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LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, and COBALT ARSENIDE and SULFIDE ORE FORMATION Nicholas Allin
Montana Tech Library Digital Commons @ Montana Tech Graduate Theses & Non-Theses Student Scholarship Spring 2019 EXPERIMENTAL INVESTIGATION OF THE THERMOCHEMICAL REDUCTION OF ARSENITE AND SULFATE: LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, AND COBALT ARSENIDE AND SULFIDE ORE FORMATION Nicholas Allin Follow this and additional works at: https://digitalcommons.mtech.edu/grad_rsch Part of the Geotechnical Engineering Commons EXPERIMENTAL INVESTIGATION OF THE THERMOCHEMICAL REDUCTION OF ARSENITE AND SULFATE: LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, AND COBALT ARSENIDE AND SULFIDE ORE FORMATION by Nicholas C. Allin A thesis submitted in partial fulfillment of the requirements for the degree of Masters in Geoscience: Geology Option Montana Technological University 2019 ii Abstract Experiments were conducted to determine the relative rates of reduction of aqueous sulfate and aqueous arsenite (As(OH)3,aq) using foils of copper, nickel, or cobalt as the reductant, at temperatures of 150ºC to 300ºC. At the highest temperature of 300°C, very limited sulfate reduction was observed with cobalt foil, but sulfate was reduced to sulfide by copper foil (precipitation of Cu2S (chalcocite)) and partly reduced by nickel foil (precipitation of NiS2 (vaesite) + NiSO4·xH2O). In the 300ºC arsenite reduction experiments, Cu3As (domeykite), Ni5As2, or CoAs (langisite) formed. In experiments where both sulfate and arsenite were present, some produced minerals were sulfarsenides, which contained both sulfide and arsenide, i.e. cobaltite (CoAsS). These experiments also produced large (~10 µm along longest axis) euhedral crystals of metal-sulfide that were either imbedded or grown upon a matrix of fine-grained metal-arsenides, or, in the case of cobalt, metal-sulfarsenide. Some experimental results did not show clear mineral formation, but instead demonstrated metal-arsenic alloying at the foil edges. -
Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Rediscovery of the Elements — a Historical Sketch of the Discoveries
REDISCOVERY OF THE ELEMENTS — A HISTORICAL SKETCH OF THE DISCOVERIES TABLE OF CONTENTS incantations. The ancient Greeks were the first to Introduction ........................1 address the question of what these principles 1. The Ancients .....................3 might be. Water was the obvious basic 2. The Alchemists ...................9 essence, and Aristotle expanded the Greek 3. The Miners ......................14 philosophy to encompass a obscure mixture of 4. Lavoisier and Phlogiston ...........23 four elements — fire, earth, water, and air — 5. Halogens from Salts ...............30 as being responsible for the makeup of all 6. Humphry Davy and the Voltaic Pile ..35 materials of the earth. As late as 1777, scien- 7. Using Davy's Metals ..............41 tific texts embraced these four elements, even 8. Platinum and the Noble Metals ......46 though a over-whelming body of evidence 9. The Periodic Table ................52 pointed out many contradictions. It was taking 10. The Bunsen Burner Shows its Colors 57 thousands of years for mankind to evolve his 11. The Rare Earths .................61 thinking from Principles — which were 12. The Inert Gases .................68 ethereal notions describing the perceptions of 13. The Radioactive Elements .........73 this material world — to Elements — real, 14. Moseley and Atomic Numbers .....81 concrete basic stuff of this universe. 15. The Artificial Elements ...........85 The alchemists, who devoted untold Epilogue ..........................94 grueling hours to transmute metals into gold, Figs. 1-3. Mendeleev's Periodic Tables 95-97 believed that in addition to the four Aristo- Fig. 4. Brauner's 1902 Periodic Table ...98 telian elements, two principles gave rise to all Fig. 5. Periodic Table, 1925 ...........99 natural substances: mercury and sulfur. -
