This Article Appeared in a Journal Published by Elsevier. the Attached

Total Page:16

File Type:pdf, Size:1020Kb

This Article Appeared in a Journal Published by Elsevier. the Attached This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Environment International 35 (2009) 1243–1255 Contents lists available at ScienceDirect Environment International journal homepage: www.elsevier.com/locate/envint Review article Secondary arsenic minerals in the environment: A review Petr Drahota a,b,⁎, Michal Filippi a a Institute of Geology, Academy of Sciences of the Czech Republic, v.v.i., Rozvojová 269, 165 00 Prague 6 — Lysolaje, Czech Republic b Institute of Geochemistry, Mineralogy and Mineral Resources, Faculty of Science, Charles University, Albertov 6, 128 43 Prague 2, Czech Republic article info abstract Article history: Information on arsenic (As) speciation in solid materials is critical for many environmental studies concerned Received 10 March 2009 with As stability and/or mobility in natural As-impacted soils and mining or industrial sites contaminated by Accepted 10 July 2009 As. The investigation of these systems has provided evidence for a number of secondary As minerals that Available online 7 August 2009 have often played a significant role in As mobility in the solid phase–water system. This paper presents a list of environmentally important secondary As minerals in contaminated soil and waste systems, summarizes Keywords: the information about their origin, occurrence, environmental stability and thermodynamics, and proposes Arsenic Secondary arsenic mineral several important avenues for further investigation. Environmental sample © 2009 Elsevier Ltd. All rights reserved. Solubility Environmental stability Contents 1. Introduction .............................................................. 1243 2. Environmentally important secondary as minerals ............................................ 1244 2.1. As oxides ............................................................ 1244 2.2. Fe arsenates .......................................................... 1244 2.2.1. Well-crystallized Fe arsenates .............................................. 1244 2.2.2. Poorly crystalline and amorphous Fe(III) arsenates .................................... 1248 2.2.3. Pharmacosiderite group ................................................. 1250 2.2.4. Ca–Fe(III) arsenates ................................................... 1250 2.3. Fe sulphoarsenates and sulphoarsenites ............................................. 1251 2.4. Ca, Mg and Ca–Mg arsenates ................................................... 1251 2.5. Other metal arsenates ...................................................... 1252 3. Summary and tasks for future research ................................................. 1253 Acknowledgements ............................................................. 1253 References ................................................................. 1253 1. Introduction sulphide minerals realgar and orpiment are also found. These primary As-bearing minerals are listed in Table 1. While As does not readily More than 300 arsenic (As) minerals are known to occur in nature. substitute into the structures of the major rock-forming minerals, it Of these approx. 60% are arsenates, approx. 