Exec Summary

Total Page:16

File Type:pdf, Size:1020Kb

Exec Summary STUDY ON PLANNING OF WATER RESOURCES OF RAJASTHAN Executive Summary Project Background The State Water Policy of Government of Rajasthan, February 2010, provides for development of its Water resources in a well planned way. All new projects shall be planned based on micro watershed planning basis so as to ensure equity in use of surplus water. It is on this account that the Government of Rajasthan took up study to review and update all River Basin Master Plans for the integrated development and management of all its water resources. In this connection necessary provision of funds were made in EC funded State Partnership Program (SPP) under implementation in Rajasthan State. The earlier comprehensive study on water planning for different river basins in Rajasthan State was carried out by TAHAL-WAPCOS Consultants during year 1994-1998. This study was considered quite old and had much reduced relevance in today’s context. The present study therefore envisages to take-up review and fresh planning of all the water resources of Rajasthan based on updated water resources data and modern techniques now available in this field of study encompassing all necessary provisions made in the new water policy of the State Government. The purpose of this assignment is to prepare a long term plan and policy for development and management of the water resources of the State of Rajasthan, both surface (internal and external) and ground water, on comprehensive and integrated basis. The period of planning envisaged is 2010-2060. Scope of Work 1. Data Collection 2. Analysis of Agroclimatic Zone wise hydrology, temperature over a period of 20 years, find all changes in precipitation, no. of rainy days, rainfall intensity, temperature, humidity and the impact on water resources, cropping pattern and productivity and suggest futuristic strategies for water uses, cropping pattern, in view of the changes. 3. Study the basin wise / sub-basin wise water availability (at various dependabilities) both surface and ground water (including interstate share of Rajasthan from Ravi, Beas, Satluj, Chambal, Mahi and Yamuna Water), indicate changes as compared to the earlier TAHAL-WAPCOS Study with reasons for change. 4. Carry out detailed study of the catchment areas of all major, medium and minor irrigation projects, identify the WHSs constructed and the watershed works carried out and mark the same on GIS mapping with requisite hydrological details and assess their impact on water flows to the project, study the transevaporation of these small water bodies and resultant water loss, their impact on ground water recharging and suggest a future policy for construction of such structures in the catchment area. 5. Agroclimatic Zone wise ground water basins studies, delineation of aquifers on microshed basis, marking them on the GIS mapping Panchayat Samiti wise Report # 4.9 – IN-24740-R13-080 October, 2014 Integrated State Water Resources Plan Executive Summary Page i STUDY ON PLANNING OF WATER RESOURCES OF RAJASTHAN and Village wise, based on the present exploitation and recharging of aquifers compute the remaining life of the aquifer so that this information could be disseminated Panchayat Samiti & Village wise. 6. Estimate the quantity of Water Pollution (Rivers, Industrial, Municipal etc.) Source wise, District wise and indicate costs of reclamation / treatment and possible uses. 7. Prepare Districtwise and Blockwise plans of supply and demand of water for various uses, crops, strategies to fill gap and estimated costs. 8. Identification of new projects in water surplus basins based on scientific study and survey and based on socio economic viability criteria. 9. Identification of projects for rehabilitation and/ or modernisation for existing major and medium projects based on socio economic viability criteria. 10. Preparation of comprehensive full scale integrated water resources plan for the State as a whole. 11. Imparting training to the staff and officers of SWRPD & WRD on planning and on use of software used in the study. Integrated State Water Resources Plan This report on Integrated State Water Resources Plan is the last one in the series of nine Final Reports. The objective of this report is to present a comprehensive full scale integrated plan for the State as a whole as well as to summarize the various aspects covered under other reports of this study on Planning of Water Resources of Rajasthan State and their conclusions and recommendations in form of an Action Plan highlighting responsible agencies for execution of the plans. Project Related Features of Rajasthan Rajasthan is the largest state in the Indian Union, with an area of 342,264 km 2. It is located in northwest India between longitudes 69°29’ and 78°17’ East and