India: Implementation of Clean Technology Through Coal Beneficiation
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Jh G Ha Go Ar Odd Kh Da Ha a and D
DISTRICT SURVEY REPORT OF SAND GOGODDADA JHHAARKHAHAND Content Table Sl. Content Page No. No. 1. Introduction 2-3 2. Overview of Mining Activity in the District 3 3. The List of Mining Leases in the District with 4-9 location, area and period of validity 4. Details of Royalty or Revenue received in last three 9 years 5. Detail of Production of Sand or Bajari or minor 9 mineral in last three years 6. Process of Deposition of Sediments in the rivers of 9-10 the District 7. General Profile of the District 10 8. Land Utilization Pattern in the district: Forest, 10 Agriculture, Horticulture, Mining etc. 9. Physiography of the District 11-12 10. Rainfall: month-wise 13 11. Geology and Mineral Wealth 13-16 12. General Recommendations 17-18 12. Annexure- I 19-22 13. Annexure- II 23-24 14. Annexure- III 25 INTRODUCTION: As per the guidelines issued in Para 7 (iii) of Part-II- Section-3-Sub Section (ii) of Extraordinary Gazette of MoEF&CC, Government of India, New Delhi dated 15.01.2016 and in concurrence to directives issued by the Chief Secretary to Government, Government of Jharkhand vide letter no. 1874/C.S. dated 01/08/17 a District Survey Report (DSR) is to be prepared for each district in Jharkhand. The main spirit of preparing this report is to encourage Sustainable Mining and development. In this direction a team comprising of Mines and Geology, Irrigation, or Remote Sensing departments were given the task for preparing this report. An extensive field work was carried on 28/08/2017 and 29/08/2017 by the members of the committee to assess the possibilities of sand mining in the Godda district. -
Correlation of Coal Seams in Chirimiri Coalfield, M.P., on the Basis of Sporae Dispersae*
CORRELATION OF COAL SEAMS IN CHIRIMIRI COALFIELD, M.P., ON THE BASIS OF SPORAE DISPERSAE* D. C. BHARADWA} & S. C. SRIVASTAVA Birbal Sahni Institute of Palaeobotany, Lucknow ABSTRACT MA TERIAL AND METHODS Fifteen samples of coal collected from different 15 samples of coal in 72 B.S. mesh size parts of Chirimiri Coalfield, M.P., have been sporo• from all over the area were studied (Table 1). logically investigated. The qualitative and quanti• These samples were subjected to similar tative composition of the samples at generic level indicates that the general dominance is consti• maceration procedure in each case. Five tuted by Lophotriletes, Microbaculispora, Indotri• gms. of material from each sample was radites and Sulcatisporites. In addition to these, treated with HNOa (comm.) for 3 days Horriditriletes, Retusotriletes, Potonieisporites, Fauni• followed by digestion with 10 per cent pollenites and Ginkgocycadophytus are characteristi• cally associated with the dominants. The asso• KOH after thorough washing with water ciation of these genera has enabled segregation of as detailed by Bharadwaj (1962) and Bhara• the samples into three assemblages. Assemblage A dwaj and Salujha (1964). The macerates is dominated by Microbaculispora. Assemblage B were mounted on slides in glycerine jelly. 500 is dominated by Microbaculispora in association with Indotriradites and Assemblage C has the miospores were counted from each sample dominance of Microbaculispora associated with at the generic level. Retusotriletes and Potonieisporites. It is suggested From Table 1 it is apparent that samples that the samples represent three coal seams corres• CACl - (129), (126), (143)E, (145)E and ponding to Assemblages A, B & C. -
