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Drinking Water Quality Analysis of Surrounding Rivers in Bhubaneswar, Odisha
International Journal of Advance Research In Science And Engineering http://www.ijarse.com IJARSE, Vol. No.3, Issue No.5, May 2014 ISSN-2319-8354(E) DRINKING WATER QUALITY ANALYSIS OF SURROUNDING RIVERS IN BHUBANESWAR, ODISHA K. Mohapatra1, S. K. Biswal2, G.Nayak3 1Asst. Professor, Department of Chemistry,GITA, Bhubaneswar(India) 2Professor, Department of Chemistry, IGIT, Sarang(India) 3Lecturer in Chemistry, EATM, Bhubaneswar (India) ABSTRACT With rapid growth of population, Industrial activities and deforestation, the water quality of surrounding rivers in Bhubaneswar, the capital of Odisha is gradually deteriorating. This city has become a environmental sensitive zone in the state of Odisha in India. Drinking water is supplied from surrounding rivers of Bhubaneswar like Kuakhai, Daya and Mahanadi. This supplied water from surrounding rivers becomes polluted when toxic substances, oxidized organics, inorganic, suspended solids, human, animal and plant pathogens enter into the water bodies. The treatment of surface water and waste water is necessary in order to maintain its quality standards for drinking water purposes. The objective of water treatment is to produce an adequate and continuous supply of water that is chemically, bacteriological free and aesthetically pleasing. Water samples from six different locations were collected in every month of pre mansoon, mansoon and post mansoon periods. Standard procedures were adopted to analyze and to calculate the different physic-chemical parameters of surface water samples using ISI standard procedure. Keywords: Surface Water Pollution; Physico-Chemical Parameter; Seasonal Variation; Mahanadi, Daya and Kuakhai Rivers. I INTRODUCTION Water plays a great role for the existence of human beings and all living organisms. -
PURI DISTRICT, ORISSA South Eastern Region Bhubaneswar
Govt. of India MINISTRY OF WATER RESOURCES CENTRAL GROUND WATER BOARD PURI DISTRICT, ORISSA South Eastern Region Bhubaneswar March, 2013 1 PURI DISTRICT AT A GLANCE Sl ITEMS Statistics No 1. GENERAL INFORMATION i. Geographical Area (Sq. Km.) 3479 ii. Administrative Divisions as on 31.03.2011 Number of Tehsil / Block 7 Tehsils, 11 Blocks Number of Panchayat / Villages 230 Panchayats 1715 Villages iii Population (As on 2011 Census) 16,97,983 iv Average Annual Rainfall (mm) 1449.1 2. GEOMORPHOLOGY Major physiographic units Very gently sloping plain and saline marshy tract along the coast, the undulating hard rock areas with lateritic capping and isolated hillocks in the west Major Drainages Daya, Devi, Kushabhadra, Bhargavi, and Prachi 3. LAND USE (Sq. Km.) a) Forest Area 90.57 b) Net Sown Area 1310.93 c) Cultivable Area 1887.45 4. MAJOR SOIL TYPES Alfisols, Aridsols, Entisols and Ultisols 5. AREA UNDER PRINCIPAL CROPS Paddy 171172 Ha, (As on 31.03.2011) 6. IRRIGATION BY DIFFERENT SOURCES (Areas and Number of Structures) Dugwells, Tube wells / Borewells DW 560Ha(Kharif), 508Ha(Rabi), Major/Medium Irrigation Projects 66460Ha (Kharif), 48265Ha(Rabi), Minor Irrigation Projects 127 Ha (Kharif), Minor Irrigation Projects(Lift) 9621Ha (Kharif), 9080Ha (Rabi), Other sources 9892Ha(Kharif), 13736Ha (Rabi), Net irrigated area 105106Ha (Total irrigated area.) Gross irrigated area 158249 Ha 7. NUMBERS OF GROUND WATER MONITORING WELLS OF CGWB ( As on 31-3-2011) No of Dugwells 57 No of Piezometers 12 10. PREDOMINANT GEOLOGICAL Alluvium, laterite in patches FORMATIONS 11. HYDROGEOLOGY Major Water bearing formation 0.16 mbgl to 5.96 mbgl Pre-monsoon Depth to water level during 2011 2 Sl ITEMS Statistics No Post-monsoon Depth to water level during 0.08 mbgl to 5.13 mbgl 2011 Long term water level trend in 10 yrs (2001- Pre-monsoon: 0.001 to 0.303m/yr (Rise) 0.0 to 2011) in m/yr 0.554 m/yr (Fall). -
