AP Chemistry!!! Summer Assignment Inside This Packer You Will Find A
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Podiform Chromite Deposits—Database and Grade and Tonnage Models
Podiform Chromite Deposits—Database and Grade and Tonnage Models Scientific Investigations Report 2012–5157 U.S. Department of the Interior U.S. Geological Survey COVER View of the abandoned Chrome Concentrating Company mill, opened in 1917, near the No. 5 chromite mine in Del Puerto Canyon, Stanislaus County, California (USGS photograph by Dan Mosier, 1972). Insets show (upper right) specimen of massive chromite ore from the Pillikin mine, El Dorado County, California, and (lower left) specimen showing disseminated layers of chromite in dunite from the No. 5 mine, Stanislaus County, California (USGS photographs by Dan Mosier, 2012). Podiform Chromite Deposits—Database and Grade and Tonnage Models By Dan L. Mosier, Donald A. Singer, Barry C. Moring, and John P. Galloway Scientific Investigations Report 2012-5157 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 This report and any updates to it are available online at: http://pubs.usgs.gov/sir/2012/5157/ For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Mosier, D.L., Singer, D.A., Moring, B.C., and Galloway, J.P., 2012, Podiform chromite deposits—database and grade and tonnage models: U.S. -
Hendrickson SP.Pdf
CHEMISTRY IN THE WORLD THIRD EDITION BY Dr. Kirstin Hendrickson ARIZONA STATE UNIVERSITY Bassim Hamadeh, CEO and Publisher Kassie Graves, Director of Acquisitions Jamie Giganti, Senior Managing Editor Jess Estrella, Senior Graphic Designer Bob Farrell, Senior Field Acquisitions Editor Natalie Lakosil, Licensing Manager Kaela Martin, Allie Kiekhofer, and Rachel Singer, Associate Editors Kat Ragudos, Interior Designer Copyright © 2017 by Cognella, Inc. All rights reserved. No part of this publication may be reprinted, reproduced, transmitted, or utilized in any form or by any electronic, mechanical, or other means, now known or hereafter invented, including photocopying, microfilming, and recording, or in any information retrieval system without the written permission of Cognella, Inc. Trademark Notice: Product or corporate names may be trademarks or registered trademarks, and are used only for identification and explanation without intent to infringe. Cover image copyright © Scott Lefler. copyright © Scott Lefler. copyright © Scott Lefler. copyright © 2011 Depositphotos/Nadezda Razvodovska. Printed in the United States of America ISBN: 978-1-63487-540-0 (pbk) / 978-1-63487-541-7 (br) For my students, from whom I have learned more than I could ever teach. DEDICATION CONTENTS Acknowledgments xi To the Student and the Instructor: xiii How to Use This Book UNIT 1: ALL AROUND US AND INSIDE OF US 1 Chapter 1: Chemistry Is Everywhere 3 1.1 Classifications of Matter 5 1.2 The Periodic Table 12 1.3 Thinking About Chemicals, Chemical 14 Reactions, -
Chromite Crystal Structure and Chemistry Applied As an Exploration Tool
Western University Scholarship@Western Electronic Thesis and Dissertation Repository February 2015 Chromite Crystal Structure and Chemistry applied as an Exploration Tool Patrick H.M. Shepherd The University of Western Ontario Supervisor Dr. Roberta L. Flemming The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Master of Science © Patrick H.M. Shepherd 2015 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geology Commons Recommended Citation Shepherd, Patrick H.M., "Chromite Crystal Structure and Chemistry applied as an Exploration Tool" (2015). Electronic Thesis and Dissertation Repository. 2685. https://ir.lib.uwo.ca/etd/2685 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Western University Scholarship@Western University of Western Ontario - Electronic Thesis and Dissertation Repository Chromite Crystal Structure and Chemistry Applied as an Exploration Tool Patrick H.M. Shepherd Supervisor Roberta Flemming The University of Western Ontario Follow this and additional works at: http://ir.lib.uwo.ca/etd Part of the Geology Commons This Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in University of Western Ontario - Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Chromite Crystal Structure and Chemistry Applied as an Exploration Tool (Thesis format: Integrated Article) by Patrick H.M. -
