Water Resources Development In Central Part Of India By Arthee.V Bte-06-004.

Slides:



Advertisements
Similar presentations
Social Studies Chapter 1: Our Nation’s Geography
Advertisements

Phosphorus Loads from Streambank Erosion to Surface Waters in the Minnesota River Basin D. J. Mulla Professor, Dept. Soil, Water, Climate University of.
What is a watershed? A watershed is the area of land where all of the water that is under it or drains off of it goes into the same place – either a.
Fresh Water Historically limiting factor in arid regions World population more than doubled 2.3 billion  5.3 billion Per capita water use doubled.
Flood Management in GBM Basin: A Mechanism for Natural Resource Management Between Co-riparians Priyanka Mallick JNU.
MAJOR LANDFORMS OF INDIA
THE PENINSULAR PLATEAU
Engineering Hydrology (ECIV 4323)
National Action Plan for Climate Change Support for the National Water Mission.
Relevance of Marketing Concepts to Indian Companies
Engineering Hydrology (ECIV 4323)
By Bimal Kumar Mishra Managing Director FISHCOPFED INDIA
‘The world’s greatest plumbing system’ An example of how a river is managed to use its water as a resource.
Welcome! The Topic For Today Is…
Transboundary supply issues
1 Module 2 Mekong Resources, Benefits to people, and Planning Issues session 1 : The Mekong and its water resources.
10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt
Sustainable Renewable Energy for Rural Areas
Hydro electric (Hydel) Power Plant
SOCIO-ECONOMIC IMPACT OF DROUGHT IN INDONESIA 2003 AND ITS HANDLING IN ACCORDANCE WITH POVERTY ALLEVIATION APPROACHES NATIONAL COORDINATING BOARD FOR.
13A.2 – California’s Water Resources
Exeter 8/12/00.
Neotech Institute of technology Department of Civil Engineering
RAVINDRA THOSAR RATE AGREEMENT TEAM.  Floods and drought have become a recurring problem in India and the project is aimed at improving the situation.
Hydro Electric Power Plant
ESET ALEMU WEST Consultants, Inc. Bellevue, Washington.
Chapter 33 Dam Construction. Objectives After reading the chapter and reviewing the materials presented the students will be able to: Give reasons why.
 Done by :KHODJAEVA D  Checked by: Halimova F.  The Aral Sea: the tradegy of the drying sea.
CE 424 HYDROLOGY 1 Instructor: Dr. Saleh A. AlHassoun.
Diversion of Flood Water from Ganga at Kanpur.  Introduction  Study Area  Flow Pattern of Ganga at Kanpur  Quantification of Divertible Flood  Downstream.
Engineering Hydrology (ECIV 4323)
Hydrosphere The hydrosphere includes all water on Earth. The abundance of water on Earth is a unique feature that clearly distinguishes our "Blue Planet"
Its Physical divisions
Choose a category. You will be given the answer. You must give the correct question. Click to begin.
El Gallo Hydroelectricity Project PDD Analysis
Chapter 2 – A Land Called Texas Section 1 – The Physical Landscape of Texas.
Prevention and Cure. Contents Introduction to Reservoirs Preventing Siltation Cure Cost Benefit Analysis Conclusion.
Beas River.
ICAP SAFA Conference 2016 South Asia: Corridor of Opportunities Lahore, January 30, 2016 Mirza Hamid Hasan.
BASIN SCALE WATER INFRASTRUCTURE INVESTMENT EVALUATION CONSIDERING CLIMATE RISK Yasir Kaheil Upmanu Lall C OLUMBIA W ATER C ENTER : Global Water Sustainability.
WATER AVAILABILITY. Total availability of water in earth-1.37X18 8 M ha m Fresh water – 2.8 % Saline water – 97.2% Surface water – 2.2% Groundwater- 0.6%
Why river linking project in India INDIA having total land area is 3,287,263 sq km in this Irrigated land is only 558,080 sq km, rest of the land are un.
Group Members Tevin Walker Deidre Brown. Objectives Define the term HYDROELECTIC ENERGY To identify the use/importance of this energy source To explain.
Stakeholder Engagement and Capacity Building in context of IWRM PROF A K GOSAIN SANKALP LAHARI (RESEARCH SCHOLAR) IIT DELHI – CWC – EWATER.
Rain Water Conservation by Sita Ram Singh, FNA, FNAE, FNAAS.
THE COASTAL PLAINS. THE COASTAL PLAINS Coastal plains are characterized by an area of flat low lying land that is situated adjacent to a water body often.
The Chesapeake Bay: How is it Doing? An Overview of The Chesapeake Bay Watershed.
Chapter 9: Surface Water BIG IDEA: Surface water moves materials produced by weathering and shapes the surface of the Earth.
MULTIPURPOSE RIVER VALLEY PROJECT.
NATIONAL HYDROLOGY PROJECT CENTRAL WATER COMMISSION.
Lecture-19: GEOGRAPHY OF BANGLADESH. Geographical Settings of Bangladesh The major natural assets of Bangladesh are its access to the open ocean, the.
Dr. B.P Das Expert Consultant FAO, UN Former Engineer In Chief & Chief Advisor Department of Water Resources, Odisha Former Vice Chairman, EAC for River.
East Asia Physical Geography. Main idea O East Asia’s landforms, bodies of water, and climate influence where people live.
WATER RESOURCES DEPARTMENT
CHAPTER 1: THE WORLD.
WELCOME!. AISHA BAWANY ACADEMY GIRLS MATRIC SECTION ISA PROJECT IN COLLABORATION WITH BRITISH COUNCIL.
Interlinking of rivers as an adaption strategy to address the impact of climate change on water resources Sustainable Lifestyle = Positive.
Dams in Jordan, a fresh resource to think about!
ASSESSMENT OF ENVIRONMENTAL FLOWS FOR THE TAPI RIVER BASIN, INDIA
Engineering Hydrology (ECIV 4323)
GANDHINAGAR INSTITUTE OF TECHNOLOGY
Preciptation.
Engineering Hydrology (ECIV 4323)
DRIANAGE SYSTEM OF INDIA
The Southern Plateaus The Central Highlands the north
Hydrology CIVL341 Introduction
You will be given the answer. You must give the correct question.
Engineering Hydrology (ECIV 4323)
Chapter Four RUNOFF When a storm occurs, a portion of rainfall infiltrates into the ground and some portion may evaporate. The rest flows as a thin sheet.
Presentation transcript:

