Ion-Exchange Minerals and Disposal of Radioactive Wastes a Survey of Literature

Total Page:16

File Type:pdf, Size:1020Kb

Ion-Exchange Minerals and Disposal of Radioactive Wastes a Survey of Literature Ion-Exchange Minerals and Disposal of Radioactive Wastes A Survey of Literature By B. P. ROBINSON GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1616 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Abstract___ _______________________________________________________ 1 Introduction._____________________________________________________ 2 Purpose and scope of study._______________--__--____-__-_-____- 2 Ion-exchange property of minerals.______________________________ 2 Radioactive waste disposal____________________________________ 3 Acknowledgements- ___________________________________________ 4 Adsorption and ion exchange: General.______________________________ 4 Colloid science ________________________________________________ 4 Colloids defined._______________________.__.______^___^___ 5 Classification of colloids.___________________________________ 5 Size of colloidal particles.__________________________________ 5 Examples of colloids.______________________________________ 5 Properties of colloids-,___________-__-_-___-_____---------_- 5 Structure and electric charge...________________________ 5 Stability of colloids.___________________________________ 6 Other references.._________________________________________ 9 Thermodynamics and adsorption._____________________^___-_____ 9 Free energy and equilibrium._______________________________ 10 Experimental studies_______________________________________ 10 Other references.__________________________________________ 12 Reaction kinetics._____________________________________________ 12 Function of kinetics________-____--------________-__----_:__ 12 Order of rate equations._.__________________________________ 12 Diffusion effect on reaction rate_____________________________ 13 Temperature effect and the Arrhenius equation._______________ 13 Partition functions________-_________-___--____-___--_--_- " 14 Experimental studies.______________________________________ 14 Reaction mechanisms._________________________________________ 17 Types of adsorption______-_____-___--____-___-_-_----_--_ 17 Physical _ __________-__________--._______--_---_----- 17 Chemisorption _______-_______________--___-_--___-___- 17 Other types_______________________________---__----__- 18 Adsorption equations and exchange equilibrium___^_________-.__-__ 19 Empirical equations._____________________________________ 19 Mass-action equations._____________________________________ 21 Kinetic equations__________________________-___-__-.--__-- 26 Surface tension_________________________________ _______ 28 Surface-active agents____________^___^______-__---_-__ 29 Gibbs' adsorption theorem..____________________________ 29 Experimental studies____________-___-___---__------_- 30 Clay minerals__.---_-___-.__---_--__---------.__-_-___--__---_-------_- 31 Definition of clay minerals.._-__-__________-.___-___----_---__-- 31 Origin of clays____________--_______-_-_-_-_---_-__--_-----_--_ 31 Classification and nomenclature-___---_--__--_-----_--__--------- 32 Classification systems-____---_-------_---_--------__------- 32 Nomenclature_ _ ___-__________-_____^.__--___--__----___- 34 Allophane.___________________________________________ 34 Kaolinite group._______-___-______-.___-____-__-__-___- 34 IV CONTENTS Clays minerals Continued Classification and nomenclature Continued Nomenclature Continued Page Halloysite ____________________________________________ 34 Montmorillonite_ _ _______--______-_--______--__--___- 35 Vermiculite. _ _____________-_____-__-_----_-_-_-_-_-___ 35 Elite____________________--_-_-__-_-____-______ 35 Chlorite_______________________________________ 35 Palygorskite-attapulgite-sepiolite. _______________________ 36 Composition and structure____________________________________ 36 Old concept_____________________________________________ 36 Modern concept____-_______-__--_-_-_-__---_---_----_--__^ 37 Modern studies of clay structures.___________________________ 37 Structure of allophane minerals______-____-__-_-_-_____-___ 40 Structure of kaolinite--__-------------------_--------__--_- 40 Structure of halloysite____________________________________ 43 Structure of montmorillonites-______________________________ 44 Structure of vermiculite.____________-___-_-______---__-____ 50 Structure of illites.