Bentonite, Kaolin, and Selected Clay Minerals
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7 Great Pottery Projects
ceramic artsdaily.org 7 great pottery projects | Second Edition | tips on making complex pottery forms using basic throwing and handbuilding skills This special report is brought to you with the support of Atlantic Pottery Supply Inc. 7 Great Pottery Projects Tips on Making Complex Pottery Forms Using Basic Throwing and Handbuilding Skills There’s nothing more fun than putting your hands in clay, but when you get into the studio do you know what you want to make? With clay, there are so many projects to do, it’s hard to focus on which ones to do first. So, for those who may wany some step-by-step direction, here are 7 great pottery projects you can take on. The projects selected here are easy even though some may look complicated. But with our easy-to-follow format, you’ll be able to duplicate what some of these talented potters have described. These projects can be made with almost any type of ceramic clay and fired at the recommended temperature for that clay. You can also decorate the surfaces of these projects in any style you choose—just be sure to use food-safe glazes for any pots that will be used for food. Need some variation? Just combine different ideas with those of your own and create all- new projects. With the pottery techniques in this book, there are enough possibilities to last a lifetime! The Stilted Bucket Covered Jar Set by Jake Allee by Steve Davis-Rosenbaum As a college ceramics instructor, Jake enjoys a good The next time you make jars, why not make two and time just like anybody else and it shows with this bucket connect them. -
Download PDF About Minerals Sorted by Mineral Name
MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky. -
A Vibrational Spectroscopic Study of the Silicate Mineral Harmotome Â
Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy 137 (2015) 70–74 Contents lists available at ScienceDirect Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy journal homepage: www.elsevier.com/locate/saa A vibrational spectroscopic study of the silicate mineral harmotome – (Ba,Na,K)1-2(Si,Al)8O16Á6H2O – A natural zeolite ⇑ Ray L. Frost a, , Andrés López a, Lina Wang a,b, Antônio Wilson Romano c, Ricardo Scholz d a School of Chemistry, Physics and Mechanical Engineering, Science and Engineering Faculty, Queensland University of Technology, GPO Box 2434, Brisbane, Queensland 4001, Australia b School of Chemistry and Chemical Engineering, Tianjin University of Technology, No. 391, Bin Shui West Road, Xi Qing District, Tianjin, PR China c Geology Department, Federal University of Minas Gerais, Belo Horizonte, MG 31270-901, Brazil d Geology Department, School of Mines, Federal University of Ouro Preto, Campus Morro do Cruzeiro, Ouro Preto, MG 35400-00, Brazil highlights graphical abstract We have studied the mineral harmotome (Ba,Na,K)1- 2(Si,Al)8O16Á6H2O. It is a natural zeolite. Raman and infrared bands are attributed to siloxane stretching and bending vibrations. A sharp infrared band at 3731 cmÀ1 is assigned to the OH stretching vibration of SiOH units. article info abstract Article history: The mineral harmotome (Ba,Na,K)1-2(Si,Al)8O16Á6H2O is a crystalline sodium calcium silicate which has Received 31 March 2014 the potential to be used in plaster boards and other industrial applications. It is a natural zeolite with cat- Received in revised form 7 July 2014 alytic potential. Raman bands at 1020 and 1102 cmÀ1 are assigned to the SiO stretching vibrations of Accepted 28 July 2014 three dimensional siloxane units. -
Ackland Ceramics Guide
! ! CERAMICS!GUIDE! Ceramics:"objects"formed"from"moistened"clay"and"hardened"by"firing;"distinguished"by" permeability"and"firing"temperatures" • Earthenware:"Porous,"low<firing" • Stoneware:"Non<porous,"high<firing" • Hard<Paste"Porcelain:"Non<porous,"high<firing" Single!firing:"clay"mixture"and"glaze"reach"maximum"density"and"hardness"in"a"single"firing,"with" the"glaze"being"applied"directly"to"the"unfired"clay"beforehand" Biscuit!firing:"glazed"objects"can"also"undergo"multiple"firings,"the"first"being"the"firing"of"the" unglazed"(biscuit)"object;"helps"stabilize"a"work"before"a"glaze"or"painted"decoration"is"applied" Glost!firing:"fuses"glaze"to"an"object"that"has"already"been"biscuit<fired" Glaze:!natural"materials"applied"to"a"clay"object"(either"as"a"powder"or"mixed"with"water)," fusing"with"the"clay"when"fired;"makes"porous"ceramics"impervious"to"liquid;"also"used"on"non< porous"ceramics"for"purely"decorative"effects,"either"as"transparent"coating"or"colored"by"the" addition"of"various"metal"oxides;"comprised"of"ground"silica,"which"melts"to"create"a"glassy" surface,"as"well"as"(1)"an"alumina"stabilizer"to"increase"viscosity"and"(2)"a"mineral"flux"to"lower" the"silica’s"melting"point." Common!glaze!types:"distinguished"by"flux"material" th • Lead:"low<firing,"used"on"earthenware;"largely"discontinued"by"the"late"19 "century"due" to"dangers"of"prolonged"lead"exposure" • Tin:"lead"glaze"with"the"addition"of"tin"oxide,"resulting"in"an"opaque"white"surface;" originates"in"Middle"East,"9th"century;"European"tin<glazed"earthenware"classified"by" -
Characterization of Clays and Clay Minerals for Industrial Applications: Substitution Non-Natural Additives by Clays in UV Protection
Characterization of Clays and Clay Minerals for Industrial Applications: Substitution non-Natural Additives by Clays in UV Protection Dissertation in fulfilment of the academic grade doctor rerum naturalium (Dr. rer. nat.) at the Faculty of Mathematics and Natural Sciences Ernst-Moritz-Arndt-University Greifswald HOANG-MINH Thao (Hoàng Thị Minh Thảo) born on 01.6.1979 in Quang Ninh, Vietnam Greifswald, Germany - 2006 Dekan: Prof. Dr. Klaus Fesser 1. Gutachter: PD. Dr. habil. Jörn Kasbohm 2. Gutachter: Prof. Roland Pusch Tag der Promotion: 17.11.2006 ii CONTENTS LIST OF TABLES . vi LIST OF FIGURES. vii ABBREVIATIONS . x STATEMENT OF ORIGINAL AUTHORSHIP (ERKLÄRUNG). xi ACKNOWLEDGMENTS . xii 1 INTRODUCTION . 1 2 POSSIBLE FUNCTIONS OF CLAYS, CLAY MINERALS IN UV PROTECTION . 2 2.1 Clays, clay minerals and sustainability in geosciences. 2 2.2 Ultraviolet radiation and human skin . 2 2.3 Actual substances as UV protection factor and their problems. 5 2.4 Pharmacy requirement in suncreams. 9 2.5 Clays, clay minerals and their application for human health. 11 2.6 Possible functions of clays, clay minerals in UV protection cream. 13 3 METHODOLOGY . 15 3.1 Clays and clay minerals analyses. 15 3.1.1 X-Ray diffraction. 17 3.1.2 TEM-EDX. 19 3.1.3 X-Ray fluorescence. 22 3.1.4 Mössbauer spectroscopy. 23 3.1.5 Atterberg sedimentation. 23 3.1.6 Dithionite treatment. 24 3.2 Non-clay samples analyses. 24 3.2.1 UV-measurement. 25 3.2.2 Light microscopy. 27 3.2.3 Skin model test by mouse-ear in vivo . -
Colonial Archaeology: 070 333 Spring 2006 Prof C. Schrire Room 201
Colonial Archaeology: 070 333 Spring 2006 Prof C. Schrire [email protected] Room 201/202 RAB Phone: 932 9006 Course Outline: This course will teach the rudiments of identification and analysis of colonial artifacts dating from about 1600-1900 AD. Our teaching collection includes a variety of ceramics, pipes, glass and small finds. The course if taught largely by supervision and not lectures. Students will sort collections, draw objects, measure objects and identify them according to numerous criteria. Course Requirements: A prerequisite for this course is 070: 208, Survey of Historical Archaeology, normally taught in the Fall term. Students for whom this requirement was waived are expected to study a suitable textbook on the subject, such as Orser, C. 1995 Historical Archaeology and Deetz, J In small things forgotten. Students will attend one three hour class, once a week. During this time they will handle material, analyze it, and draw objects. Each student will need a clean writing pad or notebook, a pad of graph paper, pencils, colored pencils, eraser, a ruler, and a divider. There will be two exams, a midterm and final. Useful Texts: 1. Noel-Hume, I. 2001. The Artifacts of Colonial America 2. Fournier, Robert. Illustrated Dictionary of Practical Pottery. Paperback, 4th ed. 2000 Radnor Pa. Available at Amazon.com ($31.96) 3. Numerous additional sources will be present at class for used during the practicals. Colonial Archaeology: 070 330 Significant technical terms: (see Fournier 2000) Absorption: The taking up of liquid into the pores of a pot. The water absorption of a ceramic is an indicator of its degree of vitrification. -
Fire Retardancy of Polypropylene/Kaolinite Composites Marcos Batistella, Belkacem Otazaghine, Rodolphe Sonnier, Carlos Petter, José-Marie Lopez-Cuesta
