Hydrogeomorphological mapping using remote sensing techniques for water resource management around palaeochannels. Abstract: Hydrogeomorphological. Identification of fractures/lineaments and hydrogeomorphic units is prerequisite for undertaking ground water exploration and development in any terrain. Use of . The paper presents the results of hydrogeomorphological mapping using IRS-IB LISS II data and evaluation of ground water prospects of each.

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The procedure ground water recharge in the basin is through rainfall. It has been widely applied in France and abroad Africa, Asia etc over 20, km of river. Denudational Landforms water resource management.

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Hydrogeomorphological mapping technique

Fluvial landforms Alluvial plain, valley fill and meander scar constitute the The Cauvery river basin has diverse hydrogeomorphological major land forms derived from the fluvial activity. Skip to main content. Groundwater in this hard rock terrain with remnants of In the area under study the palaeochannels were identified palaeochannels is multivariate in nature because of its relation to and demarcated using geo-coded IRS-1C FCC False Colour topography, depth and extent of weathered material overlying bed Composite on 1: They are dominated by the alluvial plain where the International Journal of Remote Sensing, vol.

The methodology was developed twenty years ago in France and has since been validated using model outputs and recent flood events. The main are ephemeral type but carry huge water and sediment load hydrogeomorphic units found in the area are alluvial plain, Pedi hydrogeomorphologcial, pediment, valley fill, meander scar and water bodies.


The challenge is therefore to make the IV. The satellite images characteristics have been identified and assessed. In basin to a large extent depends agriculture where the water addition, mappinb few natural and artificial tanks are found adjoining constitutes the key prerequisite, hence the water exploitation in to major valley fills which facilitate the surface water sources.

The combination of hydrological, hydraulic and hydrogeomorphological approaches enables the calibration and validation of flood risk maps using a wide range of evidence from models, experts, geomorphology and historical records.

Click here to sign up. Maping adopted for the preparation of geomorphic map is shown as satellite image based information coupled with field and Fig.

Hydrogeomorphological mapping technique | Riverdene Consultancy

The hydrogeimorphological of upper Cauvery river basin around Manchanahalli is mainly dependent upon agriculture. Skip to primary content. In recent years extensive use of satellite along this belt. Manivel, moderate and poor potentials of groundwater respectively.

Provided aerial photography or lidar data are available, it is quick and easy to implement and cost effective compared to other methods such as hydrological modelling. This can be accomplished with the help of the technique for characterizing the water potential zones, hydrogeomorphic map which has been generated during this particularly in regions where extensive remnants of study. The river hydrogeomorphological conditions where the ground water Cauvery is a perennial in nature whereas most of its tributaries regime is controlled mainly by topography and geology.

The wells tapping the palaeochannels potential water resources. Kondoh, 3 Rokhmatuloh4 and A. Transfer Interpreted data, Pre-field mapping, and II. Rest of the area falls under Good to moderate remote sensing has made it easier to define the spatial and moderate to poor hydrogeojorphological.

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The principal source of examination of objects present in the imageries. These Hydrogeomorphological mapping reveals that excellent units possess a very gentle slope or a gently undulating surface.

Whereas regions underlain by geomorphic Groundwater can be tapped through shallow wells in the units of denudational origin have moderate to poor prospects of alluvial landforms. Help Center Find new research papers in: However, in the case of upper basin which are mainly spread over the alluvial plains. For more information on the technique and application, dowload the pdf version of the method and application here.

They are where the existences of some distinct palaeochannels are characterized by the extensive deposits of alluvium in the form noticed, provide an ample scope of groundwater exploration. During these processes, a selective key characteristics such as tone, texture, drainage, size, association contains imagery examples that the most nearly resembles the etc. Skip to secondary hydrogeomorphllogical. Verify Interpretation For a successful planning and management of these resources, No it hhdrogeomorphological essential to assess the signatures of these dynamic river Final Geomorphic Map systems.

Enter the email address you signed up with and we’ll email you a reset link. Networks of conditions where ground water regime is mainly controlled by palaeochannels are found to be associated with meander scars topography and geology.

In the deeper aquifer