Development of Ceramic Uses for Nepheline Syenite

Total Page:16

File Type:pdf, Size:1020Kb

Development of Ceramic Uses for Nepheline Syenite DEVELOPMENT OF CERAMIC USES FOR NEPHELINE SYENITE TAILINGS DISSERTATION Presented In Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Robert Charles Wilson, B. A., M.Sc. The Ohio State University 1958 Approved by Adviser Department of Ceramic Engineering PREFACE The author wishes to express gratitude to his adviser, Dr. J. 0. Everhart, for his help and advice. He also wishes to thank Dr. C. J. Koenig for his suggestions and guidance throughout his graduate career. The author is indebted to the American Nepheline Limited, sponsors of the research program of which this investigation is a part. ii TO MY FATHER AND MOTHER AND MOST ESPECIALLY MY WIFE Hi TABLE OF CONTENTS Pago INTRODUCTION 1 USE OF NEPHELINE SYENITE TAILINGS lu VlTnlFIED CLa Y p i p e b o d i e s Introduction 4 Raviow of Literature 6 Procedure 8 Results 9 Discussion 26 Conclusions 28 USE OF NEPHELINE SYENITE TAILINGS IN VITRIFIED CLAY PIPE GLAZES Introduction 29 Review of Literature 32 Fusibility Tests 34 Cone 3 to 4 Glazes 39 Cone 04 to 03 Glazes 52 Conclusions 58 APPENDIX 64 REFERENCES 66 AUTOEIOGRAPHY 68 iv LIST OF TABLES Number Title Page 1 Chemical Analyses of Body Materials 10 2 Screen Analyses of the Various Grinds of Nepheline Syenite Tailings 11 3 Body Compositicus and Physical Properties for Body A 12 4 Body Compositions and Physical Properties for Body B 15 5 Body Compositions and Physical Properties for Body C 17 6 Body Compositions and Physical Properties for Body D 13 7 Body Compositions and Physical Properties for Body E 2 Q 8 Body Compositions and Physical Properties for Body F 22 9 Body Compositions and Physical Properties for Body G 23 10 Body Compositions and Physical Properties for Body H 25 11 Chemical Analyses of Glaze Materials 3 5 12 Compositions Evaluated for Fusibility by the Inclined Plane Flux Block Test Method 37 13 Molecular Formulae of Cone 4 Glazes 42 14 Batch Formulae of Cone 4 Glazes 43 15 The Effect of Glazes Studied on the Flexural Strength of a Cone 4 Vitrified Clay Pipe Body 44 16 Molecular Formulae of Cone 04 Glazes 53 v LIST OF TABLES (Continued) Number Title Page 17 Batch Formulae of Cone 04 Glazes 54 18 The Effect of Glazes Studied on the Flexural Strength of a Cone 04 Vitrified Clay Pipe Body 55 vi LIST OF ILLUSTRATIONS Figure Subject Page I Thermal expansion curves for body A. Body AC, no additive; body A 6 , 6 per cent addition of coarse-ground nepheline syenite tailings. 59 II Triaxial diagram for the pellet fusion study of B-200 nepheline syenite - talc - Gerstley Borate. 60 III Per cent Flexural Strength changes imparted by cone 4 glazes for firings 1 through V. 61 IV Per cent Flexural Strength changes Imparted by cone 4 glazes for firings VI through X. 62 V Per cent Flexural Strength changes Imparted by cone 04 glazes. 63 vll INTRODUCTION Nepheline syenite is an igneous rock, resembling granite in texture, hardness, and general appearancef1 )• The chief* mineral constituents of the rock are albite { soda feldspar ), mocrocline ( potash feldspar ), and nepheline. The mineral nepheline is higher in alkali and alumina, and lower in silica than either albite or microcline. The mineral nepheline, instead of albite, crystal­ lizes from the magma as a result of an insufficient amount of silica to form albite. The fact that it is " hungry " for silica, so to speak, enhances Its vitrifying activity in ceramic bodies. The fluxing action of nepheline syenite is unique because of the presence of the mineral nepheline. Nepheline, mineralogically, is a sodium aluminum silicate which contains, in the natural mineral, an appreciable amount of potash. An artifically prepared nepheline Is a pure sodium aluminum silicate with the formula f^O'A^O^* 2SIQ2 * The natural nepheline containing potash has the formula K2 0 »3 Na2 0 *4Al2 0 3 *9 SI0 2 . Natural nepheline has a hardness in the Moh's scale of 5.5 to 6 , specific gravity 2.55 to 2.65 and indices of refraction of 1.538 and 1.542. Research and subsequent commercial utilization 1 2 have shown not only that nepheline syenite can be used as a substitute for potash feldspar but that It is superior to feldspar in many respects{2 ). Extensive deposits of nepheline syenite occur In Canada, Russia, and India. In the United States, deposits of nepheline syenite are located in Arkansas, Montana, New Hampshire, New Jersey, and Virginia. Some excellent deposits are located at Blue Mountain, Ontario, and in the vicinity of Bancroft, Ontario, Canada. The Bancroft deposits are higher in nepheline content than the former. The Blue Mountain deposit is a long ridge rising to an elevation of about 350 feet above the surrounding country. The rock of the Blue Mountain central alkaline Intrusive is fine grained, light colored, and