Processing Technologies for Gold-Telluride Ores
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Selenium and Tellurium in 2017
2017 Minerals Yearbook SELENIUM AND TELLURIUM [ADVANCE RELEASE] U.S. Department of the Interior May 2020 U.S. Geological Survey Selenium and Tellurium By C. Schuyler Anderson Domestic survey data and tables were prepared by Robin C. Kaiser, statistical assistant. In 2017, selenium and tellurium were not refined in the selenium dioxide (SeO2) was substituted for sulfur dioxide United States. Three copper refineries produced either to reduce the power required to operate electrolytic cells. In semirefined selenium and tellurium or selenium- and tellurium- 2017, global production of manganese increased by 37% to containing copper anode slimes, and all production was 1.73 million metric tons, of which China remained the main exported for further processing. U.S. imports and exports producer (International Manganese Institute, 2018, p. 17). of selenium and tellurium increased in 2017 compared with In other metallurgical applications, selenium was used with those in 2016. The average Platts Metals Week New York bismuth to substitute for lead as a free-machining agent in brass dealer price for 99.5%-pure selenium in 2017 decreased by plumbing fixtures. Metallurgical-grade selenium also was used 54% to $10.78 per pound from $23.69 per pound in 2016, as an additive to cast iron, copper, lead, and steel alloys. reaching the lowest price since 2003. The average price for In the glass industry, selenium was used to decolorize the 99.99%-pure tellurium (in warehouse, Rotterdam), as reported green tint caused by iron impurities in container glass and other by Argus Media group—Argus Metals International, increased soda-lime silica glass. -
Inorganic Selenium and Tellurium Speciation in Aqueous Medium of Biological Samples
1 INORGANIC SELENIUM AND TELLURIUM SPECIATION IN AQUEOUS MEDIUM OF BIOLOGICAL SAMPLES ________________________ A Thesis Presented to The Faculty of the Department of Chemistry Sam Houston State University ________________________ In Partial fulfillment Of the Requirements for the Degree of Master of Science ________________________ by Rukma S. T. Basnayake December, 2001 2 INORGANIC SELENIUM AND TELLURIUM SPECIATION IN AQUEOUS MEDIUM OF BIOLOGICAL SAMPLES by Rukma S.T. Basnayake _______________________________ APPROVED: ________________________________ Thomas G. Chasteen, Thesis Director ________________________________ Paul A. Loeffler ________________________________ Benny E. Arney Jr. APPROVED: _____________________________ Dr. Brian Chapman, Dean College of Arts and Sciences 3 ABSTRACT Basnayake, Rukma ST, Inorganic Selenium and Tellurium Speciation in Aqueous Medium of Biological Samples, Master of Science (Chemistry), December 2001, Sam Houston State University, Huntsville, Texas, 60 pp. Purpose The purpose of this research was to develop methods to study the ability of bacteria, Pseudomonas fluorescens K27 to detoxify tellurium and selenium salts by biotransformation processes under anaerobic conditions. Another purpose was to make an effort to separate biologically produced Se0 from cells. Methods Pseudomonas fluorescens K27 was grown in TSN3 medium (tryptic soy broth with 0.3% nitrate) under anaerobic conditions and the production of elemental tellurium and elemental selenium was observed when amended with inorganic tellurium salts and selenium salts, respectively. The amount of soluble tellurium species in the culture medium also was determined. Samples from a 2.75 L bioreactor were taken after cultures had reached the stationary growth phase and were centrifuged in order to separate insoluble species (elemental tellurium, elemental selenium) from soluble species (oxyanions of tellurium, oxyanions of selenium). -
Old Puzzle of Incommensurate Crystal Structure of Calaverite Aute2 And
