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Nanoparticles of Lanthanide and Transition Metal Oxysulfides : from Colloidal Synthesis to Structure, Surface, Optical and Magnetic Properties Clement Larquet
Nanoparticles of lanthanide and transition metal oxysulfides : from colloidal synthesis to structure, surface, optical and magnetic properties Clement Larquet To cite this version: Clement Larquet. Nanoparticles of lanthanide and transition metal oxysulfides : from colloidal synthe- sis to structure, surface, optical and magnetic properties. Material chemistry. Sorbonne Université, 2018. English. NNT : 2018SORUS432. tel-02950055 HAL Id: tel-02950055 https://tel.archives-ouvertes.fr/tel-02950055 Submitted on 27 Sep 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. Sorbonne Université Ecole doctorale 397 : Physique et chimie des matériaux Laboratoire de Chimie de la Matière Condensée de Paris (LCMCP) Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie (IMPMC) Nanoparticles of lanthanide and transition metal oxysulfides: from colloidal synthesis to structure, surface, optical and magnetic properties Par M. Clément Larquet Thèse de doctorat de Sorbonne Université Dirigée par Clément Sanchez et Andrea Gauzzi Présentée et soutenue publiquement le 25 septembre 2018 Devant un jury composé de : Mme. Elsje Alessandra Quadrelli Directrice de recherches - CPE Lyon Rapporteur M. Stéphane Jobic Directeur de recherches - IEMN Rapporteur Mme. Catherine Louis Directrice de recherches - SU Examinatrice Mme. Asma Tougerti Chargée de recherches – Univ. -
1957 Eado.E4
1957 eado.e4 OF THE SEVENTH-DAY ADVENTIST DENOMINATION 4 I. w A DIRECTORY OF The General Conference, World Divisions, Union and Local Conferences and Missions, Educational Institutions, Hospitals and Sanitariums, Publishing Houses, Periodicals, and Denominational Workers. Edited and Compiled by H. W. Klaser, Statistical Secretary. General Conference Published by REVIEW AND HERALD PUBLISHING ASSOCIATION WASHINGTON 12, D.C. PRINTED IN U.S.A. Contents Fundamental Beliefs of Seventh-day Adventists 4 Constitution and By-Laws 5 General Conference and Departments 10 Divisions: North American 21 Australasian 68 Central European 83 China 89 Far Eastern 90 Inter-American 107 Middle East 123 Northern European 127 South American 140 Southern African 154 Southern Asia 171 Southern European 182 Union of Socialist Soviet Republics 199 Institutions: Educational 200 Food Companies 253 Medical 257 Dispensaries and Treatment Rooms 274 Old People's Homes and Orphanages 276 Publishing Houses 277 Periodicals Issued 286 Statistical Tables 299 Countries Where S.D.A. Work is Established 301 Languages in Which Publications Are Issued 394 Necrology 313 Index of Institutional Workers 314 Directory of Workers 340 Special Days and Offerings for 1957 462 Advertisers 453 Preface A directory of the conferences, mission state-wide basis in 1870, and state Sabbath fields, and institutions connected with the school associations in 1877. The name, "Se- Seventh-day Adventist denomination is given venth-day Adventists," was chosen in 1860, in the following pages. Administrative and and in 1903 the denominational headquarters workers' lists have been furnished by the were moved from Battle Creek, Mich., to organizations concerned. In cases where cur- Washington, D.C. -
Metamorphism of Sedimentary Manganese Deposits
