Electrochemically-Induced Phase Transition in Olivine Type Cathode Materials by Kai Xiang
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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 -
Maricite Nafe2+PO4
2+ Mari´cite NaFe PO4 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. Rarely as crudely formed crystals, elongated along [100], usually radial to subparallel in nodules, to 15 cm; forms include {010}, {011}, {012}, {032}. Physical Properties: Hardness = 4–4.5 D(meas.) = 3.66(2) D(calc.) = 3.69 Optical Properties: Transparent to translucent. Color: Colorless, pale gray, pale brown. Streak: White. Luster: Vitreous. Optical Class: Biaxial (–). Orientation: X = a; Y = b. Dispersion: r>v; weak. α = 1.676(2) β = 1.695(2) γ = 1.698(2) 2V(meas.) = 43.5◦ 2V(calc.) = 43.0◦ Cell Data: Space Group: P mnb. a = 6.861(1) b = 8.987(1) c = 5.045(1) Z = 4 X-ray Powder Pattern: Big Fish River area, Canada. 2.574 (100), 2.729 (90), 2.707 (80), 1.853 (60), 3.705 (40), 2.525 (30), 1.881 (30) Chemistry: (1) (2) P2O5 42.5 40.83 FeO 37.4 41.34 MnO 3.1 MgO 0.8 CaO 0.0 Na2O 16.5 17.83 Total 100.3 100.00 (1) Big Fish River area, Canada; by electron microprobe, average of six analyses; corresponding to Na0.91(Fe0.89Mn0.07Mg0.03)Σ=0.99P1.02O4. (2) NaFePO4. Occurrence: In phosphatic nodules in sideritic ironstones. Association: Ludlamite, vivianite, quartz, pyrite, wolfeite, apatite, wicksite, nahpoite, satterlyite. Distribution: From the Big Fish River area, Yukon Territory, Canada. Name: Honors Dr. Luka Mari´c(1899–?), Professor of Mineralogy and Petrology, University of Zagreb, Croatia. -
Mineralogy of Silicate-Natrophosphate Immiscible † Inclusion in Elga IIE Iron Meteorite
minerals Article Mineralogy of Silicate-Natrophosphate Immiscible y Inclusion in Elga IIE Iron Meteorite Victor V. Sharygin 1,2 1 V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the RAS, 3 Acad. Koptyuga pr., 630090 Novosibirsk, Russia; [email protected] 2 ExtraTerra Consortium, Institute of Physics and Technology, Ural Federal University, 19 Mira str., 620002 Ekaterinburg, Russia The paper was presented at the 81st Annual Meeting of the Meteoritical Society in Moscow, Russia, y 22–27 July 2018. Received: 7 April 2020; Accepted: 11 May 2020; Published: 13 May 2020 Abstract: Rare type of silicate inclusions found in the Elga iron meteorite (group IIE) has a very specific mineral composition and shows silicate ( 90%)–natrophosphate ( 10%) liquid ≈ ≈ immiscibility due to meniscus-like isolation of Na-Ca-Mg-Fe phosphates. The 3 mm wide immiscible inclusion has been first studied in detail using optical microscopy, scanning electron microscopy, electron microprobe analysis and Raman spectroscopy. The silicate part of the inclusion contains fine-grained quartz-feldspar aggregate and mafic minerals. The relationships of feldspars indicate solid decay of initially homogenous K-Na-feldspar into albite and K-feldspar with decreasing of temperature. Some mafic minerals in the silicate part are exotic in composition: the dominant phase is an obertiite-subgroup oxyamphibole (amphibole supergroup), varying from ferri-obertiite 3+ 2+ NaNa2Mg3Fe Ti[Si8O22]O2 to hypothetical NaNa2Mg3Fe 0.5Ti1.5[Si8O22]O2; minor phases are the aenigmatite-subgroup mineral (sapphirine supergroup) with composition close to median value 2+ of the Na2Fe 5TiSi6O18O2-Na2Mg5TiSi6O18O2 join, orthopyroxene (enstatite), clinopyroxene of the diopside Ca(Mg,Fe)Si2O6–kosmochlor NaCrSi2O6-Na(Mg,Fe)0.5Ti0.5Si2O6 series and chromite. -
Wigksite, a New Mineral from Northeastern Yukon