20% are sulphides and can easily occur as a minor component in the abundant Fe sulphide sulphosalts, 10% are oxides and the rest are arsenites, arsenides, native mineral pyrite (e.g., Fleet et al., 1989, 1993; Savage et al., 2000; elements and metal alloys (Bowell and Parshley, 2001). The most Zachariáš et al., 2004; Blanchard et al., 2007). When these primary important primary As-bearing minerals are those where the As occurs minerals are exposed to the atmosphere and surface or ground waters, as the anion (arsenide) or dianion (diarsenide), or as the sulfarsenide alteration reactions cause formation of secondary As minerals, such as anion(s); these anions are bonded to metals such as Fe (löllingite, simple As oxides or more complex phases with As, oxygen and various arsenopyrite), Co (cobaltite) and Ni (gersdorffite). The simple As metals. The latter group of minerals comprises arsenite and arsenate minerals that are formed by linking As(III)-oxo-anion groups or As (V)-oxo-anion groups, respectively, to a variety of mono-, di- and ⁎ Corresponding author. Institute of Geochemistry, Mineralogy and Mineral Resources, Faculty of Science, Charles University, Albertov 6, 128 43 Prague 2, Czech Republic. trivalent metal cations. Secondary arsenite minerals are rare in natural E-mail address: [email protected] (P. Drahota). environments, usually occurring as the products of hydrothermal 0160-4120/$ – see front matter © 2009 Elsevier Ltd. All rights reserved. doi:10.1016/j.envint.2009.07.004 Author's personal copy 1244 P. Drahota, M. Filippi / Environment International 35 (2009) 1243–1255 Table 1 arsenolite, is a relatively common secondary mineral formed from Ideal formulas of the most common primary As-bearing minerals referred to in the text. oxidation of native As, arsenopyrite, löllingite, and from weathering of Mineral Formula System scorodite. Arsenolite has occurred as efflorescencents on the walls of Arsenopyrite FeAsS Monoclinic former underground mine workings, such as in the Jáchymov ore district, Cobaltite CoAsS Orthorombic Czech Republic (e.g., Ondruš et al.,1997). This mineral has been also found Enargite Cu3AsS4 Orthorombic in association with scorodite and native sulphur in arsenopyrite/ fi Gersdorf te NiAsS Cubic löllingite-rich processing waste (Filippi, 2004)(Figs. 2 and 3a, b, c), Löllingite FeAs Orthorombic 2 weathered saprolite (Bowell,1994), and in an old tailings pile (e.g., Ashley Orpiment As2S3 Monoclinic Pyrite FeS2 Cubic and Lottermoser, 1999; Juillot et al., 1999; Borba et al., 2003; Haffert and Realgar AsS Monoclinic Craw, 2008). Tennantite (Cu, Ag, Fe, Zn)12As4S13 Cubic The monoclinic dimorph of As trioxide, claudetite, is often intimately associated with arsenolite. It has occurred as the oxidation product of native As in dump wastes (Matsubara et al., 2001), as the alterations under mildly reducing conditions. Conversely, secondary speleothem related to the alteration of enargite, tennantite, or arsenate compounds comprise a large class of minerals that have been arsenopyrite in the breccia-pipe mineralization at Corkscrew Cave, found in many oxidized environments. Similar to phosphate minerals, Arizona (Onac et al., 2007), and as the efflorescents at the furnace and the arsenate tetrahedra is bonded to octahedrally coordinated condensed flue sites (Ashley and Lottermoser, 1999). It is assumed transition metal ions (e.g., Fe, Mn, Ni) or to large, divalent cations that claudetite could represent an important secondary reservoir of As (e.g., Ca, Ba, Pb). Because of variations and multiples of the bonding in the metasedimentary rocks of the Maine watershed, USA, patterns, the relatively open structures of some arsenate minerals originating from the orpiment and arsenopyrite oxidation (Foley cause extensive substitution of cations, anions and water, and solid and Ayuso, 2008). In situ formation of claudetite in the absence of Fe solutions (e.g., Mutter et al., 1984; Behrens et al., 1998). All the oxyhydroxides and aqueous Fe complexes from oxidation of orpiment secondary As minerals mentioned in