Abstract

Drainages are pulses which in turn help us to understand the ongoing process in the hill ecosystem. The Kalrayan hill is known for its dissected terrain condition, rich biological diversity and depletion of natural resources. Therefore, a study on quantitative geomorphometry was carried out in the Kalrayan Hills, Eastern Ghats, Tamil Nadu, using Indian remote sensing 1D LISSIII satellite data. The study area was divided into 36 watersheds and total area is 1158.4 km2. It covers the upper part of Vellar basin. The linear, aerial and relief aspects and different morphometric parameters such as stream length, bifurcation ratio, drainage density, stream frequency, drainage texture, relief ratio, basin shape, form factor, circularity ratio, elongation ratio and length of overland flow were computed using standard methods, formulae and geo-spatial technologies. Based on the present drainage morphometric study, it is inferred that the watersheds 3, 4, 6, 9, 11, 12, 15, 17, 18, 19, 20, 22, 24, 27, 32, 33, 34 and 36 are active with reference to geological processes, mean denudational rate, peak discharge, mean annual run off, dominant watershed process and sediment yield per unit area. Multi-criteria analysis is performed to determine the drainage architecture and hydrogeological processes occurring in the present hill area.

Highlights

  • The study on basin hydrology is essential for proper management of water resources, and flood hazard in a basin depends upon the hydrological response of the upstream basin area

  • Drainage basin is a geohydrological unit area drained to a common point considering it as an ideal unit for analysis and management of natural resources and environmental planning in any ridge to valley treatment

  • The knowledge of basin hydrology is imperative for proper management of natural resources in general and water resources in particular

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Summary

Introduction

The study on basin hydrology is essential for proper management of water resources, and flood hazard in a basin depends upon the hydrological response of the upstream basin area. Drainage basin is a geohydrological unit area drained to a common point considering it as an ideal unit for analysis and management of natural resources and environmental planning in any ridge to valley treatment. The study of drainage characteristics through morphometric analysis of different watersheds in a region gives much information regarding the denudational history, sub-surface material, geological structure, soil type and vegetation status of that region, which play a crucial role in formulating a plan for watershed management.

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