Canadiun Mineralogist Vol. 19, pp. 377-380(1981) ,... WIGKSITE,A NEW MINERAL FROM NORTHEASTERNYUKON TERRITORY B. DARKO STURMAN Department of Mineralogy and Geology,Royal Ontario Museum, 100 Queen'sPark, Toronto, Ontario MSS 2C6 DONALD R. PEACOR Department of GeologicalSciences, University ol Michigan, Ann Arbor, Michigan48149, U.S.A. PETE J. DUNN Departrrlentol Mineral Sciences,Snrithsonian lnstitution, Washinsron,D.C. 20560,U.S.A. Ansrnecr (343,610). On trouve la wicksite en plaquettes bleues dans des nodules des formations ferrugineu- Wicksite NaCa2(Fe2+,Mn)aMgFes+(POo)u.2HrO ses et des shales stratifi6s le long de la rividre Big is orthorhombic, space group Pbca, with refined Fish (dans le Nord-Est du territoire du Yukon). cell parametersa 12.896(3),b l2.5ll(3), c 11.634 Cette espdce nouvelle est bleu fonc6 ou vert fonc6 (3) A; Z - 4. The strongest eight ljnes in the en sections minces, opaque en fragments 6pais. X-raydiffraction powder pattern [d in A G)&kl)l Duret| 4Vz-5, clivage {010} bon, densit6 3.54 (me- are 3.502(20)(230), 3.015(80)(411), 2.910(80) surde), 3.58 (calcul6e). Elle est biaxe positive, a (004), 2.868(30)(420), 2.837(30)(104), 2.753 1.713(3),p 1.718(3),t 1.728(3),2Y 660) fotte- (ro0)(412,042), 2.s71(40)(422) and 2.118(60) ment pl6ochroique, X bleu, Y bleu verditre, Z bttn - (343,610). Wicksite occurs as blue plates in nodules jaundtre pdle, absorption X Y > Z. Irs donn6es in bedded ironstone and shale along the Big Fish analytiques (microsonde, ADT-ATG, titration avec River in northeastern Yukon Territory, The new le dichromate de potassium) donnent AlrO3 0'51' mineral is dark blue or dark green in thin frag- Fe,Or 7.98, NazO 3.08, FeO 22.66, MgO 3.77, MnO ments; large fragments are opaque. -
Conference Guide
Organized by the Engineering Ceramics Division of The American Ceramic Society CONFERENCE GUIDE TH INTERNATIONAL CONFERENCE AND EXPOSITION ON ADVANCED CERAMICS 44AND COMPOSITES JANUARY 26 – 31, 2020 | HILTON DAYTONA BEACH RESORT AND OCEAN CENTER DAYTONA BEACH, FLORIDA, USA Apple Store Google play ceramics.org/icacc2020 WELCOME Welcome to Daytona Beach, Florida, for the 44th International Conference and Exposition on Advanced Ceramics and Composites, a showcase for cutting-edge research and product developments in advanced ceramics, armor ceramics, solid oxide fuel cells, ceramic coatings, bioceramics, and more. We hope you benefit from the technical program and Industry Expo that provide an open forum to present and exchange findings on recent advances in ceramic science and technology. The Engineering Ceramics Division of the American Ceramic Society has 2020 Program Chair organized this prestigious conference since 1977—with tremendous growth in interest and participation from ceramic communities globally. The key event of this year’s conference is the 4th Pacific Rim Engineering Ceramics Summit. The Summit will bring together experts from academia, industry, and government research institutes/laboratories to discuss the current state of the art and various technical challenges in research and development, engineering, manufacturing, and application of ceramic materials. The goal of the summit is to provide a forum for global information Valerie Wiesner exchange concerning the current status and emerging trends in various NASA Langley Research Center ceramic technologies in Pacific Rim countries. In addition, this year’s technical program consists of eighteen symposia, five focused sessions on emerging technologies, the 9th Global Young Investigator Forum, and a special focused session on Diversity, Entrepreneurship, and Commercialization to recognize the ECD Jubilee Global Diversity Award recipients. -
Marigite, a Sodium Iron Phosphate, from the Big Fish River Area, Yukon
