Abstract
Quaternary to Recent floodplains and the channel bed of the Damodar River (West Bengal, India) are gradually formed by a complex interaction of fluvial processes and anthropogenic processes but their character and evolution are essentially the product of stream power, channel dimensions, and sediment character. The relation between a stream’s ability to entrain and transport sediment and the erosional resistance of floodplain alluvium (that forms the channel boundary of the Damodar River) provides a basis of genetic classification of alluvial reaches and floodplains. The alluvial segment of the Damodar River, in between Rhondia (23°22′08′′N, 87°28′25′′E) and Paikpara (23°00′58′′N, 87°57′41′′E), was selected as the study area to identify its special hydrogeomorphic individuality and multidimensionality. The pattern and configuration of the fluvial landscape of the Damodar was recognized using ASTER DEM, GIS analytical tools, channel dimensions, and multivariate statistics, treating each segment of channel and cross-sectional profile as a unit of geomorphic study. The analysis showed that the Damodar River (Rhondia to Barddhaman) was regarded as a bed-load channel with a medium-energy noncohesive floodplain upstream of the study area, and the downstream stretch (Basrsul to Paikpara) was identified as a mix-load channel with a low-energy cohesive floodplain. Multivariate statistical analysis categorized the study unit of the Damodar River into two parts: the upstream section of the river tended to braiding and lateral expansion, and the downstream section of the river tended to meandering and lateral confinement.
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References
Basak NN (1994) Surveying and leveling. Tata McGraw Hill, New Delhi
Bhattacharya AK, Dhar N (2005) A report on geo-environmental appraisal in Barddhaman urban agglomeration and its environment for sustainable developmental activities. Geological Survey of India, Eastern Region, Kolkata
Bhattacharyya K (2011) The Lower Damodar River, India: understanding the human role in changing fluvial environment. Springer, New York
Chandra S (2003) India: flood management—Damodar River Basin. Retrieved from www.apfm.info/pdf/case_studies/cs_india.pdfon 13th October, 2011 at 9:35 am
Charlton R (2008) Fundamentals of fluvial geomorphology. Routledge, London
Chatterjee SP (1969) Damodar valley planning atlas. NATMO, Calcutta
Friend PF, Sinha R (1993) Braiding and meandering parameters. In: Best JL, Bristow CS (eds) Braided rivers. Geological Society Special Publication, New York, pp 105–111 (No. 75)
Fryirs KA, Brierley GL (2013) Geomorphic analysis of river systems: an approach to reading the landscape. Blackwell Publishing, New York
Gauckler P (1867) Etudes Theoriques sur I’Ecoulement et le Mouvement des Eaux, Comptes Rendues de I'Academie des Sciences. Tome, Paris, pp 818–822
Garde RJ (2006) River morphology. New Age International Publishers, New Delhi
Ghosh S (2011) Determination of significant variables in the evolution of Sarujharna Basin of East Singhbhum. Jharkahand Practising Geogr 15(1):25–39
Ghosh S, Bhattacharya K (2012) Multivariate erosion risk assessment of lateritic badlands of Birbhum (West Bengal, India): a case study. J Earth Syst Sci 121(6):1441–1454
Ghosh S, Guchhait SK (2014a) Hydrogeomorphic variability due to dam constructions and emerging problems: a case study of Damodar River, West Bengal, India. Environ Dev Sustain 16(3):769–796
Ghosh S, Guchhait SK (2014b) Analyzing fluvial hydrological estimates and flood geomorphology from channel dimensions using ASTER DEM, GIS and statistics in the controlled Damodar River. India J Geomatics 8(2):232–245
Ghosh S, Guchhait SK (2014c) Palaeoenvironmental significance of fluvial facies and archives of late quaternary deposits in the floodplain of Damodar River. India Arab J Geosci 7(10):4145–4161
Gregory KJ, Walling DE (1973) Drainage basin form and process: a geomorphological approach. Edward Arnold, London
Hodge SA, Tasker GD (1995) Magnitude and frequency of floods in Arkansas. USGS Water Resource Investigations Report 95–4224:1–52
IWD (2013) Irrigation and Waterways Department Government of West Bengal. Daily River and Rain-gauge Data Section, http://wbiwd.gov.in/daily_river_rain_gauge_data.php
Kale VS (1998) Monsoon floods in India: a hydro-geomorphic perspective. In: Kale VS (ed) Flood Studies in India. Geological Society of India, Bangalore, pp 229–256
Kale VS (2003) Geomorphic effects of monsoon floods on Indian rivers. Nat Hazards 28:65–84
Kale VS et al (2004) Palaeohydrological reconstructions based on analysis of a palaeochannels and toba-ash associated alluvial sediments in the Deccan Trap Region, India. In: Kale VS, Gregory KJ, Joshi VU (eds) Progress in palaeohydrology: focus on monsoonal areas. Geological Society of India, Bangalore, pp 481–489
