Study of Hydrological Behaviour of Chhoti Koli Sindh Watershed using Morphometric Parameters
DOI:
https://doi.org/10.46243/jst.2021.v6.i04.pp195-205Keywords:
Linear parameter, Relief parameter, Areal parameter, Chhoti Kali Sindh watershedAbstract
Morphometric analysis of Chhoti Koli Sindh watershed was carried out using geospatial technique. The outcome revealed that the entire study area has dendritic drainage pattern with uniform lithology. Stream length and mean stream length data also reaffirm uniform lithology and gentle slope. The low drainage density of watershed indicates less surface runoff. The morphometric analysis also indicates that the area is least susceptible to erosion. The bifurcation ratio value is less, which indicates that the present area has not under gone any tectonic disturbance. Circulatory and elongation ratios show that the watershed has elongated shape. The estimation of form factor and circularity ratio also confirm that the basin is elongated, with permeable subsurface, compactness coefficient value shows the longest time of concentration before peak flow. Relief ratio and length of overland flow let out the fact that the rain water has more residence time on the land which provides more time to percolate the water down ward and sheet flow is also larger than peak flow which reduces the run off. Value of farm factor indicating elongated shape, suggest flat hydrograph peak for longer duration, hence in elongated basins flood management is rather easier. From the analysis of morphometric parameters the hydrologic characters may be deduced
References
Morisawa,M.E. (1958) relation of morphometric proportion to runoff in the Little Mill Creak, Ohio drainage basin, project NR 389-042 Tech; Rept. 17, Colmbia university, New York
Iqbaluddin, S. and Javed, A. (1997). Geomorphology and landscape evolution of Bharatpur District, Rajasthan.Photonirvachk,jour. Indian Soc.,25(3):177-178
Singhal,S. B.B.S. and Gupta, R.P. (1999). Applied Hydrogeology of Fractured Rocks, Roorkee. Kluwer Academic Publisher London. PP. 38-41
Karanth, K.R. (2003) Groundwater Assessment, Development and Management. Tata Mc-Graw Hill Publ.Co.Ltd. New Delhi, p.720
Singh, s. (1992) “Quantitative geomorphology of the drainage basin,” in Readings on Remote Sensing Applications, T. S. Chouhan and K. N. Joshi, Eds., Scientific Publishers, Jodhpur, India
Horton, R. E. (1945) “Erosional development of streams and their drainage basins: hydrophysical approach to quantitative morphology,”Geological Society of America Bulletin, vol. 56, pp. 275–370
Schumms, S. A. (1956) “Evolution of drainage systems and slopes in Badlands at Perth Amboy, New Jersey,” Bulletin of the Geological Society of America, vol. 67, pp. 597–646
Strahler, S. A. (1957) “Quantitative analysis of watershed geomorphology,” Transactions American Geophysical Union A., vol. 38, pp. 913–920
Costa, J. E. (1987) “Hydraulics and basin morphometry of the largest flash floods in the conterminous United States,” Journal of Hydrology, vol. 93, no. 3-4, pp. 313–338
Singh, S. and Singh, M. C. (1997) “Morphometric analysis of Kanhar river basin,” The National Geographical Journal of India, vol. 43, no. 1, pp. 31–43
Howard, A. D. (1990) “Role of hypsometry and planform in basin hydrologic response,” Hydrological Processes, vol. 4, no. 4, pp. 373–385
Smith, K. G. (1950) “Standards for grading textures of erosional topography,” American Journal of Science, vol. 248, pp. 655–668
Montgomery, D. R. and Dietrich, W. E. (1989) “Source areas, drainage density, and channel initiation,” Water Resources Research, vol. 25, no. 8, pp. 1907–1918
Langbein, W. B.(1947) “Topographic characteristics of drainage basins,” U.S. Geological Survey. Water-Supply Paper, vol. 986, pp. 157–159
Demoulin, A. (2011) “Basin and river profile morphometry: a new index with a high potential for relative dating of tectonic uplift,” Geomorphology, vol. 126, no. 1-2, pp. 97–107
Youssef, A. M. and Pradhan, B. and Hassan, A. M.(2011) “Flash flood risk estimation along the St. Katherine road, southern Sinai, Egypt using GIS based morphometry and satellite imagery,” Environmental Earth Sciences, vol. 62, no. 3, pp. 611–623
Dar, R. A. and Chandra, R. and Romshoo, S. A.(2013) “Morphotectonic and lithostratigraphic analysis of intermontane Karewa basin of Kashmir Himalayas, India,” Journal of Mountain Science, vol. 10, no. 1, pp. 731–741
Miller, V. C. (1953) “A Quantitative geomorphic study of drainage basin characteristics in the Clinch Mountain area, Virginia and Tennessee,” Tech. Rep. 3 NR 389-402, Columbia University, Department of Geology, ONR, New York, NY, USA
Shulits, S. (1998) “Quantitative formulation of stream and watershed morphology,” Bulletin of the International Association of Scientific Hydrology, vol. 3, pp. 201–207
Tucker, G. E. and Bras, R. L. (1998) “Hillslope processes, drainage density, and landscape morphology,” Water Resources Research, vol. 34, no. 10, pp. 2751–2764
Potter, K. W. and Faulkner, E. B. (1987) “Catchment response time as a predictor of flood quantiles,” Journal of the American Water Resources Association, vol. 23, no. 5, pp. 857–861
Rashid, M. and Lone, M. A.(2011) and S. A. Romshoo, “Geospatial tools for assessing land degradation in Budgam district, Kashmir Himalaya, India,” Journal of Earth System Science, vol. 120, no. 3, pp. 423–433
Strahler, A. N.(1964) “Quantitative geomorphology of drainage basins and channel networks,” in Handbook of Applied Hydrology, V. T. Chow, Ed., section 4–11, McGraw-Hill, New York, NY, USA
Horton, R. E. (1932) “Drainage basin characteristics,” Transactions American Geophysical Union, vol. 13, pp. 350–361
Sameena, M. and Krishnamurthy and Jayaraman, J. V. and G. Ranganna, (2009) “Evaluation of drainage networks developed in hard rock terrain,”Geocarto International, vol. 24, no. 5, pp. 397–420
Suresh, M. and Sudhakara, S.and K. N. Tiwari, and V. M. Chowdary, (2004) “Prioritization of watersheds using morphometricn parameters and assessment of surface water potential using remote sensing,” Journal of the Indian Society of Remote Sensing, vol. 32, no. 3




