Abstract
River bank erosion is a hazardous and common phenomenon in diara region near Malda district of North East India during monsoon and post monsoon periods of every year. The left bank of Ganga river is texturally very weak along diara region of Malda district. The present work explores relations between stream power, braiding intensities and bank erosion in certain stretches of upstream of the Ganga river near Malda district of West Bengal in India. In the present study, we have tried to do a quantitative assessment of channel braiding process of the Ganga river by applying the Plan Form approach and equivalent measurement of stream power. A comparative study of discrete years has been done through braiding index to understand morphological behaviour of the channel. Beside its stream power of the selected stretches of the study area is estimated and compared with braiding intensity and bank erosion. This paper presents the dynamic behaviour of the channel pattern of the Ganga river system in Malda district over a time span of 40 years. This procedure addresses the selection of input parameters from digital satellite images comprising scenes for the years 1975, 1995 and 2015 with specific dates, from Rajmahal in Jharkhand district to Farakka barrage in Malda district. To obtain Plan Form Indices for the entire study area, required parameters were extracting through using GIS techniques. Stream power is measured through analyzing latest flood records and satellite images. The present study concluded that a wide spread and continuous braiding process has occurred in the study area due to aggradations of riverbed and temporal declination of stream power.
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References
Alekseevskiy NI, Berkovich KM, Chalov RS (2008) Erosion, sediment transportation and accumulation in rivers. Int J Sediment Res 23(2):93–105
Banerjee M (1999) A report on the impact of Farakka Barrage on the human fabric. On behalf of South Asian network on dams, rivers and people (SANDRP). https://www.sandrp.in/dams/impact_frka_wcd.pdf. Accessed 12 Feb 2008
Census of India (2001) Provisional population totals, West Bengal, Table—4. Maldah District (06). Government of West Bengal. https://web.cmc.net.in/wbcensus/DataTables/02/Table4_6.htm. Retrieved 21 July 2001
Chang HH (1979) Stream power and river channel patterns. ASCE J Hydrol Eng 41:303–311
Ferguson RI (1981) Channel form and channel changes. In: Lewin J (ed) British rivers. Allen and Unwin, London, pp 90–125
Gurnell AM, Downward SR, Jones R (1994) Channel planform change on the River Dee meanders, 1976–1992. Regul Rivers Res Manag 9:187–200
Henderson FM (1961) Stability of alluvial channels. J Hydraul Div Am Soc Civ Eng 87:109–138
Hickin EJ, Nanson GC (1984) Lateral migration rates of river bends. J Hydraul Eng Am Soc Civ Eng 110(11):1557–1567
Lane EW (1957) A study of the shape of channels formed by the natural streams flowing in erodible material, U.S Army Crops Engineering Division, Missouri River, M.R.D. Sediment, series no. 9, p 106
Leopold LB, Wolman MG (1957) River channel patterns: braided, meandering and straight, United States, Geological survey professional paper, vol 282-B, pp 35–85
Muller E, DecampsDobson HMK (1993) Contribution of space remote sensing to river studies. Freshw Biol 29:301–312
Parker G (1976) On the cause and characteristics scale of meandering and braided in rivers. J Fluid Mech 76:459–480
Richards K (1982) Rivers: forms and process in alluvial channels. Methuen and Co., Ltd, London
Schumm SA, Khan HR (1972) Experimental study of channel patterns. Bull Geol Soc Am 83:1755–1770
Sharma N (2004) Mathematical modelling and braid indicators. In: Singh VP (ed) The Brahmaputra river basin water resources, vol 47. Kluwer Academic Publishers, Dordrecht, pp 229–260
Thakur PK, Laha C, Aggarwal SP (2012) River bank erosion hazard study of river Ganga, upstream of Farakka barrage using remote sensing and GIS. Nat Hazards 61:967–987. https://doi.org/10.1007/s11069-011-9944-z
Thome CR, Osman MA (1988) The influence of bank stability on regime geometry of natural channels. In: White WR (ed) International conference on river regime. Hydraulics Research/Wiley, Chichester, pp l35–147
Yang CT (1976) Minimum unit stream power and fluvial hydraulics. ASCE J Hydraul Div 102(HY7):919–933
Yang X, Damen CJM, Zuidam AR (1999) Satellite remote sensing and GIS for the analysis of channel migration changes in the active Yellow river Delta, China. Int J Appl Earth Observ Geoinf 1(2):146–157
Acknowledgements
This work was supported by University of Gour Banga and special thanks to my research guide Prof. Sujit Mandal and my dear scholar friends whose are helped to complete my field observations and its related works. We also thank U.S. Geological Survey for providing Landsat satellite data.
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Majumdar, S., Mandal, S. Assessment of relationship of braiding intensities with stream power and bank erosion rate through Plan Form Index (PFI) method: a study on selected reaches of the upstream of Ganga river near Malda district, West Bengal, India. Sustain. Water Resour. Manag. 6, 107 (2020). https://doi.org/10.1007/s40899-020-00462-z
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DOI: https://doi.org/10.1007/s40899-020-00462-z