Minerals of the Montmorillonite Group Their Origin and Relation to Soils and Clays

Total Page:16

File Type:pdf, Size:1020Kb

Minerals of the Montmorillonite Group Their Origin and Relation to Soils and Clays If yon no longer need this publication write to the Geological Survey in Washington for an official mailing label to use in returning it UNITED STATES DEPARTMENT OF THE INTERIOR MINERALS OF THE MONTMORILLONITE GROUP THEIR ORIGIN AND RELATION TO SOILS AND CLAYS GEOLOGICAL SURVEY PROFESSIONAL PAPER 205-B UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Professional Paper 205-B MINERALS OF THE MONTMORILLONITE GROUP THEIR ORIGIN AND RELATION TO SOILS AND CLAYS BY CLARENCE S. ROSS AND STERLING B. HENDRICKS Shorter contributions to general geology, 1943-44 (Pages 23-79) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1945 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 55 cents CONTENTS Page Page Abstract............. ........................... 23 Mineralogy of the montmorillonite group—Continued. Introduction.......... ............................ 23 Derivation of formulas—Continued. Methods of study. ........................... 24 Saponite-hectorite series...................... 46 Previous work.... ........................... 24 Suggested formulas........................... 47 Acknowledgments. ........................... 25 Thermal studies...................................... 48 Nomenclature........ ........................... 25 Essential hydroxyl............................... 48 Montmorillonite.. ........................... 25 Interlayer water................................. 52 Beidellite........ ........................... 26 Optical properties.................................... 54 Saponite........................................ 26 Methods of determination......................... 54 Hectorite....................................... 27 Determinations of indices of refraction.............. 55 Nontronite...................................... 27 Pleochroism..................................... 57 Volchonskoite................................... 28 Electron-microscope photographs....................... 57 Kaolin minerals.................................. 28 Synthesis........................................... 58 Hydrous micas (illite)............................ 28 Origin and mode of occurrence................ ..... 60 Mixed-layer minerals................................. 29 General features........................ ..... 60 Crystal structure..................................... 29 Soils and rock weathering................ ..... 61 Location and description of analyzed-clays.............. 30 Discussion......................... ..... 61 Montmorillonite-beidellite series................... 30 Australian soils..................... ..... 62 Nontronites..................................... 32 Piedmont soils...................... ..... 62 Samples from soils and chromium-bearing samples... 32 Java soils.......................... ..... 63 Saponite-hectorite series .......................... 32 Glacial soils........................ ..... 63 Samples containing silica or an iron-bearing impurity 32 Summary of soils and rock weathering. ..... 64 Chemical analyses.................................... 34 Bentonites............................. ..... 64 Impurities in clays................................... 36 Structure of parent glass............. ..... 64 Minor constituents................................... 37 Physical properties........................... 65 Base exchange....................................... 37 Definition........................... ..... : . 65 Physical chemistry of base exchange................ 37 Mode of occurrence.......................... 65 Determinations of exchangeable bases.............. 38 Ordovician bentonite......................... 67 Mineralogy of the montmorillonite group................ 39 Volcanic materials at Magnet Cove, Ark............ 67 General relations................................. 39 Methods of calculation of mineral formulas.......... 41 Clays of the geyser region in Yellowstone Park...... 68 Derivation of formulas............................ 44 Vein and gouge clays............................. 69 Montmorillonite-beidellite series............... 