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Bull. Soc. belge Géologie V. 84 fasc. pp. 11-17 Bruxelles 1975 Bull. Belg. Ver. Geologie T. 84 deel blz. 11-17 Brussel 197 5 PALYNOLOGICAL COMPOSITION OF THE BASAL GONDWANA IN INDIA by R.S. TIWARI (*) ABSTRACT. - Talchir Formation represents the basal Gondwana deposits and commences with the glacial environment. The playnofloras show, in general, the overwhelming dominance of the girdling (radial) monosaccate miospore genera. In the present work, the relative position of each mioflora has been determined, and on the basis of variation analysis, dominance trends as well as the qualitative considerations of the spore-pollen-complex, three zones have been suggested to be existing in the Talchirs. 1. ACKNOWLEDGEMENTS and variegated and break up in a pattern of needles hence named « needle shales ». The I take this opportunity to express my best age of the Talchirs has been variably assessed wishes and compliments to Professor Ir. W. in the past te be the Upper Carboniferous, v AN LECKWIJCK, in whose honour this special Permo/Carboniferous or the Lower Permian. meeting has been organized. I also thank to The present knowledge of the Talchir paly the Société Belge de Géologie, de Paléontologie nology provides information that the basic et d'Hydrologie for extending an invitation for nature of the miofloras in boulder beds as contribution in this meeting. well as in the shales, closely resemble with each other by virtue of the dominance of the monosaccate genera. However, little is known 2. INTRODUCTION about the inter-relationships of these varying assemblages and their relative position in suc The Talchirs form the basal depositions of cession. -
M/S Bharat Aluminium Company Limited Korba-495684 Chhattisgarh
PRE-FEASIBILITY REPORT FOR PROPOSED 1.0 MTPA COAL MINING AT CHOTIA-II COAL MINE AT SALAIGOT VILLAGE, TEHSIL PODIUPRODHA, KORBA DISTRICT, CHHATTISGARH By M/s Bharat Aluminium Company Limited Korba-495684 Chhattisgarh Submitted to Ministry of Environment, Forest & Climate Change (MoEF&CC) New Delhi February-2016 1 CONTENTS Sr. No. Title Page no. 1 EXECUTIVE SUMMARY 3 2 PREAMBLE 3 3 LOCATION AND ACCESSIBILITY 4 4 INTRODUCTION OF THE PROJECT/BACKGROUND 9 INFORMATION 5 ENVIRONMENTAL SENSITIVITY 14 6 INFRASTRUCTURE 15 7 REHABILITATION AND RESETTLEMENT (R & R) PLAN 17 8 PROJECT SCHEDULE & COST ESTIMATES 17 2 1.0 Executive Summary 1.1 The Company Bharat Aluminium Company Ltd (BALCO) is a major player in non-ferrous metals having its headquarters in Delhi. BALCO was established in 1965 at Korba, Chhattisgarh, as a Government of India undertaking with integrated smelter capacity of 1,00,000 tpa and alumina refinery capacity of 2,45,000 tpa. BALCO was the first major Public Sector Organization which went through the economic reforms and disinvested 51% stake to Sterlite Group in 2001 remaining 49% stake is held by Government of India. 2.0 Preamble This block was earlier operated by Prakash Industries Limited. Supreme Court of India, cancelled all allocated coal block in Aug 2008. Post cancellation, Govt. of India promulgated „Coal Mines (Special Provision) Ordinance‟ and coal blocks were auction through a transparent electronic bidding process. BALCO won this mine in that bidding process and the said mine was handed over with the existing infrastructure to BALCO after making the required payment w.e.f 1st April, 2015. -
Recast Project Report for Dhankasa U/G Mine Executive
RECAST P.R. FOR DHANKASA UG MINE-1.0 Mty (MAY-2016) CMPDI RECAST PROJECT REPORT FOR DHANKASA U/G MINE EXECUTIVE SUMMARY 1.0 INTRODUCTION 1.1 GENERAL The proposed Dhankasa UG Mine has been planned in the Geological blocks of Dhankasa and Naheriya (partly). These Geological Blocks are located in the north- eastern part of Pench-Kanhan Valley Coalfield, District Chhindwara, Madhya Pradesh. The area is covered in the Survey of India Topo-sheet No. 55 N/3 (RF 1:50,000) and is defined by Latitudes N 22o17'39" and N 22 o19'33" and Longitudes E 78o59'04" and E 79o01'13". The nearby operating mines are Naheriya UG & Urdhan OC. Naheriya U/G Mine is about 6 kms from proposed Dhankasa U/G Mine. Thesgora and Mathani mines are about 22 kms on the western side of Dhankasa Block. Dhankasa UG will be under the administrative control of Western Coalfields Limited. 1.2 HISTORY OF MINING Dhankasa geological block is a virgin block. Dhankasa U/G project is aimed at bridging the deficit in supply of coal partially from Pench Kanhan Coalfield as well as WCL. The report has proposed the deployment of mass production technology in order to generate higher production and productivity levels. Dhankasa block lies between Sonpur and Naheriya Blocks and Jamunia Block forms the south western boundary. North-south flowing Junapani nalla and east- west flowing Dhankasa nalla pass along the western and southern boundaries of the block. This Report has proposed to exploit proved reserves of 9 sectors in the Geological Block-i.e. -