Norrbro Och Strömparterren
Norrbro och Strömparterren - - Stockholms Stadsmuseum augusti 2006 Samlingsavdelningen/Faktarumsenheten Framsidans målning: Klas Lundkvist Anna Palm: Utsikt över Strömmen mot Slottet från Södra Blasieholmshamnen, 1890-talet e-post: beskuren (originalets storlek 122 x 58 cm), [email protected] akvarell, INV NR SSM 0002325 (K 105) telefon: 508 31 712 - - Innehåll Uppdraget Stockholms Trafikkontor planerar för en omfattande Uppdraget ........................................................................................................ renovering av Norrbro. Åtgärderna innebär grundför- Sammanfattning .............................................................................................. 4 stärkning, tätning och fasadrenovering av delen över Platsens betydelse i staden och landet ............................................................ 4 Helgeandsholmen samt förnyelse av kör- och gångytor Norrbro idag .................................................................................................... 5 över hela Norrbro. I planeringen ingår även en översyn Gällande planer och lagstiftning ..................................................................... 7 av Strömparterrens parkyta. Stockholms stadsmuseum Kunskapsläget ................................................................................................. 7 har av Trafikkontoret genom Åsa Larsson, projektle- Kartor över Norrströms, Helgeandsholmens och broarnas utveckling ........... 8 dare Norrbro, och Bodil Hammarberg, projektledare Helgeandsholmen -
Hjalmar Fors, the Limits of Matter—Chemistry, Mining & Enlightenment
Miner Econ (2015) 28:131–132 DOI 10.1007/s13563-015-0071-2 BOOK REVIEW Hjalmar Fors, The Limits of Matter—Chemistry, mining & enlightenment The University of Chicago Press Chicago USA 2015 Magnus Ericsson1 Published online: 15 September 2015 # Springer-Verlag Berlin Heidelberg 2015 Swedish chemists have discovered more elements than scien- though at that time not united into one yet), France and tists from any other nation. Over more than 100 years, from England? Part of the answer is surprisingly bureaucratisation the early 18th century to the end of the 19th century, 20 ele- or the creation of an administrative institution called ments of which 18 metals or non-metals and 2 gases, nitrogen Bergskollegium in Swedish or English Bureau of Mines as and chlorine were independently isolated and described. Some Hjalmar Fors calls it in his new and path-breaking study of these are as follows: The Limits of Matter—Chemistry, mining & enlightenment. Another part is the need of improved processes and better Element Name Year of discovery yields in Swedish mines, which played such a vital role in Cobalt Brandt 1735 the Swedish economy during this period. The Swedish ruling Nickel Cronstedt 1751 groups saw these demands and founded the Bureau of Mines, Manganese Gahn 1774 which acted in several ways to solve problems, that had arisen in the mining industry. R&D in those days was highly Molybdenum Hjelm 1781 applied but nevertheless led to important purely scientific Yttrium Gadolin 1794 results. Tantalum Ekeberg 1802 The Bureau was set up in 1634 based on a predecessor, Cerium Berzelius 1803 which was started already in 1630. -
Polymetallic Mineralization in Ediacaran Sediments in the Żarki-Kotowice Area, Poland
