Salt in Prehistoric Europe Prehistoric in Salt
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Halite Nacl C 2001-2005 Mineral Data Publishing, Version 1
Halite NaCl c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Cubic. Point Group: 4/m32/m. Crystals cubic, to 1 m, or octahedral; elongated along [100] or [111], skeletal with hopper-shaped faces. Rarely capillary or stalactitic; granular, compact, massive. Physical Properties: Cleavage: {001}, perfect. Fracture: Conchoidal. Tenacity: Brittle. Hardness = 2–2.5 D(meas.) = 2.168 D(calc.) = 2.165 Soluble in H2O, saline taste; rarely fluoresces red under SW UV. Optical Properties: Transparent. Color: Colorless or white when pure; gray, yellow, orange, pink, red, blue, purple; colorless to faintly tinted in thin section. Streak: White. Luster: Vitreous. Optical Class: Isotropic; weakly anisotropic due to stress. Dispersion: Moderately strong. n = 1.5443 Cell Data: Space Group: Fm3m. a = 5.6404(1) Z = 4 X-ray Powder Pattern: Synthetic. 2.821 (100), 1.994 (55), 1.628 (15), 3.258 (13), 1.261 (11), 1.1515 (7), 1.410 (6) Chemistry: (1) (2) Na 39.00 39.34 K 0.12 Mg 0.03 Ca 0.08 Cl 60.27 60.66 SO4 0.27 Total 99.77 100.00 (1) Cardona, Barcelona, Spain. (2) NaCl. Occurrence: Typically in sedimentary rocks of evaporite association, may form immense beds; also as volcanic sublimates, efflorescences, cave deposits. Crystals are common in multiphase fluid inclusions; may be included in other minerals as a product of intermediate-grade metamorphism. Association: Sylvite, polyhalite, kieserite, carnallite, gypsum, anhydrite, dolomite. Distribution: Of worldwide occurrence. Well-studied deposits include: in Austria, around Hallstadt, Salzburg, and Hall, near Innsbruck, Tirol. From Bex, Vaud, Switzerland. In Germany, from Stassfurt-Leopoldshall, 34 km south of Magdeburg, Saxony-Anhalt. -
Sodium Chloride (Halite, Common Salt Or Table Salt, Rock Salt)
71376, 71386 Sodium chloride (Halite, Common Salt or Table Salt, Rock Salt) CAS number: 7647-14-5 Product Description: Molecular formula: NaCl Appearance: white powder (crystalline) Molecular weight: 58.44 g/mol Density of large crystals: 2.17 g/ml1 Melting Point: 804°C1 Density: 1.186 g/ml (5 M in water)2 2 Solubility: 1 M in H2O, 20°C, complete, clear, colorless 2 pH: 5.0-8.0 (1 M in H2O, 25°C) Store at room temperature Sodium chloride is geologically stable. If kept dry, it will remain a free-flowing solid for years. Traces of magnesium or calcium chloride in commercial sodium chloride adsorb moisture, making it cake. The trace moisture does not harm the material chemically in any way. 71378 BioUltra 71386 BioUltra for molecular biology, 5 M Solution The products are suitable for different applications like purification, precipitation, crystallisation and other applications which require tight control of elemental content. Trace elemental analyses have been performed for all qualities. The molecular biology quality is also tested for absence of nucleases. The Certificate of Analysis provides lot-specific results. Much of the sodium chloride is mined from salts deposited from evaporation of brine of ancient oceans, or recovered from sea water by solar evaporation. Due to the presence of trace hygroscopic minerals, food-grade salt has a small amount of silicate added to prevent caking; as a result, concentrated solutions of "table salt" are usually slightly cloudy in appearance. 71376 and 71386 do not contain any anti-caking agent. Applications: Sodium chloride is a commonly used chemical found in nature and in all body tissue, and is considered an essential nutrient. -
F Is for Flavor.Pdf
!! ™ This is an introductory version of Chef Jacob’s Culinary Bootcamp Workbook and F-STEP™ curriculum. You can download the complete curriculum here. 2 !! Third Edition Copyright © 2015 Jacob Burton All rights reserved. 3 4 !! WHAT IS F-STEP?!.....................................................................................11 F IS FOR FLAVOR!.....................................................................................13 UNDERSTANDING FLAVOR STRUCTURE! 14 What is flavor?! 14 Salty! 15 Sweet! 20 Sour! 21 Bitter! 22 Umami! 22 Umami Ingredient Chart! 26 Piquancy! 28 Flavor And Aroma! 28 The Importance Of Fat And Flavor! 29 Texture! 30 Tannins! 30 Flavor’s X Factor! 31 Preventing Palate Fatigue! 32 Delivering A “Flavor Punch”! 33 Using “Flavor Interruptions”! 33 CHOOSING PRIMARY AND SECONDARY FLAVORS! 34 SELECTING NON SEASONAL INGREDIENTS! 35 Buying Spices! 35 Herbs! 36 Poultry! 37 5 Seafood! 37 Beef! 39 Pork! 41 GUIDE TO SEASONAL PRODUCE! 42 Winter! 42 December! 42 January! 44 February! 45 Spring! 46 March! 46 April! 47 May! 49 Summer! 49 June! 50 July! 50 August! 52 Fall! 54 September! 54 October! 55 November! 58 S IS FOR SAUCE!.......................................................................................60 CULINARY STOCKS! 62 Basic Recipe for Protein-Based Stocks! 63 SAUCE THICKENERS! 63 Roux! 64 6 !! Liaison! 65 Other Sauce Thickeners At A Glance! 66 The Three Modern Mother Sauces! 67 REDUCTION SAUCES! 67 Reduction Sauce Process! 69 Tips For Reinforcing Flavors! 70 Reduction Stage! 70 Tips For Reduction! 71 Pan Sauces! -