____________-____-__----_-_-__--_-_-____ 51 Structure of chlorites___________________-__-__---_----_-_ 54 Structure of attapulgite-palygorskite-sepiolite_________________ 55 Structure of mixed-layer clay minerals_______________________ 56 Other cation exchange minerals____________________________________ 58 Origin and nomenclature________-_______-___-____-_-_-____-___- 58 Glauconite__ _ __-_____-___-___--__----_---__---_--___-___ 58 Ultramarines_ _ _-_-___-__--____-_--_--_---__-____-_----__ 58 Zeolites __________________________________________________ 58 Composition and structure____------_------__-------_-_--_------ 59 Glauconite. _ ____________________________________________ 59 Ultramarines_ _ __________________________________________ 59 Zeolites __________________________________________________ 59 Cation exchange and adsorption on clays and other exchange minerals. _ _ 60 Definition _____________________________________________________ 60 Cation exchange materials._____________________________________ 61 Early history_________________________________________________ 61 Cation exchange theories_____________________________________ 62 Adsorption of polar molecules and gases by clay minerals._____--___ 63 Uptake of polar molecules._________________________________ 63 Uptake of water___.________-___-____-_-__-___--___-__- 63 Uptake of ammonia _________________________________ 64 Organic polar molecules._______________________________ 64 Modern concept of cation exchange in clay minerals and exchange minerals.___________________________________________________ 64 Cation exchange in clay minerals.---_______-__--_-_____-____ 64 Cation exchange in glauconite_____________________________ 66 Cation exchange in ultramarines..___________________________ 66 Cation exchange in zeolites._________--_____----___-_-__--__ 67 Determination of cation-exchange capacity _____-__---___-___-__-_ 67 Ammonium method______________________________________ 68 Barium meth.od______________________-__---_------_-_----- 69 Radioactive tracer-chromatogram method ____________________ 70 Colorimetric method ____________ _________-_____-_-___-_-_--_-_ 70 Miscellaneous methods.________________________________________ 70 CONTENTS V Cation exchange and adsorbtion on clays and other exchange minerals Con. Page Replaceability of exchangeable cations___________________________ 71 Factors influencing cation exchange.----.------------------- 72 Binding forces_____________________-______--_---_-_- 72 Accessebility of the lattice ions-_-----------_----_------- 72 lonization of adsorbed cations____.__________-__-_-__-- 73 Relative size of ions_________-__-___.._-_-.__--.-------- 73 Particle size_______-_______________-________--*.-__--. 74 Temperature_____________-___-___-___._-___-___- 76 Valence._____________________________________________ 76 Atomic weight and atomic number_____-__-___--__-_--- 77 Concentration__ _ ____________________________________ 77 pH..__...__._. - ._.._.._______._--_-- 79 Clogging at cation exchange positions___-_____--__------- 79 Hydrolysis_________-_______________________. 80 Heat of wetting._________________-_-__-__--__--_---- 80 Anions _______________________________________________ 80 Complementary cations.__________________--_._--__--__ 81 Swelling_____________________________ 81 Zeta potential_______________________________________ 81 Cation fixation._______________________________________________ 81 Anion exchange in clay minerals___________-_-_-____--_-----_-------- 83 Types of anion exchange.__________-_-__-__-____--__-___--_--_- 83 Exchange anions and clays___________________________________ 83 Fixation of phosphate ions____________________________________ 84 Effect of grinding________________-___-_____-___--_--_---_ 84 Effect of temperature____________________----___--__------- 84 Effect of pH____________________________-_____--_--- 84 Anion and cation exchange in different clays________________-_---- 85 Factors interfering with the study of anion exchange.______-__-_--_ 85 Other references on ion exchange_____--__---_--___--_---_------- 86 Radioactive waste disposal________________________________________ 86 The problem____________._________..__.____._.___ 86 Radioactive waste defined________-.___-_______-_-----------_---_ 86 Radioactive elements____-___-___-______-___--_-_------ __ 87 Units of measurement of radioactivity.____________-____.__--- 87 Sources of radioactive wastes_________________________________ 88 Classification of radioactive wastes____________________________ 89 Gaseous wastes________-_______-_______-__----__-_--_---- 89 Liquid wastes_________________-___-_---__--------.--_---- 90 Solid wastes____________________-________-_--._------------ 90 Current methods of handling wastes.____________________________ 90 Proposed methods of handling wastes---------------------------- 92 Chemical methods--_..__________--__--_-----_--_----------- 92 Filtration__________________________________________ 93 Evaporation ______________________________________________ 94 Adsorption and ion exchange______________________________
Recommended publications
  • 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]
  • 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]
  • Experimental Data for High-Temperature Decomposition of Natural Celadonite from Banded Iron Formation
