A Fundamental Evaluation of the Atmospheric Pre-Leaching Section of the Nickel-Copper Matte Treatment Process

Total Page:16

File Type:pdf, Size:1020Kb

A Fundamental Evaluation of the Atmospheric Pre-Leaching Section of the Nickel-Copper Matte Treatment Process A FUNDAMENTAL EVALUATION OF THE ATMOSPHERIC PRE-LEACHING SECTION OF THE NICKEL-COPPER MATTE TREATMENT PROCESS by RODRICK MULENGA LAMYA Dissertation presented for the Degree of DOCTOR OF PHILOSOPHY (Extractive Metallurgical Engineering) in the Department of Process Engineering at the University of Stellenbosch, South Africa Promoter Prof. L. Lorenzen STELLENBOSCH March 2007 DECLARATION I the undersigned, hereby declare that the work contained in this dissertation is my own original work and that I have not previously in its entirety or in part submitted it at any university for a degree. Signature: ............................................... Date: ....................................................... Copyright © 2007 Stellenbosch University All rights reserved i SYNOPSIS Nickel-Copper sulphide ores are the most important Platinum Group Metal bearing ores. The South African deposits are exceptionally rich in the platinum group metals (PGMs) and production of the PGMs is the primary purpose of treating these ores. The methods used in the recovery of the PGMs from the nickel-copper ores generally consists of ore concentration by physical techniques, pyrometallurgical concentration and hydrometallurgical extraction of the base metals followed by the PGMs. Pyrometallurgical concentration produces Ni-Cu matte, which is treated by hydrometallurgical processes to recover the nickel, copper, cobalt and the precious metals. In this study, the leaching behaviour of a Ni–Cu matte in CuSO4–H2SO4 solution during the repulping (pre-leach) stage at Impala Platinum Refineries was studied. The repulping stage is basically a non–oxidative atmospheric leach stage, in which nickel, iron and cobalt are partially dissolved, while the copper is precipitated. To understand the nature of the leaching process during this stage of the base metal refining operation, the effects of variations in the key process variables such as temperature, stirring rate, particle size, pulp density, residence time, initial copper and acid concentrations were investigated. The pre-leached matte was then pressure leached to ascertain the effect of process conditions in the pre-leach stage on the subsequent pressure leach stage. It was found that the leaching mechanism entails dissolution of metal alloys out of sulphide minerals with transformation of Ni3S2 to NiS. Aqueous copper precipitates as metallic copper and as chalcocite. The matte is leached by both acid and the cementation process, especially in the early stage when the Cu2+ ions are present. Galvanic interaction of the sulphide minerals and/or the Ni alloy also enhances the leaching process. The leaching kinetics of Ni was characterized with the shrinking core model and was found to be controlled by diffusion through surface layer. An activation energy of 31 kJ/mol was obtained, which also suggested a diffusion controlled leaching reaction. Atmospheric leaching tests indicated that Ni ii extraction increased slightly in the temperature range 50 – 60 oC, however no significant increase was observed from 60 to 80 oC, probably because the leaching process was found to be diffusion controlled. The slight increase in nickel dissolution at higher temperatures (>60 oC) may be attributed to the transformation of Ni3S2 to NiS, which is easier to leach. Co extraction appeared to be insensitive to temperature changes, while Fe extraction was low at 50 oC but increased significantly at 60 – 80 oC. The Ni extraction increased gradually with increase in the stirring rate from 145 to 400 rpm while Co and Fe extractions were insensitive at 145 and 205 rpm, but increased substantially at 400 rpm. This was probably due to increased mass transfer rate and transformation of Ni3S2 to NiS. With pulp density, Ni and Co extractions appeared to be insensitive to changes in the pulp density as only a slight increase in extractions was observed when the density was reduced from 1.7 kg/L to 1.6 kg/L. Similar iron extractions were achieved at 1.7 and 1.75 kg/L but increased significantly at 1.6 kg/L. It was found that Ni and Co extractions were not significantly affected by changes in the