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Thiruvallur District
DISTRICT DISASTER MANAGEMENT PLAN FOR 2017 TIRUVALLUR DISTRICT tmt.E.sundaravalli, I.A.S., DISTRICT COLLECTOR TIRUVALLUR DISTRICT TAMIL NADU 2 COLLECTORATE, TIRUVALLUR 3 tiruvallur district 4 DISTRICT DISASTER MANAGEMENT PLAN TIRUVALLUR DISTRICT - 2017 INDEX Sl. DETAILS No PAGE NO. 1 List of abbreviations present in the plan 5-6 2 Introduction 7-13 3 District Profile 14-21 4 Disaster Management Goals (2017-2030) 22-28 Hazard, Risk and Vulnerability analysis with sample maps & link to 5 29-68 all vulnerable maps 6 Institutional Machanism 69-74 7 Preparedness 75-78 Prevention & Mitigation Plan (2015-2030) 8 (What Major & Minor Disaster will be addressed through mitigation 79-108 measures) Response Plan - Including Incident Response System (Covering 9 109-112 Rescue, Evacuation and Relief) 10 Recovery and Reconstruction Plan 113-124 11 Mainstreaming of Disaster Management in Developmental Plans 125-147 12 Community & other Stakeholder participation 148-156 Linkages / Co-oridnation with other agencies for Disaster 13 157-165 Management 14 Budget and Other Financial allocation - Outlays of major schemes 166-169 15 Monitoring and Evaluation 170-198 Risk Communications Strategies (Telecommunication /VHF/ Media 16 199 / CDRRP etc.,) Important contact Numbers and provision for link to detailed 17 200-267 information 18 Dos and Don’ts during all possible Hazards including Heat Wave 268-278 19 Important G.Os 279-320 20 Linkages with IDRN 321 21 Specific issues on various Vulnerable Groups have been addressed 322-324 22 Mock Drill Schedules 325-336 -
Ocean Drilling Program Scientific Results Volume
9. GEOCHEMICAL EXPRESSION OF EARLY DIAGENESIS IN MIDDLE EOCENE-LOWER OLIGOCENE PELAGIC SEDIMENTS IN THE SOUTHERN LABRADOR SEA, SITE 647, ODP LEG 1051 M. A. Arthur,2 W. E. Dean,3 J. C. Zachos,2 M. Kaminski,4 S. Hagerty Rieg,2 and K. Elmstrom2 ABSTRACT Geochemical analyses of the middle Eocene through lower Oligocene lithologic Unit IIIC (260-518 meters below seafloor [mbsf]) indicate a relatively constant geochemical composition of the detrital fraction throughout this deposi tional interval at Ocean Drilling Program (ODP) Site 647 in the southern Labrador Sea. The main variability occurs in redox-sensitive elements (e.g., iron, manganese, and phosphorus), which may be related to early diagenetic mobility in anaerobic pore waters during bacterial decomposition of organic matter. Initial preservation of organic matter was me diated by high sedimentation rates (36 m/m.y.). High iron (Fe) and manganese (Mn) contents are associated with car bonate concretions of siderite, manganosiderite, and rhodochrosite. These concretions probably formed in response to elevated pore-water alkalinity and total dissolved carbon dioxide (C02) concentrations resulting from bacterial sulfate reduction, as indicated by nodule stable-isotope compositions and pore-water geochemistry. These nodules differ from those found in upper Cenozoic hemipelagic sequences in that they are not associated with methanogenesis. Phosphate minerals (carbonate-fluorapatite) precipitated in some intervals, probably as the result of desorption of phosphorus from iron and manganese during reduction. The bulk chemical composition of the sediments differs little from that of North Atlantic Quaternary abyssal red clays, but may contain a minor hydrothermal component. The silicon/ aluminum (Si/Al) ratio, however, is high and variable and probably reflects original variations in biogenic opal, much of which is now altered to smectite and/or opal CT. -
Meteoric Be and Be As Process Tracers in the Environment
