Frederick Augustus Genth. 1820-1898
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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 -
Utahite, a New Mineral and Associated Copper Tellurates from the Centennial Eureka Mine, Tintic District, Juab County, Utah
UTAHITE, A NEW MINERAL AND ASSOCIATED COPPER TELLURATES FROM THE CENTENNIAL EUREKA MINE, TINTIC DISTRICT, JUAB COUNTY, UTAH Andrew C. Roberts and John A. R. Stirling Geological Survey of Canada 601 Booth Street Ottawa, Ontario, Canada K IA OE8 Alan J. Criddle Martin C. Jensen Elizabeth A. Moffatt Department of Mineralogy 121-2855 Idlewild Drive Canadian Conservation Institute The Natural History Museum Reno, Nevada 89509 1030 Innes Road Cromwell Road Ottawa, Ontario, Canada K IA OM5 London, England SW7 5BD Wendell E. Wilson Mineralogical Record 4631 Paseo Tubutama Tucson, Arizona 85750 ABSTRACT Utahite, idealized as CusZn;(Te6+04JiOH)8·7Hp, is triclinic, fracture. Utahite is vitreous, brittle and nonfluorescent; hardness space-group choices P 1 or P 1, with refined unit-cell parameters (Mohs) 4-5; calculated density 5.33 gtcm' (for empirical formula), from powder data: a = 8.794(4), b = 9996(2), c = 5.660(2);\, a = 5.34 glcm' (for idealized formula). In polished section, utahite is 104.10(2)°, f3 = 90.07(5)°, y= 96.34(3YO, V = 479.4(3) ;\3, a:b:c = slightly bireflectant and nonpleochroic. 1n reflected plane-polar- 0.8798:1 :0.5662, Z = 1. The strongest five reflections in the X-ray ized light in air it is very pale brown, with ubiquitous pale emerald- powder pattern are (dA(f)(hkl)]: 9.638(100)(010); 8.736(50)(100); green internal reflections. The anisotropy is unknown because it is 4.841(100)(020); 2.747(60)(002); 2.600(45)(301, 311). The min- masked by the internal reflections. Averaged electron-microprobe eral is an extremely rare constituent on the dumps of the Centen- analyses yielded CuO = 25.76, ZnO = 15.81, Te03 = 45.47, H20 nial Eureka mine, Tintic district, Juab County, Utah, where it (by difference) {12.96], total = {100.00] weight %, corresponding occurs both as isolated 0.6-mm clusters of tightly bound aggre- to CU49;Zn29lTe6+04)39l0H)79s' 7.1H20, based on 0 = 31. -
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. -
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. -
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THn AUERICAN MtxERALocIST JOURNAL OF THE MINERALOGICAL SOCIETY OF AMERICA Vol. 50 MAY-JUNE, 1965 Nos. 5 and 6 KITKAITE (NiTeSe), A NEW MINERAL FROM KUUSAMO, NORTHEAST FINLAND T. A. HArr-r, Y. Vuonor.ArNEN'Outohumpu Company, Outokumpu, Finland' AND Tn.G. Seuaue, Inst'itute oJ Geology,Helsinhi, Finland'. ABSTRACT Kitkaite, NiTese, occurs in carbonate-bearing veinlets in Kuusamo, NE Finland associ- ated with nickel and selenium mineralization. Kitkaite is trigonal, o:3.716+0.005 and c:5.126+0.005 A, space group PEml, Z:1, calculated density 7.19 gm/cc, measured d,ensity 7.22 gm/cc. The mineral is isostructural with melonite with which it forms a solid solution series. Kitkaite is named in allusion to the river Kitka in the valley of which the mineral was found. During prospecting work in 1961 in the valley of the Kitka river in Kuusamo, northeast Finland, a silver-white opaque mineral was en- countered by a field group of the Outokumpu Company. The mineral could not be identified in the field. Therefore, and becauseof its interest- ing mode of occurrencein a zone of nickel and selenium mineralization, it was subjected to a closer study at the researchlaboratory of the Com- pany. It was found that the mineral represents a new specieswith the chemical formula NiTeSe. In allusion to the locality of its discovery, the name kitkaite is suggestedfor the mineral. As has been pointed out by Sindeeva (1964), minerals containing both selenium and tellurium as major elements have been unknown so far. Some selenium-bearingminerals have been reported with low tellurium contents, but the amount of the latter compared with that of selenium is so small that tellurium must be regarded merely as a minor element not essential to the mineral' Thus, e'g. -
