Abstract
The strong stratification on the downstream region after the Nagara river mouth Barrage construction has been reported. The purpose of this paper is to extract the features of saline intrusion and analyze the flow mechanism of this stratification triggered by the Nagara Barrage using monitoring data. Several special features of salinity intrusion were reported and revealed salinity intrusion was effected not only the reduction of tidal prism by barrage construction but also topographical and hydraulic features of Nagara river estuary. This paper also treated the relationship between DO concentration and saline intrusion and revealed strong correlation.
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