Acta Mineralogica-Petrographica, Szeged, XX/2, 325—336, 1972. METAMORPHISM OF SEDIMENTARY MANGANESE DEPOSITS SUPRIYA ROY ABSTRACT: Metamorphosed sedimentary deposits of manganese occur extensively in India, Brazil, U. S. A., Australia, New Zealand, U. S. S. R., West and South West Africa, Madagascar and Japan. Different mineral-assemblages have been recorded from these deposits which may be classi- fied into oxide, carbonate, silicate and silicate-carbonate formations. The oxide formations are represented by lower oxides (braunite, bixbyite, hollandite, hausmannite, jacobsite, vredenburgite •etc.), the carbonate formations by rhodochrosite, kutnahorite, manganoan calcite etc., the silicate formations by spessartite, rhodonite, manganiferous amphiboles and pyroxenes, manganophyllite, piedmontite etc. and the silicate-carbonate formations by rhodochrosite, rhodonite, tephroite, spessartite etc. Pétrographie and phase-equilibia data indicate that the original bulk composition in the sediments, the reactions during metamorphism (contact and regional and the variations and effect of 02, C02, etc. with rise of temperature, control the mineralogy of the metamorphosed manga- nese formations. The general trend of formation and transformation of mineral phases in oxide, carbonate, silicate and silicate-carbonate formations during regional and contact metamorphism has, thus, been established. Sedimentary manganese formations, later modified by regional or contact metamorphism, have been reported from different parts of the world. The most important among such deposits occur in India, Brazil, U.S.A., U.S.S.R., Ghana, South and South West Africa, Madagascar, Australia, New Zealand, Great Britain, Japan etc. An attempt will be made to summarize the pertinent data on these metamorphosed sedimentary formations so as to establish the role of original bulk composition of the sediments, transformation and reaction of phases at ele- vated temperature and varying oxygen and carbon dioxide fugacities in determin- ing the mineral assemblages in these deposits. -
Profile of a Plant: the Olive in Early Medieval Italy, 400-900 CE By
Profile of a Plant: The Olive in Early Medieval Italy, 400-900 CE by Benjamin Jon Graham A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (History) in the University of Michigan 2014 Doctoral Committee: Professor Paolo Squatriti, Chair Associate Professor Diane Owen Hughes Professor Richard P. Tucker Professor Raymond H. Van Dam © Benjamin J. Graham, 2014 Acknowledgements Planting an olive tree is an act of faith. A cultivator must patiently protect, water, and till the soil around the plant for fifteen years before it begins to bear fruit. Though this dissertation is not nearly as useful or palatable as the olive’s pressed fruits, its slow growth to completion resembles the tree in as much as it was the patient and diligent kindness of my friends, mentors, and family that enabled me to finish the project. Mercifully it took fewer than fifteen years. My deepest thanks go to Paolo Squatriti, who provoked and inspired me to write an unconventional dissertation. I am unable to articulate the ways he has influenced my scholarship, teaching, and life. Ray Van Dam’s clarity of thought helped to shape and rein in my run-away ideas. Diane Hughes unfailingly saw the big picture—how the story of the olive connected to different strands of history. These three people in particular made graduate school a humane and deeply edifying experience. Joining them for the dissertation defense was Richard Tucker, whose capacious understanding of the history of the environment improved this work immensely. In addition to these, I would like to thank David Akin, Hussein Fancy, Tom Green, Alison Cornish, Kathleen King, Lorna Alstetter, Diana Denney, Terre Fisher, Liz Kamali, Jon Farr, Yanay Israeli, and Noah Blan, all at the University of Michigan, for their benevolence. -
New Mineral Names*