Insight Into Mineralizer Modified and Tailored Scorodite Crystal
RSC Advances View Article Online PAPER View Journal | View Issue Insight into mineralizer modified and tailored scorodite crystal characteristics and leachability for Cite this: RSC Adv.,2018,8, 19560 arsenic-rich smelter wastewater stabilization† Yonggang Sun,ab Qi Yao,ab Xin Zhang, *ab Hongling Yang,ab Na Li,ab Zhongshen Zhangab and Zhengping Hao ab Arsenic-rich non-ferrous smelter wastewater has the potential to cause harm to the environment and human health. The use of mineralizer modified and tailored scorodite crystals, a secondary As-bearing mineral, is considered to be the most promising strategy for arsenic stabilization. In this work, firstly, the mechanisms influencing the scorodite crystal characteristics for arsenic stabilization were investigated, and the results indicated that the scorodite stability was greatly influenced by the scorodite crystal shape and particle size. The crystal shape changes that the scorodite solids undergo during the aging period were observed, from a laminar structure to a polyhedron to a standard octahedral structure, and À1 À1 Creative Commons Attribution-NonCommercial 3.0 Unported Licence. meanwhile, the As-concentration decreased from 10.2 mg L to 3.7 mg L , with the relative particle size value (RPS) increasing from 1.50 to 2.64. Secondly, the addition of a mineralizer to further improve the scorodite crystal stability was investigated. It was meaningful to observe that the lowest As- concentration of 0.39 mg LÀ1 could be attained when trace NaF was employed, and it was of great significance to apply this strategy for the disposal of As and F-containing wastewater due to the electrostatic interaction between scorodite and sodium fluoride. -
Tungsten Minerals and Deposits
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 652 4"^ TUNGSTEN MINERALS AND DEPOSITS BY FRANK L. HESS WASHINGTON GOVERNMENT PRINTING OFFICE 1917 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 25 CENTS PER COPY CONTENTS. Page. Introduction.............................................................. , 7 Inquiries concerning tungsten......................................... 7 Survey publications on tungsten........................................ 7 Scope of this report.................................................... 9 Technical terms...................................................... 9 Tungsten................................................................. H Characteristics and properties........................................... n Uses................................................................. 15 Forms in which tungsten is found...................................... 18 Tungsten minerals........................................................ 19 Chemical and physical features......................................... 19 The wolframites...................................................... 21 Composition...................................................... 21 Ferberite......................................................... 22 Physical features.............................................. 22 Minerals of similar appearance................................. -
Utahite Cu5zn3(Te6+O4)4(OH)8 • 7H2O
