Thermal Behavior of Realgar As4s4, and of Arsenolite As2o3 and Non-Stoichiometric As8s8+X
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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 -
Theoretical Studies on As and Sb Sulfide Molecules
Mineral Spectroscopy: A Tribute to Roger G. Bums © The Geochemical Society, Special Publication No.5, 1996 Editors: M. D. Dyar, C. McCammon and M. W. Schaefer Theoretical studies on As and Sb sulfide molecules J. A. TOSSELL Department of Chemistry and Biochemistry University of Maryland, College Park, MD 20742, U.S.A. Abstract-Dimorphite (As4S3) and realgar and pararealgar (As4S4) occur as crystalline solids con- taining As4S3 and As4S4 molecules, respectively. Crystalline As2S3 (orpiment) has a layered structure composed of rings of AsS3 triangles, rather than one composed of discrete As4S6 molecules. When orpiment dissolves in concentrated sulfidic solutions the species produced, as characterized by IR and EXAFS, are mononuclear, e.g. ASS3H21, but solubility studies suggest trimeric species in some concentration regimes. Of the antimony sulfides only Sb2S3 (stibnite) has been characterized and its crystal structure does not contain Sb4S6 molecular units. We have used molecular quantum mechanical techniques to calculate the structures, stabilities, vibrational spectra and other properties of As S , 4 3 As4S4, As4S6, As4SIO, Sb4S3, Sb4S4, Sb4S6 and Sb4SlO (as well as S8 and P4S3, for comparison with previous calculations). The calculated structures and vibrational spectra are in good agreement with experiment (after scaling the vibrational frequencies by the standard correction factor of 0.893 for polarized split valence Hartree-Fock self-consistent-field calculations). The calculated geometry of the As4S. isomer recently characterized in pararealgar crystals also agrees well with experiment and is calculated to be about 2.9 kcal/mole less stable than the As4S4 isomer found in realgar. The calculated heats of formation of the arsenic sulfide gas-phase molecules, compared to the elemental cluster molecules As., Sb, and S8, are smaller than the experimental heats of formation for the solid arsenic sulfides, but shown the same trend with oxidation state. -
REVISION 1 an Insight at the Inverse Transformation of Realgar Altered By
REVISION 1 An insight at the inverse transformation of realgar altered by light Giovanni Pratesi1,2 and Matteo Zoppi1* 1Museo di Storia Naturale - Sezione Mineralogia e Litologia, Università di Firenze, via La Pira 4, I- 50121 Firenze, Italy. 2Dipartimento di Scienze della Terra, Università di Firenze, via La Pira 4, I-50121 Firenze, Italy. * E-mail: [email protected] ABSTRACT The light-induced alteration of realgar and β-As4S4 is a well known phenomenon but still displays interesting aspects not completely explained. In the transformation from realgar to pararealgar the molecule As4S4 undergoes a structural modification, and ever since the initial studies two important issues have been highlighted: the influence of the oxygen and the reversibility of the process. The previous study on the reversibility of the altered β-As4S4 points out that this polymorph exhibits a dual behaviour. When the light-induced alteration occurs with the presence of the air, pararealgar and arsenolite, along with amorphous material, are the products, while if the air is not present β-As4S4 turns completely into pararealgar. Moreover, when annealing the altered material in the realgar stability fields (220 °C), in the first case pararealgar and amorphous material turn into stoichiometric alacranite, while in the second case the alteration is completely reversible. Similarly, the present study focuses the attention on the question if realgar, when altered by means of the light and when annealed, might behave as β-As4S4 does. These results display that the phenomenon is more complex. The alteration of realgar with the presence of the air yields pararealgar along with arsenolite, a small quantity of uzonite and amorphous material, and when the air is not present pararealgar is the only product. -
Geological Controls on Pit Lake Chemistry: Implications for the Assessment of Water Quality in Inactive Open Pits