Permian Palynoflora from Lo Godavari Valley Coalfield, A
Journal of Natural Sciences Research www.iiste.org ISSN 2224-3186 (Paper) ISSN 2225-0921 (Online) Vol.2, No.7, 2012 Permian Palynoflora from Lower Gondwana Sediments of Godavari Valley Coalfield, Andhra Pradesh, South India L. Mahesh Bilwa * Nagamadhu. C. J Prameela. M Department of Earth Science, University of Mysore, Manasagangotri, Mysore – 570 006, Karnataka, Ind ia *E-mail: [email protected] -mysore.ac.in, [email protected] Abstract Palynological investigation of Lower Gondwana sediments of Goutham Khani Open Cast Mine (GKOCM) from Kothagudem sub basin of Godav ari Valley Coalfield, Andhra Pradesh of Peninsular India have revealed two palynoassemblages are related to Early Permian (Barakar Formation). Palynoassemblage – A abundantly occurrence of Scheuringipollenites along with other common taxa like Parasaccites, Ibisporites , Primuspollenites, Sulcatisporites, Rhizomaspora, Densipollenites and Corisaccites and Palynoassemblage – B dominated by Scheuringipollenites along with sub dominance of Faunipollenites, Striatopodocarpites , Parasaccites, Striatites, Tiwariasporis, Rhizomaspora, Verticipollenites , Platysaccus, Primuspollenites, Lunatisporites , Latosporites, Ibisporites and Distriatites. The above demarcated palynoassemblages are applied to correlate with other horizons of Lower Gondwana deposits of India and a lso to fix the relative age for the sediments under investigation. Key words : Permian Age, Lower Gondwana, Palynoassemblage, Godavari Valley Coalfield, Sothern India. 1.Introduction Gondwana sediments of India can be broadly classified under two main geographic areas like Peninsular and Extra Peninsular regions. Presently based o n Gondwana floral remains like mega and micro fossil evidences can be applied to divide in to Lower Gondwana and Upper Gondwana sometimes Middle Gondwana with remains of Dicardium floral (mixed characters of both Monocot and Dicots) remains. Godavari Vall ey coalfield is a store house for non coking coal varity in Southern India. -
Inventory of Geological Resource of Indian Coal I/ 1
Table-1 INVENTORY OF GEOLOGICAL RESOURCE OF INDIAN COAL (As on 01.04.2010) (Resource in million tonne) State/ Coalfield/ Type of coal Depth Proved Indicated Inferred Inferred Total (Exploration) (Mapping) 1 2 3 4 5 6 7 WEST BENGAL 1.RANIGANJ COALFIELD MEDIUM COKING 0-300 194.70 1.60 0.00 196.30 300-600 15.30 16.90 0.00 32.20 MEDIUM COKING Total 210.00 18.50 0.00 228.50 SEMI-COKING 0-300 45.75 14.19 0.00 59.94 300-600 109.51 113.23 23.48 246.22 600-1200 32.79 305.07 144.75 482.61 SEMI-COKING Total 188.05 432.49 168.23 788.77 NON-COKING COAL 0-300 9544.54 1865.79 260.99 11671.32 300-600 1682.46 3444.57 2345.87 7472.90 600-1200 13.22 1887.28 1668.82 3569.32 NON-COKING Total 11240.22 7197.64 4275.68 22713.54 TOTAL FOR RANIGANJ 11638.27 7648.63 4443.91 23730.81 2.BARJORA COALFIELD NON-COKING COAL 0-300 114.27 0.00 0.00 114.27 NON-COKING Total 114.27 0.00 0.00 114.27 TOTAL FOR BARJORA 114.27 0.00 0.00 114.27 3.BIRBHUM COALFIELD NON-COKING COAL 0-300 0.00 609.96 40.01 649.97 300-600 0.00 3597.38 523.19 4120.57 600-1200 0.00 1173.64 48.58 1222.22 NON-COKING Total 0.00 5380.98 611.78 5992.76 TOTAL FOR BIRBHUM 0.00 5380.98 611.78 5992.76 4.DARJEELING COALFIELD NON-COKING COAL 0-300 0.00 0.00 15.00 15.00 NON-COKING Total 0.00 0.00 15.00 15.00 TOTAL FOR DARJEELING 0.00 0.00 15.00 15.00 TOTAL FOR WEST BENGAL 11752.54 13029.61 5070.69 29852.84 JHARKHAND 5.RANIGANJ COALFIELD MEDIUM COKING 0-300 220.00 8.87 0.00 228.87 300-600 49.23 8.30 0.00 57.53 MEDIUM COKING Total 269.23 17.17 0.00 286.40 SEMI-COKING 0-300 51.40 0.00 0.00 51.40 300-600 0.00 40.00 -
MATHEMATICAL MODELING on CONCENTRATION LEVELS for MAXIMUM DISPOSAL of COAL WASTE in DAMODAR RIVER Dr
