Feasibility Study of the Salt Mines Storage Route, Step 1
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Accordance with the Generally Accepted Accounting Principles
TI'I TNTN FORM A (Pu6uant to Clause 31(a) of Listing Agreement) Sr Particu lars Details No. 1 Name of the Company Tata Chemicals Limited 2. Annual consolidated financial 31 March, 2015 statements for the year ended 3. Type of Audit observation Emphasis of Matter has been included in the Consolidated Audit Report. We draw atlention to Note 3o(ivxc) to the Consolidated financial statements which describes accounting of actuarial gains and losses on employee pension funds of overseas subsidiaries in "Reserves and Surplus" in accordance with the generally accepted accounting principles applicable in the country of incorporation for the reasons stated therein, as against such gains and losses being accounted in the Consolidated Statement of Profit and Loss as per the generally accepted accounting principles in lndia. Had the Group followed the practice of recognising such gains and losses in the Consolidated Statement of Profit and Loss, the Consolidated Net Profit before tax and Consolidated Net Profit after tax after the minority interest of the Group for the year ended 31"r March, 2015 would have been higher by { 285.18 crore and { 219.42 crore respectively. Our opinion is not qualified in respect o, this matter. Note 30 (ivXC) The actuarial gains and losses on the funds for employee benefits (pension plans) of the overseas subsidiaries have been accounted in "ReseNes and Surplus" in the consolidated financial statements in accordance with the generally accepted accounting principles applicable and followed in the respective country of incorporation. The Management is of the view that due to volatility and structure of the overseas pension funds, it is not considered practicable to adopt a common accounting policy and deviation is as permifted by AS 21. -
Salt Deposits in the UK
CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive Halite karst geohazards (natural and man-made) in the United Kingdom ANTHONY H. COOPER British Geological Survey, Keyworth, Nottingham, NG12 5GG, Great Britain COPYRIGHT © BGS/NERC e-mail [email protected] +44 (-0)115 936 3393 +44 (-0)115 936 3475 COOPER, A.H. 2002. Halite karst geohazards (natural and man-made) in the United Kingdom. Environmental Geology, Vol. 42, 505-512. This work is based on a paper presented to the 8th Multidisciplinary Conference on Sinkholes and the Engineering and Environmental impact of karst, Louisville, Kentucky, April 2001. In the United Kingdom Permian and Triassic halite (rock salt) deposits have been affected by natural and artificial dissolution producing karstic landforms and subsidence. Brine springs from the Triassic salt have been exploited since Roman times, or possibly earlier, indicating prolonged natural dissolution. Medieval salt extraction in England is indicated by the of place names ending in “wich” indicating brine spring exploitation at Northwich, Middlewich, Nantwich and Droitwich. Later, Victorian brine extraction in these areas accentuated salt karst development causing severe subsidence problems that remain a legacy. The salt was also mined, but the mines flooded and consequent brine extraction caused the workings to collapse, resulting in catastrophic surface subsidence. Legislation was enacted to pay for the damage and a levy is still charged for salt extraction. Some salt mines are still collapsing and the re-establishment of the post-brine extraction hydrogeological regimes means that salt springs may again flow causing further dissolution and potential collapse. -
About the Urban Development of Hallstatt
About the Urban Development of Hallstatt CONTENTS 1. STARTING POINT 2 2. TOPOGRAPHY 3 2.1. Topographical survey 3 The Lake 3 The Mountains 3 The Communes of the Lake of Hallstatt 3 The Market Commune of Hallstatt 3 Names of Streets, Meadows and Marshes 4 2.3. The Morphology of the Villages 4 The Market 4 Lahn 4 3. URBAN DEVELOPMENT 6 3.1 The Development of the Traffic Network 6 The Waterway 6 The Paths 6 The Street 7 The Railway 7 The Pipeline, the so called "Sulzstrenn" 7 3.2. The Evolution of the Buildings 9 3.2.1. The Market 9 The Early History and the Age of Romans 9 The Founding in the Middle Ages 9 The Extension in the 16th Century 9 The Stagnation