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. -
City of Bennington Ordinance Book
CITY OF BENNINGTON ORDINANCE BOOK Chapter I (1) ADMINISTRATION Article 1 City Elections Article 2 Governing Body Article 3 Officers and Employees Article 4 Oaths and Bonds Article 5 Municipal Court Article 6 Fire Department Organization Article 7 Recreation Commission Article 8 Capital Improvement Fund Article 9 Equipment Reserve Fund Article 10 Ambulance Service Organization Chapter II (2) ANIMALS AND FOWL Article 1 Animals Article 2 Dogs and Cats Chapter III (3) BEVERAGES Article 1 Alcoholic Liquor Article 2 Cereal Malt Beverage Chapter IV (4) BUILDINGS AND CONSTRUCTION Article 1 Building Code Article 2 Dangerous Structures Article 3 City Planning Commission Article 4 Miscellaneous Article 5 Solar Energy Systems Article 6 Cross – Connections Chapter V (5) LICENSES AND BUSINESS REGULATIONS Article 1 Solicitors, Canvassers, and Peddlers Article 2 Operation Licenses – Amusement Chapter VI (6) FIRE REGULATIONS Article 1 Fire Limits Article 2 Fire Regulations Article 3 Fireworks Chapter VII (7) HEALTH AND SANITATION Article 1 Health Nuisances Article 2 Refuse Regulations Article 3 Sewer Regulations Chapter VIII (8) PUBLIC OFFENSES Article 1 Uniform Public Offense Code Article 2 Supplementary Offenses Chapter IX (9) STREETS, SIDEWALKS, AND PUBLIC PROPERTY Article 1 Street Regulations Article 2 Sidewalks Article 3 Curb Cuts Article 4 Consolidation Street and Highway Fund Chapter X (10) TRAFFIC Article 1 Standard Traffic Ordinance Article 2 Additional Traffic Regulations Chapter XI (11) UTILITIES Article 1 Water Service Article 2 Sewer Service -
THE NATURAL RADIOACTIVITY of the BIOSPHERE (Prirodnaya Radioaktivnost' Iosfery)
XA04N2887 INIS-XA-N--259 L.A. Pertsov TRANSLATED FROM RUSSIAN Published for the U.S. Atomic Energy Commission and the National Science Foundation, Washington, D.C. by the Israel Program for Scientific Translations L. A. PERTSOV THE NATURAL RADIOACTIVITY OF THE BIOSPHERE (Prirodnaya Radioaktivnost' iosfery) Atomizdat NMoskva 1964 Translated from Russian Israel Program for Scientific Translations Jerusalem 1967 18 02 AEC-tr- 6714 Published Pursuant to an Agreement with THE U. S. ATOMIC ENERGY COMMISSION and THE NATIONAL SCIENCE FOUNDATION, WASHINGTON, D. C. Copyright (D 1967 Israel Program for scientific Translations Ltd. IPST Cat. No. 1802 Translated and Edited by IPST Staff Printed in Jerusalem by S. Monison Available from the U.S. DEPARTMENT OF COMMERCE Clearinghouse for Federal Scientific and Technical Information Springfield, Va. 22151 VI/ Table of Contents Introduction .1..................... Bibliography ...................................... 5 Chapter 1. GENESIS OF THE NATURAL RADIOACTIVITY OF THE BIOSPHERE ......................... 6 § Some historical problems...................... 6 § 2. Formation of natural radioactive isotopes of the earth ..... 7 §3. Radioactive isotope creation by cosmic radiation. ....... 11 §4. Distribution of radioactive isotopes in the earth ........ 12 § 5. The spread of radioactive isotopes over the earth's surface. ................................. 16 § 6. The cycle of natural radioactive isotopes in the biosphere. ................................ 18 Bibliography ................ .................. 22 Chapter 2. PHYSICAL AND BIOCHEMICAL PROPERTIES OF NATURAL RADIOACTIVE ISOTOPES. ........... 24 § 1. The contribution of individual radioactive isotopes to the total radioactivity of the biosphere. ............... 24 § 2. Properties of radioactive isotopes not belonging to radio- active families . ............ I............ 27 § 3. Properties of radioactive isotopes of the radioactive families. ................................ 38 § 4. Properties of radioactive isotopes of rare-earth elements . -
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. -
Estimations of Population Density for Selected Periods Between the Neolithic and AD 1800 Andreas Zimmermann University of Cologne, [email protected]