latitudes 23°30’ and 30°11’ North. The Tropic of Cancer passes through Rajasthan south of Banswara town. Rajasthan features a variety of landforms, which have resulted from erosional and depositional processes over a long geological time period. Four major physiographic divisions have been identified in the State: • Aravalli Hill Ranges, • Eastern Plains, • The Thar Desert, and • The South Eastern Plateau. The topography, rainfall, and geology are the most important factors affecting the extent and orientation of drainage, in Rajasthan in general and within a basin in particular. Report # 4.9 – IN-24740-R13-080 October, 2014 Integrated State Water Resources Plan Executive Summary Page ii STUDY ON PLANNING OF WATER RESOURCES OF RAJASTHAN The geological sequence of the State is highly varied and complex, showing the co- existence of the most ancient rocks of Pre-Cambrian age and the most recent alluvium, as well as wind-blown sands of Quaternary to Recent age. A total of 19 hydrogeological units have been identified on the basis of CGWB and RGWD data base. The significant and mapable hydrogeological units are considered to serve the purposes of water resources planning. The hydrogeological units were delineated using water-bearing formation data of CGWB and RGWD. The same have been delineated on micro-watershed, using GIS, and also panchayat samiti-wise (block-wise) and village-wise. Major 19 Hydrogeological Formations and their Areas in Rajasthan S. No. Hydrogeological Units / Hills Area, Km 2 1 Younger Alluvium 48,070.05 2 Older Alluvium 94 ,968.09 3 Tertiary Sandstone 24,502.65 4 Deccan Traps (Basalt) 9,580.51 5 Jurassic Sandstone (Lathi, Parihar, Baisakhi, Bhadesar) 15,213.07 6 Vindhyan Sandstone (Nagaur, Jodhpur) 25,675.64 7 Bilara Limestone 9,522.51 8 Bhander Sandstone 13,954.29 9 Limestone (Alwar, Bhander, Upper Cretaceous) 4,853.08 10 Shale 3,906.68 11 Quartzite 5,325.02 12 Slate 367.65 13 Phyllite & Schist 35,728.18 14 Gneisses 1,967.40 15 Jalore Granite 5,612.72 16 Erinpura Granite 5,229.75 17 Rhyolite 5,046.40 18 Ultra Basics 107.72 19 Gneisses(B.G.C.) 21,724.31 20 Hills 10,908.08 Total 342,263.80 Climate Average annual rainfall of the state is 604 mm and average annual monsoon rainfall is 531 mm. The state has large variance in the climatic conditions. The distribution of rainfall, both over time and area, is highly uneven and erratic. The extreme hydrological events, floods and droughts, are usual features for the State. The maximum temperature is highest in (37.4°C) the pre-monsoon season, while it is lowest (25.7°C) in cold weather season. Mean annual maximum temperature in Rajasthan is 33.2°C with a range of 25.7°C - 35.0°C. Minimum temperature attains its Mean highest value (25.1°C) during monsoon season, while it attains its Mean lowest value (9.6°C) in cold weather season. Mean annual Minimum temperature within Rajasthan is 19.1°C with a range of 11.8°C - 21.8°C. Report # 4.9 – IN-24740-R13-080 October, 2014 Integrated State Water Resources Plan Executive Summary Page iii STUDY ON PLANNING OF WATER RESOURCES OF RAJASTHAN Highest Maximum temperature attains its maximum value during Pre-Monsoon season (44.7°C) while it is lowest during Cold Weather season (34.6°C). Lowest Minimum temperature attains it lowest value during Cold weather (1.2°C) while it is highest during Monsoon season (17.8°C). The highest mean monthly rainfall occurs in the middle months of July and August, with 198.4 and 164.0 mm respectively in each month, contributing about 67.1% of the annual rainfall, while June and September rainfalls contribute 10.5% and 14.0%, respectively. It is observed that contribution of the other three seasons to annual rainfall is marginal. Winter, pre-monsoon and the post-monsoon seasons contribute 2.2%, 3.4% and 2.8%, respectively. Evaporation in Rajasthan is highly variable, both in spatial and temporal terms. Annual evaporation ranges from 140 cm to over 300 cm over the State. Values exceeding 300 cm occur over western Rajasthan (observed at the IMD weather station in Jaisalmer), which mainly comprises a desert area. It is generally the highest during May (when it ranges from about 26 cm to 43 cm) over most parts of the State and continues to be high in June too. The minimum usually occurs in December and January, when evaporation ranges from about 4 cm to 12 cm per month. Relative humidity follows a sinusoidal pattern, decreasing from 54.7% in January to a minimum of 30.5% in April, increasing to a maximum of 72.6% in August, and again decreasing to 48.4% in October. Trend analysis of different weather parameters have been studied during the past 20 years and impact of change in weather parameters on cropping pattern, productivity and water resources and future strategies in view of change in weather have been presented in detail in Final Report No.