the text are listed in Table 2. is assumed in the reaction (Eq. (1)) (Foley and Ayuso, 2008): Recently, the investigation of both the natural and anthropogenic ð Þþ ð Þþ ð Þ→ ð Þþ þð Þþ 2−ð ÞðÞ As geochemical anomalies, using modern analytical tools (micro- As2S3 s 3H2O l 6O2 g As2O3 s 6H aq 3SO4 aq 1 Raman, XAS techniques), has provided a better picture of As bonding to a The stabilities of arsenolite and claudetite are quite similar, since particular substrate. Wang and Mulligan (2008) compiled the research they have nearly similar free energies of formation: arsenolite on the surface structure and surface complexing of As species in the −576.34 kJ/mol and claudetite −576.53 kJ/mol (Nordstrom and inorganic solid phase that play an important role in governing As Archer, 2003). Nevertheless, claudetite is slightly more stable than mobility in most natural systems. As another result of this approach, a arsenolite under ambient conditions (the difference −0.19 kJ/mol). large number of secondary As minerals have been found in highly Arsenolite and claudetite dissolve at pHb8 and temperature to 90 °C contaminated soils, stream sediments, former industrial sites and mine according to the Eq. (2) (Pokrovski et al., 1996); these are stable in tailings (e.g., Utsunomiya et al., 2003; Paktunc et al., 2004; Cancès et al., equilibrium with waters of high pH (Nordstrom and Archer, 2003). 2008; Filippi et al., 2009). The ability of secondary As minerals to immobilize As and control its dissolved concentrations depends on the ð Þþ ð Þ→ 0ð ÞðÞ As2O3 s 3H2O l 2H3AsO3 aq 2 solubility of these phases, which is highly variable. Precipitation of secondary As minerals has always been
Recommended publications
  • Mg2sio4) in a H2O-H2 Gas DANIEL TABERSKY1, NORMAN LUECHINGER2, SAMUEL S
    Goldschmidt2013 Conference Abstracts 2297 Compacted Nanoparticles for Evaporation behavior of forsterite Quantification in LA-ICPMS (Mg2SiO4) in a H2O-H2 gas DANIEL TABERSKY1, NORMAN LUECHINGER2, SAMUEL S. TACHIBANA1* AND A. TAKIGAWA2 2 2 1 , HALIM , MICHAEL ROSSIER AND DETLEF GÜNTHER * 1 Department of Natural History Sciences, Hokkaido 1ETH Zurich, Department of Chemistry and Applied University, N10 W8, Sapporo 060-0810, Japan. Biosciences, Laboratory of Inorganic Chemistry (*correspondence: [email protected]) (*correspondence: [email protected]) 2Carnegie Institution of Washington, Department of Terrestrial 2Nanograde, Staefa, Switzerland Magnetism, 5241 Broad Branch Road NW, Washington DC, 20015 USA. Gray et al. did first studies of LA-ICPMS in 1985 [1]. Ever since, extensive research has been performed to Forsterite (Mg2SiO4) is one of the most abundant overcome the problem of so-called “non-stoichiometric crystalline silicates in extraterrestrial materials and in sampling” and/or analysis, the origins of which are commonly circumstellar environments, and its evaporation behavior has referred to as elemental fractionation (EF). EF mainly consists been intensively studied in vacuum and in the presence of of laser-, transport- and ICP-induced effects, and often results low-pressure hydrogen gas [e.g., 1-4]. It has been known that in inaccurate analyses as pointed out in, e.g. references [2,3]. the evaporation rate of forsterite is controlled by a A major problem that has to be addressed is the lack of thermodynamic driving force (i.e., equilibrium vapor reference materials. Though the glass series of NIST SRM 61x pressure), and the evaporation rate increases linearly with 1/2 have been the most commonly reference material used in LA- pH2 in the presence of hydrogen gas due to the increase of ICPMS, heterogeneities have been reported for some sample the equilibrium vapor pressure.