particle size, probably because metal alloys were liberated and hence exposed to the leaching solution. Iron extraction could not be determined accurately because of iron precipitation at pH above 3. Generally the leaching of metals did not depend on the initial copper concentration in the investigated range of 25 - 48 g/L Cu. It was also observed that initial acid concentration did not have an effect on Ni extraction, probably due to the fact that most of the nickel was leached by the process of cementation. However, Co and Fe extractions increased when the acid increased from 90 g/L to 110 g/L, but no further increase was noted at 125 g/L. A residence time of 5 hours was found to be adequate as there was no significant increase in metal extractions when the residence time was increased beyond 5 hours. As much as 20% Ni, 40% Co and 80% Fe can be extracted from the Ni-Cu matte during the repulping stage of the leaching process studied, provided the investigated conditions prevail. Generally the rate of Cu cementation increased with increasing temperature and pulp density, but decreased with an increase in particle size, acid and copper iii concentrations. The rate of stirring did not affected Cu cementation. It was found that aqueous copper precipitated from the solution within 90 minutes when the temperature was raised to 80 oC. However, under the present pre-leach temperature of about 60 oC complete Cu cementation can only be achieved after about 5 hours. The cementation reaction was found to follow a mixed control mechanism, with two distinct activation energies namely 18.2 kJ/mol at 70 – 80 oC and 74.6 kJ/mol at 50 – 70 oC. This suggested that the rate of cementation reaction is probably controlled by a boundary layer diffusion mechanism at higher temperatures. At low temperatures the rate is probably controlled by a surface reaction mechanism. The pressure leaching experiments, which were aimed at investigating the response of pre-leached matte to the subsequent pressure leaching process, showed that Ni extractions were similar for the investigated pre-leach temperature of 50 – 80 oC and stirring rate of 145 – 400 rpm. For the pre-leach stage conditions of 60 – 80 oC and 205 – 400 rpm Ni3S2 was transformed into NiS, which is easier to leach in the pressure leaching stage. However, because of the aggressive conditions prevailing in the pressure leaching stage, all the nickel minerals were leached at about the same rate. In the case of pulp density, Ni extraction was comparable for all the investigated pulp densities (1.6 – 1.75 kg/L). This was probably due to the fact that Ni3S2 transformed to NiS in the pre-leach stage. It was found that Ni extraction increased with increasing residence time for the investigated time of 1 hour to 9 hours, probably due to the changes in the mineral phases of the matte as indicated above. The copper minerals (Cu2S and Cu1.96S) transformed into Cu2S and Cu1.8S with aqueous copper being precipitated, and were not leached under the applied conditions. All the cobalt and iron dissolved in the pressure leaching stage. A semi-empirical kinetic model was developed for the pre-leaching stage. A comparison of the model predictions and the experimental data for the dissolved species during the batch leaching process showed that the model can satisfactorily fit the trends in the leaching of the metals. iv OPSOMMING Nikkel-koper-sulfiederts is die belangrikste platinum-groep metaaldraende erts. Die Suid-Afrikaanse afsetting in die platinum-groep metale (PGM’s) is buitengewoon ryk en die produksie van die PGM’s is die hoofdoel vir die behandeling van hierdie erts. Die metodes wat gebruik word om die PGM’s van die nikkel-koper-erts te herwin, bestaan hoofsaaklik uit ertskonsentrasie deur fisiese tegnieke, pirometallurgiese konsentrasie en hidrometallurgiese ekstraksie van die basismetale, gevolg deur die PGM’s. Pirometallurgiese konsentrasie produseer Ni- Cu swaelmetaal, wat deur hidrometallurgiese prosesse behandel word om die nikkel, koper, kobalt en edelmetale te herwin. In hierdie studie is die uitlogingsgedrag van ’n Ni–Cu swaelmetaal in ’n CuSO4– H2SO4-oplossing gedurende die herverpulping- (vooruitlogings-)fase by Impala Platinum Refineries ondersoek. Die herverpulpingsfase is basies ’n nie-oksidatiewe atmosferiese uitlogingsfase, waartydens nikkel, yster en kobalt gedeeltelik opgelos word terwyl die koper gepresipiteer