6+ Utahite Cu5Zn3(Te O4)4(OH)8 • 7H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Triclinic. Point Group: 1or1. Prismatic to thin tabular to bladed crystals, elongated along [001], showing {010} and {001}, in parallel to subparallel aggregates, to 0.6 mm, also as sheaves and bow tielike groups. Physical Properties: Fracture: Uneven. Tenacity: Brittle. Hardness = ∼4–5 D(meas.) = n.d. D(calc.) = 5.33 Optical Properties: Translucent. Color: Pale blue to blue-green. Streak: Pale blue. Luster: Vitreous to pearly. Optical Class: [Biaxial.] n = [1.83–1.90] α = n.d. β = n.d. γ = n.d. 2V(meas.) = n.d. Cell Data: Space Group: P 1or P 1. a = 8.794(4) b = 9.996(2) c = 5.660(2) α = 104.10(2)◦ β =90.07(5)◦ γ =96.34(3)◦ Z=1 X-ray Powder Pattern: Centennial Eureka mine, Utah, USA. 9.638 (100), 4.841 (100), 2.747 (60), 8.736 (50), 2.600 (45), 6.862 (40), 6.172 (40) Chemistry: (1) (2) TeO3 45.47 45.54 CuO 25.76 25.78 ZnO 15.81 15.83 H2O [12.96] 12.85 Total [100.00] 100.00 (1) Centennial Eureka mine, Utah, USA; by electron microprobe, average of six analyses, 1− H2O by difference, total Te as TeO3, (OH) and H2O confirmed by IR; corresponds to • • Cu4.98Zn2.99(TeO4)3.98(OH)8 7.1H2O. (2) Cu5Zn3(TeO4)4(OH)8 7H2O. Occurrence: A very rare secondary mineral found on dump material from the oxidized zone of a Cu–Zn–Te-bearing hydrothermal ore deposit. -
VARISCITE from CENTRAL TAJIKISTAN: PRELIMINARY RESULTS Andrey K
NOTES & NEW TECHNIQUES VARISCITE FROM CENTRAL TAJIKISTAN: PRELIMINARY RESULTS Andrey K. Litvinenko, Elena S. Sorokina, Stefanos Karampelas, Nikolay N. Krivoschekov, and Roman Serov variscite group (variscite and strengite) are isodimor- An occurrence of variscite containing strengite, phous with the metavariscite monoclinic phosphate as well as other minerals from both the variscite mineral group members metavariscite and phospho- and metavariscite groups, was discovered in the siderite, respectively. late 1970s in central Tajikistan. The material, Most of the variscite in the market today comes ranging from light blue to light green to green, is from the state of Utah, close to the cities of Lucin and suitable for cabochon cutting. The samples pre- Fairfield, though some of these mines are practically sented in this study showed traces of sulfur and exhausted (Larsen, 1942; Solodova et al., 1985; Willing arsenic, with higher iron and generally lower et al., 2008). The occurrences at Woodlands, Western vanadium and chromium concentrations than Australia, and Yauli, Peru were discovered in 2004 and variscites reported from other localities.These dif- 2011, respectively (Willing et al., 2008; Hyršl, 2011). ferences may result from the intergrowth of Among the minerals of the variscite and variscite with other minerals from the variscite metavariscite groups, variscite is most often used for and metavariscite groups. carvings and ornaments (see Koivula, 1986; Fritz and Rockwell, 2006; Willing et al., 2008; and Hyršl, 2011). Variscite has a waxy luster and is transparent to translucent with a color range from white to brown ariscite (figure 1), a relatively common cave min- and blue to green to yellow, which can cause misiden- eral that forms as a result of phosphate-bearing V tification as turquoise and chrysoprase (Willing et al., surface solutions reacting with aluminum-rich rocks 2008). -
Insight Into Mineralizer Modified and Tailored Scorodite Crystal
RSC Advances View Article Online PAPER View Journal | View Issue Insight into mineralizer modified and tailored scorodite crystal characteristics and leachability for Cite this: RSC Adv.,2018,8, 19560 arsenic-rich smelter wastewater stabilization† Yonggang Sun,ab Qi Yao,ab Xin Zhang, *ab Hongling Yang,ab Na Li,ab Zhongshen Zhangab and Zhengping Hao ab Arsenic-rich non-ferrous smelter wastewater has the potential to cause harm to the environment and human health. The use of mineralizer modified and tailored scorodite crystals, a secondary As-bearing mineral, is considered to be the most promising strategy for arsenic stabilization. In this work, firstly, the mechanisms influencing the scorodite crystal characteristics for arsenic stabilization were investigated, and the results indicated that the scorodite stability was greatly influenced by the scorodite crystal shape and particle size. The crystal shape changes that the scorodite solids undergo during the aging period were observed, from a laminar structure to a polyhedron to a standard octahedral structure, and À1 À1 Creative