China's Rare Earth Elements Industry: What Can the West Learn?
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Scholarships Facts & Figures Shanghai 2018 Rankings QS World University Rankings 62 Jiao Tong University US News & World Report 156 Times Higher Education (THE) 188 Types of Scholarships Founded in 1896, Shanghai Jiao Tong Students University (SJTU) is the second oldest International degree students 2,401 university in China and is one of the Type Duration Support (RMB) Coverage (RMB) Sponsor Undergraduate students 16,195 most prestigious universities in China. Graduate students 21,093 SJTU is very strong in engineering, Monthly stipend (3,000/Month) which listed top 0.01% in ESI ranking. Tuition (28,900/Year) Faculty With a full range of academic disciplines A: CSC 2-3 Years 80,100/Year Health insurance CSC Academicians 48 in power & energy engineering, Accommodation allowance Chair Professors 148 environmental science and engineering, (1,200/Month) Fellows 160 finance and management related to International Faculties 222 low-carbon technology, SJTU has a solid Monthly stipend (1,700/Month) Professors 891 foundation and extraordinary advantag- Tuition (28,900/Year) es in establishing the China-UK Low B 2-3 Years 64,500/Year SJTU Full-time Faculties 2,835 Health insurance Carbon College. Accommodation allowance (1,200/Month) Tuition (28,900/Year) Health insurance C 2-3 Years 44,100/Year SJTU Accommodation allowance (1,200/Month) Prominent Alumni D 2-3 Years 29,700/Year Tuition (28,900/Year) SJTU Health insurance Jiang Ze Min Former President of China Note: In general, the support duration cannot be extended. All scholarship recipients are obliged to attend the annual China-UK comprehensive scholarship assessment during April and May of each year to confirm their qualification of the scholarship for the next year. -
Determination of D003 by Capillary Gas Chromatography
Rev. CENIC Cienc. Quím.; vol. 51. (no.2): 325-368. Año. 2020. e-ISSN: 2221-2442. BIBLIOGRAPHIC REWIEW THE FAMOUS FINNISH CHEMIST JOHAN GADOLIN (1760-1852) IN THE LITERATURE BETWEEN THE 19TH AND 21TH CENTURIES El famoso químico finlandés Johan Gadolin (1760-1852) en la literatura entre los siglos XIX y XXI Aleksander Sztejnberga,* a,* Professor Emeritus, University of Opole, Oleska 48, 45-052 Opole, Poland [email protected] Recibido: 19 de octubre de 2020. Aceptado: 10 de diciembre de 2020. ABSTRACT Johan Gadolin (1760-1852), considered the father of Finnish chemistry, was one of the leading chemists of the second half of the 18th century and the first half of the 19th century. His life and scientific achievements were described in the literature published between the 19th and 21st centuries. The purpose of this paper is to familiarize readers with the important events in the life of Gadolin and his research activities, in particular some of his research results, as well as his selected publications. In addition, the names of authors of biographical notes or biographies about Gadolin, published in 1839-2017 are presented. Keywords: J. Gadolin; Analytical chemistry; Yttrium; Chemical elements; Finnland & Sverige – XVIII-XIX centuries RESUMEN Johan Gadolin (1760-1852), considerado el padre de la química finlandesa, fue uno de los principales químicos de la segunda mitad del siglo XVIII y la primera mitad del XIX. Su vida y sus logros científicos fueron descritos en la literatura publicada entre los siglos XIX y XXI. El propósito de este artículo es familiarizar a los lectores con los acontecimientos importantes en la vida de Gadolin y sus actividades de investigación, en particular algunos de sus resultados de investigación, así como sus publicaciones seleccionadas. -
AND THORIAN SYNCHYSITE-(Ce) from the NIEDERBOBRITZSCH GRANITE, ERZGEBIRGE, GERMANY: IMPLICATIONS for the DIFFERENTIAL MOBILITY of the LREE and Th DURING ALTERATION
