4.0 Characterising Sites and Salt-Producers. the Archaeology of an Ancient Craft and Identification of ‘Know-How’ 4.1 Introduction
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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. -
Benchmark 3: Evaluation of Alternatives with Respect to Existing Conditions August 2015
Salton Sea Funding and Feasibility Action Plan Benchmark 3: Evaluation of Alternatives With Respect to Existing Conditions August 2015 Prepared by: Prepared for: This document is prepared as a living document for public review and comment. Comments may be provided to: Salton Sea Authority 82995 Hwy 111, Suite 200 Indio, CA 92201 Email: [email protected] Comments will be reviewed and incorporated as appropriate. If substantive comments are received, a revised document may be produced and distributed. Preferred citation: Salton Sea Authority (2015). Salton Sea Funding and Feasibility Action Plan Benchmark 3 Report: Evaluation of Alternatives With Respect to Existing Conditions, August Report. Revision Record Revisions to this document will be reviewed and approved through the same level of authority as the original document. All changes to the Benchmark 3 Report must be authorized by the Principal in Charge. Date Version Changes January Working Posted on Salton Sea Authority website. 2015 Draft Included changes from draft review by Salton Sea TCT. June 2015 First Updated hydrology section and inflow Complete projections including Figures 48-52, along with Document editorial revisions. August Revision 1 Added this Revision Record. Corrected title of 2015 California Department of Fish and Wildlife and other minor editorial revisions. Updated discussion of historical flows from 2003-present. Tetra Tech, Inc. i August 2015 Executive Summary This report presents a review of Salton Sea restoration alternatives and their components and determine how well they would perform under current and future inflows. Alternatives are considered with respect to existing hydrologic conditions at the Sea, as of 2014, and projected future hydrology. -
The Changing Technology of Post Medieval Sea Salt Production in England
1 Heritage, Uses and Representations of the Sea. Centro de Investigação Transdisiplinar Cultura, Espaço e Memoría (CITCEM) Porto, Faculdade de Letras da Universidade do Porto, 20-22 October 2011. The changing technology of post medieval sea salt production in England Jeremy Greenwood Composition of seawater Sea water contains 3.5% evaporites of which salt (sodium chloride) comprises 77.8%. The remainder is known as bittern as it includes the bitter tasting, aperient and deliquescent sulphates of magnesium (Epsom salt) and sodium (Glauber’s salt) as well as about 11% magnesium chloride. 2 Successful commercial salt making depends on the fractional crystallisation of seawater producing the maximum amount of salt without contamination by bittern salts. As seawater is evaporated, very small amounts of calcium carbonate are precipitated followed by some calcium sulphate. This is followed by the crystallisation of sodium chloride but before this is complete, bitter Epsom salt appears; something that needs to be avoided.1 In Continental Europe, evaporation of sea water is achieved solely by the energy of the wind and sun but this is not possible in the English climate so other techniques were developed. 1 http://www.solarsaltharvesters.com/notes.htm SOLAR SALT ENGINEERING 3 Evaporation vessel Briquetage The earliest known English method of coastal saltmaking has been found in the late Bronze Age. This involved boiling seawater in crude clay dishes supported by clay firebars (briquetage) and was widespread in Europe. This technique continued into the Iron Age and into the Roman period with variations inevitably occurring in the industry, although the dating of saltworks is very problematical.2 Detailed interpretation continues to be a matter of dispute. -
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. -
UNIVERSITY of CAMBRIDGE V R SWITSUR and R G WEST Sub
[RADIOCARBON, VOL. 17, No. 1, 1975, P. 35-51] UNIVERSITY OF CAMBRIDGE NATURAL RADIOCARBON MEASUREMENTS XIII V R SWITSUR and R G WEST Sub-department of Quaternary Research, 5 Salisbury Villas, Station Road, Cambridge, England The dates presented here were calculated from measurements made at the University Radiocarbon Dating Research Laboratory mostly dur- ing 1973-74. The radioactivity of the samples was counted in gas pro- portional detectors, either silica lined (de Vries et al, 1959) or of pure copper, filled to 2 atmospheres pressure with pure carbon dioxide. The detectors were fixed in, and completely surrounded by, a plastic scintil- lator anticoincidence shield mounted inside a massive lead shield to protect against environmental radiation (Switsur, Hall and West, 1970). Modern sample gas was obtained from the combustion of AD 1845 to 1855 rings of an oak tree grown near Cambridge and felled in 1950. Background samples were prepared from Welsh anthracite. The con- temporary sample was frequently compared with the activity of the NBS oxalic acid international standard. Age calculations were based on the 14C half-life of 5568 years and the uncertainty stated as one stand- ard deviation calculated from the statistical analyses of sample and standards counting rates. Oxidation of the samples was performed in high pressure oxygen in a `bomb' combustion unit (Switsur et al, 1970; Switsur, 1972; Switsur and West, 1973) followed by purification of the carbon dioxide produced. The technique was modified slightly for samples such as limnic mud deposits or gyttja which often contain excessive electronegative impuri- ties and require more extensive purification than wood or charcoal samples. -