    [Show full text]
  • L. Jahnsite, Segelerite, and Robertsite, Three New Transition Metal Phosphate Species Ll. Redefinition of Overite, an Lsotype Of
    American Mineralogist, Volume 59, pages 48-59, 1974 l. Jahnsite,Segelerite, and Robertsite,Three New TransitionMetal PhosphateSpecies ll. Redefinitionof Overite,an lsotypeof Segelerite Pnur BnnN Moone Thc Departmcntof the GeophysicalSciences, The Uniuersityof Chicago, Chicago,Illinois 60637 ilt. lsotypyof Robertsite,Mitridatite, and Arseniosiderite Peur BmaN Moonp With Two Chemical Analvsesbv JUN Iro Deryrtrnent of GeologicalSciences, Haraard Uniuersity, Cambridge, Massrchusetts 02 I 38 Abstract Three new species,-jahnsite, segelerite, and robertsite,-occur in moderate abundance as late stage products in corroded triphylite-heterosite-ferrisicklerite-rockbridgeite masses, associated with leucophosphite,hureaulite, collinsite, laueite, etc.Type specimensare from the Tip Top pegmatite, near Custer, South Dakota. Jahnsite, caMn2+Mgr(Hro)aFe3+z(oH)rlPC)oln,a 14.94(2),b 7.14(l), c 9.93(1)A, p 110.16(8)", P2/a, Z : 2, specific gavity 2.71, biaxial (-), 2V large, e 1.640,p 1.658,t l.6lo, occurs abundantly as striated short to long prismatic crystals, nut brown, yellow, yellow-orange to greenish-yellowin color.Formsarec{001},a{100},il2oll, jl2}ll,ft[iol],/tolll,nt110],andz{itt}. Segeierite,CaMg(HrO)rFes+(OH)[POdz, a 14.826{5),b 18.751(4),c7.30(1)A, Pcca, Z : 8, specific gaavity2.67, biaxial (-), 2Ylarge,a 1.618,p 1.6t5, z 1.650,occurs sparingly as striated yellow'green prismaticcrystals, with c[00], r{010}, nlll0l and qll2l } with perfect {010} cleavage'It is the Feg+-analogueofoverite; a restudy on type overite revealsthe spacegroup Pcca and the ideal formula CaMg(HrO)dl(OH)[POr]r. Robertsite,carMna+r(oH)o(Hro){Ponlr, a 17.36,b lg.53,c 11.30A,p 96.0o,A2/a, Z: 8, specific gravity3.l,T,cleavage[l00] good,biaxial(-) a1.775,8 *t - 1.82,2V-8o,pleochroismextreme (Y, Z = deep reddish brown; 17 : pale reddish-pink), @curs as fibrous massesand small wedge- shapedcrystals showing c[001 f , a{1@}, qt031}.
    [Show full text]
  • Profesionální Referát
    Journal of the Czech Geological Society, 42/4 (1997) 115 History of secondary minerals discovered in Jáchymov (Joachimsthal) Historie objevů sekundárních minerálů z Jáchymova (Czech summary) FRANTIŠEK VESELOVSKÝ1 - PETR ONDRUŠ1 - JAN HLOUŠEK2 1 Czech Geological Survey, Klárov 3, 118 21 Prague 1 2 U Roháčových kasáren 24, 110 00 Prague 10 Jáchymov is type locality for 22 minerals, including 17 secondary minerals. Data on history of discovery and description of new minerals was extracted by search in old literature. Minerals are arranged in the chronological sequence of discovery. Explanation of names of discredited or re-defined minerals and some historical names is included at the end of this paper. Key words: secondary minerals, history description, old mineral names, Jáchymov Introduction This work was continued a decade later by Schrauf. Larsen extensively studied the optical properties of Mining in Jáchymov experienced episodes of boom as Jáchymov minerals at the beginning of the twentieth well as periods of severe decline. Its prosperity was de- century.R. Nováček (1935-1941) studied in detail mainly pendent of mineral wealth and during ages the main secondary minerals from Jáchymov. X-ray diffraction, interest moved from silver to uranium ores. Mineralogy, widely introduced after 1945, provided a new powerful mining and ore dressing proved to be often mutually method of mineral identification. Frondel and Peacock interdependent. The beginnings of mineralogy in Jáchy- continued study of Jáchymov minerals. But only mu- mov date to mining development in early 16th century. seum specimens were available by that time. The first mineralogical notes appear in texts by Agricola The secrecy surrounding uranium mining in the pe- [86], Mathesius, Ercker, and others.
