater in the region is
recharged from the first inter-monsoon and north-east monsoon events and
intensively affected by evaporation events. The findings of this study suggest that
water quality management in the Walawe River basin is essential and water
resources should critically monitor to reduce the anthropogenic stress on
groundwater resources
