The Platinum-Group Elements (PGE)
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Geological Investigations in the Bird River Sill, Southeastern Manitoba (Part of NTS 52L5): Geology and Preliminary Geochemical Results by C.A
GS-19 Geological investigations in the Bird River Sill, southeastern Manitoba (part of NTS 52L5): geology and preliminary geochemical results by C.A. Mealin1 Mealin, C.A. 2006: Geological investigations in the Bird River Sill, southeastern Manitoba (part of NTS 52L5): geology and preliminary geochemical results; in Report of Activities 2006, Manitoba Science, Technology, Energy and Mines, Manitoba Geological Survey, p. 214–225. Summary and gravitational differentiation. In 2005, this study was initiated to examine the Bird Theyer (1985) identified unusual River Sill (BRS), a mafic-ultramafic layered intrusion cooling conditions requiring several magma pulses and located in the Bird River greenstone belt in southeastern cast doubt on a single magmatic intrusion theory. Manitoba. The BRS is currently an exploration target In 2005, this study was initiated to examine the for Ni-Cu–platinum group element (PGE) deposits and, controls on Ni-Cu-PGE mineralization and test the single in the past, hosted two Ni-Cu mines (Maskwa West and versus multiple injection hypothesis to establish the Dumbarton mines). relationship between mineralization and the magmatic Nickel-copper mineralization on the western half history. Specific objectives include of the BRS consists primarily of disseminated to blebby • detailed mapping of the Chrome, Page, Peterson pyrrhotite+chalcopyrite and is present in the ultramafic Block and National-Ledin properties (Figure GS-19-1); series of the Chrome and Page properties and the mafic • determination of the sulphur source for the Ni-Cu- series of the Wards property. During this study, several PGE mineralization; new sulphide-bearing localities in both the ultramafic and • delineation of the sill’s sulphur saturation history; mafic units of the sill have been identified. -
Physical and Chemical Properties of Platinum Group Metals 2 Chapter 2 | Physical and Chemical Properties of Platinum Group Metals Contents
PHYSICAL AND CHEMICAL PROPERTIES OF PLATINUM GROUP METALS 2 CHAPTER 2 | PHYSICAL AND CHEMICAL PROPERTIES OF PLATINUM GROUP METALS CONTENTS 2.1 OVERVIEW OF PGMS 04 2.2 METALLIC PGMS 05 2.3 COMPOUNDS OF PLATINUM GROUP METALS 06 SIMPLE COMPOUNDS 06 COMPLEX COMPOUNDS 07 REFERENCES 13 2 CHAPTER 2 | PHYSICAL AND CHEMICAL PROPERTIES OF PLATINUM GROUP METALS SUMMARY • Six elements of Groups 8, 9, and 10 in the periodic table constitute the platinum group metals (PGMs): platinum (Pt), palladium (Pd), rhodium (Rh), ruthenium (Ru), iridium (Ir), and osmium (Os). • The physical and mechanical properties of the PGMs and their compounds indicate a wide range of properties with widely varying densities and solubilities (see Table 2-1). • Metallic forms of PGMs are generally considered to be ‘inert’, i.e., not chemically reactive. However, this is dependent in part on dimensional characteristics. Thus, while massive metal forms have low chemical reactivity, fi nely-divided metal powders with high surface area show greater reactivity. • Simple binary compounds exist for each of the PGMs. They also form a vast array of complex coordination compounds in which the central metal atom is bound to a variety of ligands by coordinate bonding, including halides, sulphur, amines, and other atoms and groups. • This unique coordination chemistry has made PGM compounds of great industrial value, but also can have implications for the health of workers exposed to certain of these compounds due to the linkages with biological behaviour and toxicity (see Chapter 6). • The complex halogenated platinum compounds (CHPS) are among those which are industrially and toxicologically important. -
New Exploration Methods for Platinum and Rhodium Deposits