Annual Report 2018-2019
ANNUAL REPORT 2018-2019 STATE POLLUTION CONTROL BOARD, ODISHA A/118, Nilakantha Nagar, Unit-Viii Bhubaneswar SPCB, Odisha (350 Copies) Published By: State Pollution Control Board, Odisha Bhubaneswar – 751012 Printed By: Semaphore Technologies Private Limited 3, Gokul Baral Street, 1st Floor Kolkata-700012, Ph. No.- +91 9836873211 Highlights of Activities Chapter-I 01 Introduction Chapter-II 05 Constitution of the State Board Chapter-III 07 Constitution of Committees Chapter-IV 12 Board Meeting Chapter-V 13 Activities Chapter-VI 136 Legal Matters Chapter-VII 137 Finance and Accounts Chapter-VIII 139 Other Important Activities Annexures - 170 (I) Organisational Chart (II) Rate Chart for Sampling & Analysis of 171 Env. Samples 181 (III) Staff Strength CONTENTS Annual Report 2018-19 Highlights of Activities of the State Pollution Control Board, Odisha he State Pollution Control Board (SPCB), Odisha was constituted in July, 1983 and was entrusted with the responsibility of implementing the Environmental Acts, particularly the TWater (Prevention and Control of Pollution) Act, 1974, the Water (Prevention and Control of Pollution) Cess Act, 1977, the Air (Prevention and Control of Pollution) Act, 1981 and the Environment (Protection) Act, 1986. Several Rules addressing specific environmental problems like Hazardous Waste Management, Bio-Medical Waste Management, Solid Waste Management, E-Waste Management, Plastic Waste Management, Construction & Demolition Waste Management, Environmental Impact Assessment etc. have been brought out under the Environment (Protection) Act. The SPCB also executes and ensures proper implementation of the environmental policies of the Union and the State Government. The activities of the SPCB broadly cover the following: Planning comprehensive programs towards prevention, control or abatement of pollution and enforcing the environmental laws. -
Organic Matter Depositional Microenvironment in Deltaic Channel Deposits of Mahanadi River, Andhra Pradesh
AL SC R IEN 180 TU C A E N F D O N U A N D D A E I T Journal of Applied and Natural Science 1(2): 180-190 (2009) L I O P N P JANS A ANSF 2008 Organic matter depositional microenvironment in deltaic channel deposits of Mahanadi river, Andhra Pradesh Anjum Farooqui*, T. Karuna Karudu1, D. Rajasekhara Reddy1 and Ravi Mishra2 Birbal Sahni Institute of Palaeobotany, 53, University Road, Lucknow, INDIA 1Delta Studies Institute, Andhra University, Sivajipalem, Visakhapatnam-17, INDIA 2ONGC, 9, Kaulagarh Road, Dehra dun, INDIA *Corresponding author. E-mail: [email protected] Abstract: Quantitative and qualitative variations in microscopic plant organic matter assemblages and its preservation state in deltaic channel deposits of Mahanadi River was correlated with the depositional environment in the ecosystem in order to prepare a modern analogue for use in palaeoenvironment studies. For this, palynological and palynofacies study was carried out in 57 surface sediment samples from Birupa river System, Kathjodi-Debi River system and Kuakhai River System constituting Upper, Middle and Lower Deltaic part of Mahanadi river. The apex of the delta shows dominance of Spirogyra algae indicating high nutrient, low energy shallow ecosystem during most of the year and recharged only during monsoons. The depositional environment is anoxic to dysoxic in the central and south-eastern part of the Middle Deltaic Plain (MDP) and Lower Deltaic Plain (LDP) indicated by high percentage of nearby palynomorphs, Particulate Organic Matter (POM) and algal or fungal spores. The northern part of the delta show high POM preservation only in the estuarine area in LDP but high Amorphous Organic Matter (MOA) in MDP. -