IMWA Proceedings 1998 | © International Mine Water Association 2012 | www.IMWA.info Geological Controls on Pit Lake Chemistry: Implications for the assessment of Water Quality in Inactive Open Pits 1 2 2 2 3 R.J.Bowell , J. Barta , M.Gringrich , W.Mansanares and J. Parshley 'Steffen, Robertson & Kirsten (UK) Limited, Stunmit House, 9 Windsor Place, CardiffCFI 3BX, Wales 2Getchell Gold Corporation, Golconda, Nevada NV89414, USA 3Steffen, Robertson & Kirsten (US) Inc., 1755 E. Plumb Lane, Reno, Nevada NV89502, USA ABSTRACT Open pitting is a method of mining used to exploit many mineral commodities. In many instances mining occurs below the water table leading to active dewatering of the pit during mining. On suspension of activity, pumping is terminated and as infilling of the pit is not always economic the pit is flooded, forming a pit lake. Pit Lakes are viewed as a significant environmental issue owing to their visible presence. It is often, erroneously assumed that all pit lakes will be acid and of poor quality. Consequently in many cases extensive water quality modelling is undertaken to determine the chemical characteristics of a pit lake, with only scant geological knowledge of the pit walls. However, the water quality of a mine pit lake is largely predictable from geological knowledge of the ore deposit, the host rocks and mineralogy. In this paper we present a case study from Nevada of an inactive open pit on which a detailed study was conducted to determine the environmental impacts. This study was greatly enhanced by using geological and geochemical mapping of the pit walls in order to determine controls on pit lake chemistry. -
Growth and Raman Spectroscopic Characterization of As4s4 (II) Single Crystals
*4. Manuscript Click here to view linked References Growth and Raman spectroscopic characterization of As4S4 (II) single crystals Atsushi Kyono Division of Earth Evolution Sciences, Graduate School of Life and Environmental Sciences, University of Tsukuba, 1-1-1 Tennodai Tsukuba, Ibaraki 305-8572, Japan Corresponding author: A. Kyono Present Address: Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Branch Rd. NW, Washington, DC 20015-1305, USA Email: [email protected] Phone: +1-202-478-8940, Fax: +1-202-478-8901 pg. 1 ABSTRACT As described by Kutoglu (1976), single crystals of As4S4 (II) phase have been grown using a new two-step synthesis that drastically increases the reproducibility that is attainable in synthetic experiments. First, through photoinduced phase transformation, pararealgar powder is prepared as a precursor instead of AsS melt. Then it is dissolved and recrystallized from CS2 solvent. Results show that single crystals of the As4S4 (II) phase were obtained reproducibly through the dissolution–recrystallization process. Single crystals of As4S4 (II) obtained using the method were translucent and showed a uniform yellow–orange color. The crystal exhibits a platelet-like shape as a thin film with well-developed faces (0 1 0) and (0 -1 0). The grown crystals are as large as 0.50 × 0.50 × 0.01 mm. They were characterized using powder and single crystal X-ray diffraction techniques to confirm the phase identification and the lattice parameters. The As4S4 (II) phase crystallizes in monoclinic system with cell parameters a = 11.202(4) Å, b = 9.954(4) Å, c = 7.142(4) Å, β = 92.81(4)°, V = 795.4(6) Å3, which shows good agreement with the former value. -
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338 Geologica Macedonica, Vol. 32, No. 2, pp. 95–117 (2018) GEOME 2 IISSN 0352 – 1206 Manuscript received: August 5, 2018 e-ISSN 1857 – 8586 Accepted: November 7, 2018 UDC: 553.46:550.43.08]:504(497.721) 553.497:550.43.08]:504(497.721) Original scientific paper SUPERGENE MINERALOGY OF THE LOJANE Sb-As-Cr DEPOSIT, REPUBLIC OF MACEDONIA: TRACING THE MOBILIZATION OF TOXIC METALS Uwe Kolitsch1,2, Tamara Đorđević2, Goran Tasev3, Todor Serafimovski3, Ivan Boev3, Blažo Boev3 1Mineralogisch-Petrographische Abt., Naturhistorisches Museum, Burgring 7, A-1010 Wien, Austria 2Institut für Mineralogie und Kristallographie, Universität Wien, Althanstr. 