Evaluation of the Applicability of Concrete Sludge for the Removal of Cu, Pb, and Zn from Contaminated Aqueous Solutions
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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 -
Revision 1 New Insights Into the Crystal Chemistry of Sauconite (Zn
This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America. The published version is subject to change. Cite as Authors (Year) Title. American Mineralogist, in press. DOI: https://doi.org/10.2138/am-2020-7460. http://www.minsocam.org/ Revision 1 New insights into the crystal chemistry of sauconite (Zn-smectite) from the Skorpion zinc deposit (Namibia) via a multi-methodological approach Emanuela Schingaro1*, Gennaro Ventruti1, Doriana Vinci1, Giuseppina Balassone2, Nicola Mondillo2, Fernando Nieto3, Maria Lacalamita1, Matteo Leoni4,5 1Dipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari Aldo Moro, Via Orabona 4, I-70125, Bari, Italy 2Dipartimento di Scienze della Terra dell’Ambiente e delle Risorse, Università “Federico II”, Complesso Universitario Monte S. Angelo, Via Cintia, I-80126, Napoli, Italy 3Departamento de Mineralogía y Petrología, IACT, Universidad de Granada-CSIC, Av. Fuentenueva s/n, 18002, Granada, Spain 4Saudi Aramco Research and Development Center, P.O. Box 5000, 31311, Dhahran, Saudi Arabia 5Dipartimento di Ingegneria Civile, Ambientale e Meccanica, Università di Trento, Via Mesiano, 77, Trento, 38123, Italy *Corresponding author: Emanuela Schingaro, e-mail: [email protected] RUNNING TITLE: New insights into the crystal chemistry of sauconite 1 Always consult and cite the final, published document. See http:/www.minsocam.org or GeoscienceWorld This is the peer-reviewed, final accepted version for American Mineralogist, -
The Geochemistry and Mobility of Zinc in the Regolith. Advances in Regolith 2003 289
Advances in Regolith 2003 287 THE GEOCHEMISTRY AND MOBILITY OF ZINC IN THE REGOLITH D. C. McPhail1, Edward Summerhayes1, Susan Welch1 & Joël Brugger2 CRC LEME, Department of Geology, Australian National University, Canberra, ACT, 0200 1South Australian Museum and Adelaide University, Adelaide, SA 5000 INTRODUCTION The mobility of zinc in the regolith is important for several reasons, including the weathering of zinc deposits, formation of non-sulphide zinc deposits and contamination of soils and waters from human impact. The mobility of zinc is also important more generally to geologists and geochemists, both exploration and otherwise, because of the need to understand the formation of zinc ore deposits, such as Mississippi Valley Type (MVT), volcanic-hosted massive sulphide (VHMS), zinc oxide and others in which zinc occurs. This means that exploration geochemists, economic geologists and environmental scientists need to understand how zinc exists in the regolith, different lithologies and water, how it is mobilized or trapped, how far it can be transported and whether it is bioavailable and acts as either a micronutrient or a toxin to plant and animal life. In economic geology, there is presently an increasing interest in the formation of zinc oxide, or non- sulphide zinc deposits, and this is reflected in a recent special issue in the journal Economic Geology (Sangster 2003). Although the mobility of zinc in the regolith depends on the transporting process (e.g., groundwater advection or convection, sediment or airborne physical transport, biotic), it depends substantially on the geochemistry of zinc, i.e., how does zinc exist in groundwater and the regolith materials and what are the important geochemical reactions between water and solid. -
Aurichalcite (Zn, Cu)5(CO3)2(OH)6 C 2001-2005 Mineral Data Publishing, Version 1
Aurichalcite (Zn, Cu)5(CO3)2(OH)6 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic, pseudo-orthorhombic by twinning. Point Group: 2/m. As acicular to lathlike crystals with prominent {010}, commonly striated k [001], with wedgelike terminations, to 3 cm. Typically in tufted divergent sprays or spherical aggregates, may be in thick crusts; rarely columnar, laminated or granular. Twinning: Observed in X-ray patterns. Physical Properties: Cleavage: On {010} and {100}, perfect. Tenacity: “Fragile”. Hardness = 1–2 D(meas.) = 3.96 D(calc.) = 3.93–3.94 Optical Properties: Transparent to translucent. Color: Pale green, greenish blue, sky-blue; colorless to pale blue, pale green in transmitted light. Luster: Silky to pearly. Optical Class: Biaxial (–). Pleochroism: Weak; X = colorless; Y = Z = blue-green. Orientation: X = b; Y ' a; Z ' c. Dispersion: r< v; strong. α = 1.654–1.661 β = 1.740–1.749 γ = 1.743–1.756 2V(meas.) = Very small. Cell Data: Space Group: P 21/m. a = 13.82(2) b = 6.419(3) c = 5.29(3) β = 101.04(2)◦ Z=2 X-ray Powder Pattern: Mapim´ı,Mexico. 6.78 (10), 2.61 (8), 3.68 (7), 2.89 (4), 2.72 (4), 1.827 (4), 1.656 (4) Chemistry: (1) CO2 16.22 CuO 19.87 ZnO 54.01 CaO 0.36 H2O 9.93 Total 100.39 (1) Utah; corresponds to (Zn3.63Cu1.37)Σ=5.00(CO3)2(OH)6. Occurrence: In the oxidized zones of copper and zinc deposits. Association: Rosasite, smithsonite, hemimorphite, hydrozincite, malachite, azurite. -