Tourism Under RDC, CD, Cuttack ******* Tourism Under This Central Division Revolves Round the Cluster of Magnificent Temple Beaches, Wildlife Reserves and Monuments
Tourism under RDC, CD, Cuttack ******* Tourism under this Central Division revolves round the cluster of magnificent temple beaches, wildlife reserves and monuments. Tourism specifically in Odisha is pilgrimage oriented. The famous car festival of Puri Jagannath Temple has got the world wide acclaim. It holds attraction of all domestic, national and international tourists, Sea Beaches like Puri, Konark, Astarang of Puri District, Digha, Talasari, Chandipur of Balasore, Siali of Jagatsinghpur District keeps the beholder at its clutch. Wild life reserves like Similipal of Mayurbhanj, Bhitarkanika of Kendrapara along with scenic beauty of nature makes one mesmerized and gives a feeling of oneness with nature, the part of cosmic power. BALASORE KHIRACHORA GOPINATH TEMPLE: Khirachora Gopinatha Temple is situated at Remuna. It is famous as Vaishnab shrine. Remuna is a Chunk of Brindaban in Orissa. It is a little town located 9 k.m east of Balasore. The name Remuna is resulting from the word Ramaniya which means very good looking. "Khirachora" in Odia means Stealer of Milk and Gopinatha means the Divine Consort of Gopis. The reference is to child Krishna's love for milk and milk products. (Khirachora Gopinath Temple) PANCHALINGESWAR TEMPLE: Panchalingeswar is located on a top of a hillock near the Nilagiri hill which is popular for its natural surroundings. The main attraction of this place is a temple having five lingas with a perennial stream, which is regularly washes the Shivalingas as it flows over them. So, to reach to the temple one has to lie flat on the rock parallel to the stream to touch and worship the lingas inside the water stream. -
Rise and Fall of Buddhism on Daya Basin
Orissa Review * December - 2007 Rise and Fall of Buddhism on Daya Basin Dr. Saroj Kumar Panda River Daya which originates from the river teachers used to impart here both religious and Kuakhai at Balakati near Hirapur (famous for secular instructions to people. These teachers Chausathi Yogini temple) has a south western were greatly loved and respected by the simple course of about 45 miles. It flows through Uttara, country folk for the blessed hopes they gave to Dhauli, Kakudia, Aragarh, Beguniapara, their afflicted hearts. In course of time some of Pandiakera, Balabhadrapur and finally discharges these monasteries grew up into famous university into Chilika lake.1 On its course, Daya is joined centres. As torch bearer of the Buddhist culture by the Bhargavi river, the Gangua Nalla, the these centres attracted pupils and scholars from Malaguni river, the Luna river and many smaller far and wide.3 drainages from Khurda sub-division.2 Two The development of Mahayan Buddhism important Buddhist vestige, whose traces are in Orissa may be studied through the historical found today on the Daya basin is highlighted in growth of these monastic institutions and through this paper. the activities of the sages and philosophers of this Buddhism in Orissa flourished during the religion. The Nagarjuni Konda inscription early Christian era independent of the Kusan engraved during 14th year of the Mahariputa patronage. In fact, till the coming of the Bhaumakar Virapurusadatta, testifies to the development of dynasty in the 8th century A.D., notable Buddhist some Hinayanic strongholds at Tosali, Palura, rulers were not known to have thrived here more Hirumu, Papila and Puspagiri by 3rd century A.D. -