SYNTHESIS REPORT FOR PUBLICATION CONTRACT No : BRE2-CT92-0302 PROJECT N* : BE-5793 TITLE : NEW EXPLORATION METHOD FOR PLATINUM AND RHODIUM DEPOSITS POOR IN BASE METAL SULPHIDES PROJECT COORDINATOR : BRGM PARTNERS : UNIVERSITY OF MANCHESTER UNIVERSITY OF COPENHAGEN CNRS NANCY STARTING DATE :30.11.92 DURATION :36 MONTHS *** PROJECT FUNDED BY THE EUROPEAN * * COMMUNITY UNDER THE BRITE/ELJRAM * * PROGRAMME * * *** E DATE: 30.1.96 H. TITLE, AUTHOR NAMES AND ADRESSES NEW EXPLORATION METHODS FOR PLATINUM AND RHODIUM POOR IN BASE METAL SULPHIDES NEXTPRIM (EC Contract BRE2-CT92-0302 - Project BE-5793) Coordinator BRGM : M. Ohnenstetter, Z. Johan, A. Cocherie, A.M. Fouillac. C. Guerrot 3, Avenue Claude Guillemin, BP 6009,4.5060 ORLEANS CEDEX 2, France. Partners CNRS : D. Ohnenstetter, M. Chaussidon, O. Rouer CRPG, 15, rue Notre Dame Des Pauvres, B.P. 20, 54501 Vand@uvre les Nan~ y, France. University of Couenha~en : E. Makovicky, M. Makovicky, J. Rose-Hansen, S. Karup- Mgller Geological Institute, f?kter Voldgade 10, 1350 Copenhagen K, Danemark University of Manchester : D. Vaughan, G. Turner, R.A.D. Pattrick, A.P. Gize. 1. Lyon, I. McDonald Department of Geology, Williamson Building, Oxford Road, M 13 9PL Manchester. England III. ABSTRACT A multidisciplinary approach has been applied to four subeconomic deposits of platinum metals in order to propose a new model of formation for platinum group element (PGE) deposits devoid of significant base metal sulphides (BMS). The aim was to facilitate the identification of new targets for PGE exploration. Two of the deposits occur in Albania, in the Tropoja and Bulqiza massifs respectively; these belong to an ophiolitic belt created in an oceanic environment during the Upper Jurassic. -
Origin of Platinum Group Minerals (PGM) Inclusions in Chromite Deposits of the Urals
minerals Article Origin of Platinum Group Minerals (PGM) Inclusions in Chromite Deposits of the Urals Federica Zaccarini 1,*, Giorgio Garuti 1, Evgeny Pushkarev 2 and Oskar Thalhammer 1 1 Department of Applied Geosciences and Geophysics, University of Leoben, Peter Tunner Str.5, A 8700 Leoben, Austria; [email protected] (G.G.); [email protected] (O.T.) 2 Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of Science, Str. Pochtovy per. 7, 620151 Ekaterinburg, Russia; [email protected] * Correspondence: [email protected]; Tel.: +43-3842-402-6218 Received: 13 August 2018; Accepted: 28 August 2018; Published: 31 August 2018 Abstract: This paper reviews a database of about 1500 published and 1000 unpublished microprobe analyses of platinum-group minerals (PGM) from chromite deposits associated with ophiolites and Alaskan-type complexes of the Urals. Composition, texture, and paragenesis of unaltered PGM enclosed in fresh chromitite of the ophiolites indicate that the PGM formed by a sequence of crystallization events before, during, and probably after primary chromite precipitation. The most important controlling factors are sulfur fugacity and temperature. Laurite and Os–Ir–Ru alloys are pristine liquidus phases crystallized at high temperature and low sulfur fugacity: they were trapped in the chromite as solid particles. Oxygen thermobarometry supports that several chromitites underwent compositional equilibration down to 700 ◦C involving increase of the Fe3/Fe2 ratio. These chromitites contain a great number of PGM including—besides laurite and alloys—erlichmanite, Ir–Ni–sulfides, and Ir–Ru sulfarsenides formed by increasing sulfur fugacity. Correlation with chromite composition suggests that the latest stage of PGM crystallization might have occurred in the subsolidus. -
Electrolytic Extraction of Platinum Group Metals from Dissolver Solution of Purex Process
Journal of NUCLEAR SCIENCE and TECHNOLOGY, 30(11), pp. 1195~1197 (November 1993). 1195 In this note, the proper deposition potential, SHORT NOTE nitric acid concentration, temperature, and Electrolytic Extraction of Platinum electrode materials were investigated, and the effect of coexisting ions was examined. Group Metals from Dissolver 1. Experimental Solution of Purex Process The experimental apparatus is shown in 1. The electrolytic cell (500 ml) consistedFig. KenjiKOIZUMI, Masaki OZAWA of a counter electrode (1 mmo, Pt wire), a re- and TornioKAWATA ference electrode (SCE), and a working elec- Power Reactor & Nuclear Fuel Development Corp.