67 The Canadian Mineralogist Vol. 38, pp. 67-79 (2000) CERITE-(Ce) AND THORIAN SYNCHYSITE-(Ce) FROM THE NIEDERBOBRITZSCH GRANITE, ERZGEBIRGE, GERMANY: IMPLICATIONS FOR THE DIFFERENTIAL MOBILITY OF THE LREE AND Th DURING ALTERATION HANS-JÜRGEN FÖRSTER§ GeoForschungsZentrum Potsdam, Telegrafenberg, D-14473 Potsdam, Germany ABSTRACT A detailed survey of accessory minerals in the poorly to moderately differentiated F-poor biotite granites from Niederbobritzsch, Erzgebirge, Germany, reveals the presence of various, late magmatic to postmagmatic secondary rare-earth (REE) minerals, including cerite-(Ce), thorian synchysite-(Ce), synchysite-(Ce), and an unidentified Th-rich REE fluorocarbonate(?). Cerite-(Ce) is a REE silicate that, to date, has been found in only half a dozen occurrences worldwide. It had not previously been described from a granite. The composition of cerite-(Ce) from Niederbobritzsch is characterized by lower bulk REE contents but higher abundances of Si, Al, Ca, and F than that from other occurrences. Dissolution of thorian monazite- (Ce) during interaction with a F-, CO2- and Ca-bearing fluid gave rise to the formation of thorian synchysite-(Ce) containing up to 18.1 wt% ThO2. Previously reported contents of Th in synchysite-(Ce) did not exceed 1.6 wt% ThO2. The spatial relations between the secondary REE minerals and their precursor attest to a differential mobility of the LREE and Th during fluid–rock interaction. Under the prevailing PTX-conditions, the LREE were more soluble and, thus, mobilized further away from their site of removal relative to Th, which tended to be reprecipitated next to its precursor. Virtually unchanged whole-rock REE budgets and continuous, unfractionated chondrite-normalized LREE patterns of the secondary REE minerals, however, imply that the lanthanides were transported over distances of millimeters or centimeters only. -
The Development of the Periodic Table and Its Consequences Citation: J
Firenze University Press www.fupress.com/substantia The Development of the Periodic Table and its Consequences Citation: J. Emsley (2019) The Devel- opment of the Periodic Table and its Consequences. Substantia 3(2) Suppl. 5: 15-27. doi: 10.13128/Substantia-297 John Emsley Copyright: © 2019 J. Emsley. This is Alameda Lodge, 23a Alameda Road, Ampthill, MK45 2LA, UK an open access, peer-reviewed article E-mail: [email protected] published by Firenze University Press (http://www.fupress.com/substantia) and distributed under the terms of the Abstract. Chemistry is fortunate among the sciences in having an icon that is instant- Creative Commons Attribution License, ly recognisable around the world: the periodic table. The United Nations has deemed which permits unrestricted use, distri- 2019 to be the International Year of the Periodic Table, in commemoration of the 150th bution, and reproduction in any medi- anniversary of the first paper in which it appeared. That had been written by a Russian um, provided the original author and chemist, Dmitri Mendeleev, and was published in May 1869. Since then, there have source are credited. been many versions of the table, but one format has come to be the most widely used Data Availability Statement: All rel- and is to be seen everywhere. The route to this preferred form of the table makes an evant data are within the paper and its interesting story. Supporting Information files. Keywords. Periodic table, Mendeleev, Newlands, Deming, Seaborg. Competing Interests: The Author(s) declare(s) no conflict of interest. INTRODUCTION There are hundreds of periodic tables but the one that is widely repro- duced has the approval of the International Union of Pure and Applied Chemistry (IUPAC) and is shown in Fig.1. -