Fire retardancy of polypropylene/kaolinite composites Marcos Batistella, Belkacem Otazaghine, Rodolphe Sonnier, Carlos Petter, José-Marie Lopez-Cuesta To cite this version: Marcos Batistella, Belkacem Otazaghine, Rodolphe Sonnier, Carlos Petter, José-Marie Lopez-Cuesta. Fire retardancy of polypropylene/kaolinite composites. Polymer Degradation and Stability, Elsevier, 2016, 129, pp.260-267. 10.1016/j.polymdegradstab.2016.05.003. hal-02906432 HAL Id: hal-02906432 https://hal.archives-ouvertes.fr/hal-02906432 Submitted on 26 May 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Fire retardancy of polypropylene/kaolinite composites * Marcos Batistella a, c, , Belkacem Otazaghine b, Rodolphe Sonnier b, Carlos Petter c, Jose-Marie Lopez-Cuesta b a Federal University of Santa Catarina, R. Eng. Agronomico^ Andrei Cristian Ferreira, s/n e Trindade, Florianopolis, SC, CEP 88040-900, Brazil b Ecole des Mines d’Ales, Centre des Materiaux (C2MA) e Pole^ Materiaux Polymeres Avances, 6 Avenue de Clavieres, 30319, Ales Cedex, France c Federal University of Rio Grande do Sul, Av. Bento Gonçalves, 9500, Porto Alegre, CEP 91501-970, Brazil abstract In this study the influence of surface modification of kaolinite with trisilanolisooctyl Polyhedral Oligo- SilSesquioxane (POSS) in polypropylene composites was evaluated in terms of thermal stability and fire retardancy and compared with talc. -
Color in Salt Glaze
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 8-1-1967 Color in salt glaze Daniel Lee Stevens Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Let us know how access to this document benefits ou.y Recommended Citation Stevens, Daniel Lee, "Color in salt glaze" (1967). Dissertations and Theses. Paper 561. https://doi.org/10.15760/etd.561 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. AN ABSTRACT OF THE THESIS OF Daniel Lee Stevens for the Master of Science in teaching in Cerami~s 'presented 0:0 August 7, 1967. Title: COLOR IN SALT GLAZE. , Abs tract approved: This thesis endeavors to bring a brief history of salt glaze to the reader, following i~s ge~esisin Germany to England and the American colonies and its continuation to the prese~t day. In order to conduct research on color in salt glaze~ a kiln had to be built for this purpose, meeting all the requirements 'that this tech- nique demands. Studies were ~ade on clay bodies to determine their throwing qualities as well as their ability to take a salt glaze. Finally, research was carried out 'in many serfes of tests studying the reactions of'various engobes and other coloring materials when ,fired in the salt glaze kiln. \ .' COLOR IN SALT GLAZE by Daniel Lee Stevens A THESIS submitted to .Portland State College, in partial fulfillment of the requirements for the degree of Master of Science in Teaching August 1967 \ I PORTLAND STATE COL~EGE LIBRARY' . -
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19 -
NMAM 9000: Asbestos, Chrysotile By
ASBESTOS, CHRYSOTILE by XRD 9000 MW: ~283 CAS: 12001-29-5 RTECS: CI6478500 METHOD: 9000, Issue 3 EVALUATION: FULL Issue 1: 15 May 1989 Issue 3: 20 October 2015 EPA Standard (Bulk): 1% by weight PROPERTIES: Solid, fibrous mineral; conversion to forsterite at 580 °C; attacked by acids; loses water above 300 °C SYNONYMS: Chrysotile SAMPLING MEASUREMENT BULK TECHNIQUE: X-RAY POWDER DIFFRACTION SAMPLE: 1 g to 10 g ANALYTE: Chrysotile SHIPMENT: Seal securely to prevent escape of asbestos PREPARATION: Grind under liquid nitrogen; wet-sieve SAMPLE through 10 µm sieve STABILITY: Indefinitely DEPOSIT: 5 mg dust on 0.45 µm silver membrane BLANKS: None required filter ACCURACY XRD: Copper target X-ray tube; optimize for intensity; 1° slit; integrated intensity with RANGE STUDIED: 1% to 100% in talc [1] background subtraction BIAS: Negligible if standards and samples are CALIBRATION: Suspensions of asbestos in 2-propanol matched in particle size [1] RANGE: 1% to 100% asbestos OVERALL PRECISION ( ): Unknown; depends on matrix and ESTIMATED LOD: 0.2% asbestos in talc and calcite; 0.4% concentration asbestos in heavy X-ray absorbers such as ferric oxide ACCURACY: ±14% to ±25% PRECISION ( ): 0.07 (5% to 100% asbestos); 0.10 (@ 3% asbestos); 0.125 (@ 1% asbestos) APPLICABILITY: Analysis of percent chrysotile asbestos in bulk samples. INTERFERENCES: Antigorite (massive serpentine), chlorite, kaolinite, bementite, and brushite interfere. X-ray fluorescence and absorption is a problem with some elements; fluorescence can be circumvented with a diffracted beam monochromator, and absorption is corrected for in this method. OTHER METHODS: This is NIOSH method P&CAM 309 [2] applied to bulk samples only, since the sensitivity is not adequate for personal air samples. -