* trode. Ti and Ta were used as the elec- trode material. The electrolyte was agitated Receired May 19, 1993 to maintain a constant temperature. Elec- Revised July 30, 1993 trode potential were controlled by the po- KEYWORDS: electrolytic extraction, tentiostat. Pt group metals concentration deposits, palladium, rhodium, ruthe- was adjusted to about 1.0E-4 mol/l. Urani- nium, purex process, solvent extrac- um (VI) ion was tested as a main coexisting tion, deposition potential, recovery, actinide ion in this experiments. Potential- electrodeposition, dissolver solution time sequences for metal deposition and potential-current curves corresponding to Pd- In the commercial light water reactor fuel dissolution are shown in Fig.2. First the at a burn-up of 33 MWd/kg, approximately working electrode was cathodically polarized 4 kg of Pt group metals are included per ton in nitric acid solution containing Pt group of heavy metals(1). Elimination of the ionic metal. The polarization potential (05) was Pt group metals (Pd, Rh, Ru) from dissolver changed from +0.5 to -0.5 V. -
The Platinum Group Metals As Coating Materials
Issue No. 38 – February 2012 Updated from Original August 2002 Publication The Platinum Group Metals as Coating Materials How precious is your metal - An overview on The platinum group metals consist of platinum and palladium, as well as rhodium, iridium, the use of the platinum osmium, and ruthenium. They can be found in the transition metals on the periodic table of the elements. A close-up of this part of the table is shown in Figure 1. Palladium is currently the group metals as contact surfaces for electronic only metal of the group in widespread use in electrical contacts, although platinum was widely connectors. used in the past. Rhodium is only used in electrical contact applications requiring very high hardness and wear resistance. The other three metals in the group are used mainly in other industrial applications. Pure, electroplated platinum and palladium have a hardness of around 200 to 400 HV, although . Platinum they may also be applied by cladding. Both have a conductivity of around 16% IACS. Thus they are harder than gold, but slightly less conductive. At one time, their prices were . Palladium competitive with gold, and gold-flashed palladium coatings were even used as less expensive alternatives to gold coatings. However, both of these metals are much more expensive than gold . Rhodium (at least at the time of this writing). Due to its cost, gold-flashed palladium is now used mainly in applications which require greater hardness and wear resistance than hard gold alone. Ruthenium Rhodium is much harder than platinum and palladium, typically 800-1000 HV, with an . -
Recovery of Platinum Group Metals from High Level Radioactive Waste POSSIBILITIES of SEPARATION and USE RE-EVALUATED by R
Recovery of Platinum Group Metals from High Level Radioactive Waste POSSIBILITIES OF SEPARATION AND USE RE-EVALUATED By R. P. Bush AEA Technology, Harwell Laboratory, Oxfordshire, England When nuclear fuel is irradiated in a power reactor a wide range of chemical elements is created by the fission of uranium and plutonium. These fission products include palladium, rhodium and ruthenium, and could in principle constitute a valuable source of these three metals. Their separation from the fuel during reprocessing operations is, however, a complex matter. Various processes have been proposed and evaluated, mainly on a laboratory scale. To date none of them has been established as applicable on a commercial scale, but investigations with this aim are continuing in several countries. Even a complete separation of the platinum group metals from other nuclides would yield a radioac- tive product, because of the presence of active isotopes of the platinum group metals. These would be expected to restrict the practical utilisation of platinum group metals created by nuclear jisswn, unless an isotope separation technique can be developed, or the metals are stored until the radioactivity has decayed. The irradiation of nuclear fuels in power reviewed in Platinum Metals Review in 1970 reactors leads to the production of atoms of a (1). The current revival of interest has resulted wide range of fission products, ranging in partly because of the increasing economic im- atomic mass from 70 to 160. These fission pro- portance of rhodium. This metal is a crucial ducts generally constitute components of the component of the three-way catalysts used for radioactive waste generated by the nuclear fuel automobile emission control, and the demand cycle. -