    [Show full text]
  • Mineral Processing
    Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19
    [Show full text]
  • Distribution of As, Ni and Co in Tailings and Surface Waters in the Cobalt Area, Ontario1
    DISTRIBUTION OF AS, NI AND CO IN TAILINGS AND SURFACE 1 WATERS IN THE COBALT AREA, ONTARIO Jeanne B. Percival2, Y.T. John Kwong3, Charles G. Dumaresq4, Frederick A. Michel5 Abstract: From 1904 until the mid 1930’s and intermittently until 1989, over 450 million troy ounces of silver was mined from the Cobalt area, Ontario. Currently there is no active mining of silver, but the area has seen recent exploration activities for other commodities such as diamonds. Cobalt, however, has not only a renowned mining history, but also an environmental legacy. The area is characterized by remnant historic mine workings and numerous waste rock piles and tailings ponds. Several elements of concern including arsenic, nickel and cobalt continually enter the local watershed from the tailings and waste rock piles. These elements are transported through surface waters to the wetlands in the Farr Creek drainage basin and ultimately enter Lake Timiskaming. Tailings samples are composed of abundant plagioclase with subordinate quartz, chlorite, calcite and dolomite. Less common are K-feldspar, amphibole and mica as well as trace minerals such as erythrite, scorodite and pharmocolite. When efflorescent mineral crusts form on tailings surfaces they are dominated by either gypsum or thenardite. The tailings may contain up to 3.5 wt % Co and 2.2 wt% Ni. Lake sediment and tailings cores show concentrations up to 1.8 wt% As, 0.62 wt% Co and 0.27 wt% Ni in the solids, and 160 mg/L As, 74 mg/L Co and 42 mg/L Ni in the pore waters. One core collected from the infilled Hebert Pond situated within the Nipissing Low Grade Mill tailings impoundment show pore water concentrations in excess of 1,500 mg/L As associated with an organic- rich layer.
    [Show full text]
  • The Mineralogical Fate of Arsenic During Weathering Of
    THE MINERALOGICAL FATE OF ARSENIC DURING WEATHERING OF SULFIDES IN GOLD-QUARTZ VEINS: A MICROBEAM ANALYTICAL STUDY A Thesis Presented to the faculty of the Department of Geology California State University, Sacramento Submitted in partial satisfaction of the requirements for the degree of MASTER OF SCIENCE in Geology by Tamsen Leigh Burlak SPRING 2012 © 2012 Tamsen Leigh Burlak ALL RIGHTS RESERVED ii THE MINERALOGICAL FATE OF ARSENIC DURING WEATHERING OF SULFIDES IN GOLD-QUARTZ VEINS: A MICROBEAM ANALYTICAL STUDY A Thesis by Tamsen Leigh Burlak Approved by: __________________________________, Committee Chair Dr. Charles Alpers __________________________________, Second Reader Dr. Lisa Hammersley __________________________________, Third Reader Dr. Dave Evans ____________________________ Date iii Student: Tamsen Leigh Burlak I certify that this student has met the requirements for format contained in the University format manual, and that this thesis is suitable for shelving in the Library and credit is to be awarded for the project. _______________________, Graduate Coordinator ___________________ Dr. Dave Evans Date Department of Geology iv Abstract of THE MINERALOGICAL FATE OF ARSENIC DURING WEATHERING OF SULFIDES IN GOLD-QUARTZ VEINS: A MICROBEAM ANALYTICAL STUDY by Tamsen Leigh Burlak Mine waste piles within the historic gold mining site, Empire Mine State Historic Park (EMSHP) in Grass Valley, California, contain various amounts of arsenic and are the current subject of remedial investigations to characterize the arsenic present. In this study, electron microprobe, QEMSCAN (Quantitative Evaluation of Minerals by SCANning electron microscopy), and X-ray absorption spectroscopy (XAS) were used collectively to locate and identify the mineralogical composition of primary and secondary arsenic-bearing minerals at EMSHP.