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T Hn AMERICax M INERALoGIST JOURNAL OF THE MINERALOGICAL SOCIETY OF AMERICA Vol. 25 JUNE, 1940 No.6 DEPOSITS OF RADIOACTIVE CERITE NEAR JAMESTOWN, COLORADO* Elwnr N. Gonoann aNn Jnwnu J. Gr-ass, IL S. GeologicalSuraey, Washington, D.C. CONTENTS Abstract 381 Introduction 382 Geological occurrence 383 Mineralogy 385 Occurrence.. 385 Northern group 386 Southern group, 391 List of minerals. 393 Cerite... 393 Allanite. 397 Brown epidote 399 Tijrnebohmite 400 Fluorite 4.00 Bastniisite 401 Monazite 401 Uraninite 4Ol Sulphides 402 Comparisons with other deposits of cerite 402 Radioactivity 403 Age determination 404 Assrnecr Cerite, a rare silicate of the cerium metals, occurs in small deposits in the pre-Cambrian rocks of the Front Range near Jamestolvn, colorado. They are near the north border of a stock of Silver Plume granite, to which they are genetically related. Numerous lenticular schist masses in the granite suggest proximity to the roof. The cerite rock containing about 75 per cent of cerite occurs as irregular lenses,one- fourth of an inch to 15 inches wide, in narrow aplite-pegmatite zones along the borders of small schist areas. Narrow veinlets of black allanite border the cerite rock and minute grains of uraninite (pitchblende) and pyrite are localiy present. Microscopic examination of the cerite rock shows it to be finely intergrown with * Published by permission of the Director, Geological Survey, United States Depart- ment of the Interior, the Colorado Geological Survey Board, and the Colorado Metal Mining Fund. 381 E. N, GODDARD AND T. I. GLASS varying amounts of allanite, brown epidote, tdrnebohmite, fluorite, bastniisite, monazite, uraninite, and quartz. -
Stillwellite-(Ce) (Ce, La, Ca)Bsio
Stillwellite-(Ce) (Ce; La; Ca)BSiO5 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Hexagonal. Point Group: 3: As °at rhombohedral crystals, to 4 cm, and massive. Twinning: Observed about [100]. Physical Properties: Cleavage: One imperfect. Fracture: Conchoidal. Hardness = 6.5 D(meas.) = 4.57{4.60 D(calc.) = 4.67 » Optical Properties: Transparent to translucent. Color: Red-brown to pale pink; colorless in thin section. Streak: White. Optical Class: Uniaxial (+) to biaxial (+). ! = 1.765{1.784 ² = 1.780{1.787 2V(meas.) = 0±{6± Cell Data: Space Group: P 31: a = 6.841{6.844 c = 6.700{6.702 Z = 3 X-ray Powder Pattern: Mary Kathleen mine, Australia. 3.43 (s), 2.96 (s), 2.13 (ms), 4.44 (m), 1.864 (m), 2.71 (mw), 2.24 (mw) Chemistry: (1) (2) (1) (2) (1) (2) SiO2 22.40 22.06 La2O3 27.95 19.12 MgO 0.06 UO2 0.22 Ce2O3 33.15 30.82 CaO 0.95 0.34 ThO2 5.41 Pr2O3 1.82 F 0.30 + B2O3 12.23 [13.46] Nd2O3 5.36 H2O 0.85 Al2O3 0.42 Sm2O3 0.34 H2O¡ 0.10 Y2O3 0.74 0.28 Fe2O3 0.18 P2O5 0.67 Total [100.00] [99.26] (1) Mary Kathleen mine, Australia; recalculated to 100.00% after removal of very small amounts of uraninite and apatite determined by separate analysis. (2) Vico volcano, near Vetralla, Italy; by electron microprobe, B2O3 calculated from stoichiometry, original total given as 99.23%; corresponds to (Ce0:50La0:31Nd0:08Th0:05Pr0:03Ca0:02Sm0:01)§=1:00B1:02Si0:97O5: Occurrence: Locally abundant as a metasomatic replacement of metamorphosed calcareous sediments (Mary Kathleen mine, Australia); in alkalic pegmatites in syenite in an alkalic massif (Dara-i-Pioz massif, Tajikistan). -
Preliminary Estimates of the Quantities of Rare-Earth Elements Contained in Selected Products and in Imports of Semimanufactured Products to the United States, 2010
Preliminary Estimates of the Quantities of Rare-Earth Elements Contained in Selected Products and in Imports of Semimanufactured Products to the United States, 2010 By Donald I. Bleiwas and Joseph Gambogi Open-File Report 2013–1072 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2013 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order other USGS information products, visit http://store.usgs.gov Suggested citation: Bleiwas, D.I., and Gambogi, Joseph, 2013, Preliminary estimates of the quantities of rare-earth elements contained in selected products and in imports of semimanufactured products to the United States, 2010: U.S. Geological Survey Open–File Report 2013–1072, 14 p., http://pubs.usgs.gov/of/2013/1072/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Cover. Left: Aerial photograph of Molycorp, Inc.’s Mountain Pass rare-earth oxide mining and processing facilities in Mountain Pass, California. -