44 Pyrophyllite and talc................................. 70 Nontronite.................................. 45 Bibliography........................................ 72 Montmorillonite-beidellite-nontronite series...... 46 Index............................................... 79 Ill IV CONTENTS ILLUSTRATIONS Page PLATE 1. Alteration of volcanic materials to montmorillonite and kaolinite............................................ 58 2. A, B, and C, Alteration of volcanic materials to montmorillonite and kaolinite; D, Varved sedimentary clay...... 58 3. A, Bentonite showing volcanic-ash structure; B, Vein clay with clay-filled joint cracks; C, Granite gneiss with plagi-v clase altered to beidellite; D, Plagioclase phenocryst in rhyolite partly altered to montmorillonite.............. 58 4. Bentonite showing volcanic-ash structure................................................................. 58 5. Alteration of various rock types to montmorillonite and associated minerals.................................. 58 6. Magnesium and iron-rich clays.......................................................................... 58 7. A, Beidellite replacement of molluscan shell; B, Montmorillonite from pegmatite; C and D, Electron micrograpl "" of clays............................................................................................ 58 8. Electron micrographs of hectorite and nontronite.......................................................... 58 FIGURE 5, 6, and 7. Dehydration curves of montmorillonite clays..................................................... 49-51 8. Curves showing relation of vapor pressure to cleavage spacing in montmorillonite............................. 53 9. Curves showing relation of indices of refraction to ferric iron in minerals of the montmorillonite-nontronite'series 56 TABLES Page TABLE 1. Analyses of montmorillonite-beidellite series.............................................................. 34 2. Analyses of nontronite................................................................................. 35 3. Analyses of samples from soils and chromium-bearing specimens from Russia................................. 35 4. Analyses of hectorite and saponite....................................................................... 35 5. Analyses of samples containing excess silica............................................................... 35 6. Analyses of nontronites containing an iron-bearing impurity................................................ 35 7. Analyses of specimens containing chlorite, vermiculite, or other iron-bearing impurity.......................... 35 8. Analyses of hectorite and a clay from Amargosa Valley before and after treatment with ammonium acetate...... 38 9. Base-exchange capacities of some montmorillonite clays.................................................... 39 10. Relation of ions to crystal structure..................................................................... 42 11. Calculations of impurities in representative clays.......................................................... 43 12. Proportions of end members in selected samples........................................................... 46 13. Indices of refraction and birefringence as affected by the presence of ferric iron in the montmorillonite-nontroni^e series.............................................................................................. 55 14. Indices of refraction of clays determined on films.......................................................... 57 15. Indices of refraction determined on clay grains............................................................ 57 16. Indices of refraction of minerals related to the montmorillonite group........................................ 57 17. Indices of refraction of clays dehydrated at 210° C......................................................... 57 18. Conditions of synthesis for hydrous aluminum silicates..................................................... 59 19. Analyses of bentonite and related rocks, Santa Monica Mountains, Calif...................................... 