word. Ten einde die aard van die uitlogingsproses gedurende hierdie fase van die basismetaal-affineringsproses te verstaan, is die uitwerking van die variasies in die hoofprosesveranderlikes, soos temperatuur, roertempo, partikelgrootte, pulpdensiteit, verblyftyd en aanvanklike koper- en suurkonsentrasies ondersoek. Drukuitloging is daarna op die vooruitgeloogde swaelmetaal toegepas om die uitwerking van die proses se toestande in die vooruitlogingsfase op die daaropvolgende drukuitlogingsfase te bepaal. Daar is gevind dat die uitlogingsmeganisme oplossing van metaallegerings uit sulfiedminerale met transformasie van Ni3S2 na NiS behels. Waterkoper presipiteer as metaalkoper en as chalkosiet. Die swaelmetaal word deur sowel die suur as die sementasieproses uitgeloog, veral in die vroeë fase wanneer die Cu2+-ione teenwoordig is. Galvaniese interaksie van die sulfiedminerale en/of die Ni-legering versterk ook die uitlogingsproses. Die uitlogingskinetika van Ni is deur die krimpende kernmodel gekenmerk en daar is gevind dat dit deur diffusie deur die v bolaag beheer is. ’n Aktiveringsenergie van 31 kJ/mol is verkry, wat ook ’n diffusiebeheerde uitlogingsreaksie aan die hand doen. Atmosferiese uitlogingstoetse het aangedui dat Ni-ekstraksie effens in ’n temperatuur van 50 oC tot 60 oC toegeneem het. Geen beduidende toename is egter tussen 60 oC en 80 oC waargeneem nie, waarskynlik omdat daar gevind is dat die uitlogingsproses diffusiebeheerd is. Die effense toename in nikkel-dissolusie teen hoër temperature o (>60 C) kan aan die transformasie van Ni3S2 na NiS toegeskryf word, wat makliker is om uit te loog.
Recommended publications
  • Podiform Chromite Deposits—Database and Grade and Tonnage Models
    Podiform Chromite Deposits—Database and Grade and Tonnage Models Scientific Investigations Report 2012–5157 U.S. Department of the Interior U.S. Geological Survey COVER View of the abandoned Chrome Concentrating Company mill, opened in 1917, near the No. 5 chromite mine in Del Puerto Canyon, Stanislaus County, California (USGS photograph by Dan Mosier, 1972). Insets show (upper right) specimen of massive chromite ore from the Pillikin mine, El Dorado County, California, and (lower left) specimen showing disseminated layers of chromite in dunite from the No. 5 mine, Stanislaus County, California (USGS photographs by Dan Mosier, 2012). Podiform Chromite Deposits—Database and Grade and Tonnage Models By Dan L. Mosier, Donald A. Singer, Barry C. Moring, and John P. Galloway Scientific Investigations Report 2012-5157 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: 2012 This report and any updates to it are available online at: http://pubs.usgs.gov/sir/2012/5157/ 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 this and other USGS information products, visit http://store.usgs.gov Suggested citation: Mosier, D.L., Singer, D.A., Moring, B.C., and Galloway, J.P., 2012, Podiform chromite deposits—database and grade and tonnage models: U.S.
    [Show full text]
  • Chromite Crystal Structure and Chemistry Applied As an Exploration Tool
    Western University Scholarship@Western Electronic Thesis and Dissertation Repository February 2015 Chromite Crystal Structure and Chemistry applied as an Exploration Tool Patrick H.M. Shepherd The University of Western Ontario Supervisor Dr. Roberta L. Flemming The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Master of Science © Patrick H.M. Shepherd 2015 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geology Commons Recommended Citation Shepherd, Patrick H.M., "Chromite Crystal Structure and Chemistry applied as an Exploration Tool" (2015). Electronic Thesis and Dissertation Repository. 2685. https://ir.lib.uwo.ca/etd/2685 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Western University Scholarship@Western University of Western Ontario - Electronic Thesis and Dissertation Repository Chromite Crystal Structure and Chemistry Applied as an Exploration Tool Patrick H.M. Shepherd Supervisor Roberta Flemming The University of Western Ontario Follow this and additional works at: http://ir.lib.uwo.ca/etd Part of the Geology Commons This Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in University of Western Ontario - Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Chromite Crystal Structure and Chemistry Applied as an Exploration Tool (Thesis format: Integrated Article) by Patrick H.M.