Recommended publications
  • Forest of Madhya Pradesh
    Build Your Own Success Story! FOREST OF MADHYA PRADESH As per the report (ISFR) MP has the largest forest cover in the country followed by Arunachal Pradesh and Chhattisgarh. Forest Cover (Area-wise): Madhya Pradesh> Arunachal Pradesh> Chhattisgarh> Odisha> Maharashtra. Forest Cover (Percentage): Mizoram (85.4%)> Arunachal Pradesh (79.63%)> Meghalaya (76.33%) According to India State of Forest Report the recorded forest area of the state is 94,689 sq. km which is 30.72% of its geographical area. According to Indian state of forest Report (ISFR – 2019) the total forest cover in M.P. increased to 77,482.49 sq km which is 25.14% of the states geographical area. The forest area in MP is increased by 68.49 sq km. The first forest policy of Madhya Pradesh was made in 1952 and the second forest policy was made in 2005. Madhya Pradesh has a total of 925 forest villages of which 98 forest villages are deserted or located in national part and sanctuaries. MP is the first state to nationalise 100% of the forests. Among the districts, Balaghat has the densest forest cover, with 53.44 per cent of its area covered by forests. Ujjain (0.59 per cent) has the least forest cover among the districts In terms of forest canopy density classes: Very dense forest covers an area of 6676 sq km (2.17%) of the geograhical area. Moderately dense forest covers an area of 34, 341 sqkm (11.14% of geograhical area). Open forest covers an area of 36, 465 sq km (11.83% of geographical area) Madhya Pradesh has 0.06 sq km.
    [Show full text]
  • Fish Diversity of the Vatrak Stream, Sabarmati River System, Rajasthan
    Rec. zool. Surv. India: Vol. 117(3)/ 214-220, 2017 ISSN (Online) : (Applied for) DOI: 10.26515/rzsi/v117/i3/2017/120965 ISSN (Print) : 0375-1511 Fish diversity of the Vatrak stream, Sabarmati River system, Rajasthan Harinder Singh Banyal* and Sanjeev Kumar Desert Regional Centre, Zoological Survey of India, Jodhpur – 342005, Rajasthan, India; [email protected] Abstract Five species of fishes belonging to order cypriniformes from Vatrak stream of Rajasthan has been described. Taxonomic detailsKeywords along: with ecology of the fish fauna and stream morphology are also discussed. Diversity, Fish, Rajasthan, stream morphology, Vatrak Introduction Sei joins from right. Sabarmati River originates from Aravalli hills near village Tepur in Udaipur district of Rajasthan, the biggest state in India is well known for its Rajasthan and flows for 371 km before finally merging diverse topography. The state of Rajasthan can be divided with the Arabian Sea. Thus the Basin of Sabarmati River into the following geographical regions viz.: western and encompasses states of Rajasthan and Gujarat covering north western region, well known for the Thar Desert; the an area of 21,674 Sq.km between 70°58’ to 73°51’ East eastern region famous for the Aravalli hills, whereas, the longitudes and 22°15’ to 24°47’ North latitudes. The southern part of the state with its stony landscape offers Vatrak stream basin is circumscribed by Aravalli hills typical sites for water resource development where most on the north and north-east, Rann of Kachchh on the of the man-made reservoirs are present. Mahi River basin west and Gulf of Khambhat on the south.
