Ground and Surface Water Linkages
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Visualizing Hydropower Across the Himalayas: Mapping in a Time of Regulatory Decline
HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies Volume 34 Number 2 Article 9 December 2014 Visualizing Hydropower Across the Himalayas: Mapping in a time of Regulatory Decline Kelly D. Alley Auburn University, [email protected] Ryan Hile University of Utah Chandana Mitra Auburn University Follow this and additional works at: https://digitalcommons.macalester.edu/himalaya Recommended Citation Alley, Kelly D.; Hile, Ryan; and Mitra, Chandana. 2014. Visualizing Hydropower Across the Himalayas: Mapping in a time of Regulatory Decline. HIMALAYA 34(2). Available at: https://digitalcommons.macalester.edu/himalaya/vol34/iss2/9 This work is licensed under a Creative Commons Attribution 3.0 License. This Research Article is brought to you for free and open access by the DigitalCommons@Macalester College at DigitalCommons@Macalester College. It has been accepted for inclusion in HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies by an authorized administrator of DigitalCommons@Macalester College. For more information, please contact [email protected]. Visualizing Hydropower Across the Himalayas: Mapping in a time of Regulatory Decline Acknowledgements Earlier drafts of this paper were presented at the BAPA-BEN International Conference on Water Resources in Dhaka, Bangladesh in 2013 and for the AAA panel on Developing the Himalaya in 2012. The authors appreciate the comments and support provided by members who attended these sessions. Our mapping project has been supported by the College of Liberal Arts and the Center for Forest Sustainability at Auburn University. This research article is available in HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies: https://digitalcommons.macalester.edu/himalaya/vol34/iss2/9 Visualizing Hydropower across the Himalayas: Mapping in a time of Regulatory Decline Kelly D. -
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 -
National Ganga River Basin Authority (Ngrba)
NATIONAL GANGA RIVER BASIN AUTHORITY (NGRBA) Public Disclosure Authorized (Ministry of Environment and Forests, Government of India) Public Disclosure Authorized Environmental and Social Management Framework (ESMF) Public Disclosure Authorized Volume I - Environmental and Social Analysis March 2011 Prepared by Public Disclosure Authorized The Energy and Resources Institute New Delhi i Table of Contents Executive Summary List of Tables ............................................................................................................... iv Chapter 1 National Ganga River Basin Project ....................................................... 6 1.1 Introduction .................................................................................................. 6 1.2 Ganga Clean up Initiatives ........................................................................... 6 1.3 The Ganga River Basin Project.................................................................... 7 1.4 Project Components ..................................................................................... 8 1.4.1.1 Objective ...................................................................................................... 8 1.4.1.2 Sub Component A: NGRBA Operationalization & Program Management 9 1.4.1.3 Sub component B: Technical Assistance for ULB Service Provider .......... 9 1.4.1.4 Sub-component C: Technical Assistance for Environmental Regulator ... 10 1.4.2.1 Objective ................................................................................................... -
Study of Groundwater Recharge in Rechna Doab Using Isotope Techniques