    [Show full text]
  • NEW MINEI{AL NAMES Mrcuanr, Frbrscnun Fersilicite, Ferdisilicite L
    TFIE AMI'RICAN MINERALOGIST, VOL 54, NOVEMBER DECEMBER, 1969 NEW MINEI{AL NAMES Mrcuanr, FrBrscnun Fersilicite,Ferdisilicite V. Kn. Gnvoar'ven (1969) The occurrence of natural ferrosilicon in the northern Azov region. Dokl. Ahad. Nauh.S.S.SR,185, 4lG+18 (in Russian). V. Ku. Grvonx'veN, A. L. Lrrvrw, .qNo A. S. Povannnny<u (1969) Occurrence of the new minerals fersilicite and ferdisilicate. Geol.Zh. (Lrkraine) 29 No.2,62-71 (in Russian). In placers and in drill-core samples of sandstones of the Poltava series near Zachativsk station, Donets region, fragments 0.1 to 3 mm in size were found of material with strong steely luster, although many of the grains are covered by a dark gray opaque film. Chemical 'I'ananaev analysesby N V. of fractions of size )1 mm and 0.25-0.5 mm gave, resp.; Fe 52.09,50.51; Si 43 25, 41.45;TiOz 0.05,0.55; AI2OB1.30, 2.70; MnO 0.65,2.56; MgO 0.18, O.32;CaO 092,0.42; Na2Onot detd., 0.15; K:O not detd.,0.01;NiO 0.30,not detd., sum 98.74 (given as99.74),98.67 (given as 10O.67a/).Spectrographic analyses by E. S. Nazare- vich showed also Co 0.06, 0 06; V 0.003, 0.003, Cr 0.2, 0 03; Zr 0.O03(?), 0.0a; Cu 0.6, 0.3; 2nO.01,0.02; Sn 0.02,0.027a.The analysescorrespond approximately to I'e2SL. Optical and X-ray data showed that the material consists of two distinct phases, a cubic phase with o 4.48*0.012 A corresponding to synthetic FeSi, and a tetragonal phase with a 2 69+0.012, c 5.08+ 0.02 A, correspondingto synthetic FeSi2 The cubic phase, named {ersilicate, has strongest lines 3.143 (5)(110), 2.566 (5)(111), l.ee1(10)(210), r.8r7 (9)(211), 1.347 (s)(311), 1.196 (10)(321), r.lre (s)(400),1.028 (e) (331), 0.978 (9)(421).
    [Show full text]
  • 1 the Volumetric Determination of Hydroxylamine
    VOLUMETRIC DETERMINATION OF HYDROXYLAMINE. I363 [CONTRIBUTION FROM THE CHEMICAL LABORATORYOF THE UNIVERSITY OF CALIFORNIA.1 THE VOLUMETRIC DETERMINATION OF HYDROXYLAMINE. BY WILLIAMC. BRAY,MIBUM E. SIMPSONAND ANNA A. MACKENZIE. Received July 17, 1919 In the present investigation 3 volumetric methods of determining hydroxylamine in aqueous solution have been studied : The titanous salt method,' in which the hydroxylamine is reduced by excess titanous salt in acid solution with exclusion of air, and the excess titrated with permanganate. 2NH20H + Ti2(S04)3 = (NH4)2S04 + 4TiOS04 + HzS04. (I) The ferric salt method,2 in which the hydroxylamine is oxidized in an acid solution by excess of a ferric salt, the mixture is boiled and the fer- rous salt formed titrated with permanganate. 2NH20H + 2Fe@04)3 = N2O + 4FeS04 + 2H2S04 + H20. (2) The iodine method,3 in which the hydroxylamine is oxidized by iodine in a neutral solution, e. g., in the presence of disodium phosphate. 2NH20H + 212 = N2O + 4HI + H2O (3) or 2NH20H + 213- = N20 + 61- + 4H+ + HzO. Our first experiments, with the iodine method, yielded irregular results which could not be interpreted until the concentration of the hydroxyl- amine solution was accurately determined. An examination of the literature showed a rather unsatisfactory state of affairs. The advocates of the ferric sulfate method furnish evidence that it is perfectly reliable, but Leuba4 gives detailed experimental data to prove the contrary, and Adams5 states that he could not obtain reproducible results with it. The investigators who have used the iodine method consider it to be fairly satisfactory, but some of them state that it is not very accurate, and Rupp and Maeder6 have recently concluded that correct results are obtained only by a compensation of errors.