Chapter 5 Meteoric 7Be and 10Be as Process Tracers in the Environment James M. Kaste and Mark Baskaran 7 10 Abstract Be (T1/2 ¼ 53 days) and Be (T1/2 ¼ occurring Be isotopes of use to Earth scientists are the 7 1.4 Ma) form via natural cosmogenic reactions in the short-lived Be (T1/2 ¼ 53.1 days) and the longer- 10 atmosphere and are delivered to Earth’s surface by wet lived Be (T1/2 ¼ 1.4 Ma; Nishiizumi et al. 2007). and dry deposition. The distinct source term and near- Because cosmic rays that cause the initial cascade of constant fallout of these radionuclides onto soils, vege- neutrons and protons in the upper atmosphere respon- tation, waters, ice, and sediments makes them valuable sible for the spallation reactions are attenuated by tracers of a wide range of environmental processes the mass of the atmosphere itself, production rates of operating over timescales from weeks to millions of comsogenic Be are three orders of magnitude higher in years. Beryllium tends to form strong bonds with oxygen the stratosphere than they are at sea-level (Masarik and atoms, so 7Be and 10Be adsorb rapidly to organic and Beer 1999, 2009). Most of the production of cosmo- inorganic solid phases in the terrestrial and marine envi- genic Be therefore occurs in the upper atmosphere ronment. Thus, cosmogenic isotopes of beryllium can be (5–30 km), although there is trace, but measurable used to quantify surface age, sediment source, mixing production as oxygen atoms in minerals at the Earth’s rates, and particle residence and transit times in soils, surface are spallated (in situ produced; see Lal 2011, streams, lakes, and the oceans. -
4. a Growth Model for Polymetallic Nodules
A GEOLOGICAL MODEL OF POLYMETALLIC NODULE DEPOSITS IN THE CLARION‐CLIPPERTON FRACTURE ZONE ISA TECHNICAL STUDY SERIES Technical Study No. 1 Global Non‐Living Resources on the Extended Continental Shelf: Prospects at the year 2000 Technical Study No. 2 Polymetallic Massive Sulphides and Cobalt‐Rich Ferromanganese Crusts: Status and Prospects Technical Study No. 3 Biodiversity, Species Ranges and Gene Flow in the Abyssal Pacific Nodule Province: Predicting and Managing the Impacts of Deep Seabed Mining Technical Study No. 4 Issues associated with the Implementation of Article 82 of the United Nations Convention on the Law of the Sea Technical Study No. 5 Non‐Living resources of the Continental Shelf beyond 200 nautical miles: Speculations on the Implementation of Article 82 of the United Nations Convention on the Law of the Sea PAGE | II A GEOLOGICAL MODEL OF POLYMETALLIC NODULE DEPOSITS IN THE CLARION‐ CLIPPERTON FRACTURE ZONE This report contains a summary of two documents – A Geological Model of Polymetallic Nodule Deposits in the Clarion‐Clipperton Fracture Zone and a Prospector’s Guide prepared under the project ‘Development of a Geological Model of Polymetallic Nodule Deposits in the Clarion‐Clipperton Fracture Zone, Pacific Ocean’. ISA TECHNICAL STUDY: NO. 6 International Seabed Authority Kingston, Jamaica PAGE | III The designation employed and the presentation of materials in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the International Seabed Authority concerning the legal status of any country or territory or of its authorities, or concerning the delimitation of its frontiers or maritime boundaries. All rights reserved. -
ECONOMIC ASPECTS of NODULE MINING Although Deep-Sea
CHAPTER 11 ECONOMIC ASPECTS OF NODULE MINING J. L. MERO INTRODUCTION Although deep-sea manganese nodules were discovered over a'century ago by scientists of the HMS Challenger expedition, few analyses of the nodules for the economically significant elements such as nickel, copper, cobalt and molybdenum were made in those early days and no consideration was given to these deposits as a possible commercial source of metals until the early 1950's when the mining of the nodules was advocated as a possible source of manganese (Mero, 1952). As the result of a haul of nodules taken in relatively shallow water (900 m) about 370 km east of Tahiti on the western edge of the Tuamoto Plateau during the 1957-58 International Geophysical Year (the nodules contained about 2% of cobalt, a valuable metal at that particular time), a study was initiated by the Institute of Marine Resources of the University of California to determine if it might be economic to mine and process the nodules for their cobalt, nickel and copper contents. The results of that study were favourable' with respect to the technical and economic factors involved in mining and processing the nodules. All the research and development in this matter dates from the release of the report describing the results of that study (Mero, 1958). To the present time (1975) over $150 million* has been expended in the exploration of the nodule deposits and in the development of mining and processing systems. An additional $100 million is to be spent in the next few years in these activities. -