Old puzzle of incommensurate crystal structure of calaverite AuTe2 and predicted stability of novel AuTe compound Sergey V. Streltsova,b,1, Valerii V. Roizenc, Alexey V. Ushakova, Artem R. Oganovc,d, and Daniel I. Khomskiie aDepartment of Theory of Low-Dimensional Spin Systems, Institute of Metal Physics, 620990 Yekaterinburg, Russia; bDepartment of Theoretical Physics and Applied Mathematics, Ural Federal University, 620002 Yekaterinburg, Russia; cComputational Materials Discovery Laboratory, Moscow Institute of Physics and Technology, 141701 Dolgoprudny, Moscow Region, Russian Federation; dMaterials Discovery Laboratory, Skolkovo Institute of Science and Technology, 143026 Skolkovo, Russian Federation; and eII. Physikalisches Institut, Universitat¨ zu Koln,¨ D-50937 Cologne, Germany Edited by James R. Chelikowsky, The University of Texas at Austin, Austin, Texas, and accepted by Editorial Board Member John D. Weeks August 14, 2018 (received for review February 15, 2018) Gold is a very inert element, which forms relatively few com- Old Puzzle of Calaverite’s Crystal Structure pounds. Among them is a unique material—mineral calaverite, AuTe2 has a distorted layered CdI2-type structure [the aver- AuTe2. Besides being the only compound in nature from which age structure has space group C 2=m (6)], with triangular layers one can extract gold on an industrial scale, it is a rare exam- of Au with Te atoms in between. However, there is a periodic ple of a natural mineral with incommensurate crystal structure. displacive modulation along the [010] direction, which makes Moreover, it is one of few systems based on Au, which become overall crystal structure incommensurate (7). The mechanism superconducting (at elevated pressure or doped by Pd and Pt). -
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 -
Inferred Phase Relations in Part of the System Au–Ag–Te: an Integrated Analytical Study of Gold Ore from the Golden Mile, Kalgoorlie, Australia
Mineralogy and Petrology (2005) 83: 283–293 DOI 10.1007/s00710-004-0065-1 Inferred phase relations in part of the system Au–Ag–Te: an integrated analytical study of gold ore from the Golden Mile, Kalgoorlie, Australia L. Bindi1, M. D. Rossell2, G. Van Tendeloo2, P. G. Spry3, and C. Cipriani1 1 Museo di Storia Naturale, Sezione di Mineralogia, Universita degli Studi di Firenze, Italy 2 Electron Microscopy for Materials Research (EMAT), University of Antwerp, Belgium 3 Department of Geological and Atmospheric Sciences, Iowa State University, Ames, IA, USA Received May 24, 2004; revised version accepted October 7, 2004 Published online December 7, 2004; # Springer-Verlag 2004 Editorial handling: J. G. Raith Summary Integrated X-ray powder diffraction, scanning electron microscopy, electron probe, and transmission electron microscopy studies have identified the rare contact assemblage calaverite–sylvanite–hessite in a sample of gold ore from the Golden Mile deposit, Kalgoorlie, Australia. The presence of coexisting calaverite–hessite at Kalgoorlie is a non-equilibrium assemblage whereby the stable hessite-bearing assemblage is hessite– sylvanite, which formed from the breakdown of the -phase or -phase below 120 C, stuutzite€ þ -phase, or sylvanite þ stuutzite€ þ -phase, as predicted by Cabri (1965). Introduction Epizonal and mesozonal gold and gold–silver telluride deposits spatially asso- ciated with calc-alkaline, alkaline, and mafic igneous rocks are among the largest resources of gold in the world. They include Golden Mile, Kalgoorlie, Australia (e.g., Clout et al., 1990; Shackleton et al., 2003), Emperor, Fiji (e.g., Ahmad et al., 1987; Pals and Spry, 2003), Cripple Creek, Colorado (e.g. -
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. -
Calaverite Aute2 C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Monoclinic