Spinel Group Minerals in Metamorphosed Ultramafic Rocks from Río De Las Tunas Belt, Central Andes, Argentina
Geologica Acta, Vol.11, Nº 2, June 2013, 133-148 DOI: 10.1344/105.000001836 Available online at www.geologica-acta.com Spinel group minerals in metamorphosed ultramafic rocks from Río de Las Tunas belt, Central Andes, Argentina 1 1 2 M.F. GARGIULO E.A. BJERG A. MOGESSIE 1 INGEOSUR (Universidad Nacional del Sur – CONICET) San Juan 670, B8000ICN Bahía Blanca, Argentina Gargiulo E-mail: [email protected]; [email protected] Bjerg E-mail: [email protected] 2 Institut für Erdwissenschaften, Bereich Mineralogie und Petrologie, Karl-Franzens Universität Graz Universitätsplatz 2, 8010 Graz, Austria E-mail: [email protected] ABS TRACT In the Río de Las Tunas belt, Central Andes of Argentina, spinel group minerals occur in metaperidotites and in reaction zones developed at the boundary between metaperidotite bodies and their country-rocks. They comprise two types: i) Reddish-brown crystals with compositional zonation characterized by a ferritchromite core surrounded by an inner rim of Cr-magnetite and an outer rim of almost pure magnetite. ii) Green crystals chemically homogeneous with spinel (s.s.) and/or pleonaste compositions. The mineral paragenesis Fo+Srp+Cln+Tr+Fe-Chr and Fo+Cln+Tr+Tlc±Ath+Fe-Chr observed in the samples indicate lower and middle grade amphibolite facies metamorphic conditions. Nonetheless, the paragenesis (green)Spl+En+Fo±Di indicates that granulite facies conditions were also reached at a few localities. Cr-magnetite and magnetite rims in zoned reddish-brown crystals and magnetite rims around green-spinel/pleonaste grains are attributed to a later serpentinization process during retrograde metamorphism. -
Toxic Metals in the Environment: the Role of Surfaces
Toxic Metals in the Environment: The Role of Surfaces Donald L. Sparks1 etals are prevalent in the environment. They are derived from both such as density, weight, atomic number, and degree of toxicity natural and anthropogenic sources. Certain metals are essential for (Roberts et al. 2005). Certain met- Mplant growth and for animal and human health. However, if present als and metalloids are essential for in excessive concentrations they become toxic. Metals undergo an array of plant growth and for animal and human health. With respect to biogeochemical processes at reactive natural surfaces, including surfaces of plants, these are referred to as clay minerals, metal oxides and oxyhydroxides, humic substances, plant roots, micronutrients and include B, Cu, and microbes. These processes control the solubility, mobility, bioavailability, Fe, Zn, Mn, and Mo. In addition, and toxicity of metals in the environment. The use of advanced analytical As, Co, Cr, Ni, Se, Sn, and V are essential in animal nutrition. techniques has furthered our understanding of the reactivity and mobility Micronutrients are also referred to of metals in the near-surface environment. as trace elements since they are required in only small quantities, Keywords: critical zone, metals, sorption, surface complexation, biogeochemical processes unlike major nutrients such as N, P, and K. In excess, trace elements INTRODUCTION can be toxic to plants, microbes, animals, and humans. Metals comprise about 75% of the known elements and can Problems also arise when there is a deficiency in essential form alloys with each other and with nonmetals (Morris elements. 1992). Metals have useful properties such as strength, mal- Important trace elements in the environment are As, Ag, B, leability, and conductivity of heat and electricity. -
