Phase Evolution of Ancient and Historical Ceramics
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Porcelain Cíqì 瓷 器
◀ POLO, Marco Comprehensive index starts in volume 5, page 2667. Porcelain Cíqì 瓷器 Porcelain was first made in China about 850ce . The essential ingredient is kaolin, a white clay that when fired at an extremely high temper- ature acquires a glassy surface. Porcelain wares were first exported to Europe during the twelfth century. By 1700 trade in Chinese porcelain was immense, with Ming dynasty wares, characterized by cobalt-blue-painted motifs, highly prized. orcelain is ceramic material made with kaolin, which is a fine, white clay. Porcelain wares were first made in China about 850ce during the Tang Ornately painted porcelain bowl. Potters of the dynasty (618– 907 ce). An Islamic traveler who had vis- Ming dynasty concentrated more on painted ited China in 851 saw clay vessels that resembled glass. design and less on form. Photo by Berkshire Evidence indicates that fine, white stoneware (pottery Publishing. made from high-firing clay other than kaolin) was made in China as early as 1400 bce, and potters appear to have been familiar with kaolin during the Han dynasty rather than gray or brown or rust colored) and high fusion (206 bce – 2 2 0 ce). But the forerunner of modern-day por- temperature (the high heat required to turn the ingredi- celain was not made until the Tang dynasty. Tang dynasty ents into porcelain). Chemically kaolin is made up of kao- porcelain is known as “hard-paste” or “true porcelain” and linite, quartz, feldspar, muscovite, and anastase. Kaolin was made by mixing kaolin, which is formed by the decay and petuntse are fused by firing in a kiln at 980º C, then of feldspar, a chief constituent of granite, with petuntse, dipped in glaze and refired at about 1,300º C. -
The Exploration of Sr Isotopic Analysis Applied to Chinese Glazes: Part Oneq
Journal of Archaeological Science xxx (2013) 1e8 Contents lists available at ScienceDirect Journal of Archaeological Science journal homepage: http://www.elsevier.com/locate/jas The exploration of Sr isotopic analysis applied to Chinese glazes: part oneq Hongjiao Ma a, Julian Henderson a, *, Jane Evans b a Department of Archaeology, University of Nottingham, University Park, Nottingham NG7 2RD, UK b NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK article info abstract Article history: Ash glaze and limestone glaze are two major glaze types in southern Chinese ceramic technology. In this Received 4 March 2013 study strontium isotope compositions were determined in ash glaze samples from the Yue kiln dated to Received in revised form between the 10th and 12th centuries AD, limestone glaze samples from Jingdezhen dated to between the 26 July 2013 15th and 18th centuries AD and ceramic raw materials from Jingdezhen. The Sr isotopic characteristics of Accepted 12 August 2013 limestone glaze and ash glaze are completely different. The Sr isotope characteristics of limestone glaze is characterised by low Sr concentrations, large 87Sr/86Sr variation, and a two component mixing line. On Keywords: the other hand the strontium isotope characteristic of ash glaze samples is characterised by a consistent Chinese glaze 87 86 Raw materials Sr/ Sr signature and high Sr concentrations with a large variation. The different Sr isotope composi- fl Strontium isotopes tions for the two types of glazes are a re ection of the various raw materials involved in making them. TIMS The Sr isotopic composition has been altered by the refinement process that the raw material was subjected to. -
Synthesis of Hexacelsian Barium Aluminosilicate by Film Boiling Chemical Vapour Process C
Synthesis of hexacelsian barium aluminosilicate by film boiling chemical vapour process C. Besnard, A. Allemand, P. David, Laurence Maillé To cite this version: C. Besnard, A. Allemand, P. David, Laurence Maillé. Synthesis of hexacelsian barium aluminosilicate by film boiling chemical vapour process. Journal of the European Ceramic Society, Elsevier, In press, 10.1016/j.jeurceramsoc.2020.02.021. hal-02494032 HAL Id: hal-02494032 https://hal.archives-ouvertes.fr/hal-02494032 Submitted on 28 Feb 2020 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. Synthesis of hexacelsian barium aluminosilicate by film boiling chemical vapour process C. Besnard1, A. Allemand1-2, P. David2, L. Maillé1* 1University of Bordeaux, CNRS, Safran, CEA, Laboratoire des Composites ThermoStructuraux (LCTS), UMR 5801, F-33600 Pessac 2CEA Le Ripault, F-37260, Monts * Corresponding author, email address: [email protected] Abstract An original oxide/oxide ceramic-matrix composite containing mullite-based fibers and a barium aluminosilicate matrix has been synthesized by the film boiling chemical vapour infiltration process. Alkoxides were used as liquid precursors for aluminum, silicon and barium oxides. The structure and microstructure of the oxide matrix were characterized by Scanning Electron Microscopy, Energy Dispersive Spectroscopy and X-ray diffraction. -
Synthetic Mullite Precursors: Preparation, Structure, and Transformation Behaviour
Synthetic Mullite Precursors: Preparation, Structure, and Transformation Behaviour Habilitationsschrift zur Erlangung der Lehrbefugnis für das Fachgebiet Materialwissenschaften an der Gemeinsamen Fakultät für Bergbau, Hüttenwesen und Maschinenwesen der Technischen Universität Clausthal vorgelegt von: Martin Schmücker Deutsches Zentrum für Luft- und Raumfahrt (DLR) Institut für Werkstoff-Forschung 51147 Köln 2003 2 Vorwort Die vorliegende Habilitationsschrift "Synthetic Mullite Precursors: Preparation, Structure, and Transformation Behaviour" basiert auf meinen Arbeitsschwerpunkten "Struktur nichtkristalliner Aluminiumsilikate" und "Frühstadien der Mullitbildung". Diese Themenbereiche habe ich -neben verschiedenen anderen Aktivitäten- während meiner 10-jährigen Tätigkeit im Institut für Werkstoff-Forschung des DLR konzeptionell entwickelt und kontinuierlich bearbeitet. Die Untersuchungen zur Struktur nichtkristalliner Aluminiumsilikate erfolgten zusammen mit internationalen Kooperationspartnern sowie im Rahmen des DFG-Sonderforschungsbereichs 408 (Anorganische Festkörper ohne Translationssysmmetrie, Univ. Bonn). Während diese Arbeiten überwiegend grundlagenorientiert waren, war der Hintergrund für meine Untersuchungen zur Mullitbildung stärker anwendungsbezogen: Der Einsatz von mullitbasierter Hochleistungskeramik z. B. für thermisch exponierte Bauteile im Bereich von Luftfahrt, Raumfahrt und Antriebstechnik setzt ein tieferes Verständnis der Mullitbildungsmechanismen voraus. Es zeigte sich, daß die Arbeiten zur Mullitbildung und zur Struktur -
This Dissertation Has Been 62—2136 M Icrofilm Ed Exactly As Received GIELISSE, Peter Jacob M., 1934- INVESTIGATION of PHASE EQ
This dissertation has been 62—2136 microfilmed exactly as received GIELISSE, Peter Jacob M., 1934- INVESTIGATION OF PHASE EQUILIBRIA IN THE SYSTEM ALUMINA-BORON OXIDE-SILICA. The Ohio State University, Ph.D., 1961 M ineralogy University Microfilms, Inc., Ann Arbor, Michigan INVESTIGATION OP PHASE EQUILIBRIA IN THE SYSTEM ALUMINA-BORON OXIDE-SILICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of the Ohio State University By Peter Jacob M. Gielisse, M. S. The Ohio State University 1961 Approved by Adviser Department of Mineralogy ACKNOWLEDGMENTS The writer wishes to extend his sincere thanks to the many people without whose help the preparation of this dissertation would have been impossible. He is indebted in particular to his adviser, Dr. Wilfrid R. Foster, for his invaluable aid, advice and many kindnesses; to the other members of the faculty of the Department of Mineral ogy, Drs. Ernest G. Ehlers, Henry E. Wenden, and Rodney T Tettenhorst; and to his friend and colleague, Thomas J. Rockett. Acknowledgment is also made for financial support re ceived under contract No. AF 33(616)-3189, sponsored by Aeronautical Research Laboratories, Air Force Research Division, Wright Patterson Air Force Base, Ohio; as well as for aid received through a Mershon National Graduate Fellowship awarded to the writer by the Mershon Committee on Education in National Security for 1960-‘61'. It goes without saying that he is also most grate ful to his wife, Anna, for her excellent help and encour agement over the years. TABLE OF CONTENTS Page INTRODUCTION ...................................... -