Calaverite AuTe2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m or 2. Bladed and short to slender prisms elongated k [010], striated k [010], to 1 cm; also massive, granular. Twinning: Common on {110}, less common on {031} and {111}. Physical Properties: Fracture: Uneven to subconchoidal. Tenacity: Brittle. Hardness = 2.5–3 VHN = 197–213 (100 g load). D(meas.) = 9.10–9.40 D(calc.) = 9.31 Optical Properties: Opaque. Color: Grass-yellow to silver-white; white in reflected light. Streak: Greenish to yellowish gray. Luster: Metallic. Pleochroism: Weak. Anisotropism: Weak. R1–R2: (400) 45.7–54.4, (420) 48.4–57.1, (440) 51.1–59.6, (460) 53.6–61.8, (480) 56.0–63.6, (500) 57.9–65.2, (520) 59.4–66.4, (540) 60.6–67.3, (560) 61.3–68.0, (580) 61.8–68.3, (600) 62.2–68.4, (620) 62.5–68.6, (640) 62.7–68.5, (660) 62.8–68.4, (680) 62.9–68.2, (700) 63.0–68.1 Cell Data: Space Group: C2/m or C2. a = 7.1947(4) b = 4.4146(2) c = 5.0703(3) β =90.038(4)◦ Z=2 X-ray Powder Pattern: Cripple Creek, Colorado, USA. 3.02 (10), 2.09 (8), 2.20 (4), 2.93 (3), 1.758 (3), 1.689 (3), 1.506 (3) Chemistry: (1) (2) (3) Au 41.66 42.15 43.59 Ag 0.77 0.60 Te 57.87 57.00 56.41 Total 100.30 99.75 100.00 (1) Cripple Creek, Colorado, USA. -
The Periodic Table of Elements
The Periodic Table of Elements 1 2 6 Atomic Number = Number of Protons = Number of Electrons HYDROGENH HELIUMHe 1 Chemical Symbol NON-METALS 4 3 4 C 5 6 7 8 9 10 Li Be CARBON Chemical Name B C N O F Ne LITHIUM BERYLLIUM = Number of Protons + Number of Neutrons* BORON CARBON NITROGEN OXYGEN FLUORINE NEON 7 9 12 Atomic Weight 11 12 14 16 19 20 11 12 13 14 15 16 17 18 SODIUMNa MAGNESIUMMg ALUMINUMAl SILICONSi PHOSPHORUSP SULFURS CHLORINECl ARGONAr 23 24 METALS 27 28 31 32 35 40 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 POTASSIUMK CALCIUMCa SCANDIUMSc TITANIUMTi VANADIUMV CHROMIUMCr MANGANESEMn FeIRON COBALTCo NICKELNi CuCOPPER ZnZINC GALLIUMGa GERMANIUMGe ARSENICAs SELENIUMSe BROMINEBr KRYPTONKr 39 40 45 48 51 52 55 56 59 59 64 65 70 73 75 79 80 84 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 RUBIDIUMRb STRONTIUMSr YTTRIUMY ZIRCONIUMZr NIOBIUMNb MOLYBDENUMMo TECHNETIUMTc RUTHENIUMRu RHODIUMRh PALLADIUMPd AgSILVER CADMIUMCd INDIUMIn SnTIN ANTIMONYSb TELLURIUMTe IODINEI XeXENON 85 88 89 91 93 96 98 101 103 106 108 112 115 119 122 128 127 131 55 56 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 CESIUMCs BARIUMBa HAFNIUMHf TANTALUMTa TUNGSTENW RHENIUMRe OSMIUMOs IRIDIUMIr PLATINUMPt AuGOLD MERCURYHg THALLIUMTl PbLEAD BISMUTHBi POLONIUMPo ASTATINEAt RnRADON 133 137 178 181 184 186 190 192 195 197 201 204 207 209 209 210 222 87 88 104 105 106 107 108 109 110 111 112 113 114 115 116 117 118 FRANCIUMFr RADIUMRa RUTHERFORDIUMRf DUBNIUMDb SEABORGIUMSg BOHRIUMBh HASSIUMHs MEITNERIUMMt DARMSTADTIUMDs ROENTGENIUMRg COPERNICIUMCn NIHONIUMNh -
Minerals of the San Luis Valley and Adjacent Areas of Colorado Charles F
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/22 Minerals of the San Luis Valley and adjacent areas of Colorado Charles F. Bauer, 1971, pp. 231-234 in: San Luis Basin (Colorado), James, H. L.; [ed.], New Mexico Geological Society 22nd Annual Fall Field Conference Guidebook, 340 p. This is one of many related papers that were included in the 1971 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Trace-Metal Content of the Pueblo Viejo Precious-Metal Deposits and Their Relation to Other High-Sulfidation Epithermal Systems
Mineralium Deposita (2003) 38: 668–682 DOI 10.1007/s00126-003-0356-1 ARTICLE Stephen E. Kesler Æ Norman Russell Æ Karr McCurdy Trace-metal content of the Pueblo Viejo precious-metal deposits and their relation to other high-sulfidation epithermal systems Received: 30 November 2002 / Accepted: 12 December 2002 / Published online: 12 April 2003 Ó Springer-Verlag 2003 Abstract We provide here information on the distribu- abruptly in the upper part of the deposits. This change tion of copper, zinc, lead, gold, silver, barium, arsenic, probably reflects boiling of the hydrothermal solutions antimony, mercury, selenium and tellurium in the and partitioning of mercury and tellurium into a rising Moore and Monte Negro high-sulfidation epithermal vapor phase, and it suggests that host rocks overlying deposits in the Pueblo Viejo district, Dominican the deposits will be anomalous in mercury and tellurium. Republic. Moore and Monte Negro are funnel-shaped Comparison to the Broadlands, New Zealand, hydro- zones of advanced argillic alteration and precious-metal thermal system supports these