Water Resources Development In Central Part Of India By Arthee.V Bte

Introduction:  Situated in the centre of India  It is the largest geographic unit of the country  average rainfall of 76 to 150 cm  Narmada, Tapti, Mahanadi, and Mahi  Sub-catchments -the Ganga, Yamuna, Godavari and Brahmani rivers.  Rivers originating from the highlands of Madhya Pradesh drain out in three different directions.

Narmada basin with its mainstream runs across the State from east to west, receiving tributaries on either side The Mahanadi flows eastwards and the Tapti cuts across the State diagonally in a southwesterly direction to enter the Bay of Bengal. The rivers, tributary, rivulet and streams in the State have a combined length of km.

During the monsoons, all the rivers in Madhya Pradesh turn into raging torrents, carrying enormous quantities of water. During the dry season, they shrink to rivulet. Thus, harnessing of water for irrigation and power generation is more relevant in the State, than anywhere else in India and its track record in tapping the water resources has been impressive.

RESERVOIR RESOURCES OF MADHYA PRADESH Madhya Pradesh, with its 0.46 million ha of reservoirs, has the maximum waterspread under man-made lakes of all Indian States. Gandhisagar reservoir is the second largest reservoir (in area) in the country.

Description of 32 reservoirs comprising 6 small, 21 medium and 5 large (Fig. 7.1), covering a total area of ha, is available. The average size of these small, medium and large reservoirs is 350, and ha respectively

Average size of different categories of reservoirs CategoryTotal Area (ha ) Number on units, areas of which are known Area (ha)Average of a unit (ha) Small Medium Large TOTAL

GANDHISAGAR RESERVOIR Gandhisagar reservoir is impounded on the river Chambal, which is the largest tributary of Yamuna, a component of the Ganga river system The river, at the dam site, receives catchment from the Vindhya ranges in the south and Aravalli in the northeast, covering a drainage area of km2. Gandhisagar is one among the four hydraulic structures conceived as a part of the Integrated Chambal Development Programme, the other three being Ranapratapsagar, Jawaharsagar and the Kota barrage

Gandhisagar is the best-managed reservoir in the State for fisheries. stocking, though inadequate has been regular ever since the programme was iniated in 1959–60 (Table 7.4). The impact of stocking has been phenomenal. The fish yield from the reservoir fluctuated from 0.51 kg ha-1 during 1962–63 to the level of 12 to 13 kg ha-1 during 1978–79 and 1979–80

The State Government plans to increase the stocking rate to 200 ha-1 to achieve a target of to t (40 to 60 kg ha-1 ).

Mode of exploitation The fishing rights for the reservoirs were handed over to a public sector corporation in Prior to that, fishing was done either by the cooperative societies or a group of fishermen from whom a royalty ranging from Rs to Rs was charged by the Government. The royalty rate varied with fish groups.

There were two types of cooperative societies, viz., the primary cooperatives and apex society The royalty system had many drawbacks, the fishermen did not get adequate income. middlemen and merchants made considerable profit. the cooperatives could not effectively undertake the market functions, and non-payment by the merchants/societies deprived the Government of its income in the form of royalty. It is estimated that while the Government earned Rs.2.87 million on royalty, more than one million was spent on its collection.

Since 1980, the Madhya Pradesh State Fisheries Development Corporation (MPSFDC), a public sector undertaking has taken over the functions of the apex cooperatives. The primary societies are now actively involved in fishing, their members fishing on a catch-sharing basis.

3 RAVISHANKARSAGAR Ravishankarsagar reservoir was formed in 1978, on the river Mahanadi, at 20° 38' N, 81° 34' E, 92 km south of the city of Raipur. A multi-purpose reservoir, serving irrigation, hydro-electric power-generation and the industrial requirements Steel Plant,. The lowest water spread during the lean season is ha. Total catchment area is estimated at km2, of which 625 km2 is intercepted by the upstream dam,). At full level, the reservoir holds 909 million m3 of water (mean depth of 9.53 m). Maximum depth is 32 m.

. One salient hydrographic feature of this reservoir is the continuous drawdown for industrial, irrigation and hydel purposes. Water level fluctuates by 3 to 5 m in a year The sediments of Ravishankarsagar is poor in nutrients and organic matter. With respect to the available nitrogen (12 to 30 mg 100 g-1) and organic carbon (0.2–1.2%), the reservoir has a low productivity, but the level of phosphorus (2.7 to 8.0 mg 100 g-1) suggests a high productivity.