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. -
Active Surface Salt Structures of the Western Kuqa Fold-Thrust Belt, Northwestern China
Active surface salt structures of the western Kuqa fold-thrust belt, northwestern China Jianghai Li1, A. Alexander G. Webb2,*, Xiang Mao1, Ingrid Eckhoff2, Cindy Colón2, Kexin Zhang2, Honghao Wang1, An Li2, and Dian He2,† 1The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China 2Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana 70803, USA ABSTRACT fold-thrust belt display a variety of erosion- dynamics of salt motion. Although geo scientists tectonics interactions, with nuances refl ect- have interpreted thousands of salt sheets in The western Kuqa fold-thrust belt of Xin- ing the low viscosity and high erodibility of more than 35 basins worldwide (Hudec and jiang Province, China, hosts a series of surface salt, including stream defl ections, potential Jackson, 2006, 2007), subaerial preservation of salt structures. Here we present preliminary tectonic aneurysm development, and even halite salt structures is rare (Talbot and Pohjola, analysis of the geometry, kinematics, and sur- an upper-crustal test site for channel fl ow– 2009; Barnhart and Lohman, 2012). A fraction face processes of three of these structures: the focused denudation models. of these subaerial salt structures occur in active Quele open-toed salt thrust sheet, Tuzima- settings, where boundary conditions of ongoing zha salt wall, and Awate salt fountain. The INTRODUCTION deformation can be geodetically characterized. fi rst two are line-sourced, the third appears The Kuqa fold-thrust belt of Xinjiang Prov- to be point-sourced, and all are active. The Among common solid Earth materials, salt is ince, northwestern China, offers a new prospect ~35-km-long, 200-m-thick Quele open-toed distinguished by uncommonly low density, low for subaerial investigation of a range of active salt thrust sheet features internal folding, viscosity, near incompressibility, high solubil- salt structures. -
Ventures in Salt: Compass Minerals International Rebecca M
08-064 July 10, 2009 Ventures in Salt: Compass Minerals International Rebecca M. Henderson, John Sterman, Ramana Nanda As Michael Ducey, the President and CEO of Compass Minerals International, looked out of his office in Overland Park, Kansas on the evening of December 11, 2003, he wondered how investors would react to his company going public. Ducey had joined Compass Minerals in April 2002 as CEO and strategic investor, a few months after the private equity firm Apollo Management had acquired it from IMC Global.1 Although salt companies were not typical candidates for IPOs, Compass Minerals had done very well in its two years as a stand-alone firm, and Ducey had encouraged his fellow investors to consider exiting via an IPO. With Goldman Sachs leading its IPO the following day, Ducey considered the response of investors and his strategy going forward. Where should he be focusing his attention? How could he ensure that the company lived up to the high expectations of its investors? A Short History of Salt Salt was one of the most widely used minerals in the world. Although it had thousands of applications, in the United States it was primarily used for highway deicing, and as an input into the chemicals, food-processing, water-treatment, and agricultural industries. 1 Although some parts of the current operations of Compass Minerals go back over a hundred years, its most recent structure arose from a series of ownership changes that began in 1998. On April 1, 1998 IMC Global purchased the salt and chemicals businesses of Harris Chemical Group ($450 MM in cash and $950 MM raised in debt), including the North American Salt Company, the Great Salt Lake Minerals Corp in the US, and Salt Union in the UK. -
EB018 Maldon District Historic Environment Characterisation Project
HISTORICEB018 ENVIRONMENT Maldon District Historic Environment Characterisation Project 2008 abc i EB018 Front Cover: Aerial view of the Causeway onto Northey Island ii EB018 Contents FIGURES........................................................................................................................................................... VII ABBREVIATIONS .............................................................................................................................................IX ACKNOWLEDGEMENTS..................................................................................................................................X MALDON DISTRICT HISTORIC ENVIRONMENT CHARACTERISATION PROJECT..................... 11 1 INTRODUCTION ..................................................................................................................................... 11 1.1 PURPOSE OF THE PROJECT ................................................................................................................... 12 2 THE HISTORIC ENVIRONMENT OF MALDON DISTRICT .......................................................... 14 2.1 INTRODUCTION ................................................................................................................................... 14 3 CHARACTERISATION OF THE RESOURCE.................................................................................... 33 3.1 HISTORIC ENVIRONMENT CHARACTER AREA DESCRIPTIONS.............................................................. 35 3.1.1 HECA 1 Blackwater -
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.