Preprint American Mineralogist 407
This is a preprint, the final version is subject to change, of the American Mineralogist (MSA) Cite as Authors (Year) Title. American Mineralogist, in press. (DOI will not work until issue is live.) DOI: http://dx.doi.org/10.2138/am.2012.4189 7/11 1 Semi-quantitative determination of the Fe/Mg ratio in synthetic cordierite using 2 Raman spectroscopy 3 REVISION 1 4 Authors: Udo Haefeker1, Reinhard Kaindl2, Peter Tropper1 5 6 1Institute of Mineralogy and Petrography, University Innsbruck, Innrain 52, A-6020 7 Innsbruck, Austria. 8 E-mail: [email protected] 9 2Present address: MATERIALS – Institute for Surface Technologies and Photonics, 10 Functional Surfaces, JOANNEUM RESEARCH Forschungsgesellschaft mbH, 11 Leobner Straße 94, A-8712 Niklasdorf, Austria. 12 13 ABSTRACT 14 Investigations of H2O-bearing synthetic well-ordered Mg-Fe-cordierites (XFe = 0-1) 15 with micro-Raman spectroscopy revealed a linear correlation between the Fe/Mg 16 ratio and the position of certain Raman peaks. In the range between 100 and 1250 17 cm-1 all peaks except for three peaks shift towards lower wavenumbers with 18 increasing XFe as a consequence of the substitution of the lighter Mg by the heavier 19 Fe atom on the octahedral sites and the associated structural changes. Selected 20 medium and strong peaks show a shift of 5 to 13 cm-1, respectively. Based on recent 21 quantum-mechanicalPreprint calculations American (Kaindl et al. 2011) Mineralogist these shifts can be attributed to 22 specific vibrational modes in the cordierite structure, thus showing that the Mg-Fe 23 exchange affects the vibrational modes of tetrahedral, octahedral and mixed sites. -
Kyanite and Related Minerals
KYANITE AND RELATED MINERALS (Data in metric tons unless otherwise noted) Domestic Production and Use: In Virginia, one firm with integrated mining and processing operations produced an estimated 85,000 tons of kyanite worth $30 million from two hard-rock open pit mines and synthetic mullite by calcining kyanite. Two other companies, one in Alabama and another in Georgia, produced synthetic mullite from materials mined from four sites; each company sourced materials from one site in Alabama and one site in Georgia. Synthetic mullite production data are withheld to avoid disclosing company proprietary data. Commercially produced synthetic mullite is made by sintering or fusing such feedstock materials as kyanite, kaolin, bauxite, or bauxitic kaolin. Natural mullite occurrences typically are rare and not economical to mine. Of the kyanite-mullite output, 90% was estimated to have been used in refractories and 10% in other uses, including abrasive products, such as motor vehicle brake shoes and pads and grinding and cutting wheels; ceramic products, such as electrical insulating porcelains, sanitaryware, and whiteware; foundry products and precision casting molds; and other products. An estimated 60% to 70% of the refractory use was by the iron and steel industries, and the remainder was by industries that manufacture cement, chemicals, glass, nonferrous metals, and other materials. Andalusite was commercially mined from an andalusite-pyrophyllite-sericite deposit in North Carolina and processed as a blend of primarily andalusite for use -
High Pressure Behavior of Mullite-Type Oxides: Phase Transitions, Amorphization, Negative Linear Compressibility and Microstructural Implications