\ PINSTECH/RIAD-133 STUDY OF GROUNDWATER RECHARGE IN RECHNA DOAB USING ISOTOPE TECHNIQUES M. ISHAQ SAJJAD M. AZAM TASNEEM MANZOOR AHMAD S. D. HUSSAIN IQBAL H. KHAN WAHEED AKRAM RADIATION AND ISOTOPE APPLICATIONS DIVISION Pakistan Institute of Nuclear Science and Technology P. O. Nilore, Islamabad June, 1992 PINSTECH/RIAD-133 STUDY OF GROUNDWATER RECHARGE IN RECHNA DOAB USING ISOTOPE TECHNIQUES M. ISHAQ SAJJAD M. AZAM TASNEEM MANZOOR AHMAD S. D. HUSSAIN IQBAL H. KHAN WAHEED AKRAM RADIATION AND ISOTOPE APPLICATIONS DIVISION PAKISTAN INSTITUTE OF NUCLEAR SCIENCE AND TECHNOLOGY P. 0. NILORE, ISLAMABAD. June, 1992 CONTENTS ABSTRACT INTRODUCTION THE PROJECT AREA 2.1 General Description of The Area 2.2 Climate 2.3 Surface and Subsurface Geology FIELD WORK LABORATORY WORK RESULTS AND DISCUSSION 5.1 Sources of Groundwater Recharge 5.1.1 Isotopic Data of River/Canal System 5.1.1.1 River Chenab 5.1.1.2 River Ravi 5.1.1.3 Upper Chenab Canal (UCC) 5.1.1.4 Lower Chenab Canal (LCC) 5.1.2 Isotopic Data of Rains ISOTOPIC VARIATIONS IN GROUNDWATER 6.1 Some Features of SD-S^O Diagrams 6.2 Spatial and Temporal Variations of Isotopic Data THE GROUNDWATER RECHARGE FROM DIFFERENT INPUT SOURCES TURN-OVER TIMES OF THE GROUNDWATER VERTICAL DISTRIBUTION OF ISOTOPES CONCLUSIONS ACKNOWLEDGMENTS REFERENCES \ ABSTRACT Isotopic studies were performed in the Rechna Doab area to understand the recharge mechanism, investigate the relative contributions from various sources such as rainfall, rivers and canal system and to estimate the turn-over times and replenishment rate of groundwater. The isotopic data suggest that the groundwater in the project area, can be divided into different zones each having its own characteristic isotopic composition. -
1St Year Trained HSP List 2013-2014.Xlsx
Trained HSP List- 2013-2014 S.No District Facility Name Facility Type HSP Name HSP Type Batch no. Start date End date Phone Number 1 Mahoba GH District Women Hospital Mahoba GH Renu Maurya SN 1 06-05-13 11-05-13 9919043955 2 Mahoba CHC Charkhari CHC Amrita MO 1 06-05-13 11-05-13 9616904440 3 Mahoba CHC Charkhari CHC Sapna Viswakarma SN 1 06-05-13 11-05-13 9984951270 4 Mahoba PHC Jaitpur PHC Veenita Kumari ANM 1 06-05-13 11-05-13 9453267411 5 Mahoba CHC Kulpahar PHC Ambrish Kumar MO 1 06-05-13 11-05-13 8726842604 6 Mahoba CHC Kabrai CHC Ishwar Chandra MO 1 06-05-13 11-05-13 8931988333 7 Mahoba CHC Charkhari CHC Urmila Royakwar LHV 1 06-05-13 11-05-13 9450718367 8 Mahoba PHC Gourhari PHC Sunil Kumar Sachan MO 1 06-05-13 11-05-13 8765022187 9 Mahoba PHC Jaitpur PHC Yamini Shakti ANM 1 06-05-13 11-05-13 9935824268 10 Mahoba PHC Panwari PHC Kamlesh Kumari LHV 1 06-05-13 11-05-13 9735536464 11 Mahoba GH District Women Hospital Mahoba GH Anil Kumari ANM 1 06-05-13 11-05-13 9532053603 12 Mahoba CHC Kabrai CHC Paritbha Singh ANM 1 06-05-13 11-05-13 9721427101 13 Mahoba CHC Charkhari CHC Dolly Khan SN 1 06-05-13 11-05-13 8858669132 14 Mahoba PHC Gourhari PHC Krishna Kumari ANM 1 06-05-13 11-05-13 9453768916 15 Mahoba PHC Jaitpur PHC Akeela Bano ANM 1 06-05-13 11-05-13 8198047199 16 Mahoba GH District Women Hospital Mahoba GH Asha Soni ANM 1 06-05-13 11-05-13 9936996137 17 Mahoba CHC Kabrai CHC Anjana Kushwaha SN 1 06-05-13 11-05-13 9648987818 18 Mahoba CHC Charkhari CHC Sofiya Bano SN 1 06-05-13 11-05-13 9453394798 19 Mahoba PHC Gourhari PHC Suman -
Physical Geography of the Punjab
19 Gosal: Physical Geography of Punjab Physical Geography of the Punjab G. S. Gosal Formerly Professor of Geography, Punjab University, Chandigarh ________________________________________________________________ Located in the northwestern part of the Indian sub-continent, the Punjab served as a bridge between the east, the middle east, and central Asia assigning it considerable regional importance. The region is enclosed between the Himalayas in the north and the Rajputana desert in the south, and its rich alluvial plain is composed of silt deposited by the rivers - Satluj, Beas, Ravi, Chanab