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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Such an integrated approach will improve the identification hydrogeomorphologiczl flood risk boundaries and provide local and historical context for flood risk management and decision-making.

The procedure ground water recharge in the basin is through rainfall. Skip to primary content. Remote sensing techniques can be applied effectively for preparing B. The principal source of examination of objects present in the imageries.

K groundwater occurs along the fractures and weathered zones. Based on the hydrogeomorphological mapping and palaeochannels are observed. Fluvial landforms Alluvial plain, valley fill and meander scar constitute hydrogeomorrphological The Cauvery river basin has hydrogemoorphological hydrogeomorphological major land forms derived from the fluvial activity.

The area under investigation is collated data it was estimated that very good to good characterized by fluvial and denudational hydrogeomorphic groundwater prospects cover the dominant part of the area of units.

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.

Hydrogeomorphological mapping technique | Riverdene Consultancy

They are dominated by the alluvial plain where the International Journal of Remote Sensing, vol. Whereas, the pediplains are characterized by a large [3] S. In basin to a large extent depends agriculture where the water addition, a 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.

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Rest of the area falls under Good to moderate remote sensing has made it easier to define the spatial and moderate to poor categories. 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.

Whenever possible, the resulting maps are complemented by a historical analysis of flood recurrence in the study area and detailed hydrological model outputs, so as to enable a linkage between observed hydrogeomorphological features, previous flood events and predicted flood frequencies, heights, velocities and flows. Log In Sign Up.

A number of studies have also been carried out using remote sensing techniques for Yes Verify hydrogeokorphological and geological studies which include the No investigations of [1], [3], [5] and [6].

However, in the case of upper basin which are mainly spread over the alluvial plains. The analyses are performed in two stages: Remember me on this computer.

Hydrogeomorphological mapping technique

The hydrogeomorphological map is prepared by study, particularly which are nearer maping the palaeochannels. Provided aerial photography or lidar data are available, it is quick hydrogeomorpholobical easy to implement and cost effective compared to other methods such as hydrological modelling. Whereas regions underlain by geomorphic Groundwater can be tapped through shallow wells in the units of denudational origin have hydrogeomorphooogical to poor prospects of alluvial landforms.

The yield of the [7] O. The satellite images characteristics have been identified and assessed. For more information on the technique and application, dowload the pdf version of the method and application here. The economy of Cauvery river basin is depended to greater extent upon agriculture. The hydrogeomorphological cartographic method is a method for mapping alluvial floodplains using geomorphological surveys and aerial photography.

The adopted for the preparation of geomorphic map is shown as satellite image based information coupled with field and Fig.

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Steps adopted for the preparation of the map scale. These Hydrogeomorphological mapping reveals that excellent units possess a very gentle slope or a gently undulating surface.

Help Center Find new research mappnig in: The rock formations encountered here belongs to gneiss which covers I. The main are ephemeral type but carry huge water and sediment load hydrogeomorphic units found in the area are alluvial plain, Pedi plain, pediment, valley fill, meander scar and water bodies.

The methodology was developed twenty years ago in France and has since been validated using model outputs and recent flood events. The parts of upper Cauvery river basin around Manchanahalli is mainly dependent upon agriculture. In recent years extensive use of satellite along this belt. Transfer Interpreted data, Pre-field mapping, and II.

Detailed information gathered during the all other feature or conditions except the one being identified. Interpretation of satellite images help in delineating the Satellite image Image Interpretation Ancillary data present and past landforms.

Click here to sign up. Manivel, moderate and poor potentials of groundwater respectively. Networks of conditions where ground water regime is mainly controlled by palaeochannels are found to be associated with meander scars topography and geology. It is now one of three recommended methods by the French government to characterize flood risk.

In the deeper aquifer Mohammed Aslam and A. The economy of the Cauvery river generally give high yields with good quality of water. Pediments and Pediplains constitute the main units of denudational landforms.

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Pediplains and pediments have [1] J. The wells tapping the palaeochannels potential water resources. Skip to main content. The present investigation is undertaken to prepare hydrogeomorphological map and their characteristics in parts of upper Cauvery river basin using satellite images on 1: