Salt Treatment As an Impulse for Industrial Towns’ Function Change
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The Archaeology of Mining, and Quarrying, for Salt and the Evaporites (Gypsum, Anhydrite, Potash and Celestine)
The archaeology of mining, and quarrying, for Salt and the Evaporites (Gypsum, Anhydrite, Potash and Celestine) Test drafted by Peter Claughton Rock salt, or halite (NaCl- sodium chloride), has been mined since the late 17th century, having been discovered during exploratory shaft sinking for coal at Marbury near Northwich, Cheshire, in November 1670. Prior to that the brine springs of Cheshire and those at Droitwich in Worcestershire were the source of salt produced by evaporation, along with production from a large number of coastal sites using seawater. Alabaster, fine grained gypsum (CaSO4. 2H2O - hydrated calcium sulphate), has however been quarried in the East Midlands for use in sculpture since at least the 14th century (Cheetham 1984, 11-13) and the use of gypsum for making plaster dates from about the same period. Consumption The expansion of mining and quarrying for salt and the other evaporites came in the 19th century with the development of the chemical industry. Salt (sodium chloride) was a feedstock for the production of the chlorine used in many chemical processes and in the production of caustic soda (sodium hydroxide) and soda ash (sodium carbonate). Anhydrite (anhydrous calcium sulphate) was used in the production of sulphuric acid. Salt or halite (rock salt) was first mined at Winsford in Cheshire (the site of the only remaining active rock salt mine in England) in 1844. Production expanded in the late 19th century to feed the chemical industry in north Cheshire (together with increasing brine production from the Northwich salt fields). The Lancashire salt deposits, on the Wyre estuary at Fleetwood and Preesall, not discovered until 1872 whilst boring in search of haematite (Landless 1979, 38), were a key to the development of the chemical industry in that area. -
Natural Analogues for Safety Cases of Repositories in Rock Salt, Salt
NEA/RWM/R(2013)10 Isotope monitoring of water appearances in salt mines: The Polish experience Marek Dulin ski1, Kazimierz Rozan ski1, Krzysztof Brudnik2, Piotr Kolonko3, Joanna Tadych4 1Faculty of Physics and Applied Computer Science, AGH Univ. of Science and Technology, Krakow, Poland 2W ieliczka Salt Mine S.A., Wieliczka, Poland 3Klodawa Salt Mine S.A., Klodawa, Poland 4Inowroclaw Salt Mines Solino S.A., Inowroclaw, Poland Isotope analyses of water appearances in Polish salt mines started in the early 70s of the last century. Soon after it became clear that oxygen and hydrogen stable isotope composition of water creates a unique possibility of determ ination of the origin of waters in mines and has a crucial role in the risk assessment associated with water inflows. Chem ical composition of mine waters, although useful, cannot be used to distinguish between syngenetic (safe) and meteoric (potentially dangerous) water types occurring in mines. The work provides a brief overview of isotope investigations of water appearances in four Polish salt mines (Wapno, Inowroclaw and Klodawa Salt Mines located in north central Poland and Wieliczka Salt Mine located in southern Poland) performed over the past forty years. Introduction Polish salt deposits are situated in the north-central and southern part of Poland (Figure 1). They are represented either by salt domes or salt beds, usually covered by water bearing Tertiary and Quaternary formations, sometimes surrounded by older deposits. There are three groups of water which make their appearance in salt mines: i) meteoric waters of infiltration origin , recharged during both Quaternary and pre-Quaternary climates; ii) syngenetic waters; iii) technological waters and waters of unknown origin. -
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. -
An Overview of the Sodium Chloride (Salt) Market in Western Canada (V.02)
Sodium Chloride Market: An Overview of the Sodium Chloride (Salt) Market in Western Canada (v.02) Author: WaterSMART Solutions Ltd. Date: December 21, 2012 Table of Contents Executive Summary 1 Introduction 1 Sources / Types of Salt 2 Salt Deposits 3 Extraction / Production Methods 5 Primary Uses for Salt 6 Price 6 Distribution 7 Canadian Salt Market 9 Western Canada Salt Market 9 Salt in Oil Sands Mining 12 Road Salts 14 Sodium Carbonate and Sodium Bicarbonate 17 Caustic Soda and Sodium Chloride Consumption in SAGD 18 Summary 20 Tables Table 1 - Extraction and Production Technology ______________________________________________________ 6 Table 2 - Canadian Salt Market by Form ____________________________________________________________ 7 Table 3 - Final Packaging and Price of Salt to Public Consumer __________________________________________ 7 Table 4: Western Canada Salt Market Overview _____________________________________________________ 11 Table 5 - Primary Uses for Salt in Western Canada ___________________________________________________ 12 Table 6: Chloride Based Road Salts ________________________________________________________________ 14 Table 7: Radius of Competitiveness _______________________________________________________________ 16 Figures Figure 1: Table 2.3 Survey of High-Reduction and ZLD Technologies for Municipal Utilities ____________________ 2 Figure 2: Major North American Salt Deposits ________________________________________________________ 3 Figure 3: Western Canada Salt Deposits ____________________________________________________________ -
'Wieliczka' Salt Mine (UNESCO)
Proceedings World Geothermal Congress 2015 Melbourne, Australia, 19-25 April 2015 A Concept of Making Use of Closed Underground Workings for Heat Recovery in Historical 'Wieliczka' Salt Mine (UNESCO) Andrzej Gonet1, Stanislaw Stryczek2, Aneta Sapinska-Sliwa3, Krzysztof Brudnik4, Tomasz Sliwa5 1) 2) 3) 5) Drilling, Oil&Gas Faculty, AGH University of Science and Technology, Krakow, Poland; 4) “Wieliczka” Salt Mine, Wieliczka, Poland 1) [email protected], 2) [email protected], 3) [email protected], 4) [email protected], 5) [email protected] Keywords: Salt mine, geoenergetics, closed loop, geothermal source heat pump, mining heat. ABSTRACT A concept of exploiting heat from old workings to be closed in the 'Wieliczka' Salt Mine is described in the paper. The monumental salt mine has been uninterruptedly operational since the 13th century. At present this is predominantly a museum of mining industry visited by over a million tourists from all over the world each year. The 'Wieliczka' Salt Mine has been put on the first UNESCO World Heritage List of 1978. The operations performed in the mine are related to maintaining historical workings, the Tourist Route and the extreme Miner's Route. Apart from this, an underground sanatorium was made for curing various diseases, mainly allergies. Part of over 200 km long workings and saline domes were liquidated to maintain the monumental part of the mine. Therefore a concept was proposed, according to which in part of the old workings, prior to the liquidation and backfilling, heat reception systems should be built. Thus obtained heat could be used by the underground sanatorium, e.g. -
Historic Salt Mines in Wieliczka and Bochnia Zabytkowe Kopalnie Soli W Wieliczce I Bochni
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by AGH (Akademia Górniczo-Hutnicza) University of Science and Technology: Journals Geoturystyka 4 (18) 2008: 61-70 Historic salt mines in Wieliczka and Bochnia Zabytkowe kopalnie soli w Wieliczce i Bochni Janusz Wiewiórka1, Józef Charkot2, Krzysztof Dudek3 & Małgorzata Gonera4 1 Retired geologist of the Wieliczka and Bochnia Salt Mines, Park Kingi 5, 32-020 Wieliczka 2 Cracow Saltworks Museum Wieliczka, Zamkowa 8, 32-020 Wieliczka, e-mail: [email protected] 3 Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Al. Mickiewicza 30, 30-059 Kraków, e-mail: [email protected] 4 Nature Conservation Institute, Polish Academy of Sciences, Al. Mickiewicza 33, 31-120 Kraków, e-mail: [email protected] Kraków – Krakowskie Żupy Solne. W XVI wieku był to największy ośrodek produkcyjny w Polsce i jeden z największych w Europie. Wydobycie soli kamiennej zakończyło się w Bochni w 1990, a w Wieliczce Warszawa Wieliczka w 1996 roku. Obydwa złoża znajdują się w utworach sfałdowanego Bochnia miocenu (baden – M4) jednostki zgłobickiej Karpat zewnętrznych. Seria solonośna składa się z formacji skawińskiej, wielickiej Dobczyce (ewaporaty) i warstw chodenickich. Złoże solne Wieliczki zbu- dowane jest z górnego złoża bryłowego i dolnego pokładowego. Kraków Myślenice Złoże bryłowe zostało utworzone w wyniku podmorskich spływów w południowej części basenu ewaporacyjnego. Obydwie części zło- Abstract: Historic salt mines in Wieliczka and Bochnia are situ- ża zostały ostatecznie uformowane w wyniku ruchów nasuwczych ated by the old trade road from Kraków to the east, in the region Karpat. -
CANADIAN SALT PRODUCERS Explosives, Fertilizers, Glass, and Cosmetics
Salt Michel Dumont Although dietary intake can vary for people from various countries, on average an adult’s total salt intake should be The author is with the Minerals and Metals Sector, no more than 6 g per day and a child’s no more than 4 g. Natural Resources Canada. The average person’s diet incorporates at least 9 g per day. Telephone: 613-995-2917 Dietary sodium is measured in milligrams (mg). The most E-mail: [email protected] common form of sodium used is table salt, which is 40% sodium. One teaspoon of table salt contains 2300 mg of sodium. HIGHLIGHTS The salt markets in developed regions such as North • Salt is critical to human and animal health. In insuffi- America and Western Europe are both stable and mature. cient quantities, our muscles won’t contract, our blood The main consuming regions are North America, Asia and won’t circulate, our food won’t digest, and our hearts the Middle East, and Western Europe. World salt consump- won’t beat. tion is on the rise, mainly in response to increasing demand in Southeast Asia and other developing nations. China is • Due to severe North American winter (2007-08) weather the world’s leading producer of synthetic soda ash (source: conditions, 2008 data indicate Canadian shipments of U.S. Geological Survey [USGS] 2006 salt review), which salt increased by 18.4% (or 2.2 Mt) to 14.2 Mt valued at uses large quantities of salt as feedstock, and many of $537.8 million. China’s salt operations have not been able to keep up with the strong demand created by the rise in soda ash • Preliminary 2008 Canadian data indicate total salt production. -
Irregularity of Post Mining Deformations As Indicator Revealing Effects of Processes of Unknown Origin in Area of Bochnia
DOI 10.4467/21995923GP.20.008.13073 GEOINFORMATICA POLONICA 19: 2020 Zbigniew Szczerbowski ORCID: 0000-0002-2398-559X IRREGULARITY OF POST MINING DEFORMATIONS AS INDICATOR REVEALING EFFECTS OF PROCESSES OF UNKNOWN ORIGIN IN AREA OF BOCHNIA AGH University of Science and Technology, Faculty of Mining Surveying and Environmental Engineering, Krakow, Poland [email protected] Keywords: neotectonics, salt deposit, salt mining, vertical displacements, Chebyshev polynomials Abstract The presented work deals with the problem of terrain surface and rock mass deformation in the area of the Bochnia Salt Mine. The deformations are related to natural causes (mainly the tectonic stress of the Carpathian orogen) as well as anthropogenic ones related to the past mining activity conducted directly under the buildings of the town of Bochnia. The discussed charac- teristics of land surface deformation are important from the point of view of threats to surface features and contribute to spatial development. Particularly anomalous zones