Geospatial approach to elucidate anomalies in the hierarchical organization of drainage network in Kuttiyadi River Basin, Southern India

Abstract

An assessment of anomalies in the hierarchical organization of the drainage network in the Kuttiyadi River Basin (KuRB), Kerala, has been performed by considering various morphometric parameters such as bifurcation index (R), hierarchical anomaly index (Δa), hierarchical anomaly density (ga), and stream gradient index (SL) in a geographical information system (GIS) platform. Further, a digital elevation model (DEM) of the area has been generated from Cartosat stereo pair data at 2.5-m resolution. The computed quantitative information about drainage characteristics reveals the highest drainage anomaly is observed in sub-watersheds (SW) III and IV. It is observed that neo-tectonic activity caused the development of younger stage drainage patterns of structural controls in the sub-watersheds of this river basin. The tectonic activity-induced diffusion, high energy fluvial erosion, and anthropogenic interferences altered the hierarchical organization of the drainage network of the sub-watersheds in mature to old stages of geomorphic evolution. The results of finding validated with asymmetry factor and ratio of the hierarchical index (Δa) with hierarchical anomaly number (A), bifurcation index (R), direct bifurcation ratio (R_db), stream gradient index (SL), and denudation index (logTu). From the denudation index analysis, the sediment yield of the river basin is identified as 0.67 t·km⁻²·yr⁻¹. Moreover, the asymmetric factor (AF) in the KuRB shows the imprints of Paleo−Neo Proterozoic crustal tilting toward a NNW−SSE direction.

Graphical abstract

Keywords

river basin / hierarchical anomaly / bifurcation index / stream gradient index / denudation index / Cartosat-1 DEM

References

[1] Ambili V, Narayana A C. (2014). Tectonic effects on the longitudinal profiles of the Chaliyar River and its tributaries southwest India. Geomorphology, 217: 37–47

[2] Anish A U, Baiju K R, Midhun E V, Krishnakumar K N. (2019). Hierarchical anomaly and denudation index of Karuvannur River Basin, Thrissur District, Kerala, India. Eco Chronicle, 14: 60–65

[3] Bhadran A, Vijesh V K, Gopinath G, Girishbai D, Jesiya N P, Thrivikramji K P. (2018). Morpho-hypsometric evolution of the Karuvannur River Basin, a tropical river in central Kerala, southwestern peninsular India. Arab J Geosci, 11: 430

[4] AvenaG CGiuliano GPalmieriE L(1967). On the quantitative assessment of the hierarchisation and evolution of river networks. Boll Soc Geol Ital, 86: 781–796 (in Italian)

[5] BahramiS (2013). Analyzing the drainage system anomaly of Zagros basins: implications for active tectonics, Tectonophysics, 608: 914−928

[6] BurbankDAnderson R (2001). Tectonic Geomorphology. Oxford: Blackwell Science

[7] BilousL F, Shyshchenco P, SamoilenkoV, HavrylenkoO(2020). Spatial morphometric analysis of digital elevation model in landscape research. In: Conference Proceedings, Geoinformatics: Theoretical and Applied Aspects 2020, Vol 2020

[8] ChorleyR J (1969). Introduction to Physical Hydrology, Suffolk Methuen and Co. Ltd.

[9] Dikpal R L, Renuka Prasad T J, Satish K. (2017). Evaluation of morphometric parameters derived from Cartosat-1 DEM using remote sensing and GIS techniques for Budigere Amanikere watershed, Dakshina Pinakini Basin, Karnataka, India. Appl Water Sci, 7(8): 4399–4414

[10] Ghosh S, Sivakumar R. (2018). Assessment of morphometric parameters for the development of Relative active tectonic index and its significant for seismic hazard study: an integrated geoinformatic approach. Environ Earth Sci, 77: 600

[11] Gopinath G, Swetha T V, Ashitha M K. (2014). Elicitation of erosional signature of a tropical river basin with high-resolution stereo data. App Geoma, 6(3): 149–157

[12] Gopinath G, Nair A G, Ambili G K, Swetha T V. (2016). Watershed prioritization based on morphometric analysis coupled with multi criteria decision making. Arab J Geosci, 9(2): 129

[13] Guarnieri P, Pirrotta C. (2008). The response of drainage basins to the late Quaternary tectonics in the sicilian side of the Messina Strait (NE Sicily). Geomorphology, 95(3−4): 260–273

[14] Hamdouni R E, Irigaray C, Fernández T, Chacón J, Keller E A. (2007). Assessment of relative active tectonics, southwest border of Sierra Nevada (Southern Spain). Geomorphology, 96(1−2): 150–173

[15] Horton R E. (1941). An approach toward a physical interpretation of infiltration capacity. Proc Soil Sci Soc Am, 5(C): 399–417

[16] Jesiya N, Gopinath G. (2018). A fuzzy based MCDM–GIS framework to evaluate groundwater potential index for sustainable groundwater management—a case study in an urban-periurban ensemble, southern India. Groundw Sustain Dev, 11: 100466