Khan ZA, Tewari RC (2011) Paleochannel and paleohydrology of a Middle Siwalik (Pliocene) fluvial system, northern India. J Earth Syst Sci 120(3):531–543
Kothari CR (2009) Research methodology. New Age International Publishers, New Delhi
Lahiri-Dutt K (2006) State and the community in water management case of the Damodar Valley Corporation, India. In: International symposium on community activities for the conservation of water environment—lessons learned from community activities, Institute for Global Environmental Strategies, Bangkok
Langbein WB, Iseri KT (1960) General introduction and hydrologic definitions. US Geol Surv Water-Supply Pap 1541-A:1–26
Leeder MR (1973) Fluviatile fining-upwards cycles and the magnitude of palaeochannels. Geol Mag 110:265–276
Leopold LB, Wolman MG (1957) River channel patterns: braided, meandering and straight. US Geol Surv Prof Pap 282-B:1–85
Leopold LB, Wolman WG (1960) River meanders. Geol Soc Am Bull 71(6):769–793
Leopold LB, Wolman MG, Miller JP (1969) Fluvial Processes in geomorphology. Eurasia Publishing House, New Delhi
Mahmood A (2007) Statistical methods in geographical studies. Rajesh Publications, New Delhi
Manning R (1891) On the flow of water in open channels and pipes. Trans Institution Civil Engineers Ireland 20:161–207
Mueller JR (1968) An introduction to the hydraulic and topographic sinuosity indexes. Ann Assoc Am Geogr 58(2):371–385
Nanson GC, Croke JC (1992) A genetic classification of floodplains. Geomorphology 4(6):459–486
Niyogi D (1975) Quaternary geology of the coastal plain in West Bengal and Orissa. Indian J Earth Sci 2:51–61
Niyogi D et al (1970) Geomorphic mapping in plains of West Bengal, India. In: Chatterjee SP, Das Gupta SP (eds) Selected paper on physical geography. 21st International Geographical Congress, vol 1. National Committee for Geography, Calcutta, pp 89–94
Pickup G, Warner RF (1984) Geomorphology of tropical rivers: channel adjustment to sediment load discharge in the fly and lower Purari, Papua New Guinea. Catena 5:19–41
Rosgen DL (1994) A classification of natural rivers. Catena 22:169–199
Rotnicki K (1983) Modelling past discharges of meandering rivers. In: Gregory KJ (ed) Background of palaeohydrology. Wiley, New York, pp 321–354
Sanyal J, Carbonneau P, Densmore AL (2013) Hydraulic routing of extreme floods in large ungauged river and the estimation of associated uncertainties: a case study of the Damodar River, India. Nat Hazards 66:1153–1177
Schumm SA (1963) A tentative classification of alluvial river channels. USGS Geol Surv Circular 477:1–10
Schumm SA (1972) Fluvialpalaeochannels. Mineral 16:98–107 (Spec Publ Soc Econ Paleontol)
Schumm SA (1977) The fluvial system. Wiley, New York
Schumm SA (1985) Patterns of alluvial rivers. Ann Rev Earth Planet Sci 13:5–27
Schumm SA (2005) River variability and complexity. Cambridge University Press, Cambridge
Sen PK (1985) The genesis of floods in the Lower Damodar catchment. In: Sen PK (ed) The concepts and methods in geography. The University of Burdwan, Burdwan, pp 71–85
Sen PK (1991) Flood hazards and river bank erosion in the lower Damodar Basin. In: Sharma HS (ed) Indian geomorphology. Concept Publishing Company, New Delhi, pp 95–108
Singh LP, Parkash B, Singhvi AK (1998) Evolution of the Lower Gangetic Plain landforms and soils in West Bengal, India. Catena 33:75–104
Sinha R, Friend PF (1994) River systems and their sediment flux, Indo-Gangetic plains, northern Bihar, India. Sedimentology 41:825–845
Sridhar A (2007) Discharge estimation from planform characters of the Shedhi River, Gujarat alluvial plain: present and past. J Earth Syst Sci 116(4):341–346
USGS (2013) United States Geological Survey Earth Explorer. http://earthexplorer.usgs.gov/
Williams GP (1984) Paleohydrologic equations for rivers. In: Costa JE, Fleisher PJ (eds) Developments and application of geomorphology. Springer, Berlin, pp 343–367
Williams GP (1986) River meanders and channel size. J Hydrol 88:147–164
Williams GP (1988) Paleofluvial estimates from dimensions of former channels and meanders. In: Baker VR, Kochel RC, Patton PC (eds) Flood geomorphology. Wiley, New York, pp 321–334
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Ghosh, S. (2016). Present Geomorphic Categorization of Alluvial Channel Reaches Using Channel Dimensions and Geomatics in the Damodar River of West Bengal, India. In: Das, B., Ghosh, S., Islam, A., Ismail, M. (eds) Neo-Thinking on Ganges-Brahmaputra Basin Geomorphology. Springer Geography. Springer, Cham. https://doi.org/10.1007/978-3-319-26443-1_4
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