since the Beginning of the 17th Century until the catastrophic conflagration in 175010 The "Amthof" 10 The Court Chapel 11 The Hospital 11 The Hospital Chapel 11 The "Pfannhaus" and the "Pfieseln" 11 The Recession, Starting in 1750 until the Beginning of Tourism 11 The Flourishing of Tourism 12 3.2.2. Lahn 12 The Roman Ages 12 The Modern Times 12 3.3. The Analysis of the Sites and the Structures 15 3.3.1. The Market 15 The Market Place 16 The Landing Place 16 3.3.2. Lahn 17 The Agricultural Area 17 The Industrial Area 17 The Expansion 17 The Condensing 18 4. ANHANG 19 4.1. Commissions Relation dieses hochen Mittels Hoff Raths Herrn v. Quiex die zu Haalstatt abgebrunnenen Sallz Pfannen betreffend. 19 5. -
Life at Low Water Activity
Published online 12 July 2004 Life at low water activity W. D. Grant Department of Infection, Immunity and Inflammation, University of Leicester, Maurice Shock Building, University Road, Leicester LE1 9HN, UK ([email protected]) Two major types of environment provide habitats for the most xerophilic organisms known: foods pre- served by some form of dehydration or enhanced sugar levels, and hypersaline sites where water availability is limited by a high concentration of salts (usually NaCl). These environments are essentially microbial habitats, with high-sugar foods being dominated by xerophilic (sometimes called osmophilic) filamentous fungi and yeasts, some of which are capable of growth at a water activity (aw) of 0.61, the lowest aw value for growth recorded to date. By contrast, high-salt environments are almost exclusively populated by prokaryotes, notably the haloarchaea, capable of growing in saturated NaCl (aw 0.75). Different strategies are employed for combating the osmotic stress imposed by high levels of solutes in the environment. Eukaryotes and most prokaryotes synthesize or accumulate organic so-called ‘compatible solutes’ (osmolytes) that have counterbalancing osmotic potential. A restricted range of bacteria and the haloar- chaea counterbalance osmotic stress imposed by NaCl by accumulating equivalent amounts of KCl. Haloarchaea become entrapped and survive for long periods inside halite (NaCl) crystals. They are also found in ancient subterranean halite (NaCl) deposits, leading to speculation about survival over geological time periods. Keywords: xerophiles; halophiles; haloarchaea; hypersaline lakes; osmoadaptation; microbial longevity 1. INTRODUCTION aw = P/P0 = n1/n1 ϩ n2, There are two major types of environment in which water where n is moles of solvent (water); n is moles of solute; availability can become limiting for an organism. -
Pleistocene and Flandrian Natural Rock Salt Subsidence at Arclid Green, Sandbach, Cheshire Peter Worsley
Pleistocene and Flandrian Natural Rock Salt Subsidence at Arclid Green, Sandbach, Cheshire Peter Worsley Abstract. This applied geological case study concerns the Quaternary geomorphological evolution of a small part of the lowland Cheshire characterised by ‘equifinal subsidence landforms’ resulting from the processes of rock salt dissolution and post Last Glacial Maximum glacial ice meltout. The context relates to environmental issues arising from the quarrying of Chelford Formation industrial ‘silica sands’. Problems related to natural and human induced rock salt dissolution are reviewed. The respective roles of Triassic bedrock halites, collapsed strata, periglacial alluvial sands and multiple glaciation in determining the local stratigraphy and allied landforms are discussed. The morphology and fill of a post glacial subsidence area is examined. It is concluded that natural rock salt dissolution is the principal process influencing the superficial deposits and geomorphology of the study area and that this process has been active over hundreds of thousand years. The deposition and survival of thick silica sands and the glacigenic sediments beneath is probably due to halite dissolution. In eastern Cheshire, a significant part of the lowland A further complicating factor is human induced salt geomorphology is characterised by an excellent subsidence exacerbated by historic shallow mining for example of what, in ‘General Systems Theory’ jargon, salt and wild brine pumping, for example, Ward, would be termed ‘equifinal behaviour’ (Chorley, (1887), Calvert (1915), Cooper (2002), Sherlock 1964), also known as polygenesis. Such behaviour in a (1922), Wallwork (1956, 1960), Waltham (1989), and geomorphological context envisages that different Waltham et al (2005). Following the near universal initial earth surface processes have resulted in similar enforced abandonment of these extraction techniques morphological outcomes. -
