Fibroferrite: Crystallographic, Optical And
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Download PDF About Minerals Sorted by Mineral Name
MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky. -
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 -
Raman Spectroscopy of Efflorescent
ASTROBIOLOGY Volume 13, Number 3, 2013 ª Mary Ann Liebert, Inc. DOI: 10.1089/ast.2012.0908 Raman Spectroscopy of Efflorescent Sulfate Salts from Iron Mountain Mine Superfund Site, California Pablo Sobron1 and Charles N. Alpers2 Abstract The Iron Mountain Mine Superfund Site near Redding, California, is a massive sulfide ore deposit that was mined for iron, silver, gold, copper, zinc, and pyrite intermittently for nearly 100 years. As a result, both water and air reached the sulfide deposits deep within the mountain, producing acid mine drainage consisting of sulfuric acid and heavy metals from the ore. Particularly, the drainage water from the Richmond Mine at Iron Mountain is among the most acidic waters naturally found on Earth. The mineralogy at Iron Mountain can serve as a proxy for understanding sulfate formation on Mars. Selected sulfate efflorescent salts from Iron Mountain, formed from extremely acidic waters via drainage from sulfide mining, have been characterized by means of Raman spectroscopy. Gypsum, ferricopiapite, copiapite, melanterite, coquimbite, and voltaite are found within the samples. This work has implications for Mars mineralogical and geochemical investigations as well as for terrestrial environmental investigations related to acid mine drainage contamination. Key Words: Acid mine drainage—Efflorescent sulfate minerals—Mars analogue—Iron Mountain—Laser Raman spectroscopy. Astro- biology 13, 270–278. 1. Introduction efflorescent sulfate minerals. This reconnaissance sampling resulted in characterization of the extremely acidic mine ron Mountain, California, is the host of massive sulfide waters (pH values from - 3.6 to + 0.5) and a variety of iron- Ideposits that were mined for copper, zinc, gold, silver, and sulfate efflorescent salts (Nordstrom and Alpers, 1999; pyrite (for sulfuric acid) between the early 1860s and the early Nordstrom et al., 2000). -
World Reference Base for Soil Resources 2014 International Soil Classification System for Naming Soils and Creating Legends for Soil Maps
ISSN 0532-0488 WORLD SOIL RESOURCES REPORTS 106 World reference base for soil resources 2014 International soil classification system for naming soils and creating legends for soil maps Update 2015 Cover photographs (left to right): Ekranic Technosol – Austria (©Erika Michéli) Reductaquic Cryosol – Russia (©Maria Gerasimova) Ferralic Nitisol – Australia (©Ben Harms) Pellic Vertisol – Bulgaria (©Erika Michéli) Albic Podzol – Czech Republic (©Erika Michéli) Hypercalcic Kastanozem – Mexico (©Carlos Cruz Gaistardo) Stagnic Luvisol – South Africa (©Márta Fuchs) Copies of FAO publications can be requested from: SALES AND MARKETING GROUP Information Division Food and Agriculture Organization of the United Nations Viale delle Terme di Caracalla 00100 Rome, Italy E-mail: [email protected] Fax: (+39) 06 57053360 Web site: http://www.fao.org WORLD SOIL World reference base RESOURCES REPORTS for soil resources 2014 106 International soil classification system for naming soils and creating legends for soil maps Update 2015 FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2015 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. -
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(?), -
Sodium Sulphate: Its Sources and Uses