Threats to Coastal Communities of Mahanadi Delta Due to Imminent
1 Threats to coastal communities of Mahanadi delta due to imminent 2 consequences of erosion – present and near future. 3 Anirban Mukhopadhyay*, Pramit Ghosh, Abhra Chanda, Amit Ghosh, Subhajit Ghosh, 4 Shouvik Das, Tuhin Ghosh ,Sugata Hazra 5 School of Oceanographic Studies, Jadavpur University, Kolkata, West Bengal, India 6 *Corresponding author: [email protected] 7 8 9 10 11 12 13 14 15 16 17 18 19 1 20 Abstract: Coastal erosion is a natural hazard which causes significant loss to properties 21 as well as coastal habitats. Coastal districts of Mahanadi delta, one of the most populated 22 deltas of the Indian subcontinent, are suffering from the ill effects of coastal erosion. An 23 important amount of assets is being lost every year along with forced migration of huge 24 portions of coastal communities due to erosion. An attempt has been made in this study to 25 predict the future coastline of the Mahanadi Delta based on historical trends. Historical 26 coastlines of the delta have been extracted using semi-automated Tasselled Cap technique 27 from the LANDSAT satellite imageries of the year 1990, 1995, 2000, 2006 and 2010. 28 Using Digital Shoreline Assessment System (DSAS) tool of USGS, the trend of the 29 coastline has been assessed in the form of End Point Rate (EPR) and Linear Regression 30 Rate (LRR). A hybrid methodology has been adopted using statistical (EPR) and 31 trigonometric functions to predict the future positions of the coastlines of the years 2020, 32 2035 and 2050. The result showed that most of the coastline (≈65%) is facing erosion at 33 present. -
Application of Isotope Techniques to Xa9848334 Investigate Groundwater Pollution in India
APPLICATION OF ISOTOPE TECHNIQUES TO XA9848334 INVESTIGATE GROUNDWATER POLLUTION IN INDIA K. SHIVANNA, S.V. NAVADA, K.M. KULKARNI, U.K. SINHA, S. SHARMA Isotope Division, Bhabha Atomic Research Centre, Mumbai, India Abstract -Environmental isotopes (2H, 18O, 34S, 3H, and I4C ) techniques have been used along with hydrogeology and hydrochemistry to investigate:(a), the source of salinity and origin of sulphate in groundwaters of coastal Orissa, Orissa State, India and (b) to study the source of salinity in deep saline groundwaters of charnockite terrain at Kokkilimedu, South of Chennai, India. In the first case, as a part of a large drinking water supply project, thousands of hand pumps were installed from 1985. Many of them became quickly unacceptable for potable supply due to salinity, increased iron and sulphate contents of the groundwater. In this alluvial, multiaquifer system, fresh, brackish and saline groundwaters occur in a rather complicated fashion. The conditions change from phreatic to confined flowing type with increasing depth. The results of the isotope geochemical investigation indicate that the shallow groundwater(depth;<50m) is fresh and modern. Groundwater salinity in intermediate aquifer (50 - 100m) is due to the Flandrian transgression during Holocene period. Fresh and modern deep groundwater forms a well developed aquifer which receives recharge through weathered basement rock. The saline groundwater found below the fresh deep aquifer have marine water entrapped during late Pleistocene. The source of high sulphate in the groundwater is of marine origin. In the second case, under the host rock characterization programme, the charnockite rock formation at Kokkilimedu, Kalpakkam was evaluated to assess its suitability as host medium for location of a geological repository for high level radioactive waste. -