Chromium(VI) and Oxyanion Remediation of Vadose Zone Soils with Zero Valent Iron (ZVI) and Biological Reduction
UNLV Theses, Dissertations, Professional Papers, and Capstones 5-1-2019 Chromium(VI) and Oxyanion Remediation Of Vadose Zone Soils With Zero Valent Iron (ZVI) and Biological Reduction Nicolas Kim Wong Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Environmental Engineering Commons Repository Citation Wong, Nicolas Kim, "Chromium(VI) and Oxyanion Remediation Of Vadose Zone Soils With Zero Valent Iron (ZVI) and Biological Reduction" (2019). UNLV Theses, Dissertations, Professional Papers, and Capstones. 3703. http://dx.doi.org/10.34917/15778575 This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. CHROMIUM(VI) AND OXYANION REMEDIATION OF VADOSE ZONE SOILS WITH ZERO VALENT IRON (ZVI) AND BIOLOGICAL REDUCTION By Nicolas Wong Bachelor of Science in Engineering – Civil and Environmental Engineering Bachelor of Science – Geology University of Nevada, Las Vegas 2014 A thesis submitted in partial fulfillment of the requirements for the Master of Science in Civil Engineering – Civil and Environmental Engineering Department of Civil and Environmental Engineering and Construction Howard R. -
Carbon and Silicon
INTERCHAPTER M Carbon and Silicon Carbon nanotubes have potential applications ranging from new composites for use in ultralight automobiles and bullet-proof clothing to ultrathin wires. The discovery of carbon nanotubes helped launch the newly emerging field of nanotechnology. University Science Books, ©2011. All rights reserved. www.uscibooks.com M. CARBON AND siLICON M1 Carbon is widely distributed in nature both as the free M-1. Diamond and Graphite Are Allotropic element and in compounds. The great majority of nat- Forms of Carbon urally occurring carbon is found in coal, petroleum, As discussed in Section 15-10, the two most impor- limestone, CaCO3(s), dolomite, MgCa(CO3)2(s), and a few other deposits. Carbon is also a principal ele- tant allotropic forms of solid carbon are diamond ment in all living matter, and the study of its com- and graphite. Recall that diamond has an extended, pounds forms the vast fields of organic chemistry covalently bonded tetrahedral structure and that and biochemistry. Carbon is decidedly nonmetallic, graphite has a layered structure. Because diamond whereas silicon is a semimetal. is the hardest naturally occurring mineral known, it Silicon constitutes 28% of the mass of the earth’s is extensively used as an abrasive and cutting mate- mantle and is the second most abundant element in rial where a very high resistance to wear is required. the mantle, exceeded only by oxygen. Silicon does not Graphite, however, is the stable form of carbon at occur as the free element in nature; it occurs primar- ordinary temperatures and pressures. It exists as a solid at a higher temperature than any other material ily as silicon dioxide, SiO2(s) and in numerous sili- cates. -
Conversion of Chromium Ore Processing Residue to Chrome Steel
Conversion of Chromium Ore Processing Residue to Chrome Steel Final Report Submitted by Dr. Jay N. Meegoda, P.E. Dr. Zhengbo Hu and Dr. Wiwat Kamolpornwijit Dept. of Civil & Environmental Engineering New Jersey Institute of Technology Newark, NJ 07102 For the New Jersey Department of Environmental Protection NJDEP Project Manager: Mr. Robert T. Mueller December 2007 TABLE OF CONTENTS Introduction 1 Literature Search 3 Experimental Program 15 Results and Discussion 23 Summary and Conclusions 42 Acknowledgements 43 References 44 ii Conversion of Chromium Ore Processing Residue to Chrome Steel Introduction Chromium played an important role in the industrial development of New Jersey from 1905 to 1971. During that period, chromate (Cr6+) was produced from chromite ore at three facilities in Hudson County, NJ. During the