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Implication of Drainage Basin Parameters of Chhoti Gandak River, Ganga Plain, India
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The drainage basin parameters of the groundwater-fed Chhoti Gandak River originating in the terai area of the Ganga Plain were analyzed using topographical sheets, satellite data, and field documentation with emphasis to its implication for flood mitigation and recharging of groundwater. The analyses indicate dominance of first order streams, gentle slope gradient, low surface run-off, low sediment production, high infiltration rate, and low value of basin relief. The low water storage capacity, spreading of water and concentration of peak discharge in the distal part of the river basin explain that whenever precipitation is high in the catchment area there is flood in the distal part of the basin. The bifurcation ratio value (4.34) of this basin describes that the drainage is carved naturally by slope and local relief and not influenced by geological structures like lineaments and faults.
These parameters provide useful information for the prediction of basin behavior during prolonged heavy rainfall that generate floods and suggest that water resource management and developmental planning should be done with reference to the drainage basin parameters.
Keywords
Morphometric Analysis, Flooding, Chhoti Gandak, Ganga Plain.
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