Salt (Chemistry) - Wikipedia
Salt (chemistry) - Wikipedia https://en.wikipedia.org/wiki/Salt_(chemistry) Salt (chemistry) In chemistry, a salt is a chemical compound consisting of an ionic assembly of cations and anions.[1] Salts are composed of related numbers of cations (positively charged ions) and anions (negatively charged ions) so that the product is electrically neutral (without a net charge). ese component ions can be inorganic, − − − such as chloride (Cl ), or organic, such as acetate (CH3CO2); and can be monatomic, such as fluoride (F ) 2− or polyatomic, such as sulfate (SO4 ). Contents Types of salt Properties Color Taste Odor Solubility Conductivity Melting point Nomenclature Formation Strong salt Weak salt See also References Types of salt Salts can be classified in a variety of ways. Salts that produce hydroxide ions when dissolved in water are called alkali salts. Salts that produce acidic solutions are acid salts. Neutral salts are those salts that are neither acidic nor basic. Zwierions contain an anionic and a cationic centre in the same molecule, but are not considered to be salts. Examples of zwierions include amino acids, many metabolites, peptides, and proteins.[2] Properties Color Solid salts tend to be transparent as illustrated by sodium chloride. + − In many cases, the apparent opacity or transparency are only BMIM PF6 , an ionic liquid related to the difference in size of the individual monocrystals. Since light reflects from the grain boundaries (boundaries between 1 von 6 29.03.21, 15:43 Salt (chemistry) - Wikipedia https://en.wikipedia.org/wiki/Salt_(chemistry) crystallites), larger crystals tend to be transparent, while the polycrystalline aggregates look like white powders. -
The Rise and Fall of the Marshalls of Northwich, Salt Proprietors: a Saga of the Industrial Era in Cheshire, 1720-1917
THE RISE AND FALL OF THE MARSHALLS OF NORTHWICH, SALT PROPRIETORS: A SAGA OF THE INDUSTRIAL ERA IN CHESHIRE, 1720-1917 BY D. A. IREDALE, M.A., PH.D. HEN Thomas Marshall from the Hartford Beach, near WNorthwich, appeared before a parliamentary committee in London in 1817, he proudly proclaimed himself the largest salt proprietor in the kingdom. The wealthiest merchant in mid-Cheshire, Marshall determined that his family should one day sit on committees and at table with the greatest in the land. To this end he sent his son to Eton, Cambridge, and the Middle Temple. And his grandson did indeed climb towards the highest levels of society. I FOUNDING THE FAMILY FORTUNE During the seventeenth century the Marshalls lived in Nant- wich. They began business as shoemakers, then as framework knitters. By hard work they grew prosperous, so that when Richard Marshall died in 1692 the family owned a fine "dwelling house in the welshrow" and valuable textile machinery. But living in one of Cheshire's salt towns, the family naturally acquired a "wich-house & twelve leads walling", that is, equip ment for raising and boiling brine to produce salt. Salt had long been valued as a preservative and seasoner of food by the fisheries and the navy, by dairy farmers and every housewife, but during the industrial age it was to become an important raw material in the glass, soap, and chemical industries. To invest in salt, therefore, was to plan sensibly for future prosperity. The Marshalls sent much of their cloth and, probably, small loads of salt overland to Northwich, and then by river or road to Liverpool. -
Over and Winsford Archaeological Assessment 2003