DEPARTMENT OF THE INTERIOR HUBERT WORK, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 717 SODIUM SULPHATE: ITS SOURCES AND USES BY ROGER C. WELLS WASHINGTON GOVERNMENT PRINTING OFFICE 1 923 - , - _, v \ w , s O ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PBOCUKED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 5 CENTS PEE COPY PURCHASER AGREES NOT TO RESELL OR DISTRIBUTE THIS COPY FOR PROFIT. PUB. RES. 57, APPROVED MAY 11, 1922 CONTENTS. Page. Introduction ____ _____ ________________ 1 Demand 1 Forms ____ __ __ _. 1 Uses . 1 Mineralogy of principal compounds of sodium sulphate _ 2 Mirabilite_________________________________ 2 Thenardite__ __ _______________ _______. 2 Aphthitalite_______________________________ 3 Bloedite __ __ _________________. 3 Glauberite ____________ _______________________. 4- Hanksite __ ______ ______ ___________ 4 Miscellaneous minerals _ __________ ______ 5 Solubility of sodium sulphate *.___. 5 . Transition temperature of sodium sulphate______ ___________ 6 Reciprocal salt pair, sodium sulphate and potassium chloride____ 7 Relations at 0° C___________________________ 8 Relations at 25° C__________________________. 9 Relations at 50° C__________________________. 10 Relations at 75° and 100° C_____________________ 11 Salt cake__________ _.____________ __ 13 Glauber's salt 15 Niter cake_ __ ____ ______ 16 Natural sodium sulphate _____ _ _ __ 17 Origin_____________________________________ 17 Deposits __ ______ _______________ 18 Arizona . 18 -
Jerzdissertation.Pdf (5.247Mb)
Geochemical Reactions in Unsaturated Mine Wastes Jeanette K. Jerz Dissertation submitted to the Faculty of the Virginia Polytechnic Institute and State University in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geological Sciences Committee in charge: J. Donald Rimstidt, Chair James R. Craig W. Lee Daniels Patricia Dove D. Kirk Nordstrom April 22, 2002 Blacksburg, Virginia Keywords: Acid Mine Drainage, Pyrite, Oxidation Rate, Efflorescent Sulfate Salt, Paragenesis, Copyright 2002, Jeanette K. Jerz GEOCHEMICAL REACTIONS IN UNSATURATED MINE WASTES JEANETTE K. JERZ ABSTRACT Although mining is essential to life in our modern society, it generates huge amounts of waste that can lead to acid mine drainage (AMD). Most of these mine wastes occur as large piles that are open to the atmosphere so that air and water vapor can circulate through them. This study addresses the reactions and transformations of the minerals that occur in humid air in the pore spaces in the waste piles. The rate of pyrite oxidation in moist air was determined by measuring over time the change in pressure between a sealed chamber containing pyrite plus oxygen and a control. The experiments carried out at 25˚C, 96.8% fixed relative humidity, and oxygen partial pressures of 0.21, 0.61, and 1.00 showed that the rate of oxygen consumption is a function of oxygen partial pressure and time. The rates of oxygen consumption fit the expression dn −− O2 = 10 648...Pt 05 05. dt O2 It appears that the rate slows with time because a thin layer of ferrous sulfate + sulfuric acid solution grows on pyrite and retards oxygen transport to the pyrite surface. -
Efflorescent Iron Sulfate Minerals: Paragenesis, Relative Stability, and Environmental Impact
American Mineralogist, Volume 88, pages 1919–1932, 2003 Efflorescent iron sulfate minerals: Paragenesis, relative stability, and environmental impact JEANETTE K. JERZ* AND J. DONALD RIMSTIDT Department of Geological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, Virginia 24061, U.S.A. ABSTRACT This study of a pyrrhotite-dominated massive sulfide deposit in the Blue Ridge province in south- western Virginia shows that sulfate minerals formed by the oxidation of the pyrrhotite transform from one to another by a combination of oxidation, dehydration, and neutralization reactions. Significant quantities of sulfate minerals occur in the underground adits (Area I) and under overhangs along the high sidewall of the adjoining open pit (Area II). Samples from this site were analyzed to determine mineralogy, equilibrium relative humidity, chemical composition, and acid generation potential. In Area I, pyrrhotite oxidizes to marcasite + melanterite, which eventually oxidizes to melanterite + sul- furic acid. Melanterite is extruded from the rocks as a result of the volume change associated with this reaction. It accumulates in piles where halotrichite, copiapite, and fibroferrite form. In Area II, FeSO4 solutions produced by pyrrhotite oxidation migrate to the exposed pit face, where they evaporate to form melanterite. The melanterite rapidly dehydrates to form rozenite, which falls into a pile at the base of the wall, where melanterite, copiapite, and halotrichite are present. The observed paragenesis a a can be understood using a log O2 – log H2O diagram that we developed from published thermody- namic data and observations of coexisting phases. Dissolution experiments showed that fibroferrite-rich samples had the highest acid producing po- tential, followed by copiapite-rich samples and then halotrichite-rich samples. -
New Insights on Secondary Minerals from Italian Sulfuric Acid Caves Ilenia M
International Journal of Speleology 47 (3) 271-291 Tampa, FL (USA) September 2018 Available online at scholarcommons.usf.edu/ijs International Journal of Speleology Off icial Journal of Union Internationale de Spéléologie New insights on secondary minerals from Italian sulfuric acid caves Ilenia M. D’Angeli1*, Cristina Carbone2, Maria Nagostinis1, Mario Parise3, Marco Vattano4, Giuliana Madonia4, and Jo De Waele1 1Department of Biological, Geological and Environmental Sciences, University of Bologna, Via Zamboni 67, 40126 Bologna, Italy 2DISTAV, Department of Geological, Environmental and Biological Sciences, University of Genoa, Corso Europa 26, 16132 Genova, Italy 3Department of Geological and Environmental Sciences, University of Bari Aldo Moro, Piazza Umberto I 1, 70121 Bari, Italy 4Department of Earth and Marine Sciences, University of Palermo, Via Archirafi 22, 90123 Palermo, Italy Abstract: Sulfuric acid minerals are important clues to identify the speleogenetic phases of hypogene caves. Italy hosts ~25% of the known worldwide sulfuric acid speleogenetic (SAS) systems, including the famous well-studied Frasassi, Monte Cucco, and Acquasanta Terme caves. Nevertheless, other underground environments have been analyzed, and interesting mineralogical assemblages were found associated with peculiar geomorphological features such as cupolas, replacement pockets, feeders, sulfuric notches, and sub-horizontal levels. In this paper, we focused on 15 cave systems located along the Apennine Chain, in Apulia, in Sicily, and in Sardinia, where copious SAS minerals were observed. Some of the studied systems (e.g., Porretta Terme, Capo Palinuro, Cassano allo Ionio, Cerchiara di Calabria, Santa Cesarea Terme) are still active, and mainly used as spas for human treatments. The most interesting and diversified mineralogical associations have been documented in Monte Cucco (Umbria) and Cavallone-Bove (Abruzzo) caves, in which the common gypsum is associated with alunite-jarosite minerals, but also with baryte, celestine, fluorite, and authigenic rutile-ilmenite-titanite. -
Alphabetical List
LIST L - MINERALS - ALPHABETICAL LIST Specific mineral Group name Specific mineral Group name acanthite sulfides asbolite oxides accessory minerals astrophyllite chain silicates actinolite clinoamphibole atacamite chlorides adamite arsenates augite clinopyroxene adularia alkali feldspar austinite arsenates aegirine clinopyroxene autunite phosphates aegirine-augite clinopyroxene awaruite alloys aenigmatite aenigmatite group axinite group sorosilicates aeschynite niobates azurite carbonates agate silica minerals babingtonite rhodonite group aikinite sulfides baddeleyite oxides akaganeite oxides barbosalite phosphates akermanite melilite group barite sulfates alabandite sulfides barium feldspar feldspar group alabaster barium silicates silicates albite plagioclase barylite sorosilicates alexandrite oxides