Evaluation of Selected Kaolin Clays As a Raw Material for the Turkish Cement and Concrete Industry
Evaluation of Selected Kaolin Clays as a Raw Material for the Turkish Cement and Concrete Industry Aydin Aras1, Mustafa Albayrak1, Metin Arikan2, Konstantin Sobolev3 * 1 General Directorate of Mineral Research and Exploration (MTA), Turkey 2 Civil Engineering Department, Middle East Technical University (METU), Turkey 3 Facultad de Ingenieria Civil, Universidad Autonoma de Nuevo Leon (UANL), Mexico ABSTRACT Turkey has a long tradition (starting from the prehistoric civilizations) and experience in exploring and processing clay raw materials into ceramic products. Many of these products, such as tiles and sanitary ware, are manufactured for domestic and export markets. Kaolin clay is one of the raw materials of major importance for the ceramic and paper industry, as well as for a number of auxiliary applications. There is an ongoing interest to apply kaolin clay in the construction industry as a raw material for the production of white cement clinker and as an artificial pozzolanic additive for concrete (in a form of metakaolin). This report presents the results related to search, assessment and evaluation of available resources for advanced cement and concrete additives. Keywords: kaolin, metakaolin, construction, resources, ceramics, cement, x-ray diffraction, SEM INTRODUCTION Turkey has an abundance of natural resources and its mining industry is one of the sectors showing steady growth. Among the most commonly mined minerals are borax, magnesite, chromites, barite, feldspars, different clays, and limestone [1-21]. Local ceramic industry has more than 4000 years of experience in exploring and processing widely available raw materials into useful commodities. Currently, several ceramic products, such as tiles and sanitary ware are manufactured to meet international standards (ISO 9000) and significant amounts (about 45 %) of these products are exported [21]. -
Carbonation and Decarbonation Reactions: Implications for Planetary Habitability K
American Mineralogist, Volume 104, pages 1369–1380, 2019 Carbonation and decarbonation reactions: Implications for planetary habitability k E.M. STEWART1,*,†, JAY J. AGUE1, JOHN M. FERRY2, CRAIG M. SCHIFFRIES3, REN-BIAO TAO4, TERRY T. ISSON1,5, AND NOAH J. PLANAVSKY1 1Department of Geology & Geophysics, Yale University, P.O. Box 208109, New Haven, Connecticut 06520-8109, U.S.A. 2Department of Earth and Planetary Sciences, Johns Hopkins University, 3400 N. Charles Street, Baltimore, Maryland 21218, U.S.A. 3Geophysical Laboratory, Carnegie Institution for Science, 5251 Broad Branch Road NW, Washington, D.C. 20015, U.S.A. 4School of Earth and Space Sciences, MOE Key Laboratory of Orogenic Belt and Crustal Evolution, Peking University, Beijing 100871, China 5School of Science, University of Waikato, 101-121 Durham Street, Tauranga 3110, New Zealand ABSTRACT The geologic carbon cycle plays a fundamental role in controlling Earth’s climate and habitability. For billions of years, stabilizing feedbacks inherent in the cycle have maintained a surface environ- ment that could sustain life. Carbonation/decarbonation reactions are the primary mechanisms for transferring carbon between the solid Earth and the ocean–atmosphere system. These processes can be broadly represented by the reaction: CaSiO3 (wollastonite) + CO2 (gas) ↔ CaCO3 (calcite) + SiO2 (quartz). This class of reactions is therefore critical to Earth’s past and future habitability. Here, we summarize their significance as part of the Deep Carbon Obsevatory’s “Earth in Five Reactions” project. In the forward direction, carbonation reactions like the one above describe silicate weathering and carbonate formation on Earth’s surface. Recent work aims to resolve the balance between silicate weathering in terrestrial and marine settings both in the modern Earth system and through Earth’s history.