    [Show full text]
  • Regional Geology of Malikhera- Mokanpura Area of Dariba-Rajpura- Bethunmi Polymetallic Sulphide Belt Rajasthan
    August 2017, Volume 4, Issue 08 JETIR (ISSN-2349-5162) REGIONAL GEOLOGY OF MALIKHERA- MOKANPURA AREA OF DARIBA-RAJPURA- BETHUNMI POLYMETALLIC SULPHIDE BELT RAJASTHAN 1DR. SAMIR NAWAL GSSS JHANWAR, JODHPUR, EX RESEARCH SCHOOLAR, DEPARTMENT OF GEOLOGY, JNV UNIVERSITY JODHPUR RAJASTHAN ABSTRACT: Precambrian stratigraphy of northwestern India can be assigned to the Bhilwara (>2500 Ma), Aravalli (2500 Ma to 2000 Ma) and Delhi (2000 Ma to 700 Ma) Geological Cycles on the basis of environment of deposition and tectonomagmatic events. The metasediments, concordant and discordant intrusives ad their extrusive phases, corresponding to these geological cycles have been designated as the Bhilwara, the Aravalli and the Delhi Supergroups. These have been further subdivided into several groups and still further into formation. INTRODUCTION The rocks of the Bhilwara Supergroup occur in an arcuate belt, extending from Deyi in the northeast through Kishangarh to Pipalkhunt in the southeast, underlying the Mewar plains of Rajasthan, and consist of metasedimentary sequences with associated migmatitic complex and igneous rocks. The rocks of the Arava!Ii Supergroup are exposed in south-eastern part of the Aravalli Range and northeastern part of Gujarat extending from Kankroli in the north to Champaner in the .south and mainly consist of argillaceous and arenaceous metasedimentary sequences with associated basic volcanics and ultrabasic igneous rocks. The main Aravalli Range extending from Ajmer in the north to Himmatnagar and Khed Brahma in the south. The Marwar Plains between Pali in the north and Reodhar in the southwest are occupied by the rocks of Delhi Supergroup which consist of calcareous, argillaceous and arenaceous metasedimentary sequences with associated basic volcanics and igneous rocks.
    [Show full text]
  • Impact of Sewage Discharge on Water Quality and Benthic Diversity of Kota Barrage, Kota, Rajasthan, India
    INFLUENCE OF CHLORELLA VULGARIS ON COPPER METAL CAUSED 207 Jr. of Industrial Pollution Control 30(2)(2014) pp 207-20 © EM International Printed in India. All rights reserved www.envirobiotechjournals.com IMPACT OF SEWAGE DISCHARGE ON WATER QUALITY AND BENTHIC DIVERSITY OF KOTA BARRAGE, KOTA, RAJASTHAN, INDIA N. SARANG1 AND L.L. SHARMA2 1 Chhattisgarh Kamdhenu Vishwavidyalaya, College of Fisheries Kawardha (Kabirdham) 491 995, Chhattisgarh, India 2 Maharana Pratap University of Agriculture and Technology, College of Fisheries Udaipur 313 001, Rajasthan, India Key words : Water quality, Benthic diversity, Sewage discharge, Kota Barrage Dam, Rajasthan (Received ............... February, 2014; accepted ............................, 2014) ABSTRACT The water of Kota Barrage is mainly used for domestic uses and bathing, besides irrigation and aquac- ulture. Seasonal variations in benthic fauna and selected Physico-chemical parameters of Kota Barrage Dam have been studied on the basis of the samples collected during monthly surveys for a period of one year (November, 2004 to October, 2005) which revealed interesting interrelationship among various factors. This Dam is affected by pollution (industrial specially Thermal Power Plant effluents and domestic) as indicated by low dissolved oxygen. Based on depth of visibility values Kota Barrage Dam could be categorized as “Moderately eutrophic” whereas nitrate nitrogen values of Kota Barrage dam indicated “Mesotrophic” status. On the other hand hardness values of this Dam were “Moderately hard”. The species diversity was found to influence due to water pollution in Kota Barrage. Despite this the biodiversity of macroinvertebrates was appreciably high with recorded 27 species. Most dominant benthic species encountered were Melanoides tuberculata, Bellamya bengalensis, Gyraulus convexiusculus, Indoplanorbis exustus and Lymnaea acuminata.