bassanite sulfates allanite epidote group bastnaesite carbonates and fluorides alloclasite sulfides bavenite chain silicates allophane clay minerals bayerite oxides almandine garnet group beidellite clay minerals alpha quartz silica minerals beraunite phosphates alstonite carbonates berndtite sulfides altaite tellurides berryite sulfosalts alum sulfates berthierine serpentine group aluminum hydroxides oxides bertrandite sorosilicates aluminum oxides oxides beryl ring silicates alumohydrocalcite carbonates betafite niobates and tantalates alunite sulfates betekhtinite sulfides amazonite alkali feldspar beudantite arsenates and sulfates amber organic minerals bideauxite chlorides and fluorides amblygonite phosphates biotite mica group amethyst -
Magnesiocopiapite Mgfe4 (SO4)6(OH)2 20H2O C 2001-2005 Mineral Data Publishing, Version 1
3+ • Magnesiocopiapite MgFe4 (SO4)6(OH)2 20H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Triclinic. Point Group: 1. As scaly crystals, to several mm, commonly as efflorescences. Physical Properties: Cleavage: [On {010}, perfect.] (by analogy to copiapite group members). Hardness = [2–3] D(meas.) = n.d. D(calc.) = 2.16 Optical Properties: Semitransparent. Color: Lemon-yellow, orange, greenish yellow. Optical Class: Biaxial (+). Pleochroism: Y = colorless; Z = greenish yellow. α = 1.507–1.510 β = 1.529–1.535 γ = 1.575–1.585 2V(meas.) = Moderate. 2V(calc.) = 67◦ Cell Data: Space Group: P 1. a = 7.335–7.35 b = 18.782–18.84 c = 7.377–7.39 α =91.23◦−91.7◦ β = 102.17◦−102.6◦ γ =98.79◦−99.0◦ Z=1 X-ray Powder Pattern: Knoxville, California, USA. 9.29 (100), 18.57 (90), 5.600 (80), 3.588 (50), 6.192 (45), 4.208 (40), 3.506 (40) Chemistry: (1) (2) (3) SO3 39.47 39.90 39.43 Al2O3 3.17 Fe2O3 27.44 23.58 26.21 FeO 0.52 0.17 CoO 0.16 CuO 0.15 MgO 3.26 1.97 3.31 H2O 27.84 30.90 31.05 insol. 1.16 Total 99.69 [100.00] 100.00 (1) Near Blythe, California, USA. (2) Forty Mile River, Alaska, USA; recalculated to 100% from an original total of 99.68% after deduction of remnant 1.40%; corresponds 2+ 3+ • to (Mg0.59Al0.30Fe0.03Co0.03Cu0.02)Σ=0.97(Fe3.56Al0.44)Σ=4.00(SO4)6(OH)2 19.7H2O. -
Dictionary of Geology and Mineralogy
McGraw-Hill Dictionary of Geology and Mineralogy Second Edition McGraw-Hill New York Chicago San Francisco Lisbon London Madrid Mexico City Milan New Delhi San Juan Seoul Singapore Sydney Toronto All text in the dictionary was published previously in the McGRAW-HILL DICTIONARY OF SCIENTIFIC AND TECHNICAL TERMS, Sixth Edition, copyright ᭧ 2003 by The McGraw-Hill Companies, Inc. All rights reserved. McGRAW-HILL DICTIONARY OF GEOLOGY AND MINERALOGY, Second Edi- tion, copyright ᭧ 2003 by The McGraw-Hill Companies, Inc. All rights reserved. Printed in the United States of America. Except as permitted under the United States Copyright Act of 1976, no part of this publication may be reproduced or distributed in any form or by any means, or stored in a database or retrieval system, without the prior written permission of the publisher. 1234567890 DOC/DOC 09876543 ISBN 0-07-141044-9 This book is printed on recycled, acid-free paper containing a mini- mum of 50% recycled, de-inked fiber. This book was set in Helvetica Bold and Novarese Book by the Clarinda Company, Clarinda, Iowa. It was printed and bound by RR Donnelley, The Lakeside Press. McGraw-Hill books are available at special quantity discounts to use as premi- ums and sales promotions, or for use in corporate training programs. For more information, please write to the Director of Special Sales, McGraw-Hill, Professional Publishing, Two Penn Plaza, New York, NY 10121-2298. Or contact your local bookstore. Library of Congress Cataloging-in-Publication Data McGraw-Hill dictionary of geology and mineralogy — 2nd. ed. p. cm. “All text in this dictionary was published previously in the McGraw-Hill dictionary of scientific and technical terms, sixth edition, —T.p.