of granite-like texture. The solidified mass consists predominantly of the minerals albite, nepheline, and microcline in order of abundance(3). These minerals account for approximately 95 per cent of the rock. Although this deposit Is somewhat variable mineral- ogically, the chemical composition is uniform. When the iron, mostly in the form of magnetite, is removed during processing, a remarkably uniform product is obtained(4,5). Geological surveys have disclosed many million tons of nepheline syenite in the Blue Mountain deposit(6 ). Diamond drilling in the area where mining is now being carried out Indicates a block of about ten million tons. In refining nepheline syenite, it has been found Impracticable to remove the iron from a certain percentage of the rock. Approximately 75 per cent of the ore fed to the processing mill at Nephton, Ontario, is recovered as a low iron content material. This material has found appli­ cation in many branches of ceramics; namely, as a vitrifying agent in whltewares and as a source of alumina in glasses, glazes, and porcelain enamels. The remaining 25 per cent of the ore has about the same chemical composition as the lower Iron content product but contains higher amounts of iron oxides. The high iron content ore is efficiently separated from the lower iron content ore by high intensity magnetic separators. Recently there has been an increased interest by vitrified clay pipe manufacturers in using additives to improve the finished physical and working properties of their pipe bodies, and in developing ceramic glazes to replace salt glazes for their ware. Developments of the use of the higher iron content nepheline syenite ore ( nepheline syenite tailings ) in the aforementioned applications have been the aim of this study. USE OP NEPHELINE SYENITE TAILINGS IN VITRIFIED CLAY PIPE BODIES Introduction The manufacturers of vitrified clay pipe have shown an increased interest in adding low cost additives to their fire clay and shale bodies. Some of the principal improvements sought when experimenting with additives in pipe production are lower absorption to inhibit percolation, higher initial pipe strength and less deterioration in strengths during yard storage, longer firing ranges, and reduced air checking due in part to free silica. The additive investigated here was ground nepheline syenite tailings• In the processing of nepheline syenite, the high iron- bearing product is separated from the low iron-bearing product by high intensity magnetic separators. For efficient high-intensity separation, it is necessary to remove the dust from the head feed to the magnetic separators. Until recent years, the dust varied somewhat in fineness and in iron content. Processing the dust through Sweco screens and Eriez-type magnetic separators now yields a minus 1 0 0 -mesh product with five tenths per cent iron oxide. This product, however, is still not as fine as desired in a body flux. Previous work with nepheline 4 5 syenite as an additive to structural clay bodies has been with this type of material. This study dealt with the minus 30-mesh tailings from the high-intensity separators. These tailings were ground to various degrees of fineness and contained from 2 to 3 per cent of iron oxide. From the standpoint of costs, there are two stipu­ lations which must be met oy materials added to the clays and shales used in making vitrified clay pipe: the activity of the material must be great so that small additions will suffice; and the cost of the material must be low. The ground tailings are a low-cost commodity that can be shipped at a low freight rate because of the relatively high iron content. Information was therefore desired to establish the effect of several percentages of iron oxide and fineness of grind on the fluxing characteristics of nepheline syenite in pipe bodies. Careful consideration was given to the selection of representative pipe bodies. Review of Literature Nepheline syenite has found application in all branches of ceramics. In whitewares, advantage is taken of the low fusion characteristics of nepheline syenite to lower firing temperatures of the various products. This permits savings in fuel, in refractories, and In kiln furniture, and provides a wider color palette for single fire production. In 1939, Chilcote and Koenig{7) Investigated the influence of small additions of the previously described dust by-product, and combinations of this by-product with dolomite, on the physical properties of fire clay and shale brick. It was found that the addition of small amounts lowered the absorption and increased the fired shrinkage and flexural strength. Realizing that some vitrified clay pipe bodies fall to develop a sufficiently low absorption even when fired to the maximum safe temperature, Everhart(8 ) investigated the effect of 17 fluxing materials on such bodies.
