Preliminary Estimates of the Quantities of Rare-Earth Elements Contained in Selected Products and in Imports of Semimanufactured Products to the United States, 2010
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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. -
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. -
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. -
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. -
Synthesis and Optical Characterization of Samarium Doped Lanthanum Orthophosphate Nanowires
Materials Transactions, Vol. 56, No. 9 (2015) pp. 1422 to 1424 Special Issue on Nanostructured Functional Materials and Their Applications ©2015 The Japan Institute of Metals and Materials Synthesis and Optical Characterization of Samarium Doped Lanthanum Orthophosphate Nanowires Le Van Vu+1, Duong Thi Mai Huong+2, Vu Thi Hai Yen+2 and Nguyen Ngoc Long Center for Materials Science, Faculty of Physics, VNU University of Science, 334 Nguyen Trai, Thanh Xuan, Hanoi, Vietnam 3+ LaPO4 nanowires doped with 0, 1, 2, 3, 4 and 5 mol% Sm were prepared by co-precipitation technique. These nanowires were studied by X-ray diffraction (XRD), transmission electron microscopy (TEM), photoluminescence (PL), photoluminescence excitation (PLE) spectra and energy-dispersive X-ray spectra (EDS). The PL spectra exhibited 4 groups of emission peaks, which are assigned to the transitions from the 4 6 3+ 3+ excited state G5/2 to the ground states HJ with J = 5/2; 7/2; 9/2 and 11/2ofSm ions. The intensity of PL related to Sm ion reached to a maximum when the Sm doping content was 2 mol%. The PLE spectra show 8 peaks, which are attributed to the absorption transitions from the 6 4 4 6 4 6 4 4 4 H5/2 ground state to the K15/2, D3/2, P7/2, F7/2, P5/2, G9/2, I13/2 and I11/2 excited states. [doi:10.2320/matertrans.MA201526] (Received January 27, 2015; Accepted June 25, 2015; Published August 7, 2015) Keywords: co-precipitation, samarium doped lanthanum orthophosphate, nanowires, photoluminescence 1. Introduction stirring for 3 h at room temperature. -
Regulation of Source Material
STATE OF CALIFORNIA--HEALTH AND HUMAN SERVICES AGENCY GRAY DAVIS, Governor DEPARTMENT OF HEALTH SERVICES RADIOLOGIC HEALTH BRANCH P.O. BOX 942732, MS-178 SACRAMENTO, CA 94234-7320 (916) 445-0931 August 30, 2001 t-4 Mr. Paul Lohaus U.S. Nuclear Regulatory Commission Office of State and Tribal Programs _ -o Washington, D.C. 20555 SUBJECT: REGULATION OF SOURCE MATERIAL Dear Mr. Lohaus: The State of California, Department of Health Services, Radiologic Health Branch (RHB) has recently been working to license Molycorp, Inc.'s operations in Mountain Pass, CA, as they relate to the possession and use of source material. Molycorp mines and processes rare-earth ores containing less than 0.05% source material at their facility, producing refined rare-earth compounds containing greater than 0.05% source material that are purchased by others for further processing or for incorporation into finished commercial products. Several issues have arisen related to the regulation of source material at this facility. We are contacting you for an interpretation of NRC regulations as they would apply to this material. Our questions relate primarily to issues concerning those exemptions contained in 10 CFR 40.13 for source material that is less than 0.05% by weight uranium or thorium and for rare-earth metals and compounds, mixtures and products containing not more than 0.25% by weight uranium and thorium. Our concerns involve both the regulation of active licenses and the decommissioning of sites contaminated by the materials referenced above. Thus, we are also seeking an interpretation of your regulations in 10 CFR 20, Subpart E, as they relate to decommissionings. -
Study of Xenon and Samarium Behaviour in the Leu Parr-1 Cores