    [Show full text]
  • Nickel Minerals from Barberton, South Africa: I
    American Mineralogist, Volume 58, pages 733-735, 1973 NickelMinerals from Barberton,South Africa: Vl. Liebenbergite,A NickelOlivine SvsneNoA. nn Wnar Nationnl Institute lor Metallurgy, I Yale Road.,Milner Park, I ohannesburg,South Alrica Lnwrs C. ClI.x Il. S. GeologicalSuruey, 345 Middlefield Road, Menlo Park, California 94025 Abstract Liebenbergite, a nickel olivine from the mineral assemblage trevorite-liebenbergite-nickel serpentine-nickel ludwigite-bunsenite-violarite-millerite-gaspeite-nimite, is described mineral- ogically.Ithasa-1.820,P-1.854,7-1.888,ZVa-88",specificgravity-4'60,Mohs hardness- 6 to 6.5, a - 4.727, b - 10.191,c = 5.955A, and Z - 4. X-ray powder data (48 lines) were indexed according to the space grottp Pbnm. The mean chemical composi- tion, calculated from electron microprobe analyses of eight separate liebenbergite grains, gives the mineral formula: (NL eMgoaCoo,sFeo o)Sio "nOn The name is for W. R. Liebenberg, Deputy Director-General of the National Institute for Metallurgy, South Africa. Introduction mission on New Minerals and Mineral Names (rMA). A re-investigationof the trevorite deposit at Bon Accord in the Barberton Mountain Land, South Experimental Methods Africa, led to the discovery of two peculiar but distinct nickel mineral assemblages.Minerals from The refractive indices were determined by the the assemblagewillemseite-nimite-feroan trevorite- conventional liquid immersion method using a reevesite-millerite-violarite-goethitehave been de- sodium lamp as light source.The optical and crystal scribed in earlier papers in this series (de Waal, morphologicalparameters were studiedwith the aid 1969, l97oa, 1970b;de Waal and Viljoen, I97L). of a universal stage.
    [Show full text]
  • APPENDIX G Acid Dissociation Constants
    harxxxxx_App-G.qxd 3/8/10 1:34 PM Page AP11 APPENDIX G Acid Dissociation Constants §␮ ϭ 0.1 M 0 ؍ (Ionic strength (␮ † ‡ † Name Structure* pKa Ka pKa ϫ Ϫ5 Acetic acid CH3CO2H 4.756 1.75 10 4.56 (ethanoic acid) N ϩ H3 ϫ Ϫ3 Alanine CHCH3 2.344 (CO2H) 4.53 10 2.33 ϫ Ϫ10 9.868 (NH3) 1.36 10 9.71 CO2H ϩ Ϫ5 Aminobenzene NH3 4.601 2.51 ϫ 10 4.64 (aniline) ϪO SNϩ Ϫ4 4-Aminobenzenesulfonic acid 3 H3 3.232 5.86 ϫ 10 3.01 (sulfanilic acid) ϩ NH3 ϫ Ϫ3 2-Aminobenzoic acid 2.08 (CO2H) 8.3 10 2.01 ϫ Ϫ5 (anthranilic acid) 4.96 (NH3) 1.10 10 4.78 CO2H ϩ 2-Aminoethanethiol HSCH2CH2NH3 —— 8.21 (SH) (2-mercaptoethylamine) —— 10.73 (NH3) ϩ ϫ Ϫ10 2-Aminoethanol HOCH2CH2NH3 9.498 3.18 10 9.52 (ethanolamine) O H ϫ Ϫ5 4.70 (NH3) (20°) 2.0 10 4.74 2-Aminophenol Ϫ 9.97 (OH) (20°) 1.05 ϫ 10 10 9.87 ϩ NH3 ϩ ϫ Ϫ10 Ammonia NH4 9.245 5.69 10 9.26 N ϩ H3 N ϩ H2 ϫ Ϫ2 1.823 (CO2H) 1.50 10 2.03 CHCH CH CH NHC ϫ Ϫ9 Arginine 2 2 2 8.991 (NH3) 1.02 10 9.00 NH —— (NH2) —— (12.1) CO2H 2 O Ϫ 2.24 5.8 ϫ 10 3 2.15 Ϫ Arsenic acid HO As OH 6.96 1.10 ϫ 10 7 6.65 Ϫ (hydrogen arsenate) (11.50) 3.2 ϫ 10 12 (11.18) OH ϫ Ϫ10 Arsenious acid As(OH)3 9.29 5.1 10 9.14 (hydrogen arsenite) N ϩ O H3 Asparagine CHCH2CNH2 —— —— 2.16 (CO2H) —— —— 8.73 (NH3) CO2H *Each acid is written in its protonated form.