of observed subsidence basins are examined as places of second order deformation effects. The author presents a method of determinations of these anomalous areas and he discusses their origins. NIEREGULARNOŚĆ ODKSZTAŁCEŃ POGÓRNICZYCH JAKO WSKAŹNIK UJAWNIAJĄCY EFEKTY PROCESÓW O NIEZNANYCH PRZYCZYNACH W REJONIE BOCHNI Słowa kluczowe: neotektonika, złoża solne, górnictwo soli, przemieszczenia pionowe, wielomiany Czebyszewa Abstrakt Przestawiona praca dotyczy problematyki deformacji powierzchni i górotworu w rejonie Kopalni Soli Bochnia. Deformacje te związane są zarówno z przyczynami naturalnymi (głównie nacisk tektoniczny orogenu karpackiego), jak i antropogenicznymi związanymi z minioną aktywnością górniczą prowadzoną bezpośrednio pod zabudową miejską Bochni. Omówione charak- terystyki deformacji powierzchni terenu są istotne z punktu widzenia zagrożeń dla obiektów powierzchni oraz są elementem planowania przestrzennego. -
Field Trip Guidebook
FIELD TRIP GUIDEBOOK Edited by Ewa Głowniak, Agnieszka Wasiłowska IX ProGEO Symposium Geoheritage and Conservation: Modern Approaches and Applications Towards the 2030 Agenda Chęciny, Poland 25-28th June 2018 FIELD TRIP GUIDEBOOK Edited by Ewa Głowniak, Agnieszka Wasiłowska This publication was co-financed by Foundation of University of Warsaw and ProGEO – The European Association for the Conservation of the Geological Heritage Editors: Ewa Głowniak, Agnieszka Wasiłowska Editorial Office: Faculty of Geology, University of Warsaw, 93 Żwirki i Wigury Street, 02-089 Warsaw, Poland Symposium Logo design: Łucja Stachurska Layout and typesetting: Aleksandra Szmielew Cover Photo: A block scree of Cambrian quartzitic sandstones on the slope of the Łysa Góra Range – relict of frost weathering during the Pleistocene. Photograph by Peter Pervesler Example reference: Bąbel, M. 2018. The Badenian sabre gypsum facies and oriented growth of selenite crystals. In: E. Głow niak, A. Wasiłowska (Eds), Geoheritage and Conservation: Modern Approaches and Applications Towards the 2030 Agenda. Field Trip Guidebook of the 9th ProGEO Symposium, Chęciny, Poland, 25–28th June 2018, 55–59. Faculty of Geology, University of Warsaw, Poland. Print: GIMPO Agencja Wydawniczo-Poligraficzna, Marii Grzegorzewskiej 8, 02-778 Warsaw, Poland ©2018 Faculty of Geology, University of Warsaw ISBN 978-83-945216-5-3 The content of abstracts are the sole responsibility of the authors Organised by Faculty of Geology, University of Warsaw Institute of Nature Conservation, Polish Academy -
Bulletin POLISH NATIONAL COMMISSION
biuletyn 2013 PRZEGLÑD POLSKIEGO KOMITETU DO SPRAW UNESCO PRZEGLÑD POLSKIEGO KOMITETU DO SPRAW UNESCO biuletynbiuletyn|| 2013 2013 POLISH NATIONAL COMMISSION for UNESCO Reviev bulletin | bulletin | for UNESCO Review UNESCO for POLISH NATIONAL COMMISSION COMMISSION NATIONAL POLISH bulletin 2013 covBIUL13gr.indd 1 14-11-03 14:34 POLISH NATIONAL COMMISSION for UNESCO Review bulletin| 2013 Table of Contents Andrzej Rottermund Workshop for Restorers A Few Words 53 in Nesvizh 5 About Our Activities Last Year Marek Konopka UNESCO 55 Anamnesis – Re-minding Programme Priorities 8 for the Coming Years 61 Kraków – UNESCO City of Literature What We Dealt with Sławomir Ratajski 12 in 2013 UNESCO 2005 Convention 63 A Tool of Cultural Policy Why and How to Protect Cultural 21 Heritage by Modern Means? Intercultural Education Workshops 72 for Teachers Bogusław Szmygin Protecting Our Heritage Libyan Journalists 25 – Contemporary Approach 73 on a Study Visit to Poland Leszek Kolankiewicz The Concept of Intangible Euro-Arab Dialogue Conference Cultural Heritage “Our Commonly Shared Values” 32 in the 2003 Convention 75 held in Algarve Mariusz Czuba Anna Kalinowska Wooden Orthodox Churches Contemporary Man In Dialogue (Tserkvas) of the Polish 77 With The Environment? and Ukrainian Carpathian Region 43 on the World Heritage List Magdalena Machinko-Nagrabecka How to Teach Katarzyna Piotrowska 85 on Sustainable Development? Wieliczka and Bochnia Royal Salt Mines Educating in Dialogue 46 on UNESCO World Heritage List 90 with the Environment 93 ASPnet for Global -