THE RECORD NEWS ======The Journal of the ‘Society of Indian Record Collectors’ ------ISSN 0971-7942 Volume: Annual - TRN 2011 ------S.I.R.C
THE RECORD NEWS ============================================================= The journal of the ‘Society of Indian Record Collectors’ ------------------------------------------------------------------------ ISSN 0971-7942 Volume: Annual - TRN 2011 ------------------------------------------------------------------------ S.I.R.C. Units: Mumbai, Pune, Solapur, Nanded and Amravati ============================================================= Feature Articles Music of Mughal-e-Azam. Bai, Begum, Dasi, Devi and Jan’s on gramophone records, Spiritual message of Gandhiji, Lyricist Gandhiji, Parlophon records in Sri Lanka, The First playback singer in Malayalam Films 1 ‘The Record News’ Annual magazine of ‘Society of Indian Record Collectors’ [SIRC] {Established: 1990} -------------------------------------------------------------------------------------------- President Narayan Mulani Hon. Secretary Suresh Chandvankar Hon. Treasurer Krishnaraj Merchant ==================================================== Patron Member: Mr. Michael S. Kinnear, Australia -------------------------------------------------------------------------------------------- Honorary Members V. A. K. Ranga Rao, Chennai Harmandir Singh Hamraz, Kanpur -------------------------------------------------------------------------------------------- Membership Fee: [Inclusive of the journal subscription] Annual Membership Rs. 1,000 Overseas US $ 100 Life Membership Rs. 10,000 Overseas US $ 1,000 Annual term: July to June Members joining anytime during the year [July-June] pay the full -
MF Coastal Radio Stations
M.F. Coastal & Maritime Stations 1608 kHz to 4000 kHz This list was last amended 17th September 2008 TX Freq. RX Freq. Mode Callsign Station Name/Frequency Usage Country 1609 2144 SITOR TYA Cotonou Radio Benin 1612 2417 SITOR SUQ Ismaila Radio Egypt 1613 2148 SITOR TYA Cotonou Radio Benin 1614 2149 SITOR SUH El Iskandariya (Alexandria) Radio Egypt 1615 2150 SITOR TYA Cotonou Radio Benin 1615.5 2150.5 SITOR SVH Iraklion Kritis Radio Crete Greece 1618.5 2153.5 SITOR SUK Kosseir Radio Egypt 1621.5 2156.5 DSC LGP Bödo Radio Norway 1621.5 2156.5 DSC National Norwegian Channel Norway 1621.5 2156.5 DSC LGS Svalbard Radio Svalbard 1621.5 2156.5 DSC LGT Tjome Radio Norway 1621.5 2156.5 DSC LGV Vardö Radio Norway 1624.5 2159.5 DSC OXZ Lyngby Radio Denmark 1624.5 2159.5 DSC OXJ Torshavn Radio Faeroe Islands 1627.5 2162.5 DSC Den Helder Rescue Traffic Service Netherlands 1635 2060 SSB LGV Vardö/Hammerfest Radio Norway 1636.4 2045 SSB HZH Jeddah Radio Saudi Arabia 1638 2022 SSB OFK Turku/Vaasa Radio Finland 1641 2045 SSB OXJ Torshavn Radio Faeroe Islands 1641 2066 SSB OXJ Torshavn Radio Faeroe Islands 1642.5 1642.5 SSB Den Helder Rescue (Dutch Coast Guard) Netherlands 1644 2069 SSB EAL Las Palmas/Arrecife Radio Canary Islands 1644 2069 SSB EJM Malin Head Coast Guard Radio Republic of Ireland 1650 2075 SSB TYA Cotonou Radio Benin 1650 Broadcast SSB CROSS Griz-Nez France 1650 Broadcast SSB CROSS Corsen France 1650 Broadcast SSB CROSS Jobourg France 1650 SSB Kardla Piirivalve MRSCC Estonia 1650 SSB Kuressaare Piirivalve MRSCC Estonia 1650 2182 SSB 5VA -
Study of the Structure Model of Todorokite
Title Study of the Structure Model of Todorokite Author(s) Miura, Hiroyuki Citation 北海道大学理学部紀要, 23(1), 41-51 Issue Date 1991-07 Doc URL http://hdl.handle.net/2115/36772 Type bulletin (article) File Information 23-1_p41-51.