I Investigation Into the Separation and Purification of Europium and Yttrium
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Evolution and Understanding of the D-Block Elements in the Periodic Table Cite This: Dalton Trans., 2019, 48, 9408 Edwin C
Dalton Transactions View Article Online PERSPECTIVE View Journal | View Issue Evolution and understanding of the d-block elements in the periodic table Cite this: Dalton Trans., 2019, 48, 9408 Edwin C. Constable Received 20th February 2019, The d-block elements have played an essential role in the development of our present understanding of Accepted 6th March 2019 chemistry and in the evolution of the periodic table. On the occasion of the sesquicentenniel of the dis- DOI: 10.1039/c9dt00765b covery of the periodic table by Mendeleev, it is appropriate to look at how these metals have influenced rsc.li/dalton our understanding of periodicity and the relationships between elements. Introduction and periodic tables concerning objects as diverse as fruit, veg- etables, beer, cartoon characters, and superheroes abound in In the year 2019 we celebrate the sesquicentennial of the publi- our connected world.7 Creative Commons Attribution-NonCommercial 3.0 Unported Licence. cation of the first modern form of the periodic table by In the commonly encountered medium or long forms of Mendeleev (alternatively transliterated as Mendelejew, the periodic table, the central portion is occupied by the Mendelejeff, Mendeléeff, and Mendeléyev from the Cyrillic d-block elements, commonly known as the transition elements ).1 The periodic table lies at the core of our under- or transition metals. These elements have played a critical rôle standing of the properties of, and the relationships between, in our understanding of modern chemistry and have proved to the 118 elements currently known (Fig. 1).2 A chemist can look be the touchstones for many theories of valence and bonding. -
Historical Development of the Periodic Classification of the Chemical Elements
THE HISTORICAL DEVELOPMENT OF THE PERIODIC CLASSIFICATION OF THE CHEMICAL ELEMENTS by RONALD LEE FFISTER B. S., Kansas State University, 1962 A MASTER'S REPORT submitted in partial fulfillment of the requirements for the degree FASTER OF SCIENCE Department of Physical Science KANSAS STATE UNIVERSITY Manhattan, Kansas 196A Approved by: Major PrafeLoor ii |c/ TABLE OF CONTENTS t<y THE PROBLEM AND DEFINITION 0? TEH-IS USED 1 The Problem 1 Statement of the Problem 1 Importance of the Study 1 Definition of Terms Used 2 Atomic Number 2 Atomic Weight 2 Element 2 Periodic Classification 2 Periodic Lav • • 3 BRIEF RtiVJiM OF THE LITERATURE 3 Books .3 Other References. .A BACKGROUND HISTORY A Purpose A Early Attempts at Classification A Early "Elements" A Attempts by Aristotle 6 Other Attempts 7 DOBEREBIER'S TRIADS AND SUBSEQUENT INVESTIGATIONS. 8 The Triad Theory of Dobereiner 10 Investigations by Others. ... .10 Dumas 10 Pettehkofer 10 Odling 11 iii TEE TELLURIC EELIX OF DE CHANCOURTOIS H Development of the Telluric Helix 11 Acceptance of the Helix 12 NEWLANDS' LAW OF THE OCTAVES 12 Newlands' Chemical Background 12 The Law of the Octaves. .........' 13 Acceptance and Significance of Newlands' Work 15 THE CONTRIBUTIONS OF LOTHAR MEYER ' 16 Chemical Background of Meyer 16 Lothar Meyer's Arrangement of the Elements. 17 THE WORK OF MENDELEEV AND ITS CONSEQUENCES 19 Mendeleev's Scientific Background .19 Development of the Periodic Law . .19 Significance of Mendeleev's Table 21 Atomic Weight Corrections. 21 Prediction of Hew Elements . .22 Influence -
Spectrophotometric Determination of Praseodymium by 1,4