chromate extraction process, varying amounts of lime and soda ash were added and roasted with pulverized chromite ore to a temperature between 1100ºC and 1150ºC under an oxidizing environment. Trivalent chromium in chromite ore was oxidized to hexavalent chromium. The highly soluble hexavalent chromium was then removed from the COPR (left over Chromium Ore Processing Residue) leaving un-oxidized trivalent chromium and slow-dissolving hexavalent chromium compounds [Burke et al., 1991]. In the absence of information on the toxicity of hexavalent chromium, COPR was subsequently used for the back- filling of demolition sites, preparation for building foundations, construction of tank berms, roadway construction, the filling of wetlands, and other construction and development related purposes. The US Environmental Protection Agency (EPA) has classified hexavalent chromium as a Group A Human Carcinogen. Some forms of hexavalent chromium are water soluble in the full pH range, while trivalent chromium tends to be absorbed onto COPR sample surface or precipitate as chromium hydroxide in slightly acidic and alkaline environment. -
A Cr⁶⁺⁻ Free Extraction of Chromium Oxide from Chromite Ores Using Carbothermic Reduction in the Presence of Alkali
This is a repository copy of A Cr⁶⁺⁻ Free Extraction of Chromium Oxide from Chromite Ores Using Carbothermic Reduction in the Presence of Alkali. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/112637/ Version: Accepted Version Proceedings Paper: Escudero-Castejon, L, Sanchez Segado, S orcid.org/0000-0002-3511-0723, Parirenyatwa, S et al. (2 more authors) (2017) A Cr⁶⁺⁻ Free Extraction of Chromium Oxide from Chromite Ores Using Carbothermic Reduction in the Presence of Alkali. In: Applications of Process Engineering Principles in Materials Processing, Energy and Environmental Technologies, The Minerals, Metals & Materials Series. TMS 2017 146th Annual Meeting & Exhibition, 26 Feb - 02 Mar 2017, San Diego, CA, USA. Springer International , pp. 179-188. ISBN 978-3-319-51090-3 https://doi.org/10.1007/978-3-319-51091-0_16 © The Minerals, Metals & Materials Society 2017. This is an author produced version of a paper published in Applications of Process Engineering Principles in Materials Processing, Energy and Environmental Technologies. Uploaded in accordance with the publisher's self-archiving policy. Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. -
Sd0000029 Evaluation of Chromfte Ore and The
SD0000029 EVALUATION OF CHROMFTE ORE AND THE OPTIMUM METHODS FOR INDUSTRIAL EXTRACTION OF CHROMIUM A TI1HSIS SUBMITTED BY Bakheit Mustafa Mohamed Salih IN CANDIDATURE FOR TIU:DI:GRFJ:OI MASTER OF SC1HNCT DEPARTMENT OF CHEMISTRY FACULTY OF SCIENCE (P.O.BOX 321) OCTOBER 1999 UNIVERSITY OF KHARTOUM 31/ 28 ABSTRACT Samples of chromite ore, collected from Gam and Cheikay mining area (Ingessana Hills) in east Sudan, were analysed to assess the chromium content. Methods for extraction and analysis of chromium metal were developed and established. Analysis were carried out using atomic absorption spectroscopy (AAS) to estimate the contents of chromium, iron, calcium, and magnesium. X-ray fluorescence (XRF) was used to evaluate the levels of chromium, iron, and calcium in the ore. Volumetric analysis was performed to assess chromium and iron, whilst gravimetric analysis was employed to measure the amounts of calcium, magnesium, aluminum and silicon present in the ore. The data was chemically and statistically analyzed to compare the results obtained by the given analytical methods. The results are in good agreement except iron oxide, which displayed a significantly different value when measured by x-ray fluorescence. The data obtained exhibited similarity in almost all cases, when compared with local and global researches, reports, and literature. The study has revealed the average contents of Cr2O3, FeO, CaO, MgO, A12O3, and SiO2 as 40.66. 11.96, 11.94. 0.36. 16.94, 11.45% respectively. MnO and NiO were detected in trace amounts, the corresponding levels in the ore being 72 and 27 ppm. The average chromium content in extracted potassium dichromate measured by using AAS, XRF, and volumetric methods was found to be 31.7%. -