inferred depositional mineralization which extend to depths of about 350 m processes. It shows that the behavior of arsenic and below the present surface. The uppermost part of the antimony at Broadlands was different from that at Moore deposit has been removed by erosion, whereas Pueblo Viejo, possibly because the elements were com- the Monte Negro deposit is covered by rocks containing plexed differently in the two ore fluids. Comparison of low, but still anomalous gold grades. At Moore, con- trace-element abundances at Pueblo Viejo to other high- centrations of all elements except copper increase up- sulfidation epithermal systems shows differences in base- ward through the deposit. -
Toward the Crystal Structure of Nagyagite, [Pb(Pb,Sb)S2][(Au,Te)]
American Mineralogist, Volume 84, pages 669–676, 1999 Toward the crystal structure of nagyagite, [Pb(Pb,Sb)S2][(Au,Te)] HERTA EFFENBERGER,1,* WERNER H. PAAR,2 DAN TOPA,2 FRANZ J. CULETTO,3 AND GERALD GIESTER1 1Institut für Mineralogie und Kristallographie, Universität Wien, Althanstrasse 14, A-1090 Vienna, Austria 2Institut für Mineralogie, Universität Salzburg, Hellbrunnerstrasse 34, A-5020 Salzburg 3Kärntner Elektrizitäts AG, Arnulfplatz 2, A-9021 Klagenfurt, Austria ABSTRACT Synthetic nagyagite was grown from a melt as part of a search for materials with high-tempera- ture superconductivity. Electron microprobe analyses of synthetic nagyagite and of nagyagite from the type locality Nagyág, Transylvania (now S˘ac˘arîmb, Romania) agree with data from literature. The crystal chemical formula [Pb(Pb,Sb)S2][(Au,Te)] was derived from crystal structure investi- gations. Nagyagite is monoclinic pseudotetragonal. The average crystal structure was determined from both synthetic and natural samples and was refined from the synthetic material to R = 0.045 for 657 single-crystal X-ray data: space group P21/m, a = 4.220(1) Å, b = 4.176(1) Å, c = 15.119(3) Å, β = 95.42(3)°, and Z = 2. Nagyagite features a pronounced layer structure: slices of a two slabs thick SnS-archetype with formula Pb(Pb,Sb)S2 parallel to (001) have a thickness of 9.15 Å. Te and Au form a planar pseudo-square net that is sandwiched between the SnS-archetype layers; it is [4Te] assumed that planar Au Te4 configurations are edge connected to chains and that Te atoms are in a zigzag arrangement. -
Intergrowth Texture in Au-Ag-Te Minerals from Sandaowanzi Gold Deposit, Heilongjiang Province: Implications for Ore-Forming Environment
Article Geology July 2012 Vol.57 No.21: 27782786 doi: 10.1007/s11434-012-5170-7 SPECIAL TOPICS: Intergrowth texture in Au-Ag-Te minerals from Sandaowanzi gold deposit, Heilongjiang Province: Implications for ore-forming environment XU Hong*, YU YuXing, WU XiangKe, YANG LiJun, TIAN Zhu, GAO Shen & WANG QiuShu School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China Received January 16, 2012; accepted March 16, 2012; published online May 6, 2012 Sandaowanzi gold deposit, Heilongjiang Province, is the only single telluride type gold deposit so far documented in the world, in which 90% of gold is hosted in gold-silver telluride minerals. Optical microscope observation, scanning electron microscope, electron probe and X-ray diffraction analysis identified abundant intergrowth textures in the Au-Ag-Te minerals, typified by sylvanite-hosting hessite crystals and hessite-hosting petzite crystals. The intergrown minerals and their chemistry are consistent, and the hosted minerals are mostly worm-like or as oriented stripes, evenly distributed in the hosting minerals, with clear and smooth interfaces. These suggest an exsolution origin for the intergrowth texture. With reference to the phase-transformation temperature derived from synthesis experiments of tellurides, the exsolution texture of Au-Ag-Te minerals implies that the veined tellurides formed at 150–220°C. The early stage disseminated tellurides formed at log f(Te2) from 13.6 to 7.8, log f(S2) from 11.7 to 7.6, whereas the late stage veined tellurides formed at log f(Te2) ranging from 11.2 to 9.7 and log f(S2) from 16.8 to 12.2.