14, A-1090 Wien, Austria 3Department of Mineral Deposits, Faculty of Natural and Technical Sciences, “Goce Delčev” University in Štip, Blvd. Goce Delčev 89, 2000 Štip, Republic of Macedonia [email protected] A b s t r a c t: As part of a larger project on the environmental mineralogy and geochemistry of the Lojane Sb- As-Cr deposit, Republic of Macedonia, which was mined for chromite and, later, stibnite until 1979 and is a substantial source of arsenic and antimony pollution, the supergene mineralogy of the deposit was studied. Samples collected on ore and waste dumps were used to identify and characterize the previously uninvestigated suite of supergene mineral phases by standard mineralogical techniques. The following species were determined (in alphabetical order): annaber- gite, arseniosiderite(?), gypsum, hexahydrite, hörnesite, pararealgar, roméite-group minerals, rozenite, scorodite, sen- armontite, stibiconite, sulphur, tripuhyite and valentinite. Their occurrences are described and their local conditions of formation are discussed. High-resolution Raman spectra of hörnesite, hexahydrite and rozenite are provided and com- pared with literature data. -
Clarke Jeff a 201709 Mscproj
THE CHARACTERIZATION OF ARSENIC MINERAL PHASES FROM LEGACY MINE WASTE AND SOIL NEAR COBALT, ONTARIO by Jeff Clarke A research project submitted to the Department of Geological Sciences and Geological Engineering In conformity with the requirements for the degree of Master of Science in Applied Geology Queen’s University Kingston, Ontario, Canada (July, 2017) Copyright © Jeff Clarke, 2017 i ABSTRACT The Cobalt-Coleman silver (Ag) mining camp has a long history of mining dating back to 1903. Silver mineralization is hosted within carbonate veins and occurs in association with Fe-Co-Ni arsenide and sulpharsenide mineral species. The complex mineralogy presented challenges to early mineral processing methods with varying success of Ag recovery and a significant amount of arsenic (As) in waste material which was disposed in the numerous tailings deposits scattered throughout the mining camp, and in many instances disposed of uncontained. The oxidation and dissolution of As-bearing mineral phases in these tailings and legacy waste sites releases As into the local aquatic environment. Determining the distribution of primary and secondary As mineral species in different legacy mine waste materials provides an understanding of the stability of As. Few studies have included detailed advanced mineralogical characterization of As mineral species from legacy mine waste in the Cobalt area. As part of this study, a total of 28 samples were collected from tailings, processed material near mill sites and soils from the legacy Nipissing and Cart Lake mining sites. The samples were analyzed for bulk chemistry to delineate material with strongly elevated As returned from all sample sites. This sampling returned highly elevated As with up to 6.01% As from samples near mill sites, 1.71% As from tailings and 0.10% As from soils. -
Single Crystal Raman Spectroscopy of Selected Arsenite, Antimonite and Hydroxyantimonate Minerals
SINGLE CRYSTAL RAMAN SPECTROSCOPY OF SELECTED ARSENITE, ANTIMONITE AND HYDROXYANTIMONATE MINERALS Silmarilly Bahfenne B.App.Sci (Chem.) Chemistry Discipline This thesis is submitted as part of the assessment requirements of Master of Applied Science Degree at QUT February 2011 KEYWORDS Raman, infrared, IR, spectroscopy, synthesis, synthetic, natural, X-ray diffraction, XRD, scanning electron microscopy, SEM, arsenite, antimonate, hydroxyantimonate, hydrated antimonate, minerals, crystal, point group, factor group, symmetry, leiteite, schafarzikite, apuanite, trippkeite, paulmooreite, finnemanite. i ii ABSTRACT This thesis concentrates on the characterisation of selected arsenite, antimonite, and hydroxyantimonate minerals based on their vibrational spectra. A number of natural arsenite and antimonite minerals were studied by single crystal Raman spectroscopy in order to determine the contribution of bridging and terminal oxygen atoms to the vibrational spectra. A series of natural hydrated antimonate minerals was also compared