Iridarsenite (Ir, Ru)As2 C 2001-2005 Mineral Data Publishing, Version 1
Iridarsenite (Ir, Ru)As2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. As irregular inclusions, to 60 µm, in a matrix of rutheniridosmine. Physical Properties: Hardness = n.d. VHN = 488 and 686 (100 g load) on two grains. D(meas.) = n.d. D(calc.) = 10.9 Optical Properties: Opaque. Color: In polished section, medium gray with brownish tint. Luster: Metallic. Pleochroism: Weak to none. Anisotropism: Weak but distinct, from medium gray to pale orange-brown. R1–R2: (470) 47.2–46.9, (546) 45.4–46.1, (589) 44.9–46.6, (650) 41.4–44.0 ◦ 0 Cell Data: Space Group: P 21/c (synthetic). a = 6.05 b = 6.06 c = 6.18 β = 113 17 Z=4 X-ray Powder Pattern: Papua New Guinea. 3.90 (100), 2.840 (70), 2.069 (60), 2.610 (50), 1.910 (50), 1.943 (40), 1.875 (40) Chemistry: (1) (2) Ir 40.7 52.2 Ru 10.3 1.7 Os 1.3 0.4 Pt 0.5 1.1 Rh 0.9 0.2 Pd 0.1 As 46.2 44.0 S 0.2 Total 99.0 99.9 (1) Papua New Guinea; by electron microprobe, corresponds to (Ir0.69Ru0.33Os0.02)Σ=1.04As2.00. (2) Do.; by electron microprobe, average of four other grains; corresponds to (Ir0.92Ru0.06 Os0.01Pt0.02Rh0.01)Σ=1.02(As1.97S0.03)Σ=2.00. Occurrence: In nuggets or fragments of natural Os–Ir–Ru alloys. Association: Irarsite, ruthenarsenite, rutheniridosmine. Distribution: From an unspecified locality [probably the Waria River, Bowutu Mountains, or the Yodda Goldfield] in Papua New Guinea [TL]. -
Colloform High-Purity Platinum from the Placer Deposit
Colloform high-purity platinum from the placer deposit of Koura River (Gornaya Shoriya, Russia) Nesterenko G.V.1, Zhmodik S.M.1,2, Airiyants E.V.1, Belyanin D.K.1,2, Kolpakov V.V.1, Bogush A.A.1,3,* 1V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, Novosibirsk 630090, Russia 2Novosibirsk State University, Novosibirsk 630090, Russia 3Department of Civil, Environmental & Geomatic Engineering, University College London, London WC1E 6BT, UK *Corresponding author: A.A. Bogush, E-mail: [email protected] Abstract A microinclusion of colloform high-purity platinum in a grain of platinum-group minerals (PGM) from the alluvial gold-bearing placer deposit in the south of Western Siberia (Russia) was detected and characterized for the first time. It is different in composition, texture, and conditions of formation from high-purity platinum of other regions described in the literature. The main characteristics of investigated high-purity platinum are colloform-layered texture, admixture of Fe (0.37-0.78 wt.%), and paragenesis of Cu-rich isoferroplatinum, hongshiite, and rhodarsenide. The PGM grain with high-purity platinum is multiphase and heterogeneous in texture. It is a product of intensive metasomatic transformation of Cu-rich isoferroplatinum (Pt3(Fe0.6Cu0.4)). The transformation was carried out in two stages: 1 - copper stage including three substages (Cu-rich isoferroplatinum, copper platinum and hongshiite); and 2 - arsenic (rhodarsenide). The formation of high-purity platinum was separated in time from the formation of isoferroplatinum and was carried out by precipitation from postmagmatic solutions. Keywords: platinum-group elements (PGE), platinum-group minerals (PGM), high-purity platinum, Cu-rich isoferroplatinum, hongshiite, alluvial placer, Gornaya Shoriya Introduction High-purity platinum was discovered in the gold-bearing placer deposit of Koura River situated in Gornaya Shoriya (south-western Siberia, Russia, Fig. -
Platinum Group Metal Chalcogenides
Platinum Group Metal Chalcogenides THEIR SYNTHESES AND APPLICATIONS IN CATALYSIS AND MATERIALS SCIENCE By Sandip Dey and Vimal K. Jain* Novel Materials and Structural Chemistry Division, Bhabha Atomic Research Centre, Mumbai 400085, India * E-mail: [email protected] Some salient features of platinum group metal compounds with sulfur, selenium or tellurium, known as chalcogenides, primarily focusing on binary compounds, are described here. Their structural patterns are rationalised in terms of common structural systems. Some applications of these compounds in catalysis and materials science are described, and emerging trends in designing molecular precursors for the syntheses of these materials are highlighted. Chalcogenides