Recommended publications
  • 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.
    [Show full text]
  • Minor Elements in Magnetic Concentrates from the Syenite-Shonkinite Province, Southern Asir, Kingdom of Saudi Arabia
    DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Minor elements in Magnetic concentrates from the Syenite-Shonkinite Province, Southern Asir, Kingdom of Saudi Arabia I/ I/ I/ I/ W. C. Overstreet, G. W. Day, Theodore Botinelly, and George Van Trump, Jr. Open-File Report 87 r Report prepared by the U.S. Geological Survey in cooperation with the Deputy Ministry for Mineral Resources, Saudi Arabia This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature, I/ USGS, Retired 2/ USGS, Denver, CO 1987 CONTENTS ABSTRACT............................................................ 1 ACKNOWLEDGMENT...................................................... 1 INTRODUCTION........................................................ 1 Areas covered and previous work................................ 1 Syenite plutons........................................... 3 Jabal Fayfa and Jabal Bani Malik..................... 3 Pluton southeast of Suq al Ithnayn................... 3 Shonkinite pluton at Jabal Atwid..................... 3 Mineral potential......................................... 3 Purpose of present investigation............................... 3 PROCEDURES.......................................................... 10 Collection and preparation of detrital magnetite............... 10 Mineralogical analyses......................................... 10 Semiquantitative spectrographic analyses....................... 11 Method...................................................
    [Show full text]
  • The Forsterite-Anorthite-Albite System at 5 Kb Pressure Kristen Rahilly
    The Forsterite-Anorthite-Albite System at 5 kb Pressure Kristen Rahilly Submitted to the Department of Geosciences of Smith College in partial fulfillment of the requirements for the degree of Bachelor of Arts John B. Brady, Honors Project Advisor Acknowledgements First I would like to thank my advisor John Brady, who patiently taught me all of the experimental techniques for this project. His dedication to advising me through this thesis and throughout my years at Smith has made me strive to be a better geologist. I would like to thank Tony Morse at the University of Massachusetts at Amherst for providing all of the feldspar samples and for his advice on this project. Thank you also to Michael Jercinovic over at UMass for his help with last-minute carbon coating. This project had a number of facets and I got assistance from many different departments at Smith. A big thank you to Greg Young and Dale Renfrow in the Center for Design and Fabrication for patiently helping me prepare and repair the materials needed for experiments. I’m also grateful to Dick Briggs and Judith Wopereis in the Biology Department for all of their help with the SEM and carbon coater. Also, the Engineering Department kindly lent their copy of LabView software for this project. I appreciated the advice from Mike Vollinger within the Geosciences Department as well as his dedication to driving my last three samples over to UMass to be carbon coated. The Smith Tomlinson Fund provided financial support. Finally, I need to thank my family for their support and encouragement as well as my friends here at Smith for keeping this year fun and for keeping me balanced.
