A GIS Based Morphometric Analysis of Watershed (KR 40) Around Sangli, Maharashtra (India)
DOI:
https://doi.org/10.48165/Keywords:
Drainage morphometry, GIS, Groundwater, Watershed (KR 40), Watershed (KR 40)IndiaAbstract
The study area is one of the watershed (KR 40) from Krishna river basin, around Sangli town, Maharashtra, which is drained by two major streams i.e. Sheri and Laxmi streams. The morphometric analysis has been carried out to understand the hydrogeological conditions of the study area. The modern software tool i.e. Geographical Information System (GIS) is used to evaluate linear, aerial and relief aspects. The different quantitative morphological parameters like stream number, stream length, stream frequency, bifurcation ratio, stream density, etc. of the watershed which reflect its hydrogeological behavior and helpful when quantify the hydrogeological response. The geomorphological study of the drainage network of a watershed basin gives idea about the interdependency and relationship between the surface runoff and infiltration of rainwater and relative permeability of the rocks in study area. The GIS analysis provides a relationship between morphometric parameters, lithology and structural characteristics of study area. The present watershed (KR 40) is 5th order stream with dendritic drainage pattern and drainage density (1.08 km/km2) which indicates moderate runoff causing moderate floods and moderate permeability of the catchments.
Downloads
References
Chorley, R.J., (1962. Geomorphology and general systems theory. U.S.G.S. Prof. Pap., 500-B: 1- 10.
Gottschalk LC (1964) Reservoir sedimentation in handbook of applied hydrology. McGraw Hill Book Company, New York (Section 7-1)
Horton, R.E., (1932). Drainage basin characteristics. Trans. Am. Geo.phy. Union, 13, 350-361. 4. Horton, R.E., (1945). Erosional development of streams and their drainage basin: Hydrophysical approach to quantitative morphology. Geol. Soc. Am. Bull. 56, 275-370. 5. Leopold, L.B. and Miller, J.P., (1956). Ephemeral Streams hydraulic factors and their relation to drainage network. U.S Geol. Survey. Prof. Paper 282-A, pp: 16-24.
Miller, V.C., (1953. A quantitative geomorphic study of drainage basin characteristics in Clinch Mountain area. Virginia and Tennessee Project, N.R 389-042, Tech. Report No.3, Department of Geology, Columbia University.
Morisawa M., (1968). Stream : their Dynamics and Morphology, MaGrew Hill Book co., New York, p. 138
Nageswara Rao. K., (2010). Morphometric Analysis of Gostani River Basin in Andhra Pradesh State, India Using Spatial Information Technology. International journal of geomatics and geosciences 1(2), 179 - 187
Sarangi A.C., Madramootoo C.A., Singh D.K., Singh A.K., (2004). Journal of Agricultural Engineering 41(2), 42-48.
Schumm, S.A., (1956). Evolution of drainage systems and slopes in Badlands at Perth Amboy, New Jersey. Geol. Soc. Am. Bull., 67, 597-598, 599-622, 636-641 and 645-646.
Singh S and Singh M C (1997). Morphometric analysis of Kanhar river basin. National geomorphological journal of India, 43(1), 31-43
Strahler, A.N. (1952). Hypsometric (area-altitude) analysis of erosional topography. Geo. Soc. Am. Bull., v. 63, pp. 1117-1142.
Strahler, A.N. (1957). Quantitative analysis of watershed geomorphology. Trans. Amer. Geophys. Union, 38, 913-920.
Strahler, A.N. (1964). Quantitative geomorphology of drainage basins and channel networks, in Hand book of Applied Hydrology (edited by V. T. Chow), pp 439-476.