MINERALOGIA, 43, No 3-4: 199-212 (2012) DOI: 10.2478/v10002-012-0008-0 www.Mineralogia.pl MINERALOGICAL SOCIETY OF POLAND POLSKIE TOWARZYSTWO MINERALOGICZNE __________________________________________________________________________________________________________________________ Original paper Polymetallic mineralization in Ediacaran sediments in the Żarki-Kotowice area, Poland Łukasz KARWOWSKI1*, Marek MARKOWIAK2 1University of Silesia, Faculty of Earth Sciences, ul. Będzińska 60, 41-200 Sosnowiec, Poland; e-mail: [email protected] 2Polish Geological Institute - Research and Development Unit, Upper Silesian Branch, ul. Królowej Jadwigi 1, 41-200 Sosnowiec, Poland; e-mail: [email protected] * Corresponding author Received: September 5, 2012 Received in revised form: February 20, 2013 Accepted: March 17, 2013 Available online: March 30, 2013 Abstract. In one small mineral vein in core from borehole 144-Ż in the Żarki-Kotowice area, almost all of the ore minerals known from related deposits in the vicinity occur. Some of the minerals in the vein described in this paper, namely, nickeline, hessite, native silver and minerals of the cobaltite-gersdorffite group, have not previously been reported from elsewhere in the Kraków-Lubliniec tectonic zone. The identified minerals are chalcopyrite, pyrite, marcasite, sphalerite, Co-rich pyrite, tennantite, tetrahedrite, bornite, galena, magnetite, hematite, cassiterite, pyrrhotite, wolframite (ferberite), scheelite, molybdenite, nickeline, minerals of the cobaltite- gersdorffite group, carrollite, hessite and native silver. Moreover, native bismuth, bismuthinite, a Cu- and Ag-rich sulfosalt of Bi (cuprobismutite) and Ni-rich pyrite also occur in the vein. We suggest that, the ore mineralization from the borehole probably reflects post-magmatic hydrothermal activity related to an unseen granitic intrusion located under the Mesozoic sediments in the Żarki-Pilica area. -
Discussion Paper on Mineral Groups by E. H. Nickel
Discussion Paper on Mineral Groups by E. H. Nickel INTRODUCTION There are two aspects to the compilation of mineral groups. One is the criteria to be used in defining a group. In a recent meeting of the CCM in Melbourne, it was generally agreed that the main criteria defining a group are that it should comprise at least two species, and that the species comprising the group should be isostructural, as indicated by similarity of space group and unit-cell parameters. An important additional consideration is the need to develop an arrangement of the groups in a way that makes it relatively easy to find the group to which a particular mineral species should be consigned. There are many ways in which mineral groups can be classified, and I have looked at four different possibilities with the aim of initiating discussion on this topic. To illustrate the four different classification systems, I have applied them to the sulfide and sulfosalt minerals. The four systems, demonstrated below, are as follows: I) Alphabetical; II) Hey’s chemical classification; III) A combination of Hey’s chemical classification and Smith’s structural formulae; and IV) Strunz’s chemical-structural classification. Comments and suggestions are welcomed. I) SULFIDE AND SULFOSALT GROUPS ALPHABETICAL LISTING Argyrodite Group: Orthorhombic, Pna21 (33). Argyrodite structure type Arsenopyrite Group: Monoclinic, P21/c (14). Related to marcasite structure. Berthierite Group: Orthorhombic, Pnam (62). Berthierite structure type. Bournonite Group: Orthorhombic, Pn21m (31). Bournonite structure type Bowieite Group: Orthorhombic, Pbcn (60). Bowieite structure type. Braggite Group: Tetragonal, P42/m (84). Braggite structure type. Brezinaite Group: Monoclinic, I2/m (12). -
Nickeline Nias C 2001-2005 Mineral Data Publishing, Version 1
Nickeline NiAs c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 6/m 2/m 2/m. Commonly in granular aggregates, reniform masses with radial structure, and reticulated and arborescent growths. Rarely as distorted, horizontally striated, {1011} terminated crystals, to 1.5 cm. Twinning: On {1011} producing fourlings; possibly on {3141}. Physical Properties: Fracture: Conchoidal. Tenacity: Brittle. Hardness = 5–5.5 VHN = n.d. D(meas.) = 7.784 D(calc.) = 7.834 Optical Properties: Opaque. Color: Pale copper-red, tarnishes gray to blackish; white with strong yellowish pink hue in reflected light. Streak: Pale brownish black. Luster: Metallic. Pleochroism: Strong; whitish, yellow-pink to pale brownish pink. Anisotropism: Very strong, pale greenish yellow to slate-gray in air. R1–R2: (400) 39.2–45.4, (420) 38.0–44.2, (440) 36.8–43.5, (460) 36.2–43.2, (480) 37.2–44.3, (500) 39.6–46.4, (520) 42.3–48.6, (540) 45.3–50.7, (560) 48.2–52.8, (580) 51.0–54.8, (600) 53.7–56.7, (620) 55.9–58.4, (640) 57.8–59.9, (660) 59.4–61.3, (680) 61.0–62.5, (700) 62.2–63.6 Cell Data: Space Group: P 63/mmc. a = 3.621(1) c = 5.042(1) Z = 2 X-ray Powder Pattern: Unknown locality. 