International Journal of Research in Engineering, Technology and Science, Volume VII, Special Issue, Feb 2017 www.ijrets.com, [email protected], ISSN 2454-1915 MATHEMATICAL MODELING ON CONCENTRATION LEVELS FOR MAXIMUM DISPOSAL OF COAL WASTE IN DAMODAR RIVER Dr. Shafique Ahmad1, Dr. Narayan Mahto2 and Dr. P. Mahto3 1Department of Mathematics, B.D.A. College, Pichhri, Bokaro 2Department of Mathematics, R.S.P. College, Jharia 3Department of Mathematics, R.S. More College , Dhanbad ABSTRACT: The quantity and quality of water now a day a very serious problem in many region especially in industrial and mining area of India. Damodar river basin is repository of 45% of India coal reserve. Exploitation of coal & related industries in the area has exerted a great impact on the water pollution. In this paper an attempt has been made to develop a mathematical model to obtain concentration levels of Damodar river under different dumping policies so as to select the policy which disposes maximum waste without exceeding acceptable limits. An analytical solution is obtained to study the concentration levels of pollution for different time histories in Damodar river. The model can be useful in guiding engineering and management decision concerned with the efficient utilization of Damodar river water & protect their quality. Keywords: Damodar River; water pollution; coal mining activities; time history; concentration level;environment; coal waste; Dhanbad. [1] INTRODUCTION Damodar basin extends from 23˚28’32” N. Latitudes to 24˚31’30”N. Latitude and 84˚41’ 00”E. Longitude to 86 51’45” E. Longitude. The basin starts from high hills of Palamu in Jharkhand to Hooghly in West Bengal and stretches over nearly 18,100 Sq.Km. -
A Subsidiary of Coal India Limited)
ANNUAL REPORT & ACCOUNTS 2006-2007 CENTRAL MINE PLANNING & DESIGN INSTITUTE LIMITED (A Subsidiary of Coal India Limited) GONDWANA PLACE: KANKE ROAD RANCHI - 834 008 CONTENTS Sl. No. Subjects Page 1. Management During 2006-2007 2. Present Management 3. Notice 4. Directors' Report 5. Statutory Auditors' Report and replies of Management. 6. Comments of the Comptroller & Auditor General of India under section 619(4) and replies of Management. 7. Audited Statements of Accounts 8. Annexure to Directors Report under Section 217 (2A) MANAGEMENT DURING 2006-2007 FULL - TIME 1. Shri S. Chaudhuri : CMD 2. Shri P. K. Kanchan : Director 3. Shri N. C. Jha : Director (Upto 31.12.2006) 4. Shri S. Chakrabarti : Director (Upto 31.03.2007) 5. Shri S. R. Ghosh : Director PART - TIME 6. Shri Pradeep Kumar : Director (Upto 23.10.2006) 7. Dr. S. P. Seth : Director (From 23.10.2006) 8. Prof. A. K. Ghose : Director 9. Shri Sanjiv Mittal : Director 10. Shri Lakshman Jha : Director (Upto 31.12.2006) 11. Shri N. C. Jha : Director (From 01.01.2007) COMPANY SECRETARY : Shri Udayan Chakrabarti BANKERS : State Bank of India, United Bank of India, Bank of India. Canara Bank Bank of Maharastra Union Bank of India, Oriental Bank of Commerce Indian Overseas Bank State Bank of Indore Central bank of India UCO Bank AUDITORS : M/s U. Narain & Co. Chartered Accountants Ranchi. REGISTERED OFFICE : Gondwana Place, Kanke Road, Ranchi - 834 008 Jharkhand, India PRESENT MANAGEMENT AS ON 31.10.2007 FULL - TIME 1. Shri S. Chaudhuri : Chairman cum Managing Director 2. Shri N. Khurana : Director 3. -
Coal Industry's Contribution to Water- Ecosystem
Coal Industry’s Contribution to Water- Ecosystem Through Gainful Utilization of Mine-Water WESTERN COALFIELDS LIMITED (A subsidiary of Coal India Limited) Mine Water Utilisation - Process Aquifers in Indian coal bearing formations constitute of sandstone, while coal acts as aquitards allowing formation of unconfined & confined aquifers resulting in high water table; Also low sulphur content(<1%) means no Acid Mine Drainage(AMD) Mine Dewatering Percolated & logged water from mines is removed through Treatment in settling tanks pumps Extracted water is treated through a series of settling tanks Pipeline Transport Water is transported to desired location through HDPE pipelines Filtration Water is Treated through Pressure Filters, Sand Filters, Reverse Osmosis & Ozonisation Plants GAINFUL USE OF MINE WATER 380 120 160 LtrsMil/Da LtrsMil/Da LtrsMil/Da y y y Total Discharge of All Utilised for Internal use – To Be Utilized for Mines in WCL Spraying, Washing, Dust Community Distribution