    [Show full text]
  • New Mineral Names*,†
    American Mineralogist, Volume 106, pages 1360–1364, 2021 New Mineral Names*,† Dmitriy I. Belakovskiy1, and Yulia Uvarova2 1Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18 korp. 2, Moscow 119071, Russia 2CSIRO Mineral Resources, ARRC, 26 Dick Perry Avenue, Kensington, Western Australia 6151, Australia In this issue This New Mineral Names has entries for 11 new species, including 7 minerals of jahnsite group: jahnsite- (NaMnMg), jahnsite-(NaMnMn), jahnsite-(CaMnZn), jahnsite-(MnMnFe), jahnsite-(MnMnMg), jahnsite- (MnMnZn), and whiteite-(MnMnMg); lasnierite, manganflurlite (with a new data for flurlite), tewite, and wumuite. Lasnierite* the LA-ICP-MS analysis, but their concentrations were below detec- B. Rondeau, B. Devouard, D. Jacob, P. Roussel, N. Stephant, C. Boulet, tion limits. The empirical formula is (Ca0.59Sr0.37)Ʃ0.96(Mg1.42Fe0.54)Ʃ1.96 V. Mollé, M. Corre, E. Fritsch, C. Ferraris, and G.C. Parodi (2019) Al0.87(P2.99Si0.01)Ʃ3.00(O11.41F0.59)Ʃ12 based on 12 (O+F) pfu. The strongest lines of the calculated powder X-ray diffraction pattern are [dcalc Å (I%calc; Lasnierite, (Ca,Sr)(Mg,Fe)2Al(PO4)3, a new phosphate accompany- ing lazulite from Mt. Ibity, Madagascar: an example of structural hkl)]: 4.421 (83; 040), 3.802 (63, 131), 3.706 (100; 022), 3.305 (99; 141), characterization from dynamic refinement of precession electron 2.890 (90; 211), 2.781 (69; 221), 2.772 (67; 061), 2.601 (97; 023). It diffraction data on submicrometer sample. European Journal of was not possible to perform powder nor single-crystal X-ray diffraction Mineralogy, 31(2), 379–388.
    [Show full text]
  • Villyaellenite (Mn, Ca)Mn2(Aso3oh)2(Aso4)2(H2O)4
    Villyaellenite (Mn, Ca)Mn2(AsO3OH)2(AsO4)2(H2O)4 Crystal Data: Monoclinic. Point Group: 2/m. Crystals tabular on {100}, to prismatic along [001], showing {100}, {110}, {011}, {010}, {101}, and {001}, to 4 cm; in rosettes and radial aggregates. Physical Properties: Cleavage: Good on {100}. Hardness = ∼4 D(meas.) = 3.20-3.69 D(calc.) = 3.339 Optical Properties: Transparent. Color: Pale rose-red, orange-pink, colorless; colorless in transmitted light. Streak: White. Luster: Vitreous. Optical Class: Biaxial (-). Pleochroism: Moderate; X = very pale orange-pink; Y = exceedingly pale orange-pink; Z = pale orange-pink. Orientation: X = b; Y ∧ c = 30°-40°. Absorption: Z >> X > Y. α = 1.660-1.713 β = 1.670-1.723 γ = 1.676-1.729 2V(meas.) = 70.5°-76° 2V(calc.) = 75°-75.6° Cell Data: Space Group: C2/c. a = 18.400(2) b = 9.4778(10) c = 9.9594(12) β = 96.587(3)° Z = 4 X-ray Powder Pattern: Sainte-Marie-aux-Mines, France. 3.297 (100), 8.476 (90), 3.132 (60), 4.606 (50), 4.761 (40), 3.811 (40), 3.025 (40) Chemistry: (1) (2) As2O5 52.99 50.6 FeO 0.1 MnO 22.40 36.2 ZnO 2.9 CaO 13.58 0.5 H2O 11.42 9.9 Total 100.39 100.2 (1) Sainte-Marie-aux-Mines, France; by electron microprobe, total Mn as MnO, H2O by TGA; 2+ reducing H2O to 10.7% by analogy to other group members, corresponds to (Mn 2.74Ca2.10)Σ=4.84 (H2O)4(AsO3OH)2.31(AsO4)1.69.