and Jhelam. The paper provides a detailed description of Punjab’s physical landscape and its general climatic conditions which created its history and culture and made it the bread basket of the subcontinent. ________________________________________________________________ Introduction Herodotus, an ancient Greek scholar, who lived from 484 BCE to 425 BCE, was often referred to as the ‘father of history’, the ‘father of ethnography’, and a great scholar of geography of his time. Some 2500 years ago he made a classic statement: ‘All history should be studied geographically, and all geography historically’. In this statement Herodotus was essentially emphasizing the inseparability of time and space, and a close relationship between history and geography. After all, historical events do not take place in the air, their base is always the earth. For a proper understanding of history, therefore, the base, that is the earth, must be known closely. The physical earth and the man living on it in their full, multi-dimensional relationships constitute the reality of the earth. There is no doubt that human ingenuity, innovations, technological capabilities, and aspirations are very potent factors in shaping and reshaping places and regions, as also in giving rise to new events, but the physical environmental base has its own role to play. -
Ganga As Perceived by Some Ganga Lovers Mother Ganga's Rights Are Our Rights
Ganga as Perceived by Some Ganga Lovers Mother Ganga’s Rights Are Our Rights Pujya Swami Chidanand Saraswati Nearly 500 million people depend every day on the Ganga and Her tributaries for life itself. Like the most loving of mothers, She has served us, nourished us and enabled us to grow as a people, without hesitation, without discrimination, without vacation for millennia. Regardless of what we have done to Her, the Ganga continues in Her steady fl ow, providing the waters that offer nourishment, livelihoods, faith and hope: the waters that represents the very life-blood of our nation. If one may think of the planet Earth as a body, its trees would be its lungs, its rivers would be its veins, and the Ganga would be its very soul. For pilgrims, Her course is a lure: From Gaumukh, where she emerges like a beacon of hope from icy glaciers, to the Prayag of Allahabad, where Mother Ganga stretches out Her glorious hands to become one with the Yamuna and Saraswati Rivers, to Ganga Sagar, where She fi nally merges with the ocean in a tender embrace. As all oceans unite together, Ganga’s reach stretches far beyond national borders. All are Her children. For perhaps a billion people, Mother Ganga is a living goddess who can elevate the soul to blissful union with the Divine. She provides benediction for infants, hope for worshipful adults, and the promise of liberation for the dying and deceased. Every year, millions come to bathe in Ganga’s waters as a holy act of worship: closing their eyes in deep prayer as they reverently enter the waters equated with Divinity itself. -
National Mission for Clean Ganga (NMCG)
National Mission for Clean Ganga (NMCG) Ministry of Water Resources, River Development & Ganga Rejuvenation Responses to Pre Proposal/Bid Queries Sub: Selection of Project Engineer for Development of STP at Unnao ,Shuklaganj & Pankha , rehabilitation of existing STPs & associated infrastructure and O&M of all assets for 15 years in Kanpur, Uttar Pradesh under Hybrid Annuity based PPP mode Sl. RFP Clause No. Subject/RFP Clause Bidder’s Query Response No. 1 Clause 2.2.2 (B) Financial Capacity: The Bidder shall have received We request that, as per standard practice, company RFP conditions a minimum revenue of Rs. 5 (Five) crore or US$ turnover be considered for assessing the financial shall prevail 2.5 (Two and half) million per annum from capacity of the Bidder. At the minimum, revenue of professional