Assessment of basin-scale geomorphic processes based on the analysis of longitudinal profiles: A case study of the Dwarkeswar river, Eastern India

ABSTRACTThe longitudinal profile of the river bears geomorphic signature of long-term fluvial adjustment to tectonic, structure, lithology, and climate. Therefore, analysis of the longitudinal profile can be helpful in understanding the fluvial process and the response of the river to regional geody...

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Main Author: Biman Ghosh
Format: Article
Language:English
Published: Taylor & Francis Group 2023-04-01
Series:Geology, Ecology, and Landscapes
Subjects:
Online Access:https://www.tandfonline.com/doi/10.1080/24749508.2023.2202434
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author Biman Ghosh
author_facet Biman Ghosh
author_sort Biman Ghosh
collection DOAJ
description ABSTRACTThe longitudinal profile of the river bears geomorphic signature of long-term fluvial adjustment to tectonic, structure, lithology, and climate. Therefore, analysis of the longitudinal profile can be helpful in understanding the fluvial process and the response of the river to regional geodynamics. The present study uses longitudinal profiles and related geomorphic indices, including the Stream Length-Gradient Index (SL Index) of the Dwarkeswar river and its nine major tributaries, to understand the role of regional geological structure and lithology on the landscape evolution of the basin and the stage of river-valley development. Four mathematical functions were used in the present study to fit the curves of the profiles, on the basis of which the sequence of evolution was estimated. The exponential function is the best fit, followed by the linear function for each river, indicating a dynamic equilibrium condition. Moreover, profile concavity and hypsometric integral were used in the present study to understand sediment generation and transportation dynamics. The lower concavity index in Arkasa, Beko river, and Debkhal rivers indicate that sediment production and transportation balance each other. All the indices and the shape of Hack’s profile indicate that the rivers are in non-graded condition. The concavity of the profile reveals that Dwarkeswar rivers is an energy-limited river with a lower sediment delivery ratio (SDR)(0.47). Other rivers of the basin have moderate to high SDR (0.61–0.78). The integration of the results with the geological data indicates that the segments with anomalously high values of the SL index correspond to the fault lines, lineaments, and lithological discontinuities.
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spelling doaj.art-76d9b00b939f4542afc2e94aeb22cabd2023-04-17T11:48:22ZengTaylor & Francis GroupGeology, Ecology, and Landscapes2474-95082023-04-0111710.1080/24749508.2023.2202434Assessment of basin-scale geomorphic processes based on the analysis of longitudinal profiles: A case study of the Dwarkeswar river, Eastern IndiaBiman Ghosh0Department of Geography, Visva-Bharati, A Central University, West Bengal, IndiaABSTRACTThe longitudinal profile of the river bears geomorphic signature of long-term fluvial adjustment to tectonic, structure, lithology, and climate. Therefore, analysis of the longitudinal profile can be helpful in understanding the fluvial process and the response of the river to regional geodynamics. The present study uses longitudinal profiles and related geomorphic indices, including the Stream Length-Gradient Index (SL Index) of the Dwarkeswar river and its nine major tributaries, to understand the role of regional geological structure and lithology on the landscape evolution of the basin and the stage of river-valley development. Four mathematical functions were used in the present study to fit the curves of the profiles, on the basis of which the sequence of evolution was estimated. The exponential function is the best fit, followed by the linear function for each river, indicating a dynamic equilibrium condition. Moreover, profile concavity and hypsometric integral were used in the present study to understand sediment generation and transportation dynamics. The lower concavity index in Arkasa, Beko river, and Debkhal rivers indicate that sediment production and transportation balance each other. All the indices and the shape of Hack’s profile indicate that the rivers are in non-graded condition. The concavity of the profile reveals that Dwarkeswar rivers is an energy-limited river with a lower sediment delivery ratio (SDR)(0.47). Other rivers of the basin have moderate to high SDR (0.61–0.78). The integration of the results with the geological data indicates that the segments with anomalously high values of the SL index correspond to the fault lines, lineaments, and lithological discontinuities.https://www.tandfonline.com/doi/10.1080/24749508.2023.2202434Longitudinal profileSL indexHack’s profileConcavity indexDwarkeswar basin
spellingShingle Biman Ghosh
Assessment of basin-scale geomorphic processes based on the analysis of longitudinal profiles: A case study of the Dwarkeswar river, Eastern India
Geology, Ecology, and Landscapes
Longitudinal profile
SL index
Hack’s profile
Concavity index
Dwarkeswar basin
title Assessment of basin-scale geomorphic processes based on the analysis of longitudinal profiles: A case study of the Dwarkeswar river, Eastern India
title_full Assessment of basin-scale geomorphic processes based on the analysis of longitudinal profiles: A case study of the Dwarkeswar river, Eastern India
title_fullStr Assessment of basin-scale geomorphic processes based on the analysis of longitudinal profiles: A case study of the Dwarkeswar river, Eastern India
title_full_unstemmed Assessment of basin-scale geomorphic processes based on the analysis of longitudinal profiles: A case study of the Dwarkeswar river, Eastern India
title_short Assessment of basin-scale geomorphic processes based on the analysis of longitudinal profiles: A case study of the Dwarkeswar river, Eastern India
title_sort assessment of basin scale geomorphic processes based on the analysis of longitudinal profiles a case study of the dwarkeswar river eastern india
topic Longitudinal profile
SL index
Hack’s profile
Concavity index
Dwarkeswar basin
url https://www.tandfonline.com/doi/10.1080/24749508.2023.2202434
work_keys_str_mv AT bimanghosh assessmentofbasinscalegeomorphicprocessesbasedontheanalysisoflongitudinalprofilesacasestudyofthedwarkeswarrivereasternindia