    [Show full text]
  • On the Symmetry of Tsumcorite Group Minerals Based on the New Species Rappoldite and Zincgartrellite
    Mineralogical Magazine, December 2000, Vol. 64(6), pp. 1109-1126 On the symmetry of tsumcorite group minerals based on the new species rappoldite and zincgartrellite H. EFFENBERGERI,*, W. KRAUSE2, H.-J. BERNHARDT3 AND M. MARTIN4 I Institut fUr Mineralogie und Kristallographie, Universitat Wien, Althanstra~e 14, A-I090 Vienna, Austria 2 Henriette-Lott-Weg 8, 0-50354 Hiirth, Gennany 3 Ruhr-Universitat Bochum, Institut fUr Mineralogie, Universitatsstraf.le 150, 0-44780 Bochum, Germany 4 Heinrich-Zille-Weg 8, 0-09599 Freiberg, Germany ABSTRACT Rappoldite, the Co-analogue of helmutwinklerite, and zincgartrellite, the Zn-dominant analogue of gartrellite, are two new members of the tsumcorite group. Both minerals are triclinic, their structures are closely related to the parent structure, i.e. the 'tsumcorite type' (C2/m, Z = 2). The lower symmetry is caused by two different crysta,l-ch~mical requirements. Order :Bhenomen~+ o.f the hydrogen bonds cause the 'helmutwmklente type (PI, Z = 4), ordenng of Cu and Fe' IS responsible for the 'gartrellite type' (PI, Z = I). Rappoldite was found on samples from the Rappold mine near Schneeberg, Saxony, Gennany. The new species fonns red to red-brown prismatic and tabular crystals up to I mm long. Deale. = 5.28 g/cm3. 2Vz = 85(5r, nx = 1.85 (calc.), ny = 1.87(2) and nz = 1.90(2); dispersion is distinct with r > v; orientation is Y -II [120] and X - c. The empirical fonnula derived from electron microprobe analyses II is (Pb 1.01Cao.ol h: 1.02(COO99Nio 62ZnO.35FeO.02h:1.9S[(As04)199(S04)001h:2.00[(OH)0.02(H20) I 98h:2.00 or Pb(Co,Nih(As04h.2H20.
    [Show full text]
  • Topographical Index
    997 TOPOGRAPHICAL INDEX EUROPE Penberthy Croft, St. Hilary: carminite, beudantite, 431 Iceland (fsland) Pengenna (Trewethen) mine, St. Kew: Bondolfur, East Iceland: pitchsbone, beudantite, carminite, mimetite, sco- oligoclase, 587 rodite, 432 Sellatur, East Iceland: pitchs~one, anor- Redruth: danalite, 921 thoclase, 587 Roscommon Cliff, St. Just-in-Peuwith: Skruthur, East Iceland: pitchstonc, stokesite, 433 anorthoclase, 587 St. Day: cornubite, 1 Thingmuli, East Iceland: andesine, 587 Treburland mine, Altarnun: genthelvite, molybdenite, 921 Faroes (F~eroerne) Treore mine, St. Teath: beudantite, carminite, jamesonite, mimetite, sco- Erionite, chabazite, 343 rodite, stibnite, 431 Tretoil mine, Lanivet: danalite, garnet, Norway (Norge) ilvaite, 921 Gryting, Risor: fergusonite (var. risSrite), Wheal Betsy, Tremore, Lanivet: he]vine, 392 scheelite, 921 Helle, Arendal: fergusonite, 392 Wheal Carpenter, Gwinear: beudantite, Nedends: fergusonite, 392 bayldonite, carminite, 431 ; cornubite, Rullandsdalen, Risor: fergusonite, 392 cornwallite, 1 Wheal Clinton, Mylor, Falmouth: danal- British Isles ire, 921 Wheal Cock, St. Just-in- Penwith : apatite, E~GLA~D i~D WALES bertrandite, herderite, helvine, phena- Adamite, hiibnerite, xliv kite, scheelite, 921 Billingham anhydrite mine, Durham: Wheal Ding (part of Bodmin Wheal aph~hitalite(?), arsenopyrite(?), ep- Mary): blende, he]vine, scheelite, 921 somite, ferric sulphate(?), gypsum, Wheal Gorland, Gwennap: cornubite, l; halite, ilsemannite(?), lepidocrocite, beudantite, carminite, zeunerite, 430 molybdenite(?),