CHESHIRE HISTORIC TOWNS SURVEY Over and Winsford Archaeological Assessment 2003 CHESHIRE HISTORIC TOWNS SURVEY Over and Winsford Archaeological Assessment 2003 Environmental Planning Cheshire County Council Backford Hall Backford Chester CH1 6PZ These reports are the copyright of Cheshire County Council and English Heritage. We would like to acknowledge the assistance of Cheshire and Chester Archives and Local Studies, Frodsham and District Local History Group, Winsford Local History Society, Andrew Fielding, Lion Salt Works Project Director and Dr Chris Lewis, University of Liverpool, in the preparation of these reports. The archive is held by the Cheshire County Sites and Monuments Record. The Ordnance Survey mapping within this document is provided by Cheshire County Council under licence from the Ordnance Survey, in order to fulfil its public function to make available Council held public domain information. The mapping is intended to illustrate the spatial changes that have occurred during the historical development of Cheshire towns. Persons viewing this mapping should contact Ordnance Survey copyright for advice where they wish to licence Ordnance Survey mapping/map data for their own use. The OS web site can be found at www.ordsvy.gov.uk OVER & WINSFORD ARCHAEOLOGICAL ASSESSMENT Jo Clark 1. SUMMARY The small medieval settlements of Over and Wharton, which lie 1.5km west and 0.75km east of the River Weaver respectively, have long since been subsumed by the expanding township of Winsford, which lies between the two on the banks of the river. Winsford’s prosperity was founded upon the exploitation of brine in the 18th and 19th centuries and the efficient transportation afforded by the Weaver Navigation. -
Integrated-Annual-Report-Fy-2019-20
June 14, 2020 The General Manager The Manager, Listing Department Corporate Relations Department The National Stock Exchange of India Limited BSE Limited Exchange Plaza Phiroze Jeejeebhoy Towers Bandra-Kurla Complex Dalal Street Bandra (E) Mumbai - 400 001 Mumbai - 400 051 Scrip Code: 500770 Symbol: TATACHEM Dear Sir/Madam, Sub.: Annual Report under Regulation 34(1) of the SEBI (Listing Obligations and Disclosure Requirements) Regulations, 2015 (‘Listing Regulations’) This is in furtherance to our letter dated May 22, 2020 wherein the Company had informed that the 81st Annual General Meeting (‘AGM’) of the Company will be held on Tuesday, July 7, 2020 at 3.00 p.m. (IST) via two-way Video Conference / Other Audio Visual Means only, in accordance with the General Circular issued by the Ministry of Corporate Affairs dated May 5, 2020 read with General Circulars dated April 8, 2020 and April 13, 2020 and SEBI Circular dated May 12, 2020. Pursuant to Regulation 34(1) of the Listing Regulations, please find enclosed the Integrated Annual Report of the Company along with the Notice of the 81st AGM and other Statutory Reports for the Financial Year 2019-20, which is also being sent through electronic mode to those Members whose e-mail addresses are registered with the Company/Registrar and Transfer Agent/ Depositories. The same is also available on the website of the Company at https://www.tatachemicals.com/investors/financial-reports/Yearly-reports. This is for your information and records. Thanking you, Yours faithfully, For Tata Chemicals Limited Rajiv Chandan General Counsel & Company Secretary Encl.: as above Advancing Science. -
Saltscape Project, Northwich, Cheshire
Saltscape Project A8: The salt fields investigating the salt production landscape in Northwich’s historic saltscape SALTSCAPE PROJECT, NORTHWICH, CHESHIRE ASSESSMENT OF SITES FOR ARCHAEOLOGICAL FIELDWORK PROJECT A8: THE SALT FIELDS INVESTIGATING THE SALT PRODUCTION LANDSCAPE IN NORTHWICH’S HISTORIC SALTSCAPE REPORT NO 2015-001 Chris Hewitson Senior Environment Officer Regeneration and Culture Cheshire West and Chester [email protected] February 2015 Version 1 1 Saltscape Project A8: The salt fields investigating the salt production landscape in Northwich’s historic saltscape 1. Background prevalent. The site is currently appears to be used The project seeks to investigate using for recreational off-road vehicles. archaeological methods the salt production Risks and Issues landscape north-east of Northwich. This area The area is subsiding and collapses of the Trent and contains the tourist nodes of the Lion Salt Works Mersey Canal have occurred in the last two years. and the Anderton Boat Lift. Now, these represent Open areas of water are located centrally within the the only industrial structures from the 19th and area of the mine and public and volunteer access early 20th century in an essentially post-industrial may be limited because of the potential risks. landscape. The project seeks to re-associate the wider public with the earlier landscape and aims to The land is privately owned and clearly marked as reassert the link between the visible structures and such. There is a strong likelihood that access issues the buried past. In doing so the project will training will prevent archaeological work in this area. for volunteers in archaeological techniques, increase education in the historic industrial Site 2 – Alliance Works landscape and deliver a new and updated data set Location: Adjacent to the Trent and Mersey Canal on the historic environment of the ‘Saltscape’ and the Lion Salt Works (NGR SJ 671 754). -