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP Jour. Fac. Sci., Hokkaido Univ., Ser. IV, vol. 23, no. 1, July., 1991, pp. 41 -51 STUDY OF THE STRUCTURE MODEL OF TODOROKITE by Hiroyuki Miura (with 5 text-figures and 3 tables) Abstract The X - ray diffraction study of todorokite from Japan was carried out and appropriate struc tural model was calculated by Rietveld method. The calculation of the theoretical diffraction pattern was done for a layer structural model and the calculated results show that the layer model can explain the observed diffraction data. Some of the properties of todorokite such as superstructure or shrinkage of c-axis on heating can be explained by the layer model which con tains random H 20 between the [MnOs] layers. Introduction Todorokite is a manganese oxide mineral having H 20 in its structure. It was reported first from the Todoroki gold mine, Hokkaido, Japan (Yoshimura, 1934) . This mineral occurs as aggregate of fine acicular crystals. It also contains H20, Ca, Ba and Mg. The X -ray powder diffraction data of todorokite clearly show diffraction peaks of 9.6, 4.8, 3.2, 2.45 and 1.42 A. Since 1934 there has been many reports of todorokite like minerals from all over the world (Frondel, 1953; Frondel et aI. , 1960; Ljunggren, 1960; Straczek et aI., 1960; Faulring, 1961 ; Larson, 1962; Radtke et aI., 1967; Lawrence et aI., 1968; Harada, 1982; Siegel and Turner, 1983) . -
Chennai District Origin of Chennai
DISTRICT PROFILE - 2017 CHENNAI DISTRICT ORIGIN OF CHENNAI Chennai, originally known as Madras Patnam, was located in the province of Tondaimandalam, an area lying between Pennar river of Nellore and the Pennar river of Cuddalore. The capital of the province was Kancheepuram.Tondaimandalam was ruled in the 2nd century A.D. by Tondaiman Ilam Tiraiyan, who was a representative of the Chola family at Kanchipuram. It is believed that Ilam Tiraiyan must have subdued Kurumbas, the original inhabitants of the region and established his rule over Tondaimandalam Chennai also known as Madras is the capital city of the Indian state of Tamil Nadu. Located on the Coromandel Coast off the Bay of Bengal, it is a major commercial, cultural, economic and educational center in South India. It is also known as the "Cultural Capital of South India" The area around Chennai had been part of successive South Indian kingdoms through centuries. The recorded history of the city began in the colonial times, specifically with the arrival of British East India Company and the establishment of Fort St. George in 1644. On Chennai's way to become a major naval port and presidency city by late eighteenth century. Following the independence of India, Chennai became the capital of Tamil Nadu and an important centre of regional politics that tended to bank on the Dravidian identity of the populace. According to the provisional results of 2011 census, the city had 4.68 million residents making it the sixth most populous city in India; the urban agglomeration, which comprises the city and its suburbs, was home to approximately 8.9 million, making it the fourth most populous metropolitan area in the country and 31st largest urban area in the world. -
Officials from the State of Tamil Nadu Trained by NIDM During the Year 209-10 to 2014-15
Officials from the state of Tamil Nadu trained by NIDM during the year 209-10 to 2014-15 S.No. Name Designation & Address City & State Department 1 Shri G. Sivakumar Superintending National Highways 260 / N Jawaharlal Nehru Salai, Chennai, Tamil Engineer, Roads & Jaynagar - Arumbakkam, Chennai - 600166, Tamil Nadu Bridges Nadu, Ph. : 044-24751123 (O), 044-26154947 (R), 9443345414 (M) 2 Dr. N. Cithirai Regional Joint Director Animal Husbandry Department, Government of Tamil Chennai, Tamil (AH), Animal husbandry Nadu, Chennai, Tamil Nadu, Ph. : 044-27665287 (O), Nadu 044-23612710 (R), 9445001133 (M) 3 Shri Maheswar Dayal SSP, Police Superintending of Police, Nagapattinam District, Tamil Nagapattinam, Nadu, Ph. : 04365-242888 (O), 04365-248777 (R), Tamil Nadu 9868959868 (M), 04365-242999 (Fax), Email : [email protected] 4 Dr. P. Gunasekaran Joint Director, Animal Animal Husbandary, Thiruvaruru, Tamil Nadu, Ph. : Thiruvarur, Tamil husbandary 04366-205946 (O), 9445001125 (M), 04366-205946 Nadu (Fax) 5 Shri S. Rajendran Dy. Director of Department of Agriculture, O/o Joint Director of Ramanakapuram, Agriculture, Agriculture Agriculture, Ramanakapuram (Disa), Tamil Nadu, Ph. : Tamil Nadu 04567-230387 (O), 04566-225389 (R), 9894387255 (M) 6 Shri R. Nanda Kumar Dy. Director of Statistics, Department of Economics & Statistics, DMS Chennai, Tamil Economics & Statistics Compound, Thenampet, Chennai - 600006, Tamil Nadu Nadu, Ph. : 044-24327001 (O), 044-22230032 (R), 9865548578 (M), 044-24341929 (Fax), Email : [email protected] 7 Shri U. Perumal Executive Engineer, Corporation of Chennai, Rippon Building, Chennai - Chennai, Tamil Municipal Corporation 600003, Ph. : 044-25361225 (O), 044-65687366 (R), Nadu 9444009009 (M), Email : [email protected] National Institute of Disaster Management (NIDM) Trainee Database is available at http://nidm.gov.in/trainee2.asp 58 Officials from the state of Tamil Nadu trained by NIDM during the year 209-10 to 2014-15 8 Shri M. -