UNLV Theses, Dissertations, Professional Papers, and Capstones 5-1-2015 High Pressure Behavior of Mullite-Type Oxides: Phase Transitions, Amorphization, Negative Linear Compressibility and Microstructural Implications Patricia Kalita University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Ceramic Materials Commons, Condensed Matter Physics Commons, and the Engineering Science and Materials Commons Repository Citation Kalita, Patricia, "High Pressure Behavior of Mullite-Type Oxides: Phase Transitions, Amorphization, Negative Linear Compressibility and Microstructural Implications" (2015). UNLV Theses, Dissertations, Professional Papers, and Capstones. 2369. http://dx.doi.org/10.34917/7645928 This Dissertation is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Dissertation in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/or on the work itself. This Dissertation has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. HIGH PRESSURE BEHAVIOR OF MULLITE-TYPE OXIDES: PHASE TRANSITIONS, AMORPHIZATION, NEGATIVE LINEAR COMPRESSIBILITY AND MICROSTRUCTURAL IMPLICATIONS by Patricia E. Kalita Bachelor of Sciences in Physics University of Nevada Las Vegas 2006 Master of Sciences in Physics University of Nevada Las Vegas 2008 A dissertation submitted in partial fulfillment of the requirements for the Doctor of Philosophy – Physics Department of Physics and Astronomy College of Sciences Graduate College University of Nevada, Las Vegas May 2015 Copyright by Patricia E. -
Andalusite and Na- and Li-Rich Cordierite in the La Costa Pluton, Sierras Pampeanas, Argentina: Textural and Chemical Evidence for a Magmatic Origin
Andalusite and Na- and Li-rich cordierite in the La Costa pluton, Sierras Pampeanas, Argentina: textural and chemical evidence for a magmatic origin Pablo H. Alasino . Juan A. Dahlquist . Carmen Galindo · Cesar Casquet · Julio Saavedra Abstraet The La Costa pluton in the Sierra de Velasco Keywords Andalusite· Na- and Li-rich cormerite . (NW Argentina) consists of S-type granitoids that can be S-type granite . La Costa pluton . Sierras Pampeanas grouped into three igneous facies: the alkali-rich Santa Cruz facies (SCF, Si02 ",67 wt%) mstinguished by the presence of andalusite and Na- and Li-rich cormerite Introduetion (Na20 = 1.55-1.77 wt% and LhO = 0.14---0.66 wt%), the Anillaco facies (Si02 '" 74 wt%) with a significant pro Andalusite and cormerite are important and common rock portion of Mn-rich garnet, and the Anjullón facies (Si02 forming mineral s in metapelitic rocks and may also be '" 7 5 wt%) with abundant albitic plagioc1ase. The petrog abundant in felsic peralurninous igneous rocks such as raphy, mineral chemistry and whole-rock geochemistry of granites, pegmatites, aplites and rhyolites. A fundamental the SCF are compatible with magmatic crystallization of question conceming the presence of andalusite and corm Na- and Li-rich cormerite, andalusite and muscovite from erite in peraluminous rocks is how they formed, i.e. whe the peraluminous magma under moderate P-T conditions ther they crystallized from the magma or were trapped as ('" 1.9 kbar and ca. 735°C). The high Li content of cor xenocrysts (e.g. Flood and Shaw 1975 ; Clarke et al. 1976, merite in the SCF is unusual for granitic rocks of inter 2005; Bellido and Barrera 1979; Phillips et al. -
SIN-YING HO Past Forward SIN-YING HO Past Forward
SIN-YING HO Past Forward SIN-YING HO Past Forward DENISE PATRY LEIDY professor at Queen’s College, City University of a clear glaze) in the mid-fourteenth century, began to A New York, Sin-ying Ho, whose work has been serve the Chinese court in the early fifteenth century, widely shown and collected, has developed one of and remains one of the primary centers of global the more unique voices in contemporary clay. Born porcelain production today. First used in China around in Hong Kong, she immigrated to Canada in 1992, the sixth century, porcelain, a combination of a clay initially to pursue a career in acting. After receiving a known as kaolin and the feldspathic rock petuntse that degree in ceramics from Sheridan College in Ontario fires at temperatures of 1200 to 1400 degrees Celsius, in 1995, Ho also earned a 1997 BFA in ceramics from was one of the great discoveries in global ceramic the Nova Scotia School of Art and Design in Halifax history. It was produced in Korea in the fifteenth cen- and a 2001 MFA from Louisiana State University in tury and Japan in the early seventeenth century, and it Baton Rouge. was finally created in the West in 1708 at Meissen in Germany. The reemergence of porcelain in studio, or Her training reflects the diversity of approaches to art, pottery in the 1970s and 1980s coincides with the ceramic-making in North America in the late twentieth ability of artists from around the world to live, work, century. While in Nova Scotia, Ho was introduced to and study in Jingdezhen. -