United Kingdom Minerals Yearbook 2006 British Geological Survey
United Kingdom Minerals Yearbook 2006 British Geological Survey United Kingdom Minerals Yearbook 2006 Statistical data to 2005 By L E Hetherington, T J Brown, P A J Lusty, K Hitchen and T B Colman Keyworth, Nottingham: British Geological Survey 2007 BRITISH GEOLOGICAL SURVEY © NERC 2007 All rights reserved The full range of Survey publications is available from the Copyright in materials derived from the British Geological BGS Sales Desk at Nottingham, Edinburgh and London; Survey’s work is owned by the Natural Environment see contact details below or shop online at Research Council (NERC) and/or the authority that www.geologyshop.com commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the The London Information Office also maintains a reference BGS Intellectual Property Rights Section, British Geological collection of BGS publications including maps for consultation. Survey, Keyworth, e-mail [email protected]. The Survey publishes an annual catalogue of its maps and You may quote extracts of a reasonable length without other publications; this catalogue is available from any prior permission, provided a full acknowledgement is given of the BGS Sales Desks. of the source of the extract. The British Geological Survey carries out the geological survey of Great Britain and Northern Ireland (the latter as All communications regarding the content of this an agency service for the government of Northern Ireland), publication should be addressed to the Programme and of the surrounding continental shelf, as well as its Manager, Economic Minerals, British Geological Survey, basic research projects. It also undertakes programmes of Keyworth, Nottingham NG12 5GG British technical aid in geology in developing countries as = 0115 936 3493 Fax 0115 936 3520 arranged by the Department for International Development e-mail: [email protected] and other agencies. -
United Kingdom Minerals Yearbook 2005 British Geological Survey United Kingdom Minerals Yearbook 2005
United Kingdom Minerals Yearbook 2005 British Geological Survey United Kingdom Minerals Yearbook 2005 Statistical data to 2004 By L E Taylor, T J Brown, P A J Lusty, K Hitchen, T B Colman and D E Highley Keyworth, Nottingham: British Geological Survey 2006 BRITISH GEOLOGICAL SURVEY © NERC 2006 All rights reserved The full range of Survey publications is available from the Copyright in materials derived from the British Geological BGS Sales Desk at Nottingham, Edinburgh and London; Survey’s work is owned by the Natural Environment see contact details below or shop online at Research Council (NERC) and/or the authority that www.geologyshop.com commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the The London Information Office also maintains a reference BGS Intellectual Property Rights Section, British Geological collection of BGS publications including maps for consultation. Survey, Keyworth, e-mail [email protected]. The Survey publishes an annual catalogue of its maps and You may quote extracts of a reasonable length without other publications; this catalogue is available from any prior permission, provided a full acknowledgement is given of the BGS Sales Desks. of the source of the extract. The British Geological Survey carries out the geological survey of Great Britain and Northern Ireland (the latter as All communications regarding the content of this an agency service for the government of Northern Ireland), publication should be addressed to the Programme and of the surrounding continental shelf, as well as its Manager, Economic Minerals, British Geological Survey, basic research projects. It also undertakes programmes of Keyworth, Nottingham NG12 5GG British technical aid in geology in developing countries as ຜ 0115 936 3493 Fax 0115 936 3520 arranged by the Department for International Development e-mail: [email protected] and other agencies.