    [Show full text]
  • Summary of the Mineral Information Package for the Khanneshin Carbonatite Area of Interest
    Chapter 21A. Summary of the Mineral Information Package for the Khanneshin Carbonatite Area of Interest Contribution by Robert D. Tucker, Harvey E. Belkin, Klaus J. Schulz, Stephen G. Peters, and Kim P. Buttleman Abstract The Khanneshin carbonatite is a deeply dissected igneous complex of Quaternary age that rises approximately 700 meters above the flat-lying Neogene sediments of the Registan Desert, Helmand Province, Afghanistan. The complex consists almost exclusively of carbonate-rich intrusive and extrusive igneous rocks, crudely circular in outline, with only three small hypabyssal plugs of leucite phonolite and leucitite outcropping in the southeastern part of the complex. The complex is broadly divisible into a central intrusive vent (or massif), approximately 4 kilometers in diameter, consisting of coarse-grained sövite and brecciated and agglomeratic barite-ankerite alvikite; a thin marginal zone (less than 1 kilometer wide) of outwardly dipping (5°–45°). Neogene sedimentary strata; and a peripheral apron of volcanic and volcaniclastic strata extending another 3–5 kilometers away from the central intrusive massif. Small satellitic intrusions of biotite-calcite carbonatite, no larger than 400 meters in diameter, crop out on the southern and southeastern margin of the central intrusive massif. In the 1970s several teams of Soviet geologists identified prospective areas of interest for uranium, phosphorus, and light rare earth element (LREE) mineralization in four regions of the carbonatite complex. High uranium concentrations are reported in two regions; the greatest concentrations are confined to silicified shear zones in sandy clay approximately 1.1 kilometers southwest of the peripheral part of the central vent. An area of phosphorus enrichment, primarily occurring in apatite, is present in coarse-grained agglomeratic alvikite, with abundant fenite xenoliths, approximately 750 meters south of the periphery of the central vent.
    [Show full text]
  • Feldspar and Nepheline Syenite 2016
    2016 Minerals Yearbook FELDSPAR AND NEPHELINE SYENITE [ADVANCE RELEASE] U.S. Department of the Interior January 2020 U.S. Geological Survey Feldspar and Nepheline Syenite By Arnold O. Tanner Domestic survey data and tables were prepared by Raymond I. Eldridge III, statistical assistant. In 2016, feldspar production in the United States was representing 46% of the 2016 production tonnages listed in estimated to be 470,000 metric tons (t) valued at $33.1 million, tables 1 and 2. an almost 10% decrease in quantity and a 11% decrease in Feldspar was mined in six States (table 3). North Carolina value compared with 2015 (table 1). Exports of feldspar in 2016 was by far the leading producer State; the remaining five were, decreased by 61% to 5,890 t, valued at $1.5 million, and imports in descending order of estimated output, Virginia, California, of feldspar decreased by 69% to 36,900 t, valued at $3.4 million. Idaho, Oklahoma, and South Dakota. Production was from Imports of nepheline syenite (predominantly from Canada) 10 mines and beneficiating facilities—4 in North Carolina, 2 in increased by 27% to about 572,000 t valued at $73 million. California, and 1 in each of the 4 remaining States (table 3). World production of feldspar in 2016 was 23.4 million metric I-Minerals Inc. continued the mine permitting process for tons (Mt) (tables 1, 7). its Helmer-Bovill project in north-central Idaho; the mine Feldspars, which constitute about 60% of the earth’s crust, would produce potassium feldspar, halloysite, kaolin, and are anhydrous aluminosilicate minerals of two main groupings: quartz.
    [Show full text]
  • Benefits of Utilizing Nepheline Syenite in Porcelain Tile
    1 BENEFITS OF UTILIZING NEPHELINE SYENITE IN PORCELAIN TILE AND SANITARYWARE Anais do 48º Congresso Brasileiro de Cerâmica Proceedings of the 48th Annual Meeting of the Brazilian Ceramic Society 28 de junho a 1º de julho de 2004 – Curitiba-PR SCOTT E. BARTON UNIMIN CORPORATION 500 WILSON PIKE CIRCLE, SUITE 127 BRENTWOOD, TENNESSEE 37027 USA EXECUTIVE SUMMARY Nepheline syenite is a commercially prepared, rare feldspathoid-rich rock product that contributes both potassium and sodium oxides to the ceramic formulation. It has been used in both North America and Europe for the production of porcelain tile and sanitaryware for many years. It is the unique mineralogy and high levels of alkalis of nepheline syenite that justify its use in ceramics. These characteristics promote lower firing temperatures that can enhance productivity and lower production costs. Depending on location, the use of nepheline syenite can lower raw material cost by allowing more silica to be used in the formulation. Additionally, the process control found in most nepheline syenite operations offers a controlled level of Fe2O3 that can help to improve fired color. The goal of this study is to illustrate the practical benefits of using nepheline syenite for the vitrification in a ceramic body formulation. Keywords: nepheline syenite, porcelain, tile, feldspar, sanitaryware INTRODUCTION As the porcelain tile and sanitaryware industries continue to globalize, manufacturers must continually improve the control and quality of their raw materials to effectively compete on the global scale. To do so, many manufacturers must look not only at domestic materials but also at external sources for these important requirements of quality and consistency.