    [Show full text]
  • LIST of INDIAN CITIES on RIVERS (India)
    List of important cities on river (India) The following is a list of the cities in India through which major rivers flow. S.No. City River State 1 Gangakhed Godavari Maharashtra 2 Agra Yamuna Uttar Pradesh 3 Ahmedabad Sabarmati Gujarat 4 At the confluence of Ganga, Yamuna and Allahabad Uttar Pradesh Saraswati 5 Ayodhya Sarayu Uttar Pradesh 6 Badrinath Alaknanda Uttarakhand 7 Banki Mahanadi Odisha 8 Cuttack Mahanadi Odisha 9 Baranagar Ganges West Bengal 10 Brahmapur Rushikulya Odisha 11 Chhatrapur Rushikulya Odisha 12 Bhagalpur Ganges Bihar 13 Kolkata Hooghly West Bengal 14 Cuttack Mahanadi Odisha 15 New Delhi Yamuna Delhi 16 Dibrugarh Brahmaputra Assam 17 Deesa Banas Gujarat 18 Ferozpur Sutlej Punjab 19 Guwahati Brahmaputra Assam 20 Haridwar Ganges Uttarakhand 21 Hyderabad Musi Telangana 22 Jabalpur Narmada Madhya Pradesh 23 Kanpur Ganges Uttar Pradesh 24 Kota Chambal Rajasthan 25 Jammu Tawi Jammu & Kashmir 26 Jaunpur Gomti Uttar Pradesh 27 Patna Ganges Bihar 28 Rajahmundry Godavari Andhra Pradesh 29 Srinagar Jhelum Jammu & Kashmir 30 Surat Tapi Gujarat 31 Varanasi Ganges Uttar Pradesh 32 Vijayawada Krishna Andhra Pradesh 33 Vadodara Vishwamitri Gujarat 1 Source – Wikipedia S.No. City River State 34 Mathura Yamuna Uttar Pradesh 35 Modasa Mazum Gujarat 36 Mirzapur Ganga Uttar Pradesh 37 Morbi Machchu Gujarat 38 Auraiya Yamuna Uttar Pradesh 39 Etawah Yamuna Uttar Pradesh 40 Bangalore Vrishabhavathi Karnataka 41 Farrukhabad Ganges Uttar Pradesh 42 Rangpo Teesta Sikkim 43 Rajkot Aji Gujarat 44 Gaya Falgu (Neeranjana) Bihar 45 Fatehgarh Ganges
    [Show full text]
  • Jaipur Development Plan 2025
    MASTER DEVELOPMENT PLAN-2025 JAIPUR REGION Volume-2 DEVELOPMENT PLAN-2025 Jaipur Region Jaipur City JAIPUR DEVELOPMENT AUTHORITY PREFACE olume-I outlined the existing profile and volume-II attends to the Vfollowing with two front approaches Projections based on the existing studies Requirements spread and spatial distribution The Master Development Plan-2025 covers all aspects of development including transportation, infrastructure (sewer, drainage, water and electricity), environmental protection, and land uses (residential, commercial, industrial, recreational, etc.). The Master Plan analyzes current demographic statistics and economic issues, factors to project growth scenarios, propose solutions that mitigate negative impacts of traffic, assess infrastructure capacity, and public service needs, and allocate land as needed to ensure adequate land availability and to be able to utilize them for both present and future needs of the residents. Volume-I consist of existing profile of Jaipur district, Jaipur region and U1 area and the collected data has been used for analysis which would act as base for projections and proposals. Volume-I enumerate the following chapters: 1. Background 2. Jaipur District profile 3. Jaipur Region 4. Jaipur U1 area 5. Quality of Life District level study and conclusions are given in Jaipur District Profile chapter of volume-1 while projection and proposals for Jaipur Region and U- 1 area have been made separately give in volume -2. Planning proposal for Jaipur Region and U-1 area are based on background study of volume-1. volume-2 "Development Plan" is the second part of MDP-2025 which enumerates following : 1. Projections and proposals for Jaipur region 2. Proposals for U1 area 3.
    [Show full text]
  • City Sanitation Plan –Draft Report– Udaipur City
    CITY SANITATION PLAN –DRAFT REPORT– UDAIPUR CITY CONTENTS Chapter 1 : Background ..................................................................................................... 1 1.1 Concept .................................................................................................................. 1 1.2 The CSP Initiative ................................................................................................... 1 1.2.1 Context ............................................................................................................ 1 1.2.2 NUSP-Policy and Vision .................................................................................. 2 1.2.3 Vision ............................................................................................................... 3 1.2.4 The thrust of NSUP-Totally Sanitized City ........................................................ 3 1.3 City Sanitation Plan ................................................................................................. 3 1.3.1 Components of City Sanitation Plan ................................................................. 4 1.3.2 Strategy for City Sanitation Plan ...................................................................... 4 1.4 CSP Approach and Methodology ............................................................................ 5 1.5 Detailed Plan of Action ............................................................................................ 6 1.5.1 Profiling ULB ...................................................................................................