66 20. Analyses of pyrophyllite and talc...................................................................... 70 MINERALS OF THE MONTMORILLONITE GROUP THEIR ORIGIN AND RELATION TO SOILS AND CLAYS By CLARENCE S. Ross, Geological Survey, United States Department of the Interior, and STERLING B. HEN- DRICKS, Bureau of Plant Industry, Soils, and Agricultural Engineering, United States Department of Agriculture. ABSTRACT A detailed study has been made of the montmorillonite group but potassium, magnesium, hydrogen, and aluminum may be of clay minerals, one of the most widely occurring of all mineral exchangeable. materials. Minerals of this group are exceedingly fine grained crystalline aggregates, and they present an unusually wide range The composition and mineral relations of the clay minerals are in composition. Essential information on the group was obtained intimately related to the conditions under which they form. In only after study, by all available mineralogical methods, of more general, alkalic feldspars and the micas tend to alter to kaolin than 100 carefully selected specimens. This information has minerals, whereas ferromagnesian minerals, calcic feldspar?, and made possible the determination of the limits of variation in com­ volcanic glasses commonly alter to members
Recommended publications
  • High Dose Dosimetry Using Antigorite-Teflon Composite
    2011 International Nuclear Atlantic Conference - INAC 2011 Belo Horizonte,MG, Brazil, October 24-28, 2011 ASSOCIAÇÃO BRASILEIRA DE ENERGIA NUCLEAR - ABEN ISBN: 978-85-99141-04-5 HIGH DOSE DOSIMETRY USING ANTIGORITE-TEFLON COMPOSITE René R. Rocca 1, Sonia H. Tatumi 2 and Shigueo Watanabe 1 1 Instituto de Física Universidade de São Paulo Rua do Matão 187 – Travessa R. 05508-090 Butantã, SP [email protected][email protected] 2 Faculdade de Tecnologia de São Paulo CEETESP Pça. Cel. Fernando Prestes - Bom retiro, 30 01124-060 São Paulo, SP [email protected] ABSTRACT Pellets of antigorite crystals (Mg 3-x [Si 2O5] (OH) 4-2x ) and teflon powder were obtained in order to investigate the thermoluminescence (TL) dosimetric characteristics. ICP analysis was performed showing the presence of 0.25 mol% of Fe 2O3, 0.07 mol% of Al 2O3 and 0.006 mol% of MnO impurities. These pellets show two prominent TL peaks at 150 oC and another broad one at 250 oC observed in samples previously irradiated with gamma-rays from 60 Co source. The 150 oC peak increased up to 2 kGy and after this dose the intensity reaches a maximum then decreases gradually. However the 250 oC peak increased up even with a dose of 172 kGy. A good reproducibility of TL results was obtained showing that these pellets can be used for high dose measurements. An excellent theoretical fit using second order kinects model [10] was obtained for all the peaks; however the theoretical deconvolution [4] showed the presence of two additional peaks at 206 and 316 oC.
    [Show full text]
  • Characterization of Clays and Clay Minerals for Industrial Applications: Substitution Non-Natural Additives by Clays in UV Protection
    Characterization of Clays and Clay Minerals for Industrial Applications: Substitution non-Natural Additives by Clays in UV Protection Dissertation in fulfilment of the academic grade doctor rerum naturalium (Dr. rer. nat.) at the Faculty of Mathematics and Natural Sciences Ernst-Moritz-Arndt-University Greifswald HOANG-MINH Thao (Hoàng Thị Minh Thảo) born on 01.6.1979 in Quang Ninh, Vietnam Greifswald, Germany - 2006 Dekan: Prof. Dr. Klaus Fesser 1. Gutachter: PD. Dr. habil. Jörn Kasbohm 2. Gutachter: Prof. Roland Pusch Tag der Promotion: 17.11.2006 ii CONTENTS LIST OF TABLES . vi LIST OF FIGURES. vii ABBREVIATIONS . x STATEMENT OF ORIGINAL AUTHORSHIP (ERKLÄRUNG). xi ACKNOWLEDGMENTS . xii 1 INTRODUCTION . 1 2 POSSIBLE FUNCTIONS OF CLAYS, CLAY MINERALS IN UV PROTECTION . 2 2.1 Clays, clay minerals and sustainability in geosciences. 2 2.2 Ultraviolet radiation and human skin . 2 2.3 Actual substances as UV protection factor and their problems. 5 2.4 Pharmacy requirement in suncreams. 9 2.5 Clays, clay minerals and their application for human health. 11 2.6 Possible functions of clays, clay minerals in UV protection cream. 13 3 METHODOLOGY . 15 3.1 Clays and clay minerals analyses. 15 3.1.1 X-Ray diffraction. 17 3.1.2 TEM-EDX. 19 3.1.3 X-Ray fluorescence. 22 3.1.4 Mössbauer spectroscopy. 23 3.1.5 Atterberg sedimentation. 23 3.1.6 Dithionite treatment. 24 3.2 Non-clay samples analyses. 24 3.2.1 UV-measurement. 25 3.2.2 Light microscopy. 27 3.2.3 Skin model test by mouse-ear in vivo .