Chemical Element
Федеральное государственное бюджетное образовательное учреждение высшего образования «Иркутский государственный медицинский университет» Министерства здравоохранения Российской Федерации Кафедра иностранных языков с курсами латинского языка и русского как иностранного М.О. Наймушина CHEMICAL ELEMENT Учебное пособие Иркутск ИГМУ 2017 УДК 615.011 (075.8)=111 ББК 24.12я73 Н 12 Рекомендовано ЦКМС ФГБОУ ВО ИГМУ Минздрава России в качестве учебного пособия для обучающихся по основным профессиональным образовательным программам высшего образования по специальности «Фармация», при изучении дисциплины «Иностранный (английский) язык» (протокол № 1 от 12.10.2017) М.О. Наймушина - старший преподаватель кафедры иностранных языков с курсами латинского языка и русского как иностранного ФГБОУ ВО ИГМУ Минздрава России Рецензенты: Е.Г. Горячкина – канд. фарм. наук, доцент кафедры фармакогнозии и ботаники ФГБОУ ВО ИГМУ Минздрава России В.В. Литвиненко - к.филол.н., доцент кафедры общеобразовательных дисциплин Байкальского гуманитарного института Наймушина, М.О. Н 12 Chemical Element: учебное пособие / М.О. Наймушина; ФГБОУ ВО ИГМУ Минздрава России, кафедра иностранных языков с курсами латинского языка и русского как иностранного. – Иркутск: ИГМУ, 2017. – 50 с. Учебное пособие включает в себя сокращенные адаптированные тексты на английском языке, сопровождаемые системой лексико-грамматических упражнений и коммуникативных заданий, предназначено для развития навыков различных видов чтения, перевода, аннотирования статей, а также для развития умений монологического -
The Elements.Pdf
A Periodic Table of the Elements at Los Alamos National Laboratory Los Alamos National Laboratory's Chemistry Division Presents Periodic Table of the Elements A Resource for Elementary, Middle School, and High School Students Click an element for more information: Group** Period 1 18 IA VIIIA 1A 8A 1 2 13 14 15 16 17 2 1 H IIA IIIA IVA VA VIAVIIA He 1.008 2A 3A 4A 5A 6A 7A 4.003 3 4 5 6 7 8 9 10 2 Li Be B C N O F Ne 6.941 9.012 10.81 12.01 14.01 16.00 19.00 20.18 11 12 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 3 Na Mg IIIB IVB VB VIB VIIB ------- VIII IB IIB Al Si P S Cl Ar 22.99 24.31 3B 4B 5B 6B 7B ------- 1B 2B 26.98 28.09 30.97 32.07 35.45 39.95 ------- 8 ------- 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 4 K Ca Sc Ti V Cr Mn Fe Co Ni Cu Zn Ga Ge As Se Br Kr 39.10 40.08 44.96 47.88 50.94 52.00 54.94 55.85 58.47 58.69 63.55 65.39 69.72 72.59 74.92 78.96 79.90 83.80 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 5 Rb Sr Y Zr NbMo Tc Ru Rh PdAgCd In Sn Sb Te I Xe 85.47 87.62 88.91 91.22 92.91 95.94 (98) 101.1 102.9 106.4 107.9 112.4 114.8 118.7 121.8 127.6 126.9 131.3 55 56 57 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 6 Cs Ba La* Hf Ta W Re Os Ir Pt AuHg Tl Pb Bi Po At Rn 132.9 137.3 138.9 178.5 180.9 183.9 186.2 190.2 190.2 195.1 197.0 200.5 204.4 207.2 209.0 (210) (210) (222) 87 88 89 104 105 106 107 108 109 110 111 112 114 116 118 7 Fr Ra Ac~RfDb Sg Bh Hs Mt --- --- --- --- --- --- (223) (226) (227) (257) (260) (263) (262) (265) (266) () () () () () () http://pearl1.lanl.gov/periodic/ (1 of 3) [5/17/2001 4:06:20 PM] A Periodic Table of the Elements at Los Alamos National Laboratory 58 59 60 61 62 63 64 65 66 67 68 69 70 71 Lanthanide Series* Ce Pr NdPmSm Eu Gd TbDyHo Er TmYbLu 140.1 140.9 144.2 (147) 150.4 152.0 157.3 158.9 162.5 164.9 167.3 168.9 173.0 175.0 90 91 92 93 94 95 96 97 98 99 100 101 102 103 Actinide Series~ Th Pa U Np Pu AmCmBk Cf Es FmMdNo Lr 232.0 (231) (238) (237) (242) (243) (247) (247) (249) (254) (253) (256) (254) (257) ** Groups are noted by 3 notation conventions.