Arab Journal of Sciences & Research publishing Issue (2), Volume (1) September 2015 ISSN: 2518 - 5780 Spectrophotometric Determination of Praseodymium by 1,4- Dihydroxyanthraquinone after its Selective Separation from Rosetta Monazite Rare Earth Concentrate by Solvent Extraction Abdel Fattah N. A a Sadeek A. S b Ali B. H a Abdo, A. A a Weheish, H. L.a a Nuclear Materials Authority || Egypt b Faculty of Science || Zagazig University || Egypt Abstract: A rare earths concentrate of Rosetta monazite assays about 44, 23, 16.94 and 5.91 % for Ce, La, Nd and Pr respectively. Separation of cerium by air oxidation at 200oC. Selective separation of Pr by D2EHPA at pH1 followed by a sensitive spectrophotometric method which described for the determination of praseodymium (Pr) with l,4- dihydroxyanthraquinone . The calibration curve was linear from 0.1 to 12 µgml -1 praseodymium. The influences of various parameters and reaction conditions for maximum colour development were investigated. The relative standard deviation for determination of 1 µgml-1 praseodymium has found to be 1.3 after 5 repeated determinations; percent error 5.02%, molar absorptivity (ε) was 1.23x106M-1 cm-1and detection limit was 0.1µgml-1. The method for determination of praseodymium showed good accuracy and selectivity. INTRODUCTION Rare earth elements (REEs), represent one of a set of seventeen chemical elements in the periodic table, specifically the fifteen lanthanides, as well as scandium and yttrium (Connelly, N.G., et al., 2005). It was discovered of the black mineral Gadolinite by Carl Axel Arrhenius in 1787 (Gschneidner, and Cappellen, 1987). Traditionally, the REEs are divided into two groups on the basis of atomic weight; the light REEs are lanthanum through gadolinium (atomic numbers 57 through 64); and the heavy REEs comprise terbium through lutetium (atomic numbers 65 through 71). -
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. -
Yttrium Från Ytterby Och Litium Från Utö – Del 1 En Topografisk Karta Stockholm Vid 1200-Talets Slut
Grundämnenas upptäckt Grundämnenas upptäckt Exkursioner till Ytterby och Utö 6-7 juni eller 8-9 juni 6 juni Färje 1371: Strömkajen 08:30 Ytterby 09:30 09:45 – 10:45 Ytterby gruva Buss 682: Ytterby 11:03 Engarn 11:07 Buss 670: Engarn 11:09 Tekniska högskolan 11:44 Buss 4: Östra station 11:52 S:t Eriksplan 12:02 12:15 – 14:00 Rörstrands slott (lunch och visning) 14:00 – 16:00 Birkastan 7 juni Tåg 43: Stockholm City 08:16 Västerhaninge station 08:48 Buss 846: Västerhaninge station 09:09 Årstra brygga 09:22 Färje 2173: Årsta brygga 09:30 Gruvbryggan (Utö) 10:10 10:15 – 14:15 Rävstavik och Utö gruvor (matsäck) Färje 2178: Gruvbryggan (Utö) 14:30 Årsta brygga 15:25 Buss 846: Årstra brygga 15:32 Västerhaninge station 15:50 Tåg 43: Västerhaninge station 15:57 Stockholm City 16:29 Grundämnenas upptäckt Exkursioner till Ytterby och Utö 6-7 juni eller 8-9 juni 8 juni Färje 951: Strömkajen 09:15 Ytterby 10:40 10:55 – 11:45 Ytterby gruva Buss 682: Ytterby 12:03 Engarn 12:07 Buss 670: Engarn 12:09 Tekniska högskolan 12:44 Buss 4: Östra station 12:52 S:t Eriksplan 13:02 13:15 – 15:00 Rörstrands slott (lunch och visning) 15:00 – 17:00 Birkastan 9 juni Tåg 43: Stockholm City 08:16 Västerhaninge station 08:48 Buss 846: Västerhaninge station 09:09 Årstra brygga 09:22 Färje 2173: Årsta brygga 09:30 Gruvbryggan (Utö) 10:10 10:15 – 14:15 Rävstavik och Utö gruvor (matsäck) Färje 2178: Gruvbryggan (Utö) 14:30 Årsta brygga 15:25 Buss 846: Årstra brygga 15:32 Västerhaninge station 15:50 Tåg 43: Västerhaninge station 15:57 Stockholm City 16:29 -
GLOBAL RARE-EARTH PRODUCTION: HISTORY and OUTLOOK History – the Discovery
Center for Strategic and International Studies Rare Earth Elements: Geology, Geography, and Geopolitics James B. Hedrick Hedrick Consultants, Inc. U.S. Rare Earths, Inc. Burke, Virginia December 15, 2010 Washington, DC GLOBAL RARE-EARTH PRODUCTION: HISTORY AND OUTLOOK History – The Discovery . The rare earths were discovered in 1787 by Swedish Army Lieutenant Carl Axel Arrhenius . Carl, an amateur mineralogist collected the black mineral ytterbite, later renamed gadolinite, from a small feldspar and quartz mine at Ytterby, Sweden . With similar chemical structures the rare earths proved difficult to separate . It was not until 1794 that Finnish chemist Johann Gadolin separated the first impure yttrium oxide from the mineral ytterbite History – The Discovery History – The Commercialization . The rare earths were commercialized when the incandescent lamp mantle industry was established in 1884 with mantles of zirconium, lanthanum, and yttrium oxides with later