    [Show full text]
  • Washington State Minerals Checklist
    Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite
    [Show full text]
  • First-Principles Modeling of the Infrared Spectrum of Antigorite
    Eur. J. Mineral., 33, 389–400, 2021 https://doi.org/10.5194/ejm-33-389-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. First-principles modeling of the infrared spectrum of antigorite Etienne Balan1, Emmanuel Fritsch1,2, Guillaume Radtke1, Lorenzo Paulatto1, Farid Juillot1,2, and Sabine Petit3 1Sorbonne Université, CNRS, MNHN, Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie (IMPMC), 4 place Jussieu, 75252 Paris CEDEX 05, France 2Institut de Recherche pour le Développement (IRD), Centre de Nouméa, 101 Promenade Roger Laroque, Anse Vata, 98848 Nouméa, New Caledonia 3Institut de Chimie des Milieux et Matériaux de Poitiers (IC2MP), CNRS UMR 7285, Université de Poitiers, 6 rue Michel Brunet, 86073, Poitiers CEDEX 9, France Correspondence: Etienne Balan ([email protected]) Received: 22 March 2021 – Revised: 14 June 2021 – Accepted: 22 June 2021 – Published: 19 July 2021 Abstract. The infrared absorption spectrum of a natural antigorite sample from New Caledonia is compared to its theoretical counterpart computed for the pristine antigorite m D 17 polysome within the density functional perturbation theory framework. The theoretical model reproduces most of the bands related to Si-O stretching −1 −1 in the 800–1300 cm range, OH libration, hindered OH translation and SiO4 bending in the 400–800 cm range, and OH stretching in the 3500–3700 cm−1 range. Most of the observed bands have a composite nature involving several vibrational modes contributing to their intensity, except the apical and one of the basal Si-O stretching bands whose intensity is carried by a single mode.
    [Show full text]
  • Studies of Celadonite and Glauconite
    Studies of Celadonite and Glauconite GEOLOGICAL SURVEY PROFESSIONAL PAPER 614-F Studies of Celadonite and Glauconite By MARGARET D. FOSTER SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 614-F A study of the compositional relations between celadonites and glauconites and an interpretation of the composition of glauconites UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1969 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HIGKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S- Government Printing Office Washington, D.C. 20402 - Price 40 cents (paper cover) CONTENTS Page Abstract.-_ ____-____-_--__-_-___--______-__-_______ Fl Interpretation of glauconite coniposition___-___________ F13 Introduction.______________________________________ 1 Relation between trivalent iron and octahedral aluminurn____________________________________ 13 Selection of analyses and calculation of atomic ratios___ 2 The Fe+3 :Fe+2 ratio_______________________ 13 Relation between the composition of celadonites and Relation between iron and potassium____________ 14 glauconites_ _ ___________________________________ 3 Fixation of potassium___________________________ 14 High potassium celadonites and glauconites-_______ 7 Deficiency in potassium content-_________________ 14 Relation between glauconite composition and geo­ Low potassium celadonites and glauconites_________ logic age_____________________________________ 15 Relation between Si, R+2 (VI), Al(VI), and R+3 (VI)_
    [Show full text]
  • 2016-04-09 Erg. Int. Sparda-Cup Mu16 Dusiburg
    Ergebnisliste 18. Internationales Turnier in Duisburg am 09.04.2016 Ergebnisliste U16 m -37 kg 21 Teilnehmer 1. Martin Youri Judoverein Hercules 2001 NL 2. Philip Drexler Judo Crocodiles Osnabrück 2003 NS 3. Viktor Wandtke Budokan Lübeck 2003 SH 3. Lucas Kuttalek JC Achental 2003 BY 5. Daniel Bogdanov JC Vulkaneifel 2003 RL 5. Pit Schriever TH Eilbeck 2003 HH 7. Nick Woschow Judogemeinschaft Münster 2002 NW 7. Valentin Hofgärtner JV Nürtingen 2002 WÜ -40 kg 23 Teilnehmer 1. Kersten Bono Judoverein Hercules 2001 NL 2. Levi Märkt SC Bushido 2003 BE 3. David Ickes Budokan Lübeck 2002 SH 3. Michael Krieger JC Vulkaneifel 2003 RL 5. Levin Gerlach JC Jena 2001 TH 5. Tristan