    [Show full text]
  • New Mineral Names
    NEW MINERAL NAMES Vernadite A. G. Brrnxnrrlr, Genetic types of manganese deposits. Bul,t,.Acait. Scl. I/.R.S.S., Sir. 96ol.,1944, No. 4, 1-46. (Russian with English summary 43-46.) The name vernadite is given, in honor of V. I. Vernadsky, to a mineral formed in the early stages of oxidation of manganese silicates and carbonates. The composition is stated to be MnQ2'H2o, plus a varfng amount of water. The mineral is widespread in occurrence and was previously taken to be manganite. rt is black when massive, compact; reddish to chocolate brown when finely dispersed. Streak is chocolate brown. Drscussron. So vague a description scarcely warrants a new name. Mrcnlnr Fr,nrscnnn Christensenite Tou. F. W. Banrn arn Asr,n Kv.nrneru, Christensenite, a solid solution of nepheline in tridymite. Norsh. Videnskaps-Akad. Oslo, Sci. Results Norwegian AnJarctic Erpeil,i.tions 1927-1928, N o. 22, l-9 (1944). Tridymite from a lava on Deception Island has n (Na) a:1.479, p:1.480, t:1.483, each about 0.01 higher than the corresponding r of pure tridymite. Spectrographic study showed the presence of Na, Al and traces of Fe and ca. Quantitative photometric com- parison with mixtures of quartz and nepheline sho.w'edthat this tridymite contained 5.2/s nepheline. whereas normal tridymite has inversions at 117oand 163', christensenite has a single inversion at 130o to 140o, the temperature varying somervhat for difierent crystals, rt is probable that other tridymites from lavas will be found to belong to this series. The name is for Consul Lars Christensen, who supported the expeditions financially.
    [Show full text]
  • Why Nature Chose Selenium Hans J
    Reviews pubs.acs.org/acschemicalbiology Why Nature Chose Selenium Hans J. Reich*, ‡ and Robert J. Hondal*,† † University of Vermont, Department of Biochemistry, 89 Beaumont Ave, Given Laboratory, Room B413, Burlington, Vermont 05405, United States ‡ University of WisconsinMadison, Department of Chemistry, 1101 University Avenue, Madison, Wisconsin 53706, United States ABSTRACT: The authors were asked by the Editors of ACS Chemical Biology to write an article titled “Why Nature Chose Selenium” for the occasion of the upcoming bicentennial of the discovery of selenium by the Swedish chemist Jöns Jacob Berzelius in 1817 and styled after the famous work of Frank Westheimer on the biological chemistry of phosphate [Westheimer, F. H. (1987) Why Nature Chose Phosphates, Science 235, 1173−1178]. This work gives a history of the important discoveries of the biological processes that selenium participates in, and a point-by-point comparison of the chemistry of selenium with the atom it replaces in biology, sulfur. This analysis shows that redox chemistry is the largest chemical difference between the two chalcogens. This difference is very large for both one-electron and two-electron redox reactions. Much of this difference is due to the inability of selenium to form π bonds of all types. The outer valence electrons of selenium are also more loosely held than those of sulfur. As a result, selenium is a better nucleophile and will react with reactive oxygen species faster than sulfur, but the resulting lack of π-bond character in the Se−O bond means that the Se-oxide can be much more readily reduced in comparison to S-oxides.