    [Show full text]
  • Dams, Rivers & People
    Dams, Rivers & People VOL 3 ISSUE 8-9 SEPT-OCT 2005 Rs 15/- Lead Piece The World Bank’s Motivated advocacy for large water storages In recent months the World Bank has taken a lead in Let us see the Indian situation in correct perspective. advocating more large water storages in India. The Firstly, the only figure that is available in public domain Bank advocate, John Briscoe (it is interesting to note about the existing storage capacities is that India has that nobody else from the Bank has come forward to about 212.8 BCM (billion cubic meters) of water support Briscoe’s advocacy) has used two comparative storage space. This figure is not backed by details figures to justify this advocacy. Firstly, he says, in the about the various water storages in different states, latest report from the Bank, India’s Water Economy – water basins in India. Nor is it clear how many and Bracing for a Turbulent Future released in the first which projects are included while arriving at this figure. week of October 2005, “Whereas arid rich countries (This is typical of India’s water resources (such as the United States and Australia) have built establishment, where, as far as possible, no over 5 000 cubic meters of water storage per capita, information is shared in public domain. The Right to and middle-income countries like South Africa, Mexico, Information bill that came into force on Oct 12, 2005, no Morocco and China can store about 1 000 cubic meters doubt a welcome piece in this situation, if the act were per capita, India’s dams ca store only 200 cubic meters to be implemented letter and spirit.
    [Show full text]
  • Comparative Study of Fluoride Toxicity in Ground Water of Hilly Terrain Area and Banas River Basin
    Available online a t www.pelagiaresearchlibrary.com Pelagia Research Library Der Chemica Sinica, 2015, 6(10):19-24 ISSN: 0976-8505 CODEN (USA) CSHIA5 Comparative study of fluoride toxicity in ground water of hilly terrain area and Banas river basin area of eastern Bhilwara (Rajasthan, India) and its impact, causes and prevention *P. L. Meena 1, A. S. Meena 1, K. S. Meena 2, P. K. Jain 2 and N. Kumar 3 1Department of Chemistry, University of Rajasthan, Jaipur, Rajasthan, India 2Department of Chemistry, M. L. V. Govt. College, Bhilwara, Rajasthan, India 3Department of Chemistry, M. L. S. University, Udaipur, Rajasthan, India _____________________________________________________________________________________________ ABSTRACT Fluoride is required by the human being for mineralization of bones and teeth. Hydro-Chemical condition is the main source of fluoride contamination in ground water but run off and atmospheric depositions are also responsible for additional fluoride concentration. This study was carried out to assess the fluoride concentration in ground water of Banas River Basin area and hilly terrain area of eastern Bhilwara (Rajasthan, India), effects on populace, possible sources and prevention and a comparison was made. For this purpose 98 ground water samples were collected from different locations of study area and analyzed. The fluoride toxicity in ground water of Banas river basin area determine comparatively much higher than the hilly terrain area. The maximum fluoride concentration in Banas river basin area determined is 5.2 mg/l and average concentration is 1.366 mg/l whereas in hilly terrain area is 2.33 mg/l and 0.306 mg/l. In 38.46 % samples of Banas river basin area F - concentration did not comply with BIS and WHO standard whereas 1.7% samples in hilly terrain areas.
    [Show full text]
  • Assessment of Minimum Water Flow Requirements of Chambal River
    Assessment of minimum water flow requirements of Chambal River in the context of Gharial (Gavialis gangeticus) and Gangetic Dolphin (Platanista gangetica) conservation Study Report April 2011 Assessmentofminimumwaterflowrequirements ofChambalRiverinthecontextofGharial(Gavialis gangeticus)andGangeticDolphin(Platanista gangetica)conservation StudyReport April2011 Contributors:SyedAinulHussain,R.K.Shrama,NiladriDasguptaandAngshumanRaha. CONTENTS Executivesummary 1 1. Background 3 2. Introduction 3 3. TheChambalriver 3 4. Existingandproposedwaterrelatedprojects 5 5. TheNationalChambalSanctuary 8 6. Thegharial(Gavialisgangeticus) 8 7. TheGangeticdolphin(Platanistagangetica) 9 8. Objectivesofassessment 10 9. Methodsofassessment 12 10. Results 13 11. Discussion 20 12. References 22 13. AppendixI–IV 26 