American Mineralogist, Volume 68, pages 280-2E3, 1983 NEW MINERAL NAMES* MrcnnBr- FrelscHen AND ADoLF Pnnsr Arsendescloizite* The mineral occurs at Uchucchacua,Peru, in acicular crystals up to 2fi) x 20 microns, associatedwith galena, manganoan (1982) Paul Keller and P. J. Dunn Arsendescloizite, a new sphalerite, pyrite, pyrrhotite, and alabandite, with gangue of mineral from Tsumeb. Mineralog. Record, 13, 155-157. quartz, bustamite, rhodonite, and calcite. Also found at Stitra, pyrite-pyrrhotite in rhyo- Microprobe analysis (HzO by TGA) gave AszOs 26.5, PbO Sweden,in a metamorphosed deposit 52.3,ZnO1E.5, FeO 0.3, Il2O2.9, sum 100.5%,corresponding to litic and dacitic rocks; in roundedgrains up to 50 fl.min diameter, associated with galena, freibergite, gudmundite, manganoan Pb1.s6(Zn1.63Fe6.oJ(AsOaXOH)1a or PbZn(AsO+XOH), the ar- senateanalogue ofdescloizite. The mineral is slightly soluble in sphalerite,bismuth, and spessartine. hot HNO3. The name is for A. Benavides, for his contribution to the Weissenbergand precessionmeasurements show the mineral development of mining in Peru. Type material is at the Ecole (Uchucchacua)and at the Free to be orthorhombic, space group F212121,a : 6.075, b = 9.358, Natl. Superieuredes Mines, Paris (SAtra). c = 7.$44, Z = 4, D. calc. 6.57. The strongestX-ray lines University, Amsterdam, Netherlands M.F. (31 eiven) are 4.23(6)(lll); 3.23(lOXl02);2.88(10)(210,031); 2.60 Kolfanite* (E)(13 I ) ; 2.W6)Q3r) ; I .65(6X33I, 143,233); r.559 (EX3I 3,060,25I ). Crystalsare tabular up to 1.0 x 0.4 x 0.5 mm in size, on {001}, A. -
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 -
The Secondary Phosphate Minerals from Conselheiro Pena Pegmatite District (Minas Gerais, Brazil): Substitutions of Triphylite and Montebrasite Scholz, R.; Chaves, M
The secondary phosphate minerals from Conselheiro Pena Pegmatite District (Minas Gerais, Brazil): substitutions of triphylite and montebrasite Scholz, R.; Chaves, M. L. S. C.; Belotti, F. M.; Filho, M. Cândido; Filho, L. Autor(es): A. D. Menezes; Silveira, C. Publicado por: Imprensa da Universidade de Coimbra URL persistente: URI:http://hdl.handle.net/10316.2/31441 DOI: DOI:http://dx.doi.org/10.14195/978-989-26-0534-0_27 Accessed : 2-Oct-2021 20:21:49 A navegação consulta e descarregamento dos títulos inseridos nas Bibliotecas Digitais UC Digitalis, UC Pombalina e UC Impactum, pressupõem a aceitação plena e sem reservas dos Termos e Condições de Uso destas Bibliotecas Digitais, disponíveis em https://digitalis.uc.pt/pt-pt/termos. Conforme exposto nos referidos Termos e Condições de Uso, o descarregamento de títulos de acesso restrito requer uma licença válida de autorização devendo o utilizador aceder ao(s) documento(s) a partir de um endereço de IP da instituição detentora da supramencionada licença. Ao utilizador é apenas permitido o descarregamento para uso pessoal, pelo que o emprego do(s) título(s) descarregado(s) para outro fim, designadamente comercial, carece de autorização do respetivo autor ou editor da obra. Na medida em que todas as obras da UC Digitalis se encontram protegidas pelo Código do Direito de Autor e Direitos Conexos e demais legislação aplicável, toda a cópia, parcial ou total, deste documento, nos casos em que é legalmente admitida, deverá conter ou fazer-se acompanhar por este aviso. pombalina.uc.pt digitalis.uc.pt 9 789892 605111 Série Documentos A presente obra reúne um conjunto de contribuições apresentadas no I Congresso Imprensa da Universidade de Coimbra Internacional de Geociências na CPLP, que decorreu de 14 a 16 de maio de 2012 no Coimbra University Press Auditório da Reitoria da Universidade de Coimbra. -
Democratic Republic of the Congo
COMMUNICABLE DISEASE TOOLKIT PPPRRROOOFFFIIILLLEEE AAA NNN NNN EEE XXX EEE SSS Democratic Republic of the Congo WHO Communicable Disease Working Group on Emergencies WHO Regional Office for Africa WHO Office, Kinshasa COMMUNICABLE DISEASE TOOLKIT WHO/CDS/2005.36a PPRROOFFIILLEE Democratic Republic of the Congo WHO Communicable Disease Working Group on Emergencies WHO Regional Office for Africa WHO Office, Kinshasa © World Health Organization 2005 All rights reserved. The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the World Health Organization concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. Dotted lines on maps represent approximate border lines for which there may not yet be full agreement. The mention