Development and Properties of New Mullite Based Refractory Grog
materials Article Development and Properties of New Mullite Based Refractory Grog David Zemánek 1,2 , Karel Lang 2, Lukáš Tvrdík 2, Dalibor Všianský 3, Lenka Nevˇrivová 1,2, Petr Štursa 2,3, Pavel Kováˇr 3, Lucie Keršnerová 3 and Karel Dvoˇrák 1,* 1 Faculty of Civil Engineering, Brno University of Technology, Veveˇrí 331/95, 602 00 Brno, Czech Republic; [email protected] (D.Z.); [email protected] (L.N.) 2 P-D Refractories CZ JSC, Nádražní 218, 679 63 Velké Opatovice, Czech Republic; [email protected] (K.L.); [email protected] (L.T.); [email protected] (P.Š.) 3 Department of Geological Sciences, Faculty of Science, Masaryk University, Kotláˇrská 267/2, 602 00 Brno, Czech Republic; [email protected] (D.V.); [email protected] (P.K.); [email protected] (L.K.) * Correspondence: [email protected]; Tel.: +420-54114-7511 (ext. 8067) Abstract: The presented study is focused on optimization and characterization of a high-alumina refractory aggregate based on natural raw materials—kaolins, claystone, and mullite dust by-product (used to increase the alumina and mullite contents, respectively). In total, four individual formulas with the Al2O3 contents between 45 and 50 wt.% were designed; the samples were subsequently fired, both in a laboratory oven and an industrial tunnel furnace. The effects of repeated firing were examined during industrial pilot tests. Mineral and chemical compositions and microstructures, of both the raw materials and designed aggregates, were thoroughly investigated by the means of X-ray fluorescence spectroscopy, powder X-ray diffraction, and optical and scanning electron microscopies. -
Structural Characteristics of Gas Hydrates Within the Framework of Generalized Crystallography A
Crystallography Reports, Vol. 48, No. 3, 2003, pp. 347–350. Translated from Kristallografiya, Vol. 48, No. 3, 2003, pp. 391–394. Original Russian Text Copyright © 2003 by Talis. THEORY OF CRYSTAL STRUCTURES Structural Characteristics of Gas Hydrates within the Framework of Generalized Crystallography A. L. Talis Russian Institute of Synthesis of Mineral Raw Materials, Aleksandrov, Vladimir oblast, 601650 Russia e-mail: [email protected] Received September 16, 2002 Abstract—It is shown that the symmetry of the {5, 3, 3} polytope (four-dimensional dodecahedron) embedded into E4 enables one to derive all the polyhedra–cavities that make up gas hydrates from the {5, 3} dodecahedron. Consideration is given to the allomorphic embedding of the {5, 3} subgraph into the incidence graph of the Desargues configuration 103, which determines the mechanism of incorporation of guest molecules into the polyhedra–cavities of gas hydrates and their escape from these polyhedra at the symmetry level. The relation- ships obtained may be considered as a basis for an a priori derivation of the determined (periodic and aperiodic) structures of gas hydrates. © 2003 MAIK “Nauka/Interperiodica”. The impossibility of dividing the three-dimensional pentagonal “cap” of the icosahedron into a hexagonal Euclidean space E3 into regular tetrahedra determines 2π one (if a wedge with an angle ------ is inserted), with the the structural characteristics of tetrahedrally coordi- 5 nated aqueous frameworks of gas hydrates that cannot disclination interactions being determined by the prod- be adequately reflected within the framework of classi- uct of the corresponding elements of group Y'. The cal crystallography. For example, the polyhedra–cavi- 2π introduction of two, three, and four Ð------ disclinations ties D, T, P, and H (dodecahedron, tetra-, penta-, and 5 hexadecahedra), the constituent fragments of the struc- into an icosahedron along its fivefold axes results in the tures of gas hydrates, are determined as dual to the Z12, formation of the Z14, Z15, and Z16 polyhedra [2].