DISASTER MANAGEMENT PLAN. [Dowr] ****************************************** 1
DISASTER MANAGEMENT PLAN. [DoWR] ****************************************** 1. Introduction The state Odisha is ranked as the 5th most flood prone state of the country after UP, Bihar, Assam and West Bengal with a flood prone area of 33400 km2. The south-west monsoon brings rains to the state from June to September every year. The state receives an average annual rainfall of 1500 mm and more than 80% of it occurs during monsoon period only. The coastal districts of the state are more vulnerable to frequent low pressure, cyclonic storms, depression and deep depression. The state has five major river basins namely Mahanadi, Brahmani, Baitarani, Subarnarekha and Rushikulya which cause high floods in their respective deltas. The rivers like Vamshadhara and Burhabalang also cause flash floods due to instant runoff from their hilly catchment. It is a fact that the three major river system Mahanadi, Brahmani and Baitarani forms a single delta during high flood and in most of the cases the flood water of these three systems blend together causing considerable flood havoc. Besides the state has 476.40 kms of coastline on the west of Bay of Bengal. The flood problem becomes more severe when the flood synchronies with high tides causing slow recede of flood. The silt deposited constantly by the waves in the delta area raises the flood level and the rivers often overflow their banks. The flood problem in the state generally aggravated due to some or all of the reasons as below: - Erratic monsoon, heavy monsoon rainfall accompanied by low pressures, depressions, deep depressions and cyclones. - Dam releases due to heavy inflows, thus causing massive outflows in the river. -
The Life of Krishna Chaitanya
The Life of Krishna Chaitanya first volume of the series: The Life and Teachings of Krishna Chaitanya by Parama Karuna Devi published by Jagannatha Vallabha Vedic Research Center (second edition) Copyright © 2016 Jagannatha Vallabha Vedic Research Center All rights reserved. ISBN-13: 978-1532745232 ISBN-10: 1532745230 Our Jagannatha Vallabha Vedic Research Center is a non-profit organization, dedicated to the research, preservation and propagation of Vedic knowledge and tradition, commonly described as “Hinduism”. Our main work consists in publishing and popularizing, translating and commenting the original scriptures and also texts dealing with history, culture and the peoblems to be tackled to re-establish a correct vision of the original Tradition, overcoming sectarianism and partisan political interests. Anyone who wants to cooperate with the Center is welcome. We also offer technical assistance to authors who wish to publish their own works through the Center or independently. For further information please contact: Mataji Parama Karuna Devi [email protected], [email protected] +91 94373 00906 Contents Introduction 11 Chaitanya's forefathers 15 Early period in Navadvipa 19 Nimai Pandita becomes a famous scholar 23 The meeting with Keshava Kashmiri 27 Haridasa arrives in Navadvipa 30 The journey to Gaya 35 Nimai's transformation in divine love 38 The arrival of Nityananda 43 Advaita Acharya endorses Nimai's mission 47 The meaning of Krishna Consciousness 51 The beginning of the Sankirtana movement 54 Nityananda goes begging -
Comprehensive Disaster Management Plan (Updated Strategic Plan for Disaster Management)