Suppression PROJECTS DRIKING WATER Boreholes, Checkdams, Pressure Filters IRRIGATION Desilting and Widening of RO Plants in Villages ponds GROUND WATER RECHARGE Creating Shared Value Reconceiving needs, Redefining Improving the local products, and customers productivity in the business environment Meeting societal needs value chain through products Using resources, Improving the suppliers, logistics, Addressing unserved or communities in which a and employees more underserved customers company operates productively RO Water Plants & Disposal of mine RO Water Plants & Coal Neer water into local Ground water Initiatives channels recharge • Creating new • Improves • Clean drinking customers livelihoods of water local populace • Products at • Irrigation lower price Water Supply for Drinking Water Hybrid Water Cooperatives •WCL has invested in setting up Water Treatment plants with 1000 liters per hour capacity in villages. -
Project Report for U/G Mine
Pre-feasibility Report of Giridih-Kabribad Group of Mines (1.3 MTY), CCL Kabribad OC 1.1 BACKGROUND OF THE PROJECT Giridih Coalfield is one of the earliest coalfields to be worked in India. Mining activity in the coalfield started as early as 1871 by M/s Bengal Coal Company & then by State Railway and subsequently transferred to National Coal Development Corporation (NCDC) about 60 years back. Later in the year 1973, it came under the control of Central Coalfields limited (CCL), a subsidiary of Coal India Limited. Presently it is under the administrative control of B&K Area of CCL. The Kabribad Re-organisation mine falls in Giridih Coalfield. It is situated in Giridih district in the state of Jharkhand. This colliery belongs to the Giridih Project, which is under B&K Area of CCL. It is located about 5km to the south of Giridih Town and is covered in Survey of India toposheet 72L/8. The block under consideration is Deep Pit Sector (Kabribad sub-basin) of Giridih Coalfield which has an area of about 2.79 sq km. The sector has been mined extensively by a number of UG inclines and quarries in the past. Although the underground workings has been discontinued/ abandoned but the quarry operation is still being carried out in the central part of the sector. Project report of Kabribad OCP (0.6 MTY) is being prepared based on the Report on the Exploratory Operations in the Selected Blocks, Giridih Coalfield, District – Hazaribagh, Bihar, IBM, 1959 and Geological Report on Coal Exploration of Jubilee Pit, U.K. -
UNIT – I PHYSIOGRAPHIC DIVISIONS of INDIA Geological Structure
UNIT – I PHYSIOGRAPHIC DIVISIONS OF INDIA Geological Structure 1. THE ARCHAEAN FORMATIONS (PRE-CAMBRIAN) The Archaean Era is also known as the Precambrian Period. The division of geologic time scale from the formation of the Earth (about 4.6 billion years ago) to the beginning of the Cambrian Period of the Paleozoic Era (about 570 million years ago}. The Precambrian time constitutes about 86.7% of the Earth's history. The term 'Archaean', introduced by J.D. Dana in 1782, refers to the oldest rocks of the Earth's crust. The oldest known rocks of the Earth, the evolutionary atmosphere, the first chemosynthesis, the first photosynthesis, the life-supporting atmosphere and the Earth's modem atmosphere, were developed during the Precambrian Era (Archaean and Protozoic). Rocks of the Archaean System are devoid of any form of life. The Archaean rocks are all azoic or non fossiliferous. They are thoroughly crystalline, extremely contorted and faulted, and practically devoid of any sediment. They are largely intruded by plutonic intrusions and generally have a well-defined foliated structure. These rocks are known as the basement complex or fundamental gneisses. Cover two-thirds of Peninsular India. In the Peninsular region, the Archaean rocks are known to be of three well-defined types: a) The Bengal Gneiss occurs in the Eastern Ghats, Orissa (known as Khodoliles after Khond tribes in Koraput and Bolangir districts), stretching over Manbhum and Hazaribagh districts of Jharkhand, Nellore district of Andhra Pradesh and Salem district of Tamil Nadu. Occur in the Son Valley, Meghalaya Plateau and Mikir HiUs. Thinly foliated.