Cawdian Mineralogist VoI. 15, pp.396-398 (1977) MARIGITE,A SODIUMIRON PHOSPHATE,FROM THE BIG FISH RIVERAREA, YUKON TERRITORY, CANADA B. D. STURMAN emr J. A. MANDARINO Department ol MineralogX and Geology, Royal Ontario Museum, Toronto, Ontaio MsS 2C6 M.I. CORLER Department ol Geological Sciences,Queen's University, Kingson, Ontario K7L 3N6 Ansrrecr INTRoDUcTIoN UariJite in nodules in sideriti,c ironstones rn the In addition to the phosphate occurrence in Big Fish River area, Yukon Territory, is colorless, which kulanite (Mandarino & Sturman L976), Erey, or pale brown, has a white streak, and hard- baribite (Sturman & Mandarino 1976), and peni- ness of 4 to 4/2. The measureddgnsif is 3.66 kisite (Mandarno et al. L977) have been found, g/cm3. There is no cleavage. Maricite is biaxial another locality about 15 km to the east has negativewith 2v 43Y2", na, 1.676,ng I.695, ny yielded some interesting species.The locality is 1.698;dispersion weak, r>v; no pleochroism;orien- on the Big Fish fuver at about Latitude 68o 30'N tatson" mineral a-X, b-Y. Tfu is orthorhombic, and Longitude 136'30'W, almost at the eastern space Pmnb, a 6,867, b 8.989, c 5.049L; V _group as the ku- 3ll,7N; Z-4.T\e strongestlines in the X-ray pow- border of Yukon Territory. Ilere, at der pattern (CuKa, Guinier camera) are: 3.705(40) lanite-baricite-penikisite type locality, the rocks (l lI), 2.729 (90) (22O), 2.707 (80X2LI), 2.574 ( t0O\ are interbedded shales and sideritic ironstones. -
Stratigraphic Setting of Some New and Rare Phosphate Minerals in the Yukon Territory
STRATIGRAPHIC SETTING OF SOME NEW AND RARE PHOSPHATE MINERALS IN THE YUKON TERRITORY A Thesis Submitted to the Faculty of Graduate Studies and Research in Partial Fulfilment of the Requirements For the Degree of Master of Science in the Department of Geological Sciences University of Saskatchewan by Benjamin Telfer Robertson Saskatoon, Saskatchewan May, 1980 The author claims copyright. Use shall not be made of the material contained herein without proper acknowledgement, as indicated on the following page. - i i - The author has agreed that the Library, University of Saskatchewan, may make this thesis freely available for inspection. Moreover, the author has agreed that permission for extensive copying of this thesis for scholarly purposes may be \ granted by the professor or professors who supervised the thesis work recorded herein, or, in their absence, by the Head of the Department or the Dean of the College in which the thesis work was done. It is understood that due recognition will be given to the author of this thesis and to the University of Saskatchewan in any use of the material in this thesis. Copying or publication or any other use of the thesis for financial gain without approval by the University of Saskatchewan and the author•s written permission is prohibited. Requests for permission to copy or to make other use of material in this thesis in whole or in part should be addressed to; Head of the Department of Geological Sciences University of Saskatchewan Saskatoon, Saskatchewan - iii - ABSTRACT The Big ~ish River - Rapid Creek phosphatic iron formation, in the Richardson Mountains, Yukon, is a unique sedimentary deposit of lowermost Albian age. -
Editorial for Special Issue “Mineralogy of Meteorites”