Koslan SV Holzhausen 2001 SN 7. Maxim Koserog Post SV Bamberg 2003 BY 7. Salman Kahn Said TH Eilbeck 2002 HH -43 kg 30 Teilnehmer 1. David Hohn JC Hennef 2001 NW 2. Silas Florian Dörner JC Wermelskirchen 2001 NW 3. Lasse Schriever TH Eilbeck 2003 HH 3. Silas Dell Jülicher Judoclub e.V. 2001 NW 5. Moritz Rödler JC Ettlingen 2002 BA 5. Richard Eisel JSV Werdau 2002 SN 7. Patrick Weisser TuS Bad Aibling 2001 BY 7. Jahim Waldenburg Beueler JC 2003 NW -46 kg 34 Teilnehmer 1. Luis Schmidt JV Ammerland-Münsing 2002 BY 2. Karl Bschlangaul TSG Backnang 2001 WÜ 3. Etienne Zeiger JSC Villingen 2001 BA 3. Keanu Ochs UJKC Potsdam 2002 BB 5. Michael Löb SSG Humboldt zu Berlin 2002 BE 5. Felix Ebner Sport-Dojo Berlin 2001 BE 7. Denis Fleischer SK Pro Sport Teplice 2001 CZ 7.
    [Show full text]
  • Duration of Hydrothermal Activity at Steamboat Springs, Nevada, from Ages of Spatially Associated Volcanic Rocks
    Duration of Hydrothermal Activity at Steamboat Springs, Nevada, From Ages of Spatially Associated Volcanic Rocks GEOLOGIC AiL SURVEY PROFESSIONAL PAPER 458-D Duration of Hydrothermal Activity at Steamboat Springs, Nevada, From Ages of Spatially Associated Volcanic Rocks By M. L. SILBERMAN, D. E. WHITE, T. E. C. KEITH, and R. D. DOCKTER GEOLOGY AND GEOCHEMISTRY OF THE STEAMBOAT SPRINGS AREA, NEVADA GEOLOGICAL SURVEY PROFESSIONAL PAPER 458-D UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1979 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Main entry under title: Duration of hydrothermal activity at Steamboat Springs, Nevada, from ages of spatially associated volcanic rocks. (Geology and geochemistry of the Steamboat Springs area, Nevada) (United States. Geological Survey. Professional paper ; 45 8-D) Bibliography: p. D13-D14. 1. Geothermal resources-Nevada-Steamboat Springs. 2. Geology- Nevada Steamboat Springs. 3. Potassium-argon dating. I. Silberman, Miles L. II. Series. III. Series: United States. Geological Survey. Professional paper ; 45 8-D. QE75.P9no. 458-D [GB1199.7.N3] 557.3'08s [553] 79-16870 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03215-5 CONTENTS Page Abstract __________ _______.._____________ Dl Potassium-argon ages Continued Introduction ______________________________________________ 1 Rhyolite domes______________________
    [Show full text]
  • The Properties of Moulding Sand with Halloysite
    ARCHIVES of ISSN (2299-2944) FOUNDRY ENGINEERING Volume 12 Issue 2/2012 DOI: 10.2478/v10266-012-0062-5 Published quarterly as the organ of the Foundry Commission of the Polish Academy of Sciences 205 – 210 The Properties of Moulding Sand with Halloysite M. Cholewa, Ł. Kozakiewicz* Silesian University of Technology, Foundry Department, Towarowa 7, 44-100 Gliwice, PL *Corresponding author: E-mail address: [email protected] Received 25-05-2012; accepted in revised form 31-05-2012 Abstract Until now, the mould sand in general use in the foundry industry are based on bentonite, which resulted from the fact that a good recognition properties and phenomena associated with this material. Come to know and normalized content of montmorillonite and carbonates and their important role in the construction of bentonite, and mass properties of the participation of compressive strength or scatter. Halloysite is widely used in industry and beyond them. However, little is known about its use in the foundry in Poland and abroad. This article presents preliminary research conducted at the Foundry Department of Silesian University of Technology on this material. Will raise the question of the representation of this two materials, which contains information connected with history and formation of materials, their structure and chemical composition. In the research, the results of compressive strength tests in wet masses of quartz matrix, where as a binder is used halloysite and bentonite in different proportions. Keywords: Halloysite, Bentonite, Moulding Sand Automation in the previous period concerned the processes 1. Introduction related mainly to the implementation of form, hence the early arrangements are known as automatic molding lines (ALF).