Nickeloan Hydrozincite" a New Variety
MINERALOGICAL MAGAZINE, SEPTEMBER I979, VOL. 43, PP. 397-8 Nickeloan hydrozincite" a new variety A. K. ALWAN AND P. A. WILLIAMS Department of Inorganic Chemistry, University College, PO Box 78, Cardiff CFI IXL, Wales SU M M A R Y. Extensive substitution of Ni for Zn in hydro- specimen are of the order of I mm in thickness and zincite from the Parc Mine, North Wales, has been have a pure white streak. No difficulty was ex- observed. This is the first time that a substantial concen- perienced in obtaining specimens suitable for ana- tration of another transition metal in this mineral has lysis which were free from limonite, which is also been reported. The average composition of the nickeloan present in large quantities in the workings as a hydrozincite is Zn4.63Nio.37(CO3h(OH)6. The relation- ship of this new variety to other secondary carbonate- result of oxidation of the sulphide orebody (Alwan containing nickel minerals is discussed, as is the and Williams, i979). The material obtained was possibility of substitution of other transition metal ions analysed by atomic absorption spectrophotometry, into the hydrozincite lattice. using a Varian AA6 instrument fitted with a carbon rod analyser, after dissolution in Analar| 0.05 mol dm-3HNO3. A summary of the analytical results are given in Table I. Very minor amounts of Cu and DURING the course of a study (Alwan and Fe were found to be present. Concentrations of Co, Williams, I979) on the formation of hydrozincite, Ca, and Mg are less than the detection limit, and A1 Zns(CO3)2(OH)6, from aqueous solution in the was not detected. -
Crystal Structure and Compressibility of Lead Dioxide up to 140 Gpa
American Mineralogist, Volume 99, pages 170–177, 2014 Crystal structure and compressibility of lead dioxide up to 140 GPa BRENT GROCHOLSKI1,*, SANG-HEON SHIM2, ELIZABETH COTTRELL1 AND VITALI B. PRAKAPENKA3 1Department of Mineral Sciences, National Museum of Natural History, Smithsonian Institution, 10th and Constitution Avenue, Washington, D.C. 20560, U.S.A. 2School of Earth and Space Exploration, Arizona State University, 781 S. Terrace Road, Tempe, Arizona 85281 U.S.A. 3Center for Advanced Radiation Sources, University of Chicago, 5640 South Ellis Avenue, Chicago, Illinois 60637, U.S.A. ABSTRACT Lead dioxide is an important silica analog that has high-pressure behavior similar to what has been predicted for silica, only at lower pressures. We have measured the structural evolution and compres- sional behavior of different lead dioxide polymorphs up to 140 GPa in the laser-heated diamond-anvil cell using argon as a pressure medium. High-temperature heating prevents the formation of multi-phase mixtures found in a previous study conducted at room temperature using a silicone grease pressure medium. We find diffraction peaks consistent with a baddeleyite-type phase in our cold-compressed samples between 30 and 40 GPa, which was not observed in the previous measurements. Lead dioxide undergoes a phase transition to a cotunnite-type phase at 24 GPa. This phase remains stable to at least 140 GPa with a bulk modulus of 219(3) GPa for K0′ = 4. Decompression measurements show a pure cotunnite-type phase until 10.5 GPa, where the sample converts to a mixture of baddeleyite-type, pyrite-type, and OI-type (Pbca) phases. -
Thirty-Seventh List of New Mineral Names. Part 1" A-L