improvements requiring only the oxides of thorium and cerium. The lamp mantle was discovered by Baron Carl Auer von Welsbach . The mantles also used small amounts of neodymium and praseodymium as an indelible brand name Welsbach label History – The Early Mining . Rare earths were first produced commercially in the 1880s with the mining in Sweden and Norway of the rare-earth thorium phosphate mineral monazite . Foreign Production Brazil produced monazite as early as 1887 India produced monazite starting in 1911 . Domestic Production Monazite production in the United States was first recorded in 1893 in North Carolina - a small tonnage of monazite was reportedly mined in 1887 Monazite mining in South Carolina began in 1903 History – The Processing . Three main methods for separating and refining the rare- earth elements since they were discovered . -
Transmittal of Draft EIR for Molycorp Mountain Pass Mine Expansion, for Review and Comment
COUNTY OF SAN BERNARDINO PLANNING DEPARTMENT I,regular-! I PUBLIC WORKS GROUP -- W&- Sw1. NENNO lorth Arrowhead Avenue * San Bernardino, CA 924154182 * (909) 3874131 VALERY PILMER Director of Planning December 9, 1996No. 909) 3873223 IY RESPONSIBLE AND TRUSTEE AGENCIES INTERESTED ORGANIZATIONS AND INDIVIDUALS RE: NOTICE OF AVAILABILITY FOR THE DRAFT EIR ON THE MOLYCORP MOUNTAIN PASS MINE EXPANSION Dear Reader/Reviewer: Enclosed for your review and comment is the Draft EIR for the Molycorp Mountain Pass Mine Expansion. The purpose of the document is to identify and describe the probable environmental impacts that would result from the proposed expansion of Molycorp's existing mine and processing plant complex located at Mountain Pass, California. Mountain Pass is within the unincorporated portion San Bernardino County along Interstate 15 approximately 30 miles northeast of Baker and approximately 14 miles southwest of the Nevada stateline. The proposed quarry and waste rock areas would add 696 acres of disturbance to the existing mine site, resulting in a total disturbed area of approximately 1,044 acres. sag_> This document has been prepared to meet the State requirements of the California Environmental Quality Act. The Draft EIR has been prepared under the supervision of the County of San Bernardino Planning Department. The public comment period will end on January 27, 1997. Written comments should be addressed to: County of San Bemnardino- Planning Dgparnn 385 N. Arrowhead Avenue, Third Floor San Bernardino, CA 92415-0182 Attn: Randy Scott Sincerely, Randy Scottjlanning Manager, San Berardo County Planning Department ~-! - nLA ,;;K Scr.'Eperviscs .,* 1:,. 3 - -, I- . 1 12 4~ ..!A','V34-' TUrCCI Vi~i D;s~ri:n, BARBA~RA CPANM FURtOPAN . -
Producers Case Study the Changing
Producers Case Study The Changing Geography of Rare Earth Element Production Introduction The locations where rare earth elements are produced changed repeatedly throughout the 1900s and early 2000s. This variation suggests that production is not determined primarily by the geographic location of rare earth ores. Instead, the location of mines and separation plants is driven by a combination of market prices, government policies, and the actions of producers and manufacturers. As a result where and how rare earth elements are produced could change in the future. Initial Rare Earth Metal Production Although a mineral containing rare earth elements was identified in Sweden in 1788, it took more than 100 years for the first significant industrial product to be made using the rare earths. In the 1890s chemist Carl Auer von Welsbach developed a mantle made of a mixture of 99% thorium and 1% cerium for use with gas streetlights. More than five billion mantles were sold worldwide through the 1930s. Welsbach also developed mischmetal, a mixture of rare earth elements cerium, lanthanum, neodymium, and praseodymium. When alloyed with iron, mischmetal produced a metal that sparked when struck. It was widely used in pocket cigarette lighters as well as automobile ignition switches. The Welsbach Company mined rare earth deposits located in coastal sands in Brazil, India, and North Carolina. India’s coastal sands are also rich in the radioactive element thorium, which is not a rare earth element. India banned the export of these sands in 1948 to preserve its thorium supply for a potential nuclear energy program. At that time the price of rare earth metals spiked until newly established mining locations briefly made South Africa the world’s leading exporter of rare earth ores in the 1950s. -
