Geo-spatial technique-based approach on drainage morphometric analysis at Kalrayan Hills, Tamil Nadu, India

被引:21
|
作者
Sakthivel, R. [1 ]
Raj, N. Jawahar [2 ]
Sivasankar, V. [3 ,4 ]
Akhila, P. [1 ]
Omine, Kiyoshi [3 ]
机构
[1] Bharathidasan Univ, Sch Geosci, Dept Geol, Tiruchirappalli 620024, Tamil Nadu, India
[2] Natl Coll, Post Grad & Res Dept Geol, Tiruchirappalli 620001, Tamil Nadu, India
[3] Nagasaki Univ, Sch Engn, Dept Civil Engn, 1-14 Bunkyo Machi, Nagasaki 8528521, Japan
[4] Pachaiyappas Coll, Post Grad & Res Dept Chem, Chennai 600030, Tamil Nadu, India
关键词
Basin hydrology; Morphometric parameters; Water resource management; Kalrayan hills; Multi-criteria analysis; SUBWATERSHEDS; CHEMISTRY; DISTRICT; BASINS;
D O I
10.1007/s13201-019-0899-7
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
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 1158.4km(2). 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.
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页数:18
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