EMD Uranium (Nuclear Minerals) Committee
EMD Uranium (Nuclear Minerals) Committee EMD Uranium (Nuclear Minerals) Mid-Year Committee Report Michael D. Campbell, P.G., P.H., Chair December 12, 2011 Vice-Chairs: Robert Odell, P.G., (Vice-Chair: Industry), Consultant, Casper, WY Steven N. Sibray, P.G., (Vice-Chair: University), University of Nebraska, Lincoln, NE Robert W. Gregory, P.G., (Vice-Chair: Government), Wyoming State Geological Survey, Laramie, WY Advisory Committee: Henry M. Wise, P.G., Eagle-SWS, La Porte, TX Bruce Handley, P.G., Environmental & Mining Consultant, Houston, TX James Conca, Ph.D., P.G., Director, Carlsbad Research Center, New Mexico State U., Carlsbad, NM Fares M Howari, Ph.D., University of Texas of the Permian Basin, Odessa, TX Hal Moore, Moore Petroleum Corporation, Norman, OK Douglas C. Peters, P.G., Consultant, Golden, CO Arthur R. Renfro, P.G., Senior Geological Consultant, Cheyenne, WY Karl S. Osvald, P.G., Senior Geologist, U.S. BLM, Casper WY Jerry Spetseris, P.G., Consultant, Austin, TX Committee Activities During the past 6 months, the Uranium Committee continued to monitor the expansion of the nuclear power industry and associated uranium exploration and development in the U.S. and overseas. New power-plant construction has begun and the country is returning to full confidence in nuclear power as the Fukushima incident is placed in perspective. India, Africa and South America have recently emerged as serious exploration targets with numerous projects offering considerable merit in terms of size, grade, and mineability. During the period, the Chairman traveled to Columbus, Ohio to make a presentation to members of the Ohio Geological Society on the status of the uranium and nuclear industry in general (More). -
To Ytterbium(II)
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Masters Theses Graduate School 12-2008 The Use of Lanthanide Triflates as a Method for Reducing Ytterbium(III) to Ytterbium(II) Latasha Michelle Garrett University of Tennessee - Knoxville Follow this and additional works at: https://trace.tennessee.edu/utk_gradthes Part of the Chemistry Commons Recommended Citation Garrett, Latasha Michelle, "The Use of Lanthanide Triflates as a Method for Reducing tterbium(III)Y to Ytterbium(II). " Master's Thesis, University of Tennessee, 2008. https://trace.tennessee.edu/utk_gradthes/378 This Thesis is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Masters Theses by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a thesis written by Latasha Michelle Garrett entitled "The Use of Lanthanide Triflates as a Method for Reducing tterbium(III)Y to Ytterbium(II)." I have examined the final electronic copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Master of Science, with a major in Chemistry. George Schweitzer, Major Professor We have read this thesis and recommend its acceptance: Ben Xue, Jamie Adcock Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) To the Graduate Council: I am submitting herewith a thesis written by Latasha Michelle Garrett entitled “The Use of Lanthanide Triflates as a Method for Reducing Ytterbium(III) to Ytterbium(II).” I have examined the final electronic copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the requirements for the degree of Master of Science, with a major in chemistry. -
Periodic Table 1 Periodic Table