    [Show full text]
  • Controls on Syenite-Hosted Gold Mineralization in the Western Timmins Camp
    Western University Scholarship@Western Electronic Thesis and Dissertation Repository 11-24-2014 12:00 AM Controls on Syenite-Hosted Gold Mineralization in the Western Timmins Camp Robert A. Campbell The University of Western Ontario Supervisor Bob Linnen 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 © Robert A. Campbell 2014 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geology Commons Recommended Citation Campbell, Robert A., "Controls on Syenite-Hosted Gold Mineralization in the Western Timmins Camp" (2014). Electronic Thesis and Dissertation Repository. 2636. https://ir.lib.uwo.ca/etd/2636 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]. Controls on Syenite-Hosted Gold Mineralization in the Western Timmins Camp (Thesis format: Monograph) by Randy Campbell Graduate Program in Earth Sciences A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science The School of Graduate and Postdoctoral Studies The University of Western Ontario London, Ontario, Canada © Randy Campbell 2014 ABSTRACT The Abitibi granite-greenstone belt has long been known for its’ world-class Archean lode gold deposits. While a spatial relationship between felsic intrusions and gold deposits has been noted for some time, it is not clear whether porphyries are genetically related to gold mineralization or just provided a brittle host for unrelated mineralization.
    [Show full text]
  • Multiple Processes of Geochemical Evolution for the Alkaline Rocks Of
    213213 https://doi.org/10.11606/issn.2316-9095.v20-151049 Revista do Instituto de Geociências - USP Geol. USP, Sér. cient., São Paulo, v. 20, n. 4, p. 221-214, Dezembro 2020 Multiple processes of geochemical evolution for the alkaline rocks of Rio Bonito intrusive complex, Rio de Janeiro State, Brazil: 40Ar/39Ar and U-Pb ages and Lu-Hf isotopes on zircon and constraints on crustal signature Múltiplos processos de evolução geoquímica para as rochas alcalinas do complexo intrusivo de Rio Bonito, Estado do Rio de Janeiro, Brasil: idades 40Ar/39Ar e U-Pb e isótopos Lu-Hf em zircão – considerações sobre assinatura crustal Daniel Adelino da Silva1 , Akihisa Motoki1Ϯ, Anderson Costa dos Santos1 , Julio Mendes2 , Fred Jourdan3 , Mauro César Geraldes1 , Cristiano de Carvalho Lana4 2Universidade do Estado do Rio de Janeiro - UERJ, Departamento de Mineralogia e Petrologia Ígnea, Rua São Francisco Xavier, 524, CEP 20550-900, Rio de Janeiro, RJ, BR ([email protected]; [email protected]; [email protected]); Ϯin memoriam. 2Universidade Federal do Rio de Janeiro - UFRJ, Instituto de Geociências, Rio de Janeiro, RJ, BR ([email protected]) 1University of Technology - GPO, Western Australian Argon Isotope Facility, Department of Applied Geology & JdL Centre, Curtin, Perth, Australia ([email protected]) 4Universidade Federal de Ouro Preto - UFOP, Isotope Geochemistry Laboratory, Ouro Preto, MG, BR ([email protected]) Received on October 22, 2028; accepted on November 6, 2020 Abstract This article presents geochemical characteristics of the alkaline rocks of Rio Bonito intrusive complex, State of Rio de Janeiro, Brazil, which is constituted mainly by nepheline syenite.
    [Show full text]
  • Geology of the Saline County Xenolith and Surrounding Area
    A.G.E.S. Brochure Series 005 State of Arkansas Arkansas Geological Survey Bekki White, State Geologist Geology of the Saline County Xenolith and surrounding area By J. Michael Howard Illustrations and photos by Angela Chandler _______________________________________________________ _______________________________________________________ Xenolith – “ a foreign inclusion in an igneous rock.” Glossary of Geology American Geological Institute 1987 (from the Greek words Xenos, meaning guest or stranger, and Lithos, meaning stone.) _______________________________________________________ _______________________________________________________ Introduction Located in Saline County, Arkansas, at the south edge of the community of Bauxite, this natural outcrop of nepheline syenite contains several geologically interesting features, including a xenolith. Sloping west, the outcrop encompasses about one-quarter acre near the center of section 21, Township 2 South, Range 14 West. In early 1990, the Aluminum Company of America (ALCOA) donated the outcrop along with approximately five surrounding acres of land to the Arkansas Geological Commission so that the site can be preserved for educational purposes. Outcrop of nepheline syenite at xenolith locality. History of the site The outcrop and its geologic features were first described by J. Francis Williams in 1891 in The Igneous Rocks of Arkansas, Arkansas Geological Survey Annual Report for 1890, Volume II. Williams discussed the outcrop and xenolith in some detail and included a sketch of the xenolith (see title page). However, for many years the outcrop location remained unknown to most scientists. In the late 2 1960’s employees in the mining division of ALCOA, suspecting that the site was on their property, began a concerted search. Soon afterward the outcrop was rediscovered and was visited by a staff member of the Arkansas Geological Commission, who in turn told Dr.