2.66 (100), 1.961 (90), 1.811 (80), 1.071 (40), 1.328 (30), 1.033 (30), 0.821 (30) Chemistry: (1) (2) Ni 43.2 43.93 Co 0.4 Fe 0.2 As 55.9 56.07 Sb 0.1 S 0.1 Total 99.9 100.00 (1) J´achymov, Czech Republic; by electron microprobe, corresponds to (Ni0.98Co0.01 Fe0.01)Σ=1.00As1.00. -
Museums in Stockholm
Museums in Stockholm PHOTO: OLA ERICSON FOR THE LATEST UPDATES ON STOCKHOLM, VISIT THE OFFICIAL WEBSITE VISITSTOCKHOLM.COM Museums in Stockholm BERGIANSKA TRÄDGÅRDEN BERGIUS BOTANIC GARDEN Discover Stockholm´s museums with their world-class collections, pioneering exhibitions and extraordinary historical objects. Botanical garden beautifully situated at Lake Brunnsviken. A paradise for plant enthusiasts with thousands of trees, shrubs and herbs from around the world. Exotic, heat-loving plants thrive in the Victoria House and Edvard Anderson Conservatory. AQUARIA VATTENMUSEUM Café, shop and restaurant. AQUARIA WATER MUSEUM Opening hours: The Park daily. Edvard Anderson Conservatory: Oct-Mar Mon- Fri 11am- 4pm, Sat- Sun Falkenbergsgatan 2. Djurgården 11am-5pm Apr-Sep daily 11am- 5pm. www.aquaria.se The Victoria House: May-Sep Mon- Fri 11am- 4pm, Sat-Sun 11am-5pm. ARKITEKTURMUSEUM Metro station: Universitetet, Bus:40 MUSEUM OF ARCHITECTURE Bergianska trädgården All you need to know about Swedish architecture and construction from +46 (0) 8 545 91 700 the 19th century until today. Exhibitions featuring drawings, models, design www.bergianska.se and examples of sustainable urban development. Take a tour and participate in creative activities for children on Sundays. Library, BIOLOGISKA MUSEET collections, book store and café. BIOLOGICAL MUSEUM Opening hours: Tues 10am- 8pm, Wed-Sun Lejonslätten, Djurgården 10am-6pm. www.biologiskamuseet.com Metro station: Kungsträdgården Bus: 2, 55, 62, 65, 76 Skeppsholmen BONNIERS KONSTHALL +46 (0) 8 587 270 00 BONNIERS CONTEMPORARY ART www.arkitekturmuseet.se Torsgatan 19. Norrmalm ARMÉMUSEUM www.bonnierskonsthall.se ARMY MUSEUM CARL ELDHS ATELJÉMUSEUM Riddargatan 13. Östermalm CARL ELDH’S STUDIO MUSEUM www.armemuseum.se Lögebodavägen 10. -
RBRC-32 BNL-6835.4 PARITY ODD BUBBLES in HOT QCD D. KHARZEEV in This ~A~Er We Give a Pedawwicalintroduction~0 Recent Work Of
RBRC-32 BNL-6835.4 PARITY ODD BUBBLES IN HOT QCD D. KHARZEEV RIKEN BNL Research Center, Br$ookhauenNational Laboratory, . Upton, New York 11973-5000, USA R.D. PISARSKI Department of Physics, Brookhaven National Laboratoy, Upton, New York 11973-5000, USA M.H.G. TYTGAT Seruice de Physique Th&orique, (7P 225, Uniuersitc4Libre de Bruzelles, B[ud. du !t%iomphe, 1050 Bruxelles, Belgium We consider the topological susceptibility for an SU(N) gauge theory in the limit of a large number of colors, N + m. At nonzero temperature, the behavior of the topological susceptibility depends upon the order of the reconfining phrrse transition. The meet interesting possibility is if the reconfining transition, at T = Td, is of second order. Then we argue that Witten’s relation implies that the topological suscepti~lfity vanishes in a calculable fdion at Td. Ae noted by Witten, this implies that for sufficiently light quark messes, metaetable etates which act like regions of nonzero O — parity odd bubbles — can arise at temperatures just below Td. Experimentally, parity odd bubbles have dramatic signature% the rI’ meson, and especially the q meson, become light, and are copiously produced. Further, in parity odd bubbles, processes which are normally forbidden, such as q + rr”ro, are allowed. The most direct way to detect parity violation is by measuring a parity odd global seymmetry for charged pions, which we define. 1 Introduction In this .-~a~er we give a Pedawwicalintroduction~0 recent work of ours? We I consider an SU(IV) gau”ge t~e~ry in the limit of a large number of colors, N + co, This is, of course, a familiar limit? We use the large N expansion I to investigate the behavior of the theory at nonzero temperature, especially for the topological susceptibility. -