Thirty-seventh list of new mineral names. Part 1" A-L A. M. CLARK Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK AND V. D. C. DALTRYt Department of Geology and Mineralogy, University of Natal, Private Bag XO1, Scottsville, Pietermaritzburg 3209, South Africa THE present list is divided into two sections; the pegmatites at Mount Alluaiv, Lovozero section M-Z will follow in the next issue. Those Complex, Kola Peninsula, Russia. names representing valid species, accredited by the Na19(Ca,Mn)6(Ti,Nb)3Si26074C1.H20. Trigonal, IMA Commission on New Minerals and Mineral space group R3m, a 14.046, c 60.60 A, Z = 6. Names, are shown in bold type. Dmeas' 2.76, Dc~ac. 2.78 g/cm3, co 1.618, ~ 1.626. Named for the locality. Abenakiite-(Ce). A.M. McDonald, G.Y. Chat and Altisite. A.P. Khomyakov, G.N. Nechelyustov, G. J.D. Grice. 1994. Can. Min. 32, 843. Poudrette Ferraris and G. Ivalgi, 1994. Zap. Vses. Min. Quarry, Mont Saint-Hilaire, Quebec, Canada. Obschch., 123, 82 [Russian]. Frpm peralkaline Na26REE(SiO3)6(P04)6(C03)6(S02)O. Trigonal, pegmatites at Oleny Stream, SE Khibina alkaline a 16.018, c 19.761 A, Z = 3. Named after the massif, Kola Peninsula, Russia. Monoclinic, a Abenaki Indian tribe. 10.37, b 16.32, c 9.16 ,~, l~ 105.6 ~ Z= 2. Named Abswurmbachite. T. Reinecke, E. Tillmanns and for the chemical elements A1, Ti and Si. H.-J. Bernhardt, 1991. Neues Jahrb. Min. Abh., Ankangite. M. Xiong, Z.-S. -
Mineralization of the Hansonburg Mining District, Bingham, New Mexico John Rakovan and Frederick Partey, 2009, Pp
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/60 Mineralization of the Hansonburg Mining District, Bingham, New Mexico John Rakovan and Frederick Partey, 2009, pp. 387-398 in: Geology of the Chupadera Mesa, Lueth, Virgil; Lucas, Spencer G.; Chamberlin, Richard M.; [eds.], New Mexico Geological Society 60th Annual Fall Field Conference Guidebook, 438 p. This is one of many related papers that were included in the 2009 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
A Specific Gravity Index for Minerats
A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951). -
Crystal Structure, Morphology and Formation Mechanism of a Novel
Crystal structure, morphology and formation mechanism of a novel polymorph of lead dioxide, γ-PbO 2 Hiba Kabbara, Jaafar Ghanbaja, Abdelkrim Redjaïmia, Thierry Belmonte To cite this version: Hiba Kabbara, Jaafar Ghanbaja, Abdelkrim Redjaïmia, Thierry Belmonte. Crystal structure, morphology and formation mechanism of a novel polymorph of lead dioxide, γ-PbO 2. Jour- nal of Applied Crystallography, International Union of Crystallography, 2019, 52 (2), pp.304-311. 10.1107/S1600576719001079. hal-02105360 HAL Id: hal-02105360 https://hal.univ-lorraine.fr/hal-02105360 Submitted on 20 Apr 2019 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. electronic reprint ISSN: 1600-5767 journals.iucr.org/j Crystal structure, morphology and formation mechanism of a novel polymorph of lead dioxide, γ-PbO2 Hiba Kabbara, Jaafar Ghanbaja, Abdelkrim Redja¨ımia and Thierry Belmonte J. Appl. Cryst. (2019). 52, 304–311 IUCr Journals CRYSTALLOGRAPHY JOURNALS ONLINE Copyright c International Union of Crystallography Author(s) of this article may load this reprint on their own web site or institutional repository provided that this cover page is retained. Republication of this article or its storage in electronic databases other than as specified above is not permitted without prior permission in writing from the IUCr. -
Bulletin 65, the Minerals of Franklin and Sterling Hill, New Jersey, 1962
THEMINERALSOF FRANKLINAND STERLINGHILL NEWJERSEY BULLETIN 65 NEW JERSEYGEOLOGICALSURVEY DEPARTMENTOF CONSERVATIONAND ECONOMICDEVELOPMENT NEW JERSEY GEOLOGICAL SURVEY BULLETIN 65 THE MINERALS OF FRANKLIN AND STERLING HILL, NEW JERSEY bY ALBERT S. WILKERSON Professor of Geology Rutgers, The State University of New Jersey STATE OF NEw JERSEY Department of Conservation and Economic Development H. MAT ADAMS, Commissioner Division of Resource Development KE_rr_ H. CR_V_LINCDirector, Bureau of Geology and Topography KEMBLEWIDX_, State Geologist TRENTON, NEW JERSEY --1962-- NEW JERSEY GEOLOGICAL SURVEY NEW JERSEY GEOLOGICAL SURVEY CONTENTS PAGE Introduction ......................................... 5 History of Area ................................... 7 General Geology ................................... 9 Origin of the Ore Deposits .......................... 10 The Rowe Collection ................................ 11 List of 42 Mineral Species and Varieties First Found at Franklin or Sterling Hill .......................... 13 Other Mineral Species and Varieties at Franklin or Sterling Hill ............................................ 14 Tabular Summary of Mineral Discoveries ................. 17 The Luminescent Minerals ............................ 22 Corrections to Franklln-Sterling Hill Mineral List of Dis- credited Species, Incorrect Names, Usages, Spelling and Identification .................................... 23 Description of Minerals: Bementite ......................................... 25 Cahnite ..........................................