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Digital Commons@Wayne State University Human Biology Volume 81 Issue 2 Special Issue on Demography and Cultural Article 13 Macroevolution 2009 Estimations of Population Density for Selected Periods Between the Neolithic and AD 1800 Andreas Zimmermann University of Cologne, [email protected] Johanna Hilpert University of Cologne Karl Peter Wendt University of Cologne Follow this and additional works at: http://digitalcommons.wayne.edu/humbiol Recommended Citation Zimmermann, Andreas; Hilpert, Johanna; and Wendt, Karl Peter (2009) "Estimations of Population Density for Selected Periods Between the Neolithic and AD 1800," Human Biology: Vol. 81: Iss. 2-3, Article 13. Available at: http://digitalcommons.wayne.edu/ humbiol/vol81/iss2/13 Estimations of Population Density for Selected Periods Between the Neolithic and AD 1800 Abstract We describe a combination of methods applied to obtain reliable estimations of population density using archaeological data. The ombc ination is based on a hierarchical model of scale levels. The necessary data and methods used to obtain the results are chosen so as to define transfer functions from one scale level to another. We apply our method to data sets from western Germany that cover early Neolithic, Iron Age, Roman, and Merovingian times as well as historical data from AD 1800. Error margins and natural and historical variability are discussed. Our results for nonstate societies are always lower than conventional estimations compiled from the literature, and we discuss the reasons for this finding. At the end, we compare the calculated local and global population densities with other estimations from different parts of the world. -
The Significance of the Ancient Standing Stones, Villages, Tombs on Orkney Island
The Proceedings of the International Conference on Creationism Volume 5 Print Reference: Pages 561-572 Article 43 2003 The Significance of the Ancient Standing Stones, Villages, Tombs on Orkney Island Lawson L. Schroeder Philip L. Schroeder Bryan College Follow this and additional works at: https://digitalcommons.cedarville.edu/icc_proceedings DigitalCommons@Cedarville provides a publication platform for fully open access journals, which means that all articles are available on the Internet to all users immediately upon publication. However, the opinions and sentiments expressed by the authors of articles published in our journals do not necessarily indicate the endorsement or reflect the views of DigitalCommons@Cedarville, the Centennial Library, or Cedarville University and its employees. The authors are solely responsible for the content of their work. Please address questions to [email protected]. Browse the contents of this volume of The Proceedings of the International Conference on Creationism. Recommended Citation Schroeder, Lawson L. and Schroeder, Philip L. (2003) "The Significance of the Ancient Standing Stones, Villages, Tombs on Orkney Island," The Proceedings of the International Conference on Creationism: Vol. 5 , Article 43. Available at: https://digitalcommons.cedarville.edu/icc_proceedings/vol5/iss1/43 THE SIGNIFICANCE OF THE ANCIENT STANDING STONES, VILLAGES AND TOMBS FOUND ON THE ORKNEY ISLANDS LAWSON L. SCHROEDER, D.D.S. PHILIP L. SCHROEDER 5889 MILLSTONE RUN BRYAN COLLEGE STONE MOUNTAIN, GA 30087 P. O. BOX 7484 DAYTON, TN 37321-7000 KEYWORDS: Orkney Islands, ancient stone structures, Skara Brae, Maes Howe, broch, Ring of Brodgar, Standing Stones of Stenness, dispersion, Babel, famine, Ice Age ABSTRACT The Orkney Islands make up an archipelago north of Scotland. -
A State of the Art Paper on Improving Salt Extraction from Lake Katwe Raw Materials in Uganda
A State of the Art Paper on Improving Salt Extraction from Lake Katwe Raw Materials In Uganda Kasedde H.1,2 , Kirabira J.B.2, Bäbler M.U. 3, Tilliander A.1, Jonsson S.1 1. Department of Materials Science and Engineering, Royal Institute of Technology KTH, Brinellvägen 23, SE-100 44 Stockholm, Sweden. 2. Department of Mechanical Engineering, College of Engineering, Design, Art and Technology, Makerere University, P.O Box 7062, Kampala, Uganda. 3. Department of Chemical Engineering and Technology, Royal Institute of Technology KTH, Teknikringen 42, SE-100 44 Stockholm, Sweden. Abstract The characteristics of Katwe salt lake are briefly discussed. The lake is the largest of the eight saline lakes in the Katwe-Kikorongo volcanic field and is a major source of salt production in Uganda. Today, salt production at the lake is carried out using traditional and artisanal mining methods. Attempts to mechanize the production of domestic and commercial grade salt at the lake were unsuccessful due to the use of a wrong technology. In this paper, the most common available technologies for salt extraction from brine are described. These are divided into four broad categories, namely thermal, membrane, chemical and hybrid processes. A review of the state of the art, previous research and developments in these technologies is presented. A detailed analysis of the processes used was done based on studies reported in the literature. From the analysis, it was observed that thermal salt production processes, especially distillation and solar evaporation have the highest share in installed capacities worldwide. Membrane technologies such as Electro-dialysis, Reverse Osmosis and chemical technologies have not found wide application in the commercial salt industry. -
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.