Commons Attribution-NonCommercial 3.0 Unported Licence. meanwhile, the As-concentration decreased from 10.2 mg L to 3.7 mg L , with the relative particle size value (RPS) increasing from 1.50 to 2.64. Secondly, the addition of a mineralizer to further improve the scorodite crystal stability was investigated. It was meaningful to observe that the lowest As- concentration of 0.39 mg LÀ1 could be attained when trace NaF was employed, and it was of great significance to apply this strategy for the disposal of As and F-containing wastewater due to the electrostatic interaction between scorodite and sodium fluoride. -
Petzite Ag3aute2 C 2001-2005 Mineral Data Publishing, Version 1
Petzite Ag3AuTe2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Cubic. Point Group: 432. Massive, fine granular to compact and as irregular shaped blebs, to 2 mm. Physical Properties: Cleavage: {001}. Fracture: Subconchoidal. Tenacity: Slightly sectile to brittle. Hardness = 2.5–3 VHN = 48 (10 g load). D(meas.) = 8.7–9.4 D(calc.) = 8.74 Optical Properties: Opaque. Color: Bright steel-gray to iron-gray to iron-black, commonly tarnished from bronze-yellow to sooty black; in reflected light, grayish white with a pale bluish tint. Luster: Metallic. Anisotropism: Noticeable in part. R: (400) 45.0, (420) 43.7, (440) 42.4, (460) 41.4, (480) 40.6, (500) 39.9, (520) 39.3, (540) 38.8, (560) 38.5, (580) 38.3, (600) 38.2, (620) 38.1, (640) 38.0, (660) 37.8, (680) 37.8, (700) 37.8 Cell Data: Space Group: I4132. a = 10.385(4) Z = 8 X-ray Powder Pattern: Bot´es,Romania. 2.77 (100), 2.12 (80), 2.03 (70), 2.44 (60), 2.32 (60), 7.31 (50), 1.893 (50) Chemistry: (1) (2) (3) Ag 41.37 41.87 41.71 Au 23.42 25.16 25.39 Te 33.00 33.21 32.90 Hg 2.26 Cu 0.16 Total 100.21 100.24 100.00 (1) Kalgoorlie, Australia. (2) Mother Lode district, California, USA. (3) Ag3AuTe2. Occurrence: With other tellurides in vein-controlled gold deposits. Association: Gold, hessite, sylvanite, krennerite, calaverite, altaite, montbrayite, melonite, frohbergite, tetradymite, rickardite, vulcanite, pyrite. Distribution: Noted in small amounts at a number of localities other than those listed here. -
PROCEEDINGS of the TWENTY-SIXTH ANNUAL MEETING of the MINERALOGICAL SOCIETY of AMERICA at PITTSBURGH, PENNSYLVANIA C. S. Hunrnut
PROCEEDINGSOF THE TWENTY-SIXTH ANNUAL MEETING OF THE MINERALOGICAL SOCIETY OF AMERICA AT PITTSBURGH, PENNSYLVANIA C. S. Hunrnut, Jn., SecretarY The twenty-sixth annual meeting of the Society was held at the Hotel William Penn, Pittsburgh, Pennsylvania, on December 27-29, 1945. The registration figures show that 74 fellows and 56 members attended. Four scientific sessionswere held, two in the afternoon of December 27th and two in the afternoon of December 28th. Because of lack of time the routine business of the Society was not presented at a general session. The luncheon of the Mineralogical Society, which was held on December 27th, was attended by 108 fellows, members and guests. After the luncheon the Society was addressed by Past Presidents R' C. Emmons on "The Shift in Emphasis" and A. F. Buddington on "Some Mineralogical Re- flections.t' The report of the election of officers and fellows lot 1946 and the reports of the officers for the year 1945 are given on the following pages. ELECTION OF OFFICERS AND FELLOWS FOR 1946 The secretary reports that 343 ballots were cast for the officers of the Society as nomi- nated by the Council. The offrcers for 1946 are: Presid.ent: PauI F. Kerr, Columbia University, New York City. Vice-Presiilent: S. B. Hendricks, Bureau of Plant Industry, U' S. Department of Agri- culture, Beltsville, Maryland. Suretary: C. S. Hurlbut, Jr., Harvard University, Cambridge, Mass. Treaswer: Earl Ingerson, Geophysical Laboratory, Washington, D' C. Eilitor: Walter F. Hunt, University ol Michigan, Ann Arbor, Michigan. Councilor (1946-a\: Joseph Murdoch, University of California at Los Angeles, Los Angeles, California.