fees during each of the 3 (three) water, waste water, drainage and area infrastructure financial years preceding the Proposal Due Date. projects to be considered against this clause. For the avoidance of doubt, professional fees hereunder refers to the fees received by the Bidder for providing advisory or consultancy services (excluding audit, accounting, taxation and information technology) to its clients for project development services / preparation of DPRs, Technical Feasibility Studies, Project Management Consultancy Services, Third Party / Independent Engineer / Owner’s Engineer Services, Technical Audit services, assessment of existing assets etc for waste water projects. 2 Clause 2.1.4, Minimum educational qualification and O&M activities require expertise in mechanical and Please refer to the S. No. 8, discipline – O&M Engineer – Graduation in electrical disciplines. Addendum Civil Engineering/Environment Engineering / Hence, it is requested to add Electrical / Mechanical Post graduation in Civil / Public Health / to the acceptable list of disciplines for O&M Environmental Engineering Engineer. -
Ganga River Basin Planning Assessment Report
Strategic Basin Planning for Ganga River Basin in India Ganga River Basin Planning Assessment Report Final November 2018 Title Ganga River Basin Planning Assessment Report Client Project Reference Pages World Bank and 1220123-002 1220123-002-ZWS-0003 170 Government of India Keywords India, Ganga, Model, Information System, Hydrology, Geohydrology, Water quality, Ecology, Water allocation, Integrated Water Resources Management Summary The World Bank has assigned Deltares and its partners AECOM India and FutureWater to carry out the project “Analytical Work and Technical Assistance to support Strategic Basin Planning for Ganga River Basin in India” in cooperation with the Government of India. The objectives of the project are 1) to strengthen the capacity with respect to strategic basin planning, 2) to develop a set of scenarios for the development of the Ganga basin, 3) to build a strong and accessible knowledge base and 4) to establish a multi-stakeholder engagement process to support strategic basin planning. This report contains: • The scenario and strategy assessment; • The environmental flow assessment; • The groundwater-surface water interaction assessment. This report contributes to project milestone 5 of the project. Reference Bons, C.A. (Ed.), 2018. Ganga River Basin Planning Assessment Report. Main volume and Appendices. Deltares with AECOM and FutureWater for the World Bank and the Government of India, Report 1220123-002-ZWS-0003. State Final Ganga River Basin Planning Assessment Report 1220123-002-ZWS-0003, November 2018, final -
Comparative Physiography of the Lower Ganges and Lower Mississippi Valleys
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1955 Comparative Physiography of the Lower Ganges and Lower Mississippi Valleys. S. Ali ibne hamid Rizvi Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Rizvi, S. Ali ibne hamid, "Comparative Physiography of the Lower Ganges and Lower Mississippi Valleys." (1955). LSU Historical Dissertations and Theses. 109. https://digitalcommons.lsu.edu/gradschool_disstheses/109 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. COMPARATIVE PHYSIOGRAPHY OF THE LOWER GANGES AND LOWER MISSISSIPPI VALLEYS A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geography ^ by 9. Ali IJt**Hr Rizvi B*. A., Muslim University, l9Mf M. A*, Muslim University, 191*6 M. A., Muslim University, 191*6 May, 1955 EXAMINATION AND THESIS REPORT Candidate: ^ A li X. H. R iz v i Major Field: G eography Title of Thesis: Comparison Between Lower Mississippi and Lower Ganges* Brahmaputra Valleys Approved: Major Prj for And Chairman Dean of Gri ualc School EXAMINING COMMITTEE: 2m ----------- - m t o R ^ / q Date of Examination: ACKNOWLEDGMENT The author wishes to tender his sincere gratitude to Dr. Richard J. Russell for his direction and supervision of the work at every stage; to Dr. -