of specific companies or of certain manufacturers’ products does not imply that they are endorsed or recommended by the World Health Organization in preference to others of a similar nature that are not mentioned. Errors and omissions excepted, the names of proprietary products are distinguished by initial capital letters. All reasonable precautions have been taken by WHO to verify the information contained in this publication. However, the published material is being distributed without warranty of any kind, either express or implied. The responsibility for the interpretation and use of the material lies with the reader. In no event shall the World Health Organization be liable for damages arising from its use. The named authors alone are responsible for the views expressed in this publication. -
Utahite, a New Mineral and Associated Copper Tellurates from the Centennial Eureka Mine, Tintic District, Juab County, Utah
UTAHITE, A NEW MINERAL AND ASSOCIATED COPPER TELLURATES FROM THE CENTENNIAL EUREKA MINE, TINTIC DISTRICT, JUAB COUNTY, UTAH Andrew C. Roberts and John A. R. Stirling Geological Survey of Canada 601 Booth Street Ottawa, Ontario, Canada K IA OE8 Alan J. Criddle Martin C. Jensen Elizabeth A. Moffatt Department of Mineralogy 121-2855 Idlewild Drive Canadian Conservation Institute The Natural History Museum Reno, Nevada 89509 1030 Innes Road Cromwell Road Ottawa, Ontario, Canada K IA OM5 London, England SW7 5BD Wendell E. Wilson Mineralogical Record 4631 Paseo Tubutama Tucson, Arizona 85750 ABSTRACT Utahite, idealized as CusZn;(Te6+04JiOH)8·7Hp, is triclinic, fracture. Utahite is vitreous, brittle and nonfluorescent; hardness space-group choices P 1 or P 1, with refined unit-cell parameters (Mohs) 4-5; calculated density 5.33 gtcm' (for empirical formula), from powder data: a = 8.794(4), b = 9996(2), c = 5.660(2);\, a = 5.34 glcm' (for idealized formula). In polished section, utahite is 104.10(2)°, f3 = 90.07(5)°, y= 96.34(3YO, V = 479.4(3) ;\3, a:b:c = slightly bireflectant and nonpleochroic. 1n reflected plane-polar- 0.8798:1 :0.5662, Z = 1. The strongest five reflections in the X-ray ized light in air it is very pale brown, with ubiquitous pale emerald- powder pattern are (dA(f)(hkl)]: 9.638(100)(010); 8.736(50)(100); green internal reflections. The anisotropy is unknown because it is 4.841(100)(020); 2.747(60)(002); 2.600(45)(301, 311). The min- masked by the internal reflections. Averaged electron-microprobe eral is an extremely rare constituent on the dumps of the Centen- analyses yielded CuO = 25.76, ZnO = 15.81, Te03 = 45.47, H20 nial Eureka mine, Tintic district, Juab County, Utah, where it (by difference) {12.96], total = {100.00] weight %, corresponding occurs both as isolated 0.6-mm clusters of tightly bound aggre- to CU49;Zn29lTe6+04)39l0H)79s' 7.1H20, based on 0 = 31. -
September 16-30, 1971
RICHARD NIXON PRESIDENTIAL LIBRARY DOCUMENT WITHDRAWAL RECORD DOCUMENT DOCUMENT SUBJECT/TITLE OR CORRESPONDENTS DATE RESTRICTION NUMBER TYPE 1 Manifest Helicopter Passenger Manifest – 9/18/1971 A Appendix “A” 2 Manifest Helicopter Passenger Manifest – 9/19/1971 A Appendix “A” 3 Manifest Helicopter Passenger Manifest – 9/23/1971 A Appendix “A” 4 Manifest Helicopter Passenger Manifest – 9/25/1971 A Appendix “A” 5 Manifest Helicopter Passenger Manifest – 9/26/1971 A Appendix “B” 6 Manifest Helicopter Passenger Manifest – 9/27/1971 A Appendix “B” 7 Manifest Helicopter Passenger Manifest – 9/30/1971 A Appendix “E” COLLECTION TITLE BOX NUMBER WHCF: SMOF: Office of Presidential Papers and Archives RC-8 FOLDER TITLE President Richard Nixon’s Daily Diary September 16, 1971 – September 30, 1971 PRMPA RESTRICTION CODES: A. Release would violate a Federal statute or Agency Policy. E. Release would disclose trade secrets or confidential commercial or B. National security classified information. financial information. C. Pending or approved claim that release would violate an individual’s F. Release would disclose investigatory information compiled for law rights. enforcement purposes. D. Release would constitute a clearly unwarranted invasion of privacy G. Withdrawn and return private and personal material. or a libel of a living person. H. Withdrawn and returned non-historical material. DEED OF GIFT RESTRICTION CODES: D-DOG Personal privacy under deed of gift -------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------- -