and contrasted using single crystal Raman spectroscopy to determine the contribution of the isolated antimonate ion. The single crystal data allows each band in the spectrum to be assigned to a symmetry species. The contribution of bridging and terminal oxygen atoms in the case of the arsenite and antimonite minerals was determined by factor group analysis, the results of which are correlated with the observed symmetry species. In certain cases, synthetic analogues of a mineral and/or synthetic compounds isostructural or related to the mineral of interest were also prepared. These synthetic compounds are studied by non-oriented Raman spectroscopy to further aid band assignments of the minerals of interest. Other characterisation techniques include IR spectroscopy, SEM and XRD. From the single crystal data, it was found that good separation between different symmetry species is observed for the minerals studied. -
Current Research on Artificial Arsenic Sulphide Pigments in Artworks: Ashort Review
CONSERVATION OF CULTURAL HERITAGE 903 doi:10.2533/chimia.2008.903 CHIMIA 2008, 62,No. 11 Chimia 62 (2008) 903–907 ©Schweizerische Chemische Gesellschaft ISSN 0009–4293 Current Research on Artificial Arsenic Sulphide Pigments in Artworks: AShort Review Günter Grundmann*a and Mark Richterb Abstract: Ageneral re-examination of the artificial arsenic sulphide pigments orpiment, realgar and alacranite using polarised light microscopy (PLM), scanning electron microscopy (SEM) combined with energy and wavelength dis- persive X-ray analysis (EDX, WDX) and X-ray diffraction analysis (XRD) revealed the following results: wet-process precipitation products of artificial orpiment consist of golden yellow,amorphous, spherical particles ranging from 0.2 to 2 µmØ.Dry-process roasting and/or sublimation products with an arsenolite/sulphur mixtureconsist mainly of amorphous golden yellow oval drops and spherules of amorphous arsenic sulphide glass (g-AsxSx)with a smooth surface ranging from 1to20µmØinassociation with arsenolite crystal aggregates and members of the alacranite solid solution series (As8S8)–(As8S9). Abright lemon yellow to orange-red arsenic sulphide pigment on a sixteenth/seventeenth-century South German polychrome recumbent sculptureand aseventeenth-century Dutch painting attributed to Rembrandt’sstudio has been identified as an artificial orpiment produced with dry-process (roasting/sublimation) methods. The recumbent figurecontains (i) yellow,orange or red-brown amorphous splintery fragments and spherules of arsenic sulphide glass of up to 25 µm Ø, (ii) yellow,brown or red-brown crystalline spherules and splintery fragments of alacranite, (iii) lemon yellow to red-brown agglomerates of arsenic sulphide glass, and (iv) colourless irregular fragments or octahedral crystals of arsenolite. This type can be classified as ‘complex artificial orpiment’. -
Allchar Mineral Assemblage 3
Geologica Macedonica, Vol. 15-16, p. 1-23 (2001-2002) Suppl. GEOME2 SSN 0352 - 1206 Manuscript received: December 15, 200 1 UDC: 553.08 (497 .7) Accepted: March 3, 2002 Original scientific paper ~• ALLCHAR l\1INERAL ASSEMBLAGE l 3 l 4 Blazo Boev , Vladimir Bermanec , Todor Serafimovski\ Sonja Lepitkova , Snezana Mikulcic , 5 5 5 Marin ~oufek\ Gligor Jovanovski , Trajce Stafilov , Metodija Najdoski IDepartment ofPetrology, Mineralogy and Geochemistry, Faculty ofMining and Geology, "Sv. Kiril i Metodij" University, Goce Delcev 89, MK-2000 Stip, Republic ofMacedonia 2Department ofMineral Deposits, Faculty ofMining and Geology, "Sv. Kiril i Metodij" University, Goce Delcev 89, MK-2000 Stip, Republic of Macedonia 3Institute ofMineralogy and Petrology, Department ofGeology, Faculty ofScience, University ofZagreb, Horvatovac bb, HR-JOOOO Zagreb, Croatia 4Department ofMineralogy and Petrology, Croatian Natural History Museum, Demetrova I, HR-JOOOO Zagreb, Croatia 5Institute of Chemistry, Faculty ofScience, "Sv. Kiril i Metodij" University, P.o. Box 162, MK-JOOI Skopje, Republic ofMacedonia Abstract. The paper is a summary of investigatioris carried out on minerals of the Allchar deposit. It discusses the TI-As-Sb-Au mineral ill emblage after detailed and intense research work. Four types of mineralization have been distinguished based on the mineral assemblage present: I. The first ly pe is characterised by high c ment of iron and sulphur, but lower arsenic and thalli um contenl. The pyrite-marcasite mineral assemblage is characterized by the presence of some quantities of arsenic-pyrite. 2. The second type is characterized by the high antimony and low iron and thallium content. Stibnite is the most common mineral in the group. -