Jallikattu’ in Tamil Nadu, India
Vol. 11(3),pp. 20-30, March 2019 DOI: 10.5897/JMCS2018.0644 Article Number: 75BE85960500 ISSN: 2141-2545 Copyright © 2019 Journal of Media and Communication Author(s) retain the copyright of this article http://www.academicjournlas.org/JMCS Studies Review The voices of culture, conservation and the media event around bullfight ‘Jallikattu’ in Tamil Nadu, India Jayashree B1*, Arul Aram1 and Yasmin Ibrahim2 1Department of Media Science, Faculty of Humanities and Social Sciences, Anna University, Chennai, India. 2International Business and Communication, Queen Mary, University of London, UK. Received 1 December, 2018; Accepted 11 February, 2019 In the Southern Indian ‘State of Tamil Nadu’, the traditional Jallikattu sport involving young men competing against bulls is described as one of the ancient living sports in the modern era. Based on petitions by animal rights groups, the Supreme Court of India banned the ancient sport of Jallikattu in 2014 on the grounds of animal cruelty. The ban of this traditional sport ignited protests culminating in a large-scale 15-day movement across the state from January 8 to 23, 2017 with a massive mobilization on the world’s second longest beach, the Marina in the state capital of Chennai. Largely propelled by the youths, the ban was perceived as an attack on Tamil culture and identity. The anger was directed at foreign animal rights activism and an unstable political situation gained momentum with media attention. This resulted in the promulgation of a central Act to overturn the ban and facilitate conduct of the sport. This paper examines the role of social media rallying the public and activism against the Jallikattu ban. -
Petrogenesis of Ferromanganese Nodules from East of the Chagos Archipelago, Central Indian Basin, Indian Ocean
ELSEVIER Marine Geology 157 (1999) 145±158 Petrogenesis of ferromanganese nodules from east of the Chagos Archipelago, Central Indian Basin, Indian Ocean Ranadip Banerjee a,Ł, Supriya Roy b, Somnath Dasgupta b, Subir Mukhopadhyay b, Hiroyuki Miura c a Geological Oceanography Division, National Institute of Oceanography, Dona Paula, Goa 403004, India b Department of Geological Sciences, Jadavpur University, Calcutta, 700032, India c Department of Geology and Mineralogy, Faculty of Science, Hokkaido University, Sapporo, 060, Japan Received 28 May 1997; accepted 24 July 1998 Abstract Deep-sea ferromanganese nodules occur over a large area and on many different sediment types of the Central Indian Basin, Indian Ocean. Selected samples were studied to determine their chemical and mineralogical compositions and microstructural features. Repeated laminations of variable thickness, alternately dominated by todorokite and vernadite, are characteristic of these nodules. These laminae show, on electron microprobe line scans, corresponding interlaminar partitioning of Mn±Cu±Ni and Fe±Co. The bulk chemical compositions of these nodules plot in both the hydrogenetic and early diagenetic ®elds on the Fe±Mn±(Ni C Cu C Co) ð10 ternary diagram. The binary diagram depicting the covariation of Mn C Ni C Cu against Fe C Co shows two distinct parallel regression lines, one delineated by nodules from terrigenous, siliceous ooze and siliceous ooze±terrigenous sediments and the other by nodules from red clay, siliceous ooze±red clay and calcareous ooze±red clay. An increasing diagenetic in¯uence in the nodules with the nature of the host sediment types was observed in the sequence: terrigenous ! siliceous ooze and red clay ! siliceous=calcareous ooze±red clay.