DEPARTMENT OF WATER RESOURCES COMPREHENSIVE DISASTER MANAGEMENT PLAN (UPDATED STRATEGIC PLAN FOR DISASTER MANAGEMENT) MAHANADI- BURHABALANGA- PHAILIN-LEHAR-HELEN MAY’2018 BRAHAMANI-BAITARANI SUBARNAREKHA SOMETIMESDISASTERS AREINEVITABLE, BUTTIMELYTAKENPRECAUTIONARY MEASURES AND POST DISASTER RESCUE AND REHABILITATION ACTIVITIES MINIMISES THE LOSS TO A GREATER EXTENT. THE REPORT DESCRIBES THE STRATEGICPLANSFOR DISASTERMANAGEMENT BYSTATEWATERRESOURCES DEPARTMENT. DEPARTMENT O F WATER RESOURCES GOVERNMENT O F ODISHA DEPARTMENT OFWATER RESOURCES, GOVERNMENT OFODISHA COMPREHENSIVE DISASTER MANAGEMENT PLAN MAY’2018 Sl.No. Description of Items Page No. Chapter – 1: Introduction 1.1 Objective 1 1.2 Scope of the Plan 1 1.3 Overview of the Department 3 1.4 Acts, Rules and Policies governing the business of the department. 4 1.5 Institutional Arrangement for disaster management 4 1.5.1 Junior Engineer/Assistant Engineer 5 1.5.1.1 Pre-flood measures 5 1.5.1.2 Measures during flood 6 1.5.1.3 Post-flood measures 6 1.5.1.4 General 7 1.5.2 Assistant Executive Engineer (AEE) 7 1.5.2.1 Pre-flood measures 7 1.5.2.2 Measures during flood 8 1.5.2.3 Post-flood measures 8 1.5.2.4 General 9 1.5.3 Executive Engineer 9 1.5.3.1 Pre-flood measures 9 1.5.3.2 Measures during floods 9 1.5.3.3 Post-flood measures 10 1.5.3.4 General 10 1.5.4 Superintending Engineer 10 1.5.5 Chief Engineer / Chief Engineer & Basin Manager (CE & BM): 11 1.6 Preparation and implementation of departmental disaster management plan 12 Chapter – 2: Hazard, Risk and Vulnerability Analysis 2.1 Historical/past disaster/losses in the department 14 2.2 Emerging Concerns 22 Chapter-3: Capacity – Building Measures 3.1 Trainings and Capacity Building 23 3.2 Community Awareness and Community Preparedness Planning 23 3.3 Capacity Building of Community Task forces 24 3.4 Sustainable Management 25 3.5 Mitigation 25 3.6 DRR Master Planning for the Future 25 3.6.1 Community Engagement 26 3.6.2 Organizing Teams 26 3.7 Mitigation Capacity Building Needs & Workshop Planning 26 3.8 Workshop Planning. -
List of Rivers in India
Sl. No Name of River 1 Aarpa River 2 Achan Kovil River 3 Adyar River 4 Aganashini 5 Ahar River 6 Ajay River 7 Aji River 8 Alaknanda River 9 Amanat River 10 Amaravathi River 11 Arkavati River 12 Atrai River 13 Baitarani River 14 Balan River 15 Banas River 16 Barak River 17 Barakar River 18 Beas River 19 Berach River 20 Betwa River 21 Bhadar River 22 Bhadra River 23 Bhagirathi River 24 Bharathappuzha 25 Bhargavi River 26 Bhavani River 27 Bhilangna River 28 Bhima River 29 Bhugdoi River 30 Brahmaputra River 31 Brahmani River 32 Burhi Gandak River 33 Cauvery River 34 Chambal River 35 Chenab River 36 Cheyyar River 37 Chaliya River 38 Coovum River 39 Damanganga River 40 Devi River 41 Daya River 42 Damodar River 43 Doodhna River 44 Dhansiri River 45 Dudhimati River 46 Dravyavati River 47 Falgu River 48 Gambhir River 49 Gandak www.downloadexcelfiles.com 50 Ganges River 51 Ganges River 52 Gayathripuzha 53 Ghaggar River 54 Ghaghara River 55 Ghataprabha 56 Girija River 57 Girna River 58 Godavari River 59 Gomti River 60 Gunjavni River 61 Halali River 62 Hoogli River 63 Hindon River 64 gursuti river 65 IB River 66 Indus River 67 Indravati River 68 Indrayani River 69 Jaldhaka 70 Jhelum River 71 Jayamangali River 72 Jambhira River 73 Kabini River 74 Kadalundi River 75 Kaagini River 76 Kali River- Gujarat 77 Kali River- Karnataka 78 Kali River- Uttarakhand 79 Kali River- Uttar Pradesh 80 Kali Sindh River 81 Kaliasote River 82 Karmanasha 83 Karban River 84 Kallada River 85 Kallayi River 86 Kalpathipuzha 87 Kameng River 88 Kanhan River 89 Kamla River 90