Periodic table 1 Periodic table This article is about the table used in chemistry. For other uses, see Periodic table (disambiguation). The periodic table is a tabular arrangement of the chemical elements, organized on the basis of their atomic numbers (numbers of protons in the nucleus), electron configurations , and recurring chemical properties. Elements are presented in order of increasing atomic number, which is typically listed with the chemical symbol in each box. The standard form of the table consists of a grid of elements laid out in 18 columns and 7 Standard 18-column form of the periodic table. For the color legend, see section Layout, rows, with a double row of elements under the larger table. below that. The table can also be deconstructed into four rectangular blocks: the s-block to the left, the p-block to the right, the d-block in the middle, and the f-block below that. The rows of the table are called periods; the columns are called groups, with some of these having names such as halogens or noble gases. Since, by definition, a periodic table incorporates recurring trends, any such table can be used to derive relationships between the properties of the elements and predict the properties of new, yet to be discovered or synthesized, elements. As a result, a periodic table—whether in the standard form or some other variant—provides a useful framework for analyzing chemical behavior, and such tables are widely used in chemistry and other sciences. Although precursors exist, Dmitri Mendeleev is generally credited with the publication, in 1869, of the first widely recognized periodic table. -
(Skarn)-Type Ore Deposits in Western Bergslagen,Sweden
UNIVERSITY OF GOTHENBURG Department of Earth Sciences Geovetarcentrum/Earth Science Centre PREDICTIVE PROSPECTIVITY MAPPING OF RARE EARTH ELEMENTS IN BASTNÄS (SKARN)-TYPE ORE DEPOSITS IN WESTERN BERGSLAGEN,SWEDEN INTEGRATION AND ANALYSIS OF GEOSCIENCE DATASETS IN ARCGIS Ejiro Obotuke-Agbonifo ISSN 1400-3821 B961 Master of Science (120 credits) thesis Göteborg 2017 Mailing address Address Telephone Telefax Geovetarcentrum Geovetarcentrum Geovetarcentrum 031-786 19 56 031-786 19 86 Göteborg University S 405 30 Göteborg Guldhedsgatan 5A S-405 30 Göteborg SWEDEN Table of contents 1. INTRODUCTION .................................................................................................................................... 4 1.1 AIM AND APPROACH ...................................................................................................................... 4 1.2 ABOUT RARE EARTH ELEMENTS .................................................................................................. 7 1.3 GENERAL CHARACTERISTICS OF BASTNÄS-TYPE REE MINERALIZATION ............................... 9 1.4 MINING HISTORY OF BERGSLAGEN ............................................................................................ 13 2. BACKGROUND .................................................................................................................................... 15 2.1 REGIONAL GEOLOGY OF BERGSLAGEN....................................................................................... 15 2.2 LOCAL GEOLOGY OF BERGSLAGEN ............................................................................................ -
Rare Earth Elements Deposits of the United States—A Summary of Domestic Deposits and a Global Perspective
The Principal Rare Earth Elements Deposits of the United States—A Summary of Domestic Deposits and a Global Perspective Gd Pr Ce Sm La Nd Scientific Investigations Report 2010–5220 U.S. Department of the Interior U.S. Geological Survey Cover photo: Powders of six rare earth elements oxides. Photograph by Peggy Greb, Agricultural Research Center of United States Department of Agriculture. The Principal Rare Earth Elements Deposits of the United States—A Summary of Domestic Deposits and a Global Perspective By Keith R. Long, Bradley S. Van Gosen, Nora K. Foley, and Daniel Cordier Scientific Investigations Report 2010–5220 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2010 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. This report has not been reviewed for stratigraphic nomenclature. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Suggested citation: Long, K.R., Van Gosen, B.S., Foley, N.K., and Cordier, Daniel, 2010, The principal rare earth elements deposits of the United States—A summary of domestic deposits and a global perspective: U.S.