    [Show full text]
  • Nature of Interlayer Material in Silicate Clays of Selected Oregon Soils
    AN ABSTRACT OF THE THESIS OF PAUL C, SINGLETON for the Ph.D. in Soils (Name) (Degree) (Major) Date thesis is presented July 28, 1965 Title NATURE OF INTERLAYER MATERIAL IN SILICATE CLAYS OF SELECTED OREGON SOILS - Redacted for Privacy Abstract approved = ajor professor) Ç A study was conducted to investigate the nature of hydroxy interlayers in the chlorite -like intergrade clays of three Oregon soils with respect to kind, amount, stability, and conditions of formation. The clays of the Hembre, Wren, and Lookout soils, selected to represent weathering products originating from basaltic materials under humid, subhumid, and semi -arid climatic conditions respectively, were subjected to a series of progressive treatments designed to effect a differential dissolution of the materials intimately asso- ciated with them. The treatments, chosen to represent a range of increasing severity of dissolution, were (1) distilled water plus mechanical stirring, (2) boiling 2% sodium carbonate, (3) buffered sodium citrate -dithionite, (4) boiling sodium hydroxide, and (5) preheating to 400 °C for 4 hours plus boiling sodium hydroxide. Extracts from the various steps of the dissolution procedure were chemically analyzed in order to identify the materials removed from the clays. X -ray diffraction analysis and cation exchange capacity determinations were made on the clays after each step, and any differences noted in the measured values were attributed to the removal of hydroxy interlayers from the clays. Hydroxy interlayers were found to occur more in the Hembre and Wren soils than in the Lookout soil, with the most stable interlayers occurring in the Wren. Soil reaction was one of the major differences between these soils.
    [Show full text]
  • Clay Minerals Soils to Engineering Technology to Cat Litter
    Clay Minerals Soils to Engineering Technology to Cat Litter USC Mineralogy Geol 215a (Anderson) Clay Minerals Clay minerals likely are the most utilized minerals … not just as the soils that grow plants for foods and garment, but a great range of applications, including oil absorbants, iron casting, animal feeds, pottery, china, pharmaceuticals, drilling fluids, waste water treatment, food preparation, paint, and … yes, cat litter! Bentonite workings, WY Clay Minerals There are three main groups of clay minerals: Kaolinite - also includes dickite and nacrite; formed by the decomposition of orthoclase feldspar (e.g. in granite); kaolin is the principal constituent in china clay. Illite - also includes glauconite (a green clay sand) and are the commonest clay minerals; formed by the decomposition of some micas and feldspars; predominant in marine clays and shales. Smectites or montmorillonites - also includes bentonite and vermiculite; formed by the alteration of mafic igneous rocks rich in Ca and Mg; weak linkage by cations (e.g. Na+, Ca++) results in high swelling/shrinking potential Clay Minerals are Phyllosilicates All have layers of Si tetrahedra SEM view of clay and layers of Al, Fe, Mg octahedra, similar to gibbsite or brucite Clay Minerals The kaolinite clays are 1:1 phyllosilicates The montmorillonite and illite clays are 2:1 phyllosilicates 1:1 and 2:1 Clay Minerals Marine Clays Clays mostly form on land but are often transported to the oceans, covering vast regions. Kaolinite Al2Si2O5(OH)2 Kaolinite clays have long been used in the ceramic industry, especially in fine porcelains, because they can be easily molded, have a fine texture, and are white when fired.