    [Show full text]
  • Rare Earth Element Mobility During Conversion of Nepheline Syenite Into Lateritic Bauxite at Passa Quatro, Minais Gerais, Brazil B
    Applied Geochemistry, Vol. 9, pp. 701-711,1994 Pergamon Copyright 01994 Elsevier Science Ltd Printed in Great Britain. All rights reserved 0883-2927/94 $7.00+0.00 0883-2927(94)E0025-5 Rare earth element mobility during conversion of nepheline syenite into lateritic bauxite at Passa Quatro, Minais Gerais, Brazil B. BOULANGÉand F. COLÌN- ORSTOM, UM GECO, Laboratoire de Géosciences de l’Environnement, Université Aix Marseille III, 13397 Marseille CBdex 20, France (Received 10 July 1992; accepted in revised form 4 May 1994) Abstract-In a lateritic bauxite formed by weathering of nepheline syenite at Passa Quatro, Minas Gerais State, Brazil, bauxites on the hill-tops directly develop from the syenite bed-rock, while downslope, a kaolinitic layer occurs between bauxite and syenite. A petrological investigation was performed on undisturbed weathered rock samples collected from a representative upslope pit. The undisturbed weathered rocks were chemically analysed for major and trace elements including REE and Zr. Mass balance calculations were applied, and the behaviour of the REE in the Passa Quatro weathering system was established compared to REE reference chondrite and to REE reference parent rock. In the lateritic bauxite, the results suggest that the first stages of weathering induce a volumetric change of 50%, i.e. collapse, with respect to the parent rock, and remove REE with a slightly larger loss of the LREE, except Ce, compared to the HREE. In the upper layers, where bauxite is more mature, a net mass gain in REE is observed relative to the underlying layers. This gain takes place during the reduction of the upper layer during the downward progression of the weathering front.
    [Show full text]
  • Part 629 – Glossary of Landform and Geologic Terms
    Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition.
    [Show full text]
  • Rhyolite and Trachyte Formation at Lake City Caldera: Insight from Quantitative Textural and Geochemical Analyses
    Michigan Technological University Digital Commons @ Michigan Tech Dissertations, Master's Theses and Master's Reports 2016 Rhyolite and Trachyte Formation at Lake City Caldera: Insight from Quantitative Textural and Geochemical Analyses Jordan Lubbers Michigan Technological University, [email protected] Copyright 2016 Jordan Lubbers Recommended Citation Lubbers, Jordan, "Rhyolite and Trachyte Formation at Lake City Caldera: Insight from Quantitative Textural and Geochemical Analyses", Open Access Master's Thesis, Michigan Technological University, 2016. https://doi.org/10.37099/mtu.dc.etdr/99 Follow this and additional works at: https://digitalcommons.mtu.edu/etdr Part of the Geochemistry Commons, and the Geology Commons RHYOLITE AND TRACHYTE FORMATION AT LAKE CITY CALDERA: INSIGHT FROM QUANTITATIVE TEXTURAL AND GEOCHEMICAL ANALYSES By Jordan E. Lubbers A THESIS Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE In Geology MICHIGAN TECHNOLOGICAL UNIVERSITY 2016 © 2016 Jordan E. Lubbers This thesis has been approved in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE in Geology. Geological and Mining Engineering and Sciences ThesisDepartment Advisor: ofChad Deering Committee Member: Olivier Bachmann Committee Member: William Rose Department Chair: John Gierke Table of Contents Acknowledgements ................................................................................................................................................. 6 Abstract ......................................................................................................................................................................
    [Show full text]