Critical Materials and US Import Reliance
Testimony Critical Materials and U.S. Import Reliance Recent Developments and Recommended Actions Richard Silberglitt CT-485 Testimony presented before House Natural Resources Committee, Subcommittee on Energy and Mineral Resources on December 12, 2017. For more information on this publication, visit www.rand.org/pubs/testimonies/CT485.html Testimonies RAND testimonies record testimony presented or submitted by RAND associates to federal, state, or local legislative committees; government-appointed commissions and panels; and private review and oversight bodies. Published by the RAND Corporation, Santa Monica, Calif. © Copyright 2017 RAND Corporation is a registered trademark. Limited Print and Electronic Distribution Rights This document and trademark(s) contained herein are protected by law. This representation of RAND intellectual property is provided for noncommercial use only. Unauthorized posting of this publication online is prohibited. Permission is given to duplicate this document for personal use only, as long as it is unaltered and complete. Permission is required from RAND to reproduce, or reuse in another form, any of its research documents for commercial use. For information on reprint and linking permissions, please visit www.rand.org/pubs/permissions.html. www.rand.org Critical Materials and U.S. Import Reliance: Recent Developments and Recommended Actions Testimony of Richard Silberglitt1 The RAND Corporation2 Before the Committee on Natural Resources Subcommittee on Energy and Mineral Resources United States House of Representatives December 12, 2017 hank you Chairman Gosar, Ranking Member Lowenthal, and distinguished members of the Subcommittee for inviting me to testify today. My testimony is based on the results of a 2013 study conducted by the RAND Corporation at the request of the National T 3 Intelligence Council, taking into account relevant developments and data since the publication of that report. -
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). -
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. -
Europium-Doped Phosphors for Lighting: the Past, the Present and the Future
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Ghent University Academic Bibliography Europium-doped phosphors for lighting: the past, the present and the future Dirk Poelman*, Philippe F. Smet Lumilab, Dept. Solid State Sciences, Ghent University, Krijgslaan 281/S1, B-9000 Gent, Belgium *[email protected] The past Europium, the 63rd element of the periodic table, was isolated and identified as one of the last in the rare earth series by Eugène-Anatole Demarçay in 1901, and named after the European continent. Europium does not occur as a metallic element in nature, as it readily oxidizes. It is found in small quantities (of the order of 1 ppm) in the earth crust. It is mined from a few minerals, where the Eu-content can reach a few tenths of % [1]. Fluorite (CaF2), a mineral which is widely found in nature, has been known to be luminescent since early times, and gave its name to the process of fluorescence. A specific mine in England, the Blue John Cavern, was known for its blue fluorescing fluorite crystals [2]. Later, it was found that not the CaF2 itself is luminescent, but rather the Eu2+ ions which are incorporated as impurities in the crystals are responsible for the blue fluorescence. Therefore, the history of Eu-doped phosphors dates back thousands of years. 3+ When in the 1960s, europium-doped yttrium orthovanadate (YVO4:Eu ) was developed as a red phosphor, this formed the breakthrough of color television: until then, no bright phosphors were available for the red 3+ component of CRTs.