Hexagon Fall
Redis co very of the Elements The Rare Earth s–The Beginnings I I I James L. Marshall, Beta Eta 1971 , and Virginia R. Marshall, Beta Eta 2003 , Department of Chemistry, University of North Texas, Denton, TX 76203-5070, [email protected] 1 Rare earths —introduction. The rare earths Figure 1. The “rare earths” are defined by IUPAC as the 15 lanthanides (green) and the upper two elements include the 17 chemically similar elements of the Group III family (yellow). These elements have similar chemical properties and all can exhibit the +3 occupying the f-block of the Periodic Table as oxidation state by the loss of the highest three electrons (two s electrons and either a d or an f electron, well as the Group III chemical family (Figure 1). depending upon the particular element). A few rare earths can exhibit other oxidation states as well; for These elements include the 15 lanthanides example, cerium can lose four electrons —4f15d 16s 2—to attain the Ce +4 oxidation state. (atomic numbers 57 through 71, lanthanum through lutetium), as well as scandium (atomic number 21) and yttrium (atomic number 39). The chemical similarity of the rare earths arises from a common ionic configuration of their valence electrons, as the filling f-orbitals are buried in an inner core and generally do not engage in bonding. The term “rare earths” is a misnome r—these elements are not rare (except for radioactive promethium). They were named as such because they were found in unusual minerals, and because they were difficult to separate from one another by ordinary chemical manipula - tions. -
För Sverige I Tiden? En Studie Om Den Svenska Monarkins Relation Till Samhället Och Sekulariseringsprocessen Mellan 1858-2012
Kandidatuppsats För Sverige i tiden? En studie om den svenska monarkins relation till samhället och sekulariseringsprocessen mellan 1858-2012 Författare: Joel Håkansson Examinator: Åsa Trulsson Handledare: Stefan Arvidsson Termin: HT12 Ämne: Religionsvetenskap Nivå: Grundnivå Kurskod: GI1203 Abstract For Sweden – with the times? A study of the Swedish monarchy's relation to society and the secularization process 1858-2012. Christendom has under a long period of time in Swedish history been the central component in legitimating the monarchs' power, a continuous process than can be clearly observed through the customs of royal coronation and baptism rites. However, during the 20th century those close ties between the state and the church of Sweden have been dissolving at a steady rate, alongside a growing societal democratization and modernization process. Officially the monarch still had a clear constitutional power legitimated through the transcendent, but unofficially his power was in reality heavily reduced. How do the Swedish monarchy relate to a rapidly changing society and secularization process? This pilot study investigates this relation by analyzing the news reports of the royal coronation and baptism rites between 1858 and 2012 from two leading newspapers, Aftonbladet and Dagens Nyheter. Principally two sides of the monarchy could be identified, one slow changing external side with a close connection with the national identity through history, religion and tradition, and a more swift and growing internal side with a clear connection with the ordinary citizen, family values and social norms. In conclusion the Swedish monarchy seemed to have progressed from a clear sacral foundation to a more family oriented development.