Characterization and Comparative Physico-Chemical Studies Of
RESEARCH COMMUNICATIONS 19. Peng, L. and Yu, B., Numerical study of regional environmental Characterization and comparative carrying capacity for livestock and poultry farming based on planting-breeding balance. J. Environ. Sci., 2013, 25(9), 1882– physico-chemical studies of 1889. 20. State Environmental Protection Administration, Investigation and Manahshila (traditionally used arsenic Control Counter Measures of Pollution Situation of Livestock and mineral) and the corresponding Poultry Breeding Industry in China, China Environmental Science Press, Beijing, 2002, pp. 14–103. polymorphs of realgar (As4S4) 21. Peng, L. and Wang, D., Estimation of annual quantity of total excretion from livestock and poultry in Chongqing municipality. 1, 2 Trans. Chin. Soc. Agric. Eng., 2004, 20(1), 288–292. Vinamra Sharma *, Amiya K. Samal , 22. Yan, B. J. and Pan, Y. C., Estimation of nitrogen pollution load of Anand K. Chaudhary1 and Rajesh K. Srivastava2 farmland from livestock manure in China based on grid. Bull. Soil 1Department of Rasa Shastra, Faculty of Ayurveda, Water Conserv., 2015, 35(5), 133–137. Institute of Medical Sciences, and 23. Yan, B. J., Zhao, C. J., Pan, Y. C. and Wang, Y., Estimation of the 2Centre of Advanced Study in Geology, Institute of Science, amount of livestock manure and its environmental influence of Banaras Hindu University, Varanasi 221 005, India large-scaled culture based on spatial information. China Environ. Sci., 2009, 29(7), 733–737. 24. Yan, B. J., Zhao, C. J., Pan, Y. C., Yan, J. J. and Guo, X., Estima- This communication presents characterization and tion of livestock manure nitrogen load and pollution risk evalua- comparison of the physico-chemical properties of dif- tion of farmland in Daxing District. -
Primary Minerals of the Jáchymov Ore District
Journal of the Czech Geological Society 48/34(2003) 19 Primary minerals of the Jáchymov ore district Primární minerály jáchymovského rudního revíru (237 figs, 160 tabs) PETR ONDRU1 FRANTIEK VESELOVSKÝ1 ANANDA GABAOVÁ1 JAN HLOUEK2 VLADIMÍR REIN3 IVAN VAVØÍN1 ROMAN SKÁLA1 JIØÍ SEJKORA4 MILAN DRÁBEK1 1 Czech Geological Survey, Klárov 3, CZ-118 21 Prague 1 2 U Roháèových kasáren 24, CZ-100 00 Prague 10 3 Institute of Rock Structure and Mechanics, V Holeovièkách 41, CZ-182 09, Prague 8 4 National Museum, Václavské námìstí 68, CZ-115 79, Prague 1 One hundred and seventeen primary mineral species are described and/or referenced. Approximately seventy primary minerals were known from the district before the present study. All known reliable data on the individual minerals from Jáchymov are presented. New and more complete X-ray powder diffraction data for argentopyrite, sternbergite, and an unusual (Co,Fe)-rammelsbergite are presented. The follow- ing chapters describe some unknown minerals, erroneously quoted minerals and imperfectly identified minerals. The present work increases the number of all identified, described and/or referenced minerals in the Jáchymov ore district to 384. Key words: primary minerals, XRD, microprobe, unit-cell parameters, Jáchymov. History of mineralogical research of the Jáchymov Chemical analyses ore district Polished sections were first studied under the micro- A systematic study of Jáchymov minerals commenced scope for the identification of minerals and definition early after World War II, during the period of 19471950. of their relations. Suitable sections were selected for This work was aimed at supporting uranium exploitation. electron microprobe (EMP) study and analyses, and in- However, due to the general political situation and the teresting domains were marked.