[17] KellerE A, Pinter N(2002). Active Tectonics: Earthquakes, Uplift, and Landscape (2nd ed). Upper Saddle River: Prentice Hall

[18] KumarB A, Gopinath G, Chandran M S S(2014). River sinuosity in a humid tropical river basin, south west coast of India. Arab J Geosci, 7(5): 1763−1772

[19] Kumar D, Duarah B P. (2019). Neo-tectonic signatures in the Mishmi Massif, Eastern Himalayas: an interpretation on the basis of the Lohit River Basin geometry. Arab J Geosci, 12(21): 665

[20] Kumar D, Duarah B P. (2020). Geomorphic signatures of active tectonics in Subansiri River Basin eastern Himalayas. J Mt Sci, 17(6): 1523–1540

[21] Manu M S, Anirudhan S. (2008). Drainage characteristics of Achankovil River Basin, Kerala. J Geol Soc India, 71: 841–850

[22] Marta D S, Maurizio D M, Paola F, Enrico M, Olivia N, Gilberto P, Tommaso P, Francesco T. (2008). Morphotectonic evolution of the Adriatic piedimont of the Apennines: an advancement in the knowledge of the Marche – Abruzzo border area. Geomorphology, 102(1): 119–129

[23] Martinez M, Hayakawa E H, Stevaux J C, Profeta J D. (2011). Sl index as indicator of anomalies in the longitudinal profile of Pirapó River. Geosciences, 30(1): 63–76

[24] Nair M M. (1990). Structural trendline patterns and lineaments of the Western Ghats, south of 13° Latitude. J Geol Soc India, 35: 99–105

[25] OzkaymakC, Sozbilir H(2012). Tectonic geomorphology of the Spildagi high ranges western Anatolia. Geomorphology, 173−174: 128−140

[26] KellerE A, Pinter N(1996). Active Tectonics, Earthquake Uplift and Landscape. Upper Saddle River: Prentice Hall

[27] Prasannakumar V, McCaig A M. (2016). Reactivation and strain localisation in Bhavani Shear Zone, South India. J Geol Soc India, 88(4): 421–432

[28] Prashant P M, Nirupama P M. (2016). Application of Hack’s stream gradient index (SL index) to longitudinal profiles of the rivers flowing across Satpura-Purna Plain, Western Vidarbha, Maharashtra. J Indian Geomorph, 4: 65–72

[29] Rai P K, Singh P, Mishra V N, Singh A, Sajan B, Shahi A P. (2019). Geospatial approach for quantitative drainage morphometric analysis of Varuna river basin, India. J Landsc Ecol, 12(2): 1–25

[30] Rajendran C P, John B, Sreekumari K, Rajendran K. (2009). Reassessing the earthquake hazard in Kerala based on the historical and current seismicity. J Geol Soc India, 73(6): 785–802

[31] Ramasamy S M, Kumanan C J, Selvakumar R, Saravanavel J. (2011). Remote sensing revealed drainage anomalies and related tectonics of South India. Tectonophysics, 501(1–4): 41–51

[32] Rekha V B, George A V, Rita M. (2011). Morphometric analysis and micro-watershed prioritization of Peruvanthanam sub-watershed, the Manimala River Basin, Kerala, South India. Environ Res Eng Manag, 57: 6–14

[33] Santosh M, Yang Q Y, Shaji E, Tsunogae T, Mohan M R, Satyanarayanan M. (2015). An exotic mesoarchaean microcontinent: the Coorg block, southern India. Gondwana Res, 27(1): 165–195

[34] SchummS A, Dumont J F, HolbrookJ M(2000). Active Tectonics and Alluvial Rivers. New York: Cambridge University Press

[35] SomanK(2013). Geology of Kerala. Bangalore: Geological Society of India

[36] StrahlerA N(1964). Quantitative geomorphology of drainage basins and channel networks. In: Chow V T, ed. Handbook of Applied Hydrology. New York: McGraw-Hill, 439−476

[37] Swetha T V, Gopinath G, Thrivikramji K P, Jesiya N P. (2017). Geospatial and MCDM tool mix for identification of potential groundwater prospects in a tropical river basin, Kerala. Environ Earth Sci, 76(12): 428

[38] Swetha T V, Gopinath G. (2020). Landslides susceptibility assessment by analytical network process: a case study for Kuttiyadi River Basin (Western Ghats, southern India). SN Applied Science, 2: 1776

[39] Vijith H, Satheesh R. (2006). GIS Based Morphometric analysis of two major upland subwatersheds of Meenachil River in Kerala. Photonirvachak (Dehra Dun), 34(2): 181–185

[40] Vijith H, Prasannakumar V, Sharath Mohan M A, Ninu Krishnan M V, Pratheesh P. (2017). River and basin morphometric indexes to detect tectonic activity: a case study of selected river basins in the South Indian Granulite Terrain (SIGT). Phys Geogr, 38(4): 360–378

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