    [Show full text]
  • Hectorite: Synthesis, Modification, Assembly and Applications Jing Zhang, Chun Hui Zhou, Sabine Petit, Hao Zhang
    Hectorite: Synthesis, modification, assembly and applications Jing Zhang, Chun Hui Zhou, Sabine Petit, Hao Zhang To cite this version: Jing Zhang, Chun Hui Zhou, Sabine Petit, Hao Zhang. Hectorite: Synthesis, modification, assembly and applications. Applied Clay Science, Elsevier, 2019, 177, pp.114-138. 10.1016/j.clay.2019.05.001. hal-02363196 HAL Id: hal-02363196 https://hal-cnrs.archives-ouvertes.fr/hal-02363196 Submitted on 2 Dec 2020 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. 1 Hectorite:Synthesis, Modification, Assembly and Applications 2 3 Jing Zhanga, Chun Hui Zhoua,b,c*, Sabine Petitd, Hao Zhanga 4 5 a Research Group for Advanced Materials & Sustainable Catalysis (AMSC), State Key Laboratory 6 Breeding Base of Green Chemistry-Synthesis Technology, College of Chemical Engineering, Zhejiang 7 University of Technology, Hangzhou 310032, China 8 b Key Laboratory of Clay Minerals of Ministry of Land and Resources of the People's Republic of 9 China, Engineering Research Center of Non-metallic Minerals of Zhejiang Province, Zhejiang Institute 10 of Geology and Mineral Resource, Hangzhou 310007, China 11 c Qing Yang Institute for Industrial Minerals, You Hua, Qing Yang, Chi Zhou 242804, China 12 d Institut de Chimie des Milieux et Matériaux de Poitiers (IC2MP), UMR 7285 CNRS, Université de 13 Poitiers, Poitiers Cedex 9, France 14 15 Correspondence to: Prof.
    [Show full text]
  • Alumohydrocalcite Caal2(CO3)2(OH)4 • 3H2O C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Triclinic
    Alumohydrocalcite CaAl2(CO3)2(OH)4 • 3H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Triclinic. Point Group: 1or1. As fibers and needles, to 2.5 mm; commonly in radial aggregates and spherulites, feltlike crystal linings, and powdery to chalky masses. Physical Properties: Cleavage: {100} perfect; {010} imperfect. Tenacity: Brittle. Hardness = 2.5 D(meas.) = 2.21–2.24 D(calc.) = 2.213 Decomposes in boiling H2O to calcite and hydrous aluminum oxide. Optical Properties: Transparent to opaque. Color: Chalky white to pale blue, pale yellow, cream, gray; pale rose or brownish pink to dark violet in chromian varieties; colorless in transmitted light. Luster: Vitreous to pearly, earthy. Optical Class: Biaxial (–). Orientation: X = b; extinction inclined 6◦–10◦. α = 1.485–1.502 β = 1.553–1.563 γ = 1.570–1.585 2V(meas.) = 64◦ 2V(calc.) = 50◦–55◦ Cell Data: Space Group: P 1or P 1 (chromian). a = 6.498(3) b = 14.457(4) c = 5.678(3) α =95.83(5)◦ β =93.23(3)◦ γ =82.24(3)◦ Z=2 X-ray Powder Pattern: Bergisch-Gladbach, Germany. 6.25 (100), 6.50 (70), 3.23 (60), 2.039 (50), 2.519 (40), 7.21 (30), 2.860 (30) Chemistry: (1) (2) (3) (1) (2) (3) CO2 24.2 26.4 26.19 CaO 17.8 16.5 16.68 Al2O3 31.3 22.0 30.33 H2O 26.7 26.6 26.80 Cr2O3 8.3 Total 100.0 99.8 100.00 2− 1− (1) Bergisch-Gladbach, Germany; (CO3) , (OH) , and H2O confirmed by IR.
    [Show full text]