AssessmentofminimumwaterflowrequirementsofChambalRiver ʹͲͳͳ EXECUTIVESUMMARY The Chambal River originates from the summit of Janapav hill of the Vindhyan range at an altitudeof854mabovethemslat22027’Nand75037’EinMhow,districtIndore,Madhya Pradesh.Theriverhasacourseof965kmuptoitsconfluencewiththeYamunaRiverinthe EtawahdistrictofUttarPradesh.ItisoneofthelastremnantriversinthegreaterGangesRiver system, which has retained significant conservation values. It harbours the largest gharial population of the world and high density of the Gangetic dolphin per river km. Apart from these,themajorfaunaoftheRiverincludesthemuggercrocodile,smoothͲcoatedotter,seven speciesoffreshwaterturtles,and78speciesofwetlandbirds.Themajorterrestrialfaunaofthe
    [Show full text]
  • Geography of Rajasthan
    GEOGRAPHY OF RAJASTHAN RIVERS OF RAJASTHAN All aspects relating to Rivers of Rajasthan have been simplified and summarized by the Delhi Law Academy in 21 pages. This sample contains the first 3 pages… Delhi Law Academy – India’s Finest Coaching RAJASTHAN ADMINISTRATIVE SERVICE www.delhilawacademy.com All materials, copyrights and trademarks are rights of their respective owners Banas River & its Tributaries • Banas river originates in the Khamnor Hills of the Aravalli Range, near Kumbhalgarh in Rajsamand. • It is a tributary of the Chambal River and is approximately 512 kilometres in length. • It is also known as 'Van Ki Asha' (Hope of forest). • There is another river in Rajasthan with name of Banas, which flows in western direction and is also called as West Banas River. Origin Khamnor Hills, near Kumbhalgarh in Raisamand. Length 512 Kms Discharge Chambal near Rameshwar in Sawai Madhopur District States & Major Cities Nathdwara, Jahazpur and Tonk. Right Bank Tributaries Berach, Menali Left Bank Tributaries Kothari, Khari, Dai, Morel and Kalisil Major Dams Bisalpur Banas River in Indian mythology • Lord Parshuram, an avatar (incarnation) of Lord Vishnu, is linked strongly with Banas. Parshuram had killed his mother, Renukaji, on the order of his father. He went to several places seeking salvation. He saw that a calf, who had turned black on killing a man, turned white again after taking a dip in river Banas. Parshuram did the same and was relieved of the sin. The place is now called Matrikundya and falls in Bhilwara district. It is also known as the ‘Haridwar of Rajasthan’. • Jargaji, an important pilgrimage, is located around 10 km from the origin point.
    [Show full text]
  • Dam Break Analysis of JAWAI Dam PALI, Rajasthan Using HEC-RAS
    IOSR Journal of Mechanical and Civil Engineering (IOSR-JMCE) e-ISSN: 2278-1684,p-ISSN: 2320-334X, Volume 17, Issue 2 Ser. I (Mar - Apr 2020), PP 43-52 www.iosrjournals.org Dam Break Analysis of JAWAI Dam PALI, Rajasthan Using HEC-RAS Ankush kumar Gupta1, Ishu Narang2, Pooja Goyal3 (Assistant Professor, MBM Engineering College,Jodhpur) (Junior Engineer, PHED Rajasthan) (Assistant Engineer, Nagar Parishad, Bhilwara) Abstract: Due to old methods of construction dam was under designed and with use of poor materials of construction it is prone to collapse due to aging. Moreover the magnitude of peak floods to be used for the spillway design was based upon rough estimates which do not according to the modern estimates of extreme floods as suggested by experts of the International committee on large dams and the seismic potential was also under- estimated thus there are more chances for the dam to failure and such an accident will result in economic loss of states which mainly depends on river water. So keeping these points in mind an analysis of Jawai dam failure which is situated in Sumerpur town of Pali district Rajasthan and built in 1957 by Raja Umaid Singh has been done with the help of HEC-RAS to get the breach characteristics of dam and with the help of Arc-GIS and HEC-GeoRAS inundation mapping is made of downstream area of dam so that proper hazard prevention and mitigation measures can be taken at the time of such an accident and economic losses can be reduced.And results shown by HEC-RAS describe that for PMF 7267.34 m3/s, maximum stage will be 243.89 meter upto 7 km downstream and from there it reduces to 133.38 meter and it ahead it little varies .from the above results it is proved that flow area is different for different cross section, near the dam flow area is 101697 to approximately 12000 square meter and from 7 km downstream it suddenly reduces to 25929.12 to approximately 15000 square meter area.
    [Show full text]