Eastern Plateau

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No rain, no grain - A film by Video Volunteers
Agriculture is the backbone of the Indian Economy. India is a huge exporter of various agricultural products such as rice, pulses, sugar, oil, etc.
Mukesh Rajak
Posted on 12 Jul, 2011 10:30 AM

 

 
Development of regional flood frequency relationships using L-moments for South Bihar – A research report by the National Institute of Hydrology
In this study, regional flood frequency relationships have been developed using L-moments for the alluvial plains of Indo-Gangetic basin and Kaimur-Chhotanagpur Santhal Pargana plateau.
National Institute of Hydrology
Posted on 14 Jul, 2010 10:55 PM

In this study, regional flood frequency relationships have been developed using L-moments for South Bihar, in the alluvial plains of Indo-Gangetic basin and Kaimur-Chhotanagpur Santhal Pargana plateau. The annual maximum peak flood data of twenty-two gauging sites whose catchment areas vary from 11.7 to 3171 sqkm have been used. The mean annual peak floods of these sites vary from 29.15 cumec to 1293.2 cumec. Comparative regional flood frequency analysis studies have been carried out using some of the commonly used frequency distributions viz Extreme Value (EV1), General Extreme Value (GEV), Normal, Log Pareto (GPA) and Wakeby based on L-moments approach.

A study of saline freshwater interface phenomenon in the Mahanadi delta region, Orissa
The subsurface aquifer systems in Mahanadi delta region in Orissa (India) is largely characterized by two groups of freshwater aquifer systems: 1. The south western Mahanadi delta region is represented by unconfined to semi-confined freshwater aquifers underlained by brackish/ saline aquifer systems with a diffusion boundary 2. The north eastern parts of Mahanadi delta is represented by deep freshwater confined aquifers overlained by brackish/saline water aquifers with aquitard/ aquiclude boundary. Both the systems are prone to saline water mixing/ migration with time and development. The present paper incorporates results of a simulation study using a finite element based FEFLOW model and examines saline water migration scenarios when subjected to increasing rates of pumping under steady state conditions with the help of a calibrated groundwater model. The results indicate the unconfined and semi-confined aquifer systems in the south western part of Mahanadi delta are prone for faster rates of saline water mixing of the contamination when compared to the deep confined systems in the north eastern parts of Mahanadi delta.
SVN Rao
I Radhakrishna
Nitin Joshi
Ajay Sharma
Shashank Sharma
Posted on 02 Jul, 2010 04:47 PM

ABSTRACT
Watershed scale planning- Application of rainwater harvesting techniques
Two examples of a watershed scale application of rainwater harvesting techniques.
rajshekar
Posted on 15 Sep, 2009 04:20 PM

The first project was conducted by the BAIF Development Research Foundation in the Hassan District of Karnataka. They created a linked network of 350 farm ponds covering 700 hectares of the watershed.

Impact of climate change in India: An agro - ecological zone level analysis
A detailed look at the possible impacts of climate change on the different agro - ecological zones demarcated in India
Rama Mani
Posted on 20 Aug, 2009 06:04 PM

India is gifted with heterogeneous landforms and variety of climatic conditions such as the lofty mountains, the raverine deltas, high altitude forests, peninsular plateaus, variety of geological formations endowed with temperature varying from arctic cold to equatorial hot, and rainfall from extreme aridity with a few cms (<10 cm) to pre humid with world's maxim
India - Physical Map from the Survey of India (2002)
A definitive physical features map of the country from the Survey of India, showing elevation in metres of different regions and major rivers and land formations.
Survey of India
Posted on 18 Aug, 2009 05:35 PM

Download the map from the attachment listed below:
Geographic information system (GIS) and groundwater for windows (GWW) helps in creating interactive groundwater information system (GWIS) of Barakar basin in Bihar
The paper discusses the approach adopted for establishing groundwater information system (GWIS) where data from various sources can be stored and analysed in time and space
Ashok Kumar
B. B. Prasad
L. B. Prasad
Nisha Mendiratta
Posted on 20 May, 2009 10:21 AM

This paper on the GIS Development site discusses the approach adopted for establishing ground water information system (GWIS) of the Upper Barakar Basin using geographic informati
Groundwater modeling of unconfined aquifer system of crystalline area - a case study in Lapsiya watershed (Hazaribagh)
The paper concludes that the success of unconfined aquifer system in a hard rock area depend upon the thickness of the aquifer material
Ashok Kumar
Posted on 20 May, 2009 10:18 AM

This paper on the GIS Development site discusses the findings of a  modeling exercise that was attempted in Lapasiya watershed, Hazaribagh, India.
Groundwater prospects analysis through hydrogeophysical parameters and hydrogeomorphic zonation - a case study in parts of Kewta watershed - upper Barakar basin - Bihar
The study integrates hydrogeomorphic and hydrogeophysical approach for groundwater exploration for Kewta watershed, upper Barakar basin, Bihar
Ashok Kumar
Savita Tomar
L.B. Prasad
Posted on 19 May, 2009 01:43 PM

 In this paper from the GIS Development site present study, hydrogeomorphic zonation has been carried out through remote sensing technique.
Analysis of hydrogeophysical properties of aquifer and reserve estimation for sustainable development of groundwater in Kewta watershed, Hazaribagh, Bihar
Several sub-surface basins/ underground reservoirs, can be used for groundwater storage and retrieval which has storage capacity to irrigate 50 per cent geographical area of Kewta watershed
Ashok Kumar
B. B. Prasad
L. B. Prasad
Savita Tomar
Posted on 19 May, 2009 01:39 PM

In this study from the GIS Development site,  the hydrogeophysical parameters generated from vertical sounding, geohydrological, inferred fractures and geomorphic zones derived from remotely sensed data have been analysed in Kewta watershed of upper Barakar Basin, Hazaribagh. The study area is part of lower Hazaribagh plateau and is part of pediplain developed over Chotanagpur granite gneiss and meta- sedimentary.

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