minerals Editorial Editorial for Special Issue “Mineralogy of Meteorites” Victor V. Sharygin 1,2 1 V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the RAS, 3 Acad. Koptyuga pr., 630090 Novosibirsk, Russia; [email protected]; Tel.: +7-383-330-80-84 2 ExtraTerra Consortium, Institute of Physics and Technology, Ural Federal University, 19 Mira str., 620002 Ekaterinburg, Russia Over 435 mineral species have been found in different types of meteorites (updated list for 2016) [1]. Classification of meteorites is based on their mineralogy and petrography, bulk-rock chemical and O-isotopic compositions, as well as the chemical composition of the main minerals [2–8]. For example, compositions in endmembers for olivine and low-Ca pyroxene and microstructural features of minerals are the powerful instruments for classification of ordinary chondrites (determination of the chemical group and petrologic type) [4–8]. In general, the individual minerals and mineral associations may record the history of meteorites (and their parental bodies) before and after their landing on the Earth. Rubin and Ma [1] outlined the basic processes responsible for mineral formation in meteorites: condensation from gaseous media around evolved stars and in the solar nebula; crystallization in chondrule, CAI (calcium-aluminium-rich inclusions), and AOA (amoeboid olivine aggregates) melts; exsolution during the cooling of CAIs, chondrules, and opaque assemblages; rapid quenching of amorphous phases; thermal and shock meta- morphism; aqueous/hydrothermal alteration and metasomatism; condensation during impact events; crystallization of melts in parental bodies; condensation from residual fluid in differentiated bodies; post-solidus transformations within cooling igneous materials; heating and remelting near perihelion; melting during atmospheric entrance; and terrestrial replacements. -
(O,F) Phases: Synthesis, Crystal Chemistry and Electrochemical Performance in Sodium – Based Batteries
Study of Na-M-(O,F) phases: synthesis, crystal chemistry and electrochemical performance in sodium – based batteries Jessica María Nava Avendaño PhD dissertation Materials Science Program Director: Dr. M. Rosa Palacín Peiró UAB Mentor: Dr. José A. Ayllón Esteve Chemistry Department Faculty of Sciences 2014 Estudio de fases Na-M-(O,F): síntesis, cristaloquímica y rendimiento electroquímico en baterías de sodio Jessica María Nava Avendaño Tesis Doctoral Programa de Doctorado en Ciencia de Materiales Director: Dra. M. Rosa Palacín Peiró Tutor UAB: Dr. José A. Ayllón Esteve Departamento de Química Facultad de Ciencias 2014 To my family, the country of my heart Acknowledgements I would like to deeply acknowledge my advisor Dr. M.R. Palacín for her unconditional support and guidance. Her optimism and diligence have encouraged me to work hard and commit with this project. She gave me the opportunity to keep learning and has trusted me all the way on. With her I am greatly indebted. I am also especially thankful to Dr. C. Frontera, who has walked with me along the elucidation of crystal structures and had the patience to discuss all the crazy ideas that came to my mind. A vosaltres, moltes gràcies per acompanyar-me en aquesta experiència de vida! Also, I would like to acknowledge all the collaborative work with Dr. J.A. Ayllón, the UAB mentor of this work, which widened the scope of the synthesis methods used and with Dr. M. Alfredsson for her disposition to help me and for giving me the opportunity to learn XAS basics. To Dr. G. Rousse, my gratitude for her compromise to the structural studies of the sodium titanate developed during this work and to Dr. -
MINERALOGY of INCLUSION with SILICATE-NATROPHOSPHATE IMMISCIBILITY, METEORITE ELGA (IIE) Victor V