    [Show full text]
  • Scorodite Precipitation in the Presence of Antimony
    Title Scorodite precipitation in the presence of antimony Authors Kossoff, D; Welch, MD; Hudson-Edwards, KA Description publisher: Elsevier articletitle: Scorodite precipitation in the presence of antimony journaltitle: Chemical Geology articlelink: http://dx.doi.org/10.1016/j.chemgeo.2015.04.013 content_type: article copyright: Copyright © 2015 The Authors. Published by Elsevier B.V. Date Submitted 2015-03-31 Chemical Geology 406 (2015) 1–9 Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Scorodite precipitation in the presence of antimony David Kossoff a,MarkD.Welchb, Karen A. Hudson-Edwards a,⁎ a Department of Earth and Planetary Sciences, Birkbeck, University of London, Malet St., London WC1E 7HX, UK b Department of Earth Science, The Natural History Museum, Cromwell Road, London SW7 5BD, UK article info abstract Article history: The effects of Sb on the precipitation of synthetic scorodite, and the resultant phases formed, were investigated. Received 7 October 2014 Nine synthetic precipitates with varying concentrations of Sb, together with As-only and Sb-only end members, Received in revised form 12 April 2015 were prepared using a scorodite synthesis method, and these were characterised using XRD, SEM, chemical Accepted 13 April 2015 digestion and μXRF mapping. XRD analysis shows that the end members are scorodite (FeAsO ·2H O) Available online 27 April 2015 4 2 and tripuhyite (FeSbO4), and that the intermediate members are not Sb-substituted scorodite, but instead are Editor: Carla M Koretsky physical mixtures of scorodite and tripuhyite, with tripuhyite becoming more prominent with increasing amounts of Sb in the synthesis. Electron microprobe analysis on natural scorodites confirms that they contain Keywords: negligible concentrations of Sb.
    [Show full text]
  • Polarized Infrared Reflectance Spectra of Brushite
    Polarized infrared reflectance spectra of brushite (CaHPO4 center dot 2H(2)O) crystal investigation of the phosphate stretching modes Jean-Yves Mevellec, Sophie Quillard, Philippe Deniard, Omar Mekmene, Frederic Gaucheron, Jean-Michel Bouler, Jean-Pierre Buisson To cite this version: Jean-Yves Mevellec, Sophie Quillard, Philippe Deniard, Omar Mekmene, Frederic Gaucheron, et al.. Polarized infrared reflectance spectra of brushite (CaHPO4 center dot 2H(2)O) crystal investigation of the phosphate stretching modes. Spectrochimica Acta Part A: Molecular and Biomolecular Spec- troscopy, Elsevier, 2013, 111, pp.7. 10.1016/j.saa.2013.03.047. hal-00980658 HAL Id: hal-00980658 https://hal.archives-ouvertes.fr/hal-00980658 Submitted on 29 May 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy 111 (2013) 7–13 Contents lists available at SciVerse ScienceDirect Spectr ochimica Acta Part A: Molecul ar and Biomo lecular Spectrosco py journal homepage: www.elsevier.com/locate/saa Polarized infrared reflectance spectra of brushite (CaHPO4Á2H2O) crystal investigation of the phosphate stretching modes ⇑ Jean-Yves Mevellec a, , Sophie Quillard b, Philippe Deniard a, Omar Mekmene c, Frédéric Gaucheron c, Jean-Michel Bouler b, Jean-Pierre Buisson a a CNRS, Institut des Matériaux Jean-Rouxel (IMN) – UMR 6502, Université de Nantes, 2 rue de la Houssinière, B.P.
    [Show full text]