are a range of compounds that will consider first a selection of the structures primarily contain oxygen, sulfur, selenium, telluri- adopted, followed by their catalytic and electronic um or polonium and which may also occur in uses. nature. The compounds may be in binary, ternary or quaternary form. Platinum group metal chalco- Ruthenium and Osmium genides have attracted considerable attention in Chalcogenides recent years due to their relevance in catalysis and Ruthenium and osmium dichalcogenides of materials science. Extensive application of palladi- composition ME2 (M = Ru, Os; E = S, Se, Te) are um (~ 27% of global production in year 2000) in usually prepared by heating stoichiometric quanti- the electronic industry in multilayer ceramic capac- ties of the elements in evacuated sealed ampoules itors (MLCCs) and ohmic contacts has further at elevated temperatures (~ 700ºC) (13). Single accelerated research activity on platinum group crystals, such as RuS2, see Figure 1, are grown metal chalcogenide materials. either from a tellurium flux (4) or by chemical The platinum group metals form several vapour transport techniques using interhalogens as chalcogenides: transporting agent (5). -
Osmium (Os, Ir, Ru) C 2001-2005 Mineral Data Publishing, Version 1
Osmium (Os, Ir, Ru) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 6/m 2/m 2/m. Rare crystals are hexagonal tabular, to 3 mm; commonly as euhedral prismatic inclusions in Pt–Fe alloys. Physical Properties: Hardness = n.d. VHN = 1206–1246 (25 g load). D(meas.) = 22.48 D(calc.) = 22.59 Optical Properties: Opaque. Color: White with a bluish gray tinge in reflected light. Pleochroism: Noticeable. Anisotropism: Strong, reddish orange. R1–R2: (400) — , (420) 62.7–63.9, (440) 63.9–64.7, (460) 63.9–64.6, (480) 63.8–64.4, (500) 63.3–63.8, (520) 62.7–63.2, (540) 62.1–62.7, (560) 61.5–61.8, (580) 60.9–61.4, (600) 60.4–60.7, (620) 59.9–60.2, (640) 59.6–59.8, (660) 59.3–59.9, (680) 59.2–60.0, (700) 59.4–60.0 Cell Data: Space Group: P 63/mmc. a = 2.7341 c = 4.3197 Z = 2 X-ray Powder Pattern: Synthetic osmium. 2.076 (100), 2.367 (35), 2.160 (35), 1.3668 (20), 1.2300 (20), 1.1551 (20), 1.595 (18) Chemistry: (1) (2) (3) Os 94.1 84.8 98.8 r 5.4 12.0 0.3 Ru 0.8 2.2 Pt 0.1 1.7 Rh 0.5 Pd 0.1 0.2 Total 100.4 101.3 99.3 (1) Atlin, Canada; by electron microprobe. (2) Joubdo stream, Ethiopia; by electron microprobe. (3) Gusevogorskii pluton, Russia; by electron microprobe, average of four analyses. -
Platinum-Group Metals in New Mexico
ity within the Dakota to allow passageof the solutions; 4) presence of an impermeable Platinum-groupmetals in NewMexico caprock to contain the solutions, which are thought to have risen stratigraphically dur- by VirginiaT. McLemore, Robeft W. Eveleth, Lynn A. Brandvold,and James M. Robensln ing their migration northward toward the NewMexico Bureau of Minesand Mineral Resources. Socorro. NM 87801 San |uan Basin or westward toward the Gal- lup sag;and 5) availability of organic material in the Dakota to reduce and thereby precip- PGM reported in New Mexico itate the uranium from the rising solutions. Introduction (Blairet al.,1977) The author's observations agree with those Platinum-group metals (PGM) consist of of Piersonand Green (1980). six elements:platinum (Pt), palladium (Pd), Tampa mine, Bromide district, AcxNowlrpcrr.rrr.rrs-This report would not rhodium (Rh), iridium (Ir), osmium (Os), and Rio Arriba County have been completed without the encour- ruthenium (Ru); platinum and palladium are The Tampa mine in the northern part of agement of Virginia T. Mclemore of the New the most abundant of the group. The PGM the county is one of the largest mines in the Mexico Bureau of Mines and Mineral Re- typically occur together as natural alloys (for Bromide district with a 400-ft shaft and 800- sources. Thanks are owed to Leo E. Little, example, osmiridium-an alloy of osmium 1000ft of drifts (Bingler, 1968).Sulfide re- Manager of the Grand Junction projects of- and iridium) and to a lesserextent as sulfides placement veins containing chalcopyrite, fice of the DOE for accessto the AEC records and arsenides.All the metals are rare (Table molybdenite, pyrite, malachite,and somefree stored in the DOE archives at Grand Junc- 1) and therefore expensive.