Surface Water/Groundwater Relationship in Chaj Doab
PINSTECH/RIAD-122 . SURFACE WATER/GROUNDWATER RELATIONSHIP IN CHAJ DOAB RADIATION & ISOTOPE APPLICATIONS DIVISION Pakistan Institute of Nuclear Science & Technology P. O. Nilore Islamabad. JULY, 1990 PINSTECH/RIAD-122 SURFACE WATER/GROUNDWATER RELATIONSHIP , IN CHAJ DOAB S. D. HUSSAIN M. I. SAJJAD W.AKRAM M. AHMAD M. RAFIQ J. A. TARIQ RADIATION & ISOTOPE APPLICATIONS DIVISION Pakistan Institate of Nuclear Science & Technology P. O. Nilore Islamabad. JULY, 1990 PIMSTKCH/RIAD-122 SURFACE WATER/GROUNDWATER RELATIONSHIP IN CHAJ DOAB S.D.HOSSAIN M.I.SAJJAD W.AKRAM M.AHMAD M.RAFIQ J.A.TARIQ RADIATION & ISOTOPE APPLICATIONS DIVISION PAKISTAN INSTITOTE OF NUCLEAR SCIENCE & TECHNOLOGY P.O. NILORE, ISLAMABAD JULY-1990 CONTENTS ABSTRACT INTRODUCTION 1 DESCRIPTION OF THE AREA UNDER INVESTIGATION 2 2.1 General 2 2.2 Physiography 2 2.3 Geology 3 2.4 Climate 4 SAMPLING PLAN 5 ANALYSIS 6 ISOTOPIC CHARACTERISATION OF DIFFERENT HATERS 8 5.1 Rainfall 8 5.2 Surface Hater: Rivers and Canals 9 5.3 Groundwater 11 INTERRELATION OF DIFFERENT WATERS 12 6.1 Surface Water/Shallow Groundwater 12 6.2 Shallow Water/Deep Water 14 6.3 Surface Water/Deep Water 15 PROCESS OF SALINIZATION OF GROUNDWATER 16 CONCLUSIONS 17 ACKNOWLEDGEMENTREFERENCES S 1189 ABSTRACT In order to understand the relationship between surface water and groundwater in Chaj Doab, isotopic and chenical studies were undertaken. The data show that north-eantern part of the doab is mainly recharged by raini;. In the rest o* the doab, surface water and groundwater are generally well connected and the recharge is mostly from the rivers either directly or through irrigation channels. -
Soft Sediments and Damage Pattern-A Few
Nat Hazards (2014) 74:1829–1851 DOI 10.1007/s11069-014-1283-4 ORIGINAL PAPER Soft sediments and damage pattern: a few case studies from large Indian earthquakes vis-a-vis seismic risk evaluation Mithila Verma • R. J. Singh • B. K. Bansal Received: 27 November 2012 / Accepted: 2 June 2014 / Published online: 19 June 2014 Ó Springer Science+Business Media Dordrecht 2014 Abstract India is prone to earthquake hazard; almost 65 % area falls in high to very high seismic zones, as per the seismic zoning map of the country. The Himalaya and the Indo- Gangetic plains are particularly vulnerable to high seismic hazard. Any major earthquake in Himalaya can cause severe destruction and multiple fatalities in urban centers located in the vicinity. Seismically induced ground motion amplification and soil liquefaction are the two main factors responsible for severe damage to the structures, especially, built on soft sedimentary environment. These are essentially governed by the size of earthquake, epi- central distance and geology of the area. Besides, lithology of the strata, i.e., sediment type, grain size and their distribution, thickness, lateral discontinuity and ground water depth, play an important role in determining the nature and degree of destruction. There has been significant advancement in our understanding and assessment of these two phenomena. However, data from past earthquakes provide valuable information which help in better estimation of ground motion amplification and soil liquefaction for evaluation of seismic risk in future and planning the mitigation strategies. In this paper, we present the case studies of past three large Indian earthquakes, i.e., 1803 Uttaranchal earthquake (Mw 7.5); 1934 Bihar–Nepal earthquake (Mw 8.1) and 2001 Bhuj earthquake (Mw 7.7) and discuss the role of soft sediments particularly, alluvial deposits in relation to the damage pattern due to amplified ground motions and soil liquefaction induced by the events.