Adamsite-(Y), a New Sodium–Yttrium Carbonate Mineral
1457 The Canadian Mineralogist Vol. 38, pp. 1457-1466 (2000) ADAMSITE-(Y), A NEW SODIUM–YTTRIUM CARBONATE MINERAL SPECIES FROM MONT SAINT-HILAIRE, QUEBEC JOEL D. GRICE§ and ROBERT A. GAULT Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ANDREW C. ROBERTS Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A 0E8, Canada MARK A. COOPER Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada ABSTRACT Adamsite-(Y), ideally NaY(CO3)2•6H2O, is a newly identified mineral from the Poudrette quarry, Mont Saint-Hilaire, Quebec. It occurs as groups of colorless to white and pale pink, rarely pale purple, flat, acicular to fibrous crystals. These crystals are up to 2.5 cm in length and form spherical radiating aggregates. Associated minerals include aegirine, albite, analcime, ancylite-(Ce), calcite, catapleiite, dawsonite, donnayite-(Y), elpidite, epididymite, eudialyte, eudidymite, fluorite, franconite, gaidonnayite, galena, genthelvite, gmelinite, gonnardite, horváthite-(Y), kupletskite, leifite, microcline, molybdenite, narsarsukite, natrolite, nenadkevichite, petersenite-(Ce), polylithionite, pyrochlore, quartz, rhodochrosite, rutile, sabinaite, sérandite, siderite, sphalerite, thomasclarkite-(Y), zircon and an unidentified Na–REE carbonate (UK 91). The transparent to translucent mineral has a vitreous to pearly luster and a white streak. It is soft (Mohs hardness 3) and brittle with perfect {001} and good {100} and {010} cleav- ␣  ␥ ° ° ages. Adamsite-(Y) is biaxial positive, = V 1.480(4), = 1.498(2), = 1.571(4), 2Vmeas. = 53(3) , 2Vcalc. = 55 and is nonpleochroic. Optical orientation: X = [001], Y = b, Z a = 14° (in  obtuse). It is triclinic, space group P1,¯ with unit-cell parameters refined from powder data: a 6.262(2), b 13.047(6), c 13.220(5) Å, ␣ 91.17(4),  103.70(4), ␥ 89.99(4)°, V 1049.1(5) Å3 and Z = 4. -
Infrare D Transmission Spectra of Carbonate Minerals
Infrare d Transmission Spectra of Carbonate Mineral s THE NATURAL HISTORY MUSEUM Infrare d Transmission Spectra of Carbonate Mineral s G. C. Jones Department of Mineralogy The Natural History Museum London, UK and B. Jackson Department of Geology Royal Museum of Scotland Edinburgh, UK A collaborative project of The Natural History Museum and National Museums of Scotland E3 SPRINGER-SCIENCE+BUSINESS MEDIA, B.V. Firs t editio n 1 993 © 1993 Springer Science+Business Media Dordrecht Originally published by Chapman & Hall in 1993 Softcover reprint of the hardcover 1st edition 1993 Typese t at the Natura l Histor y Museu m ISBN 978-94-010-4940-5 ISBN 978-94-011-2120-0 (eBook) DOI 10.1007/978-94-011-2120-0 Apar t fro m any fair dealin g for the purpose s of researc h or privat e study , or criticis m or review , as permitte d unde r the UK Copyrigh t Design s and Patent s Act , 1988, thi s publicatio n may not be reproduced , stored , or transmitted , in any for m or by any means , withou t the prio r permissio n in writin g of the publishers , or in the case of reprographi c reproductio n onl y in accordanc e wit h the term s of the licence s issue d by the Copyrigh t Licensin g Agenc y in the UK, or in accordanc e wit h the term s of licence s issue d by the appropriat e Reproductio n Right s Organizatio n outsid e the UK. Enquirie s concernin g reproductio n outsid e the term s state d here shoul d be sent to the publisher s at the Londo n addres s printe d on thi s page.