    [Show full text]
  • Alphabetical List
    LIST L - MINERALS - ALPHABETICAL LIST Specific mineral Group name Specific mineral Group name acanthite sulfides asbolite oxides accessory minerals astrophyllite chain silicates actinolite clinoamphibole atacamite chlorides adamite arsenates augite clinopyroxene adularia alkali feldspar austinite arsenates aegirine clinopyroxene autunite phosphates aegirine-augite clinopyroxene awaruite alloys aenigmatite aenigmatite group axinite group sorosilicates aeschynite niobates azurite carbonates agate silica minerals babingtonite rhodonite group aikinite sulfides baddeleyite oxides akaganeite oxides barbosalite phosphates akermanite melilite group barite sulfates alabandite sulfides barium feldspar feldspar group alabaster barium silicates silicates albite plagioclase barylite sorosilicates alexandrite oxides bassanite sulfates allanite epidote group bastnaesite carbonates and fluorides alloclasite sulfides bavenite chain silicates allophane clay minerals bayerite oxides almandine garnet group beidellite clay minerals alpha quartz silica minerals beraunite phosphates alstonite carbonates berndtite sulfides altaite tellurides berryite sulfosalts alum sulfates berthierine serpentine group aluminum hydroxides oxides bertrandite sorosilicates aluminum oxides oxides beryl ring silicates alumohydrocalcite carbonates betafite niobates and tantalates alunite sulfates betekhtinite sulfides amazonite alkali feldspar beudantite arsenates and sulfates amber organic minerals bideauxite chlorides and fluorides amblygonite phosphates biotite mica group amethyst
    [Show full text]
  • A Specific Gravity Index for Minerats
    A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951).
    [Show full text]
  • Risk-Based Closure Guide Draft
    Risk-based Closure Guide July 1, 2021 Office of Land Quality Indiana Department of Environmental Management Disclaimer This Nonrule Policy Document (NPD) is being established by the Indiana Department of Environmental Management (IDEM) consistent with its authority under IC 13-14-1-11.5. It is intended solely as guidance and shall be used in conjunction with applicable rules or laws. It does not replace applicable rules or laws, and if it conflicts with these rules or laws, the rules or laws shall control. Pursuant to IC 13-14-1-11.5, this NPD will be available for public inspection for at least forty-five (45) days prior to presentation to the appropriate State Environmental Board, and may be put into effect by IDEM thirty (30) days afterward. If the NPD is presented to more than one board, it will be effective thirty (30) days after presentation to the last State Environmental Board. IDEM also will submit the NPD to the Indiana Register for publication. 2 Table of Contents 1 Introduction ..................................................................................................................................... 7 1.1 Applicability .............................................................................................................................. 8 1.2 Types of Closure ...................................................................................................................... 9 1.3 Process Overview ...................................................................................................................
    [Show full text]
  • Sulfur Dioxide and “Sulfurous Acid” Solutions. S + O 2 → SO2 (G
    Sulfur Dioxide and “Sulfurous Acid” Solutions. S + O2 → SO2 (g) Structure: sp2 at sulfur, two used for σ bonds, one for lone pair. : δ+ S - δ- δ O O Liquid SO2: Easy to get (bp = -10 °C) and easy to keep liquid at room T under slight pressure. It is quite a good solvent; SO2 is a polar molecule, and the liquid is associated by dipole-dipole attraction. Dissolves polar molecules and ionic compounds, and easy to remove by evaporation. Aqueous solutions: SO2 is soluble in water. Most of it stays in the form of hydrogen bonded “hydrate” (see CO2). At equilibrium in neutral water (no added base) a small portion of it reacts: - H+ - H+ - 2- SO2 (aq) + H2O HO-SO2 SO3 (sulfite - pyramidal) + H+ + H+ - H-SO3 (bisulfite) - 2- 2- Also, 2 HSO3 S2O5 + H2O (structure = [O2S-SO3] ) Many salts of all these anions are known. Complexes formed with sulfite ion and SO2 itself. Sulfur Trioxide and Sulfuric Acid. 2 SO2 + O2 → 2 SO3 (g) Condenses to a liquid at room T, liquid contains monomer and trimer. O O S O O O O O S S S O O O O O Also get solid polymers. SO3 is a powerful oxidant, with water, gives sulfuric acid – H2SO4. A viscous, hydrogen bonded liquid; which is a good strongly acidic solvent. In dilute solutions in water it is a dibasic acid. - H+ - H+ - 2- H2SO4 (aq) HSO4 (bisulfate) SO4 (sulfate) + H+ + H+ Many salts known for both anions. Sulfate can be monodentate or bidentate ligand. SO3 dissolves in concentrated H2SO4 to give “fuming” sulfuric acid which contains some pyrosulfuric acid – VERY CORROSIVE H2SO4 + SO3 H2S2O7 Halides of Sulfur Sulfur hexafluoride (SF6) is a gas a stp.
    [Show full text]