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Titlebook: Environmental Management of River Basin Ecosystems; Mu. Ramkumar,K Kumaraswamy,R. Mohanraj Book 2015 Springer International Publishing Swi

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GIS Based Quantitative Geomorphic Analysis of Fluvial System and Implications on the Effectiveness s of the host rocks and climatic effects. The resultant changes are exhibited by the geomorphic indices and landform assemblages within a river basin. This paper presents the results of integrated quantitative geomorphic analysis conducted for understanding the prevalent tectonic activities in a med
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Sand Mining, Channel Bar Dynamics and Sediment Textural Properties of the Kaveri River, South Indiadjoining its channel. In addition to its dwindling natural flow due to the failing monsoonal supply, and constructions of major, medium and minor dams, the extensive mining of sand from its channel bed causes severe stress on its natural fluvial processes. Reduction of carrying capacity of the chann
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Hydro-Geomorphology and Hydrogeology of the Pennar River Basin, India: Implications on Basin Scale ground water level variations, fluctuations and recharge. The landforms are classified into denudational, fluvio-denudational, fluvial, aeolian and coastal categories. Hydro-geomorphologically, the deltaic plains and fluvial plains are grouped under excellent ground water potential, irrigated plain
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Hydrogeochemical Drivers and Processes Controlling Solute Chemistry of Two Mountain River Basins of Basin (PRB) during monsoon (MON), post-monsoon (POM) and pre-monsoon (PRM) seasons, and were analyzed to understand the spatio-temporal variability as well as the sources and processes controlling hydrogeochemistry. In MRB and PRB, Ca. and Mg. dominate the cations, while Cl. dominates the anions in
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A Review on the Riverine Carbon Sources, Fluxes and Perturbations,ystems is a key link in the global carbon cycle. Rivers also provide a key link in the geological scale carbon cycle. Nevertheless, an appreciation of their roles is yet to be made. Even when their roles are included, data are drawn only from selected large rivers, often neglecting the small mountai
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