MINERALOGY OF INCLUSION WITH SILICATE-NATROPHOSPHATE IMMISCIBILITY, METEORITE ELGA (IIE) Victor V. Sharygin1,2,3 1V.S.Sobolev Institute of Geology and Mineralogy, 3 Akad. Koptyuga pr., Novosibirsk, 630090, Russia, E-mail: [email protected], 2Novosibirsk State University, 2 Pirogov str., Novosibirsk, 630090, Russia; 3ExtraTerra Consortium, Institute of Physics and Technology, Ural Federal University, 19 Mira str., Ekaterinburg 620002, Russia. Iron meteorite Elga (group IIE) from Yakutia is a fine-grained octahedrite with silicate inclusions (up to 15 vol.%) and with clear features of local Different types of inclusions in metal, meteorite Elga Fragment of the Elga meteorite shock metamorphism melting (Plyashkevich, 1962; Kvasha et al., 1974; Osadchii et al., 1981; Khisina et al., 2017). The inclusions are rounded or Elga-3 Elga-11 Tro Elga-8 oval; sizes – 1-5 mm, sometimes up to 10-15 mm. Their mineral composition strongly varies. Most inclusions are gray-green and consist of glass (45-70%), diopside (25-50%) and enstatite (1-5%), rarely phosphates (fluorapatite, merrillite, panethite), olivine, chromite and rutile. Spheric milky-white inclusions contain glass or quartz-feldspathic aggregate with minimal mafic silicates. Schreibersite and troilite commonly occurs Gl+Cpx Tro Cpx around all inclusions. Inclusions with equal content of silicates and troilite as well as troilite-schreibersite segregations were also observed in Fe- Gl+Cpx Gl+Cpx Sch Ni-metal. Sch List of mineral phases found in the Elga meteorite Sch Tro Mineral Formula Mineral -
New Mineral Names*
American Mineralogist, Volume 67, pages 854-860, 1982 NEW MINERAL NAMES* Arsenocrandallite* Although single-crystal X-ray diffraction study showed no departure from cubic symmetry, the burtite unit cell is consid- Kurt Walenta (1981) Minerals of the beudantite-crandallite group ered to be rhombohedral with spacegroup RT, a, = 8. 128~, = from the Black Forest: Arsenocrandallite and sulfate-free 900, = (a = 11.49, = 14.08A in hexagonal setting). The weilerite. Schweiz. Mineralog. Petrog. Mitt., 61, 23-35 (in strongest lines in the X-ray powder diffraction pattern are (in A, German). for CoKa, indexing is based on the pseudo-cubic cell): Microprobe analysis gave As205 22.9, P20J 10.7, AI2O3 28.7, 4.06(vs)(200), 1.814(~)(420),1.657(~)(422), 0.9850(~)(820,644) and Fez03 1.2, CaO 6.9, SrO 6.0, BaO 4.3, CuO 1.8, ZnO 0.3, Biz03 0.9576(~)(822,660). 2.4, Si02 3.2, H20 (loss on ignition) 11.7, sum 100.1% cor- Electron microprobe analysis (with H20calculated to provide responding to (C~O.~IS~~.~~B~O.14Bio.0~)~.09(A12.79C~~. I Feo'& the stoichiometric quantity of OH) gave Sn02 56.3, CaO 20.6, Zn0.02)2.99 (As0.99 p0.7~ Si0.26)2.00 H6.44 013.63, Or MgO 0.3, H20 20.2, total 97.4 wt.%. These data give an (Ca,Sr)Al3H[(As,P)O4I2(0H),.Spectrographic analysis showed empirical formula of (Cao.9s2Mgo.020)Zl.oo2Sno.999(OH)6or, ideal- small amounts of Na, K, and C1. A second sample is nearly free ly, Casn(OH)6. -
New Mineral Names*
American Mineralogist, Volume 64, pages 652-659, 1979 NEW MINERAL NAMES* MICHAEL FLEISCHER, G. Y. CHAO AND J. A. MANDARINO Aleksite* Electron microprobe analyses, with pure Au, Ag, Cu, Fe, Te, A. G. Lipovetskii, Yu. S. Borodaev, and E. N. Zav'yalov (1978) and Se, and chemically analyzed altaite, clausthalite, and chalcopy- Aleksite, PbBi,Te,S" a new mineral. Zap. Vses. Mineral. rite as standards, of 8 spots from 2 samples from Far Eastern Obshch.. 107, 315-321 (in Russian). USSR gave Au 40.7-50.5, av 48.4; Ag 0.63-3.05, avo 1.54; Cu 7.43- 11.8, avo 9.35; Fe 0.13,0.36, avo 0.19; Pb 16.7-22.5, avo 19.2, Te Electron microprobe analyses of 2 samples gave Pb 20.3,20.5; Bi 18.5-22.9, avo 21.6; Se 0-1.35, avo 0.34; sum 99.4,101.7, avo 100.6%, 46.0,45.5; Te 27.3,27.3; S 6.3, 6.3; Ag, Sb, Se not found, sum 99.9, giving the formula (Au,..oAgo.17 )(Cu1."Feo.o4)Pbl.lo(Te,.ooSeo.o5)' 99.6, corresponding to Pbo."Bi,.l1Te,.o8S1.8. and Pbo..5Bi2.1oTe,.o8 X-ray study gave 12 lines, the strongest being 2.37( 10)(III), S1.8.' 2.05(7)(200), 1.448(6)(220), and 1.232(8)(311). The pattern is simi- The X-ray pattern (55 lines given) (Fe radiation, Mn filter) has lar to that of gold with primitive pseudocubic cell a = 4.IOA.