PINSTECH-142 PK9600216 STUDY OF XENON AND SAMARIUM BEHAVIOUR IN THE LEU PARR-1 CORES 1 t; » Muhammad Arshad* ! » ( « li { • i Reactor Physics Group Nuclear Engineering Division Pakistan Institute of Nuclear Science & Technology P. O. Nilore, Islamabad. October, 1994 PINSTECH- STUDY OF XENON AND SAMARIUM BEHAVIOUR IN THE LEU PARR-1 GORES Reactor Physics Group Nuclear Engineering Division Pakistan Institute of Nuclear Science and Technology P. 0. Nilore, Islamabad * Present address Institute for Nuclear Power P.O. Box 3140 Islamabad October, 1994 In order to study behaviour of important fission product poisons, i.e. xenon and samarium, in PARR-1 after power upgradation and conversion to low enriched uranium (LEU) fuel, typical PARR-1 cores have been analysed using various models. It is found that negative reactivity due to equilibrium xenon increases when the reactor power is increased from 5 to 9 or 10 MW. However, the build-up of post-shutdown xenon is more pronounced at upgraded power. Thus at 10 MW the reactor will be poisoned out more quickly compared with 5 MW and remain so for a longer duration. As a result the time available for restarting the reactor after an unscheduled shutdown will be reduced and once the reactor is poisoned out the restart will be possible after a much longer time. 1. INTRODUCTION 1 2. THEORY 2 2.1 Build-up and Decay of Xenon 2 2.2 Build-up of Samarium 3 3. RESULTS AND DISCUSSION 5 3.1 Build-up of Xenon After Start-up 5 3.2 Equilibrium. Xenon Reactivity 6 3.3 Xenon Build-up after Reactor Shutdown 7 4. -
A Historical Geography of Rare Earth Elements: from Discovery to the Atomic Age
The Extractive Industries and Society 2 (2015) 572–580 Contents lists available at ScienceDirect The Extractive Industries and Society journal homepage: www.elsevier.com/locate/exis Review article A historical geography of rare earth elements: From discovery to the atomic age Julie Michelle Klinger* Frederick S. Pardee School of Global Studies, Boston University, United States ARTICLE INFO ABSTRACT Article history: This article presents a historical geography of rare earth elements from their discovery to the atomic age Received 16 January 2015 with a focus on the period between 1880 and 1960 in order to lend greater depth to the growing body of Received in revised form 19 May 2015 scholarship on the relationship between rare earth elements and global political change. Drawing on Available online 7 July 2015 archival and field research undertaken in the United States, China, Brazil, and Germany between 2011 and 2014, this article advances the following argument. Rare earth elements, and the production of geological Keywords: knowledge about them, have entangled with contentious politics since their first industrial applications Rare earth elements in the late 19th century. The historical geography of rare earth exploration and extraction is defined by a Historical geography fundamental tension between the military-industrial necessity of these elements and the hazards Geology fi Politics associated with their production. This tension played a de nitive role in international colonial, Cold War, Cold war and atomic politics. ã 2015 Elsevier Ltd. All rights reserved. Contents 1. Introduction . ................................................................................................... 572 2. Discovery and classification .......................................................................................... 573 3. Geology, territory, and power . ..................................................................................... 573 4. The political life of rare earth elements ............................................................................... -
BNL-79513-2007-CP Standard Atomic Weights Tables 2007 Abridged To
BNL-79513-2007-CP Standard Atomic Weights Tables 2007 Abridged to Four and Five Significant Figures Norman E. Holden Energy Sciences & Technology Department National Nuclear Data Center Brookhaven National Laboratory P.O. Box 5000 Upton, NY 11973-5000 www.bnl.gov Prepared for the 44th IUPAC General Assembly, in Torino, Italy August 2007 Notice: This manuscript has been authored by employees of Brookhaven Science Associates, LLC under Contract No. DE-AC02-98CH10886 with the U.S. Department of Energy. The publisher by accepting the manuscript for publication acknowledges that the United States Government retains a non-exclusive, paid-up, irrevocable, world-wide license to publish or reproduce the published form of this manuscript, or allow others to do so, for United States Government purposes. This preprint is intended for publication in a journal or proceedings. Since changes may be made before publication, it may not be cited or reproduced without the author’s permission. DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, nor any of their contractors, subcontractors, or their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or any third party’s use or the results of such use of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof or its contractors or subcontractors.