Leena, M. C. – Aamer, A
Leena et al.: Physiological, biochemical and phylogenetic characterization of extremely halophilic bacteria isolated from Khewra mine, Pakistan - 1243 - PHYSIOLOGICAL, BIOCHEMICAL AND PHYLOGENETIC CHARACTERIZATION OF EXTREMELY HALOPHILIC BACTERIA ISOLATED FROM KHEWRA MINE, PAKISTAN LEENA, M. C. – AAMER, A. S. – ABDUL, H. – FARIHA, H.* Department of Microbiology, Quaid-i-Azam University Islamabad 44000, Pakistan *Corresponding author e-mail: [email protected]; phone: +92-51-9064-3065 (Received 3rd Aug 2017; accepted 30th Nov 2017) Abstract. Microflora entrapped in the salt deposits of Khewra salt mine, Pakistan has adapted to extreme conditions and nutrient scarcity to survive. Due to assumption that halophilic archaea dominate hypersaline environments, bacteria have often remained unexplored. The reports on extremely halophilic bacteria indigenous to Khewra mine are quite limited resulting in largely unexplored biodiversity of the salt mine. Here we attempted to fill that gap by isolating eight halophilic bacteria, out of which four extremely halophilic bacteria were selected for physiological, biochemical and molecular characterization. The phylogenetic characterization inferred through comparative partial 16S rRNA sequences identified these strains as HSL1-Oceanobacillus onchorhynci subsp. Incaldanensis, HSL4- Staphylococcus lentus, HSL6-Bacillus endophyticus and HSL7-Bacillus aquimaris. These isolates could tolerate a wide range of temperatures (15–45°C), pH (5–9) and survived up to 16% NaCl concentration. This tolerance is due to the stability of their enzymes. Enzyme assays revealed a substantial amount of production of protease, amylase, lipase, xylanase, urease, gelatinase, cellulose, and DNase. Conclusively, isolation and characterization of the extremely halophilic bacteria from Khewra mine indicated their important ecological role and contribution towards the microbial diversity. The ability to produce extreme-enzymes also established the potential of the isolates as valuable resources for significant biotechnological applications. -
Wieliczka and Bochnia Royal Salt Mines (Poland)
drainage works, the property was removed from the List of World Heritage in Danger in 1998 (22 COM VII.2). A buffer Wieliczka and Bochnia Royal Salt zone was proposed by the State Party and accepted by Mines the World Heritage Committee in 2008 (32 COM 8B.63). (Poland) Consultations No 32ter ICOMOS consulted TICCIH and several independent experts. Technical Evaluation Mission An ICOMOS technical evaluation mission visited the Official name as proposed by the State Party property from 18 to 22 September 2012. Wieliczka and Bochnia Royal Salt Mines Additional information requested and received from Location the State Party Małopolska region, Bochnia municipality ICOMOS sent a letter to the State Party on 19 December Poland 2012, asking it to: Examine whether the property can be extended to Brief description include technical elements above ground; The rock salt mines of Wieliczka and Bochnia have been Clarify whether the Goluchowski level of the Bochnia th worked since the 13 century. They are the oldest of their mine forms part of the property or not; type in Europe. They have a number of underground Set up a common Steering Committee for the three levels, forming hundreds of kilometres of galleries with component parts of the serial property; numerous excavated rock salt chambers. The chambers Update and approve the conservation master plan have been transformed into underground chapels, for the Bochnia mine; storerooms, and diverse other rooms, in which altars and Be particularly vigilant in the control of urban statues have been sculpted from the rock salt. Above development in the buffer zone.