    Chin. J. Geochem. (2015) 34(4):507–514 DOI 10.1007/s11631-015-0066-2 ORIGINAL ARTICLE Experimental data for high-temperature decomposition of natural celadonite from banded iron formation 1 1 1 K. A. Savko • S. M. Piliugin • N. S. Bazikov Received: 5 March 2015 / Revised: 1 May 2015 / Accepted: 6 July 2015 / Published online: 17 July 2015 Ó Science Press, Institute of Geochemistry, CAS and Springer-Verlag Berlin Heidelberg 2015 Abstract Three experiments were set up to evaluate (KMA), Russia. Subalkaline BIF contains widespread conditions for the high-temperature decomposition of riebeckite, aegirine, celadonite, tetraferribiotite, and Al- celadonite from a banded iron formation in an alumina-free free chlorite instead of grunerite, stilpnomelane, minneso- system and identify its decomposition products. It was taite, and greenalite, which are the usual minerals in BIF estimated that at 650 and 750 °C, with a NiNiO buffer and elsewhere. At the KMA iron deposits, BIF with alkali pressure of 3 kbar, celadonite completely decomposes and amphibole were metamorphosed at 370–520 °C and 2–3 the decomposition products were tetraferribiotite, mag- kbar (Savko and Poskryakova 2003). netite and quartz. Under more oxidizing conditions (he- In the KMA, BIF green mica, which is responsible in matite-magnetite buffer instead of NiNiO), ferrous composition to the celadonite with the formula KFe3?(Mg, 2? potassium feldspar sanidine forms instead of magnetite. Fe ) = [Si4O10](OH)2, is quite abundant (Savko and During the celadonite decomposition in oxidizing condi- Poskryakova 2003). Celadonite forms emerald-green scales tions more magnesian and aluminous tetraferribiotite, sizing from a few tenths to 1.5–2 mm, composing up to along with ferrous sanidine, are formed than at reducing 30 %–40 % modal.
    [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]
  • 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,
    [Show full text]
  • Geochemical and Geochronological Constraints on the Genesis of Ion-Adsorption-Type REE Mineralization in the Lincang Pluton, SW China
    minerals Article Geochemical and Geochronological Constraints on the Genesis of Ion-Adsorption-Type REE Mineralization in the Lincang Pluton, SW China Lei Lu 1,2, Yan Liu 3,4,*, Huichuan Liu 5,*, Zhi Zhao 2, Chenghui Wang 2 and Xiaochun Xu 1 1 School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China; [email protected] (L.L.); [email protected] (X.X.) 2 MLR Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; [email protected] (Z.Z.); [email protected] (C.W.) 3 Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China 4 Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Science, Beijing 100037, China 5 State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing 102249, China * Correspondence: [email protected] (Y.L.); [email protected] (H.L.) Received: 3 November 2020; Accepted: 2 December 2020; Published: 12 December 2020 Abstract: Granites are assumed to be the main source of heavy rare-earth elements (HREEs), which have important applications in modern society. However, the geochemical and petrographic characteristics of such granites need to be further constrained, especially as most granitic HREE deposits have undergone heavy weathering. The LC batholith comprises both fresh granite and ion-adsorption-type HREE deposits, and contains four main iRee (ion-adsorption-type REE) deposits: the Quannei (QN), Shangyun (SY), Mengwang (MW), and Menghai (MH) deposits, which provide an opportunity to elucidate these characteristics The four deposits exhibit light REE (LREE) enrichment, and the QN deposit is also enriched in HREEs.
    [Show full text]
  • 2019 10-11:00 A.M
    X-ray Diffraction Methods Subcommittee Meeting Minutes Wednesday, 13 March 2019 10-11:00 a.m. Chris Gilmore, Chairman 1. Call to Order C. Gilmore 2. Appointment of Minutes Secretary Nicole Ernst Boris 3. Approval of Minutes from 2018 So moved by Scott Misture. Seconded by John Faber. 4. Review of Mission Statement The X-ray Methods Subcommittee will recommend data for inclusion in the PDF by considering instrument configurations, data collection, and powder pattern calculations, emphasis on state-of-the-art methods. 5. Directors’ Liaison Report T. Ida Last years’ motion: The XRD Subcommittee recommends to the Technical Committee that Headquarters explore possibilities given by traditional and advanced machine learning (e.g. partial least squares) for expanding the capabilities of the database software towards quantification. BoD response – positive, noting ICDD chairman at IUCr and DXC presentation/paper on this topic and more discussion at the Fall Strategy Review. 6. Short presentations • How to win the Reynold’s Cup S. Hillier Named for Bob Reynolds – Competition to promote quantitative mineral analysis– 3 samples are provided and has international participation. Suggestions on how to win: get phase ID right; factors of quantitative analysis (avoid texture); cross check results (see slides). • Clustering and the ICDD Databases J. Kaduk As applied to Zeolite task group. Polysnap. Similarity index. MMBS. Jim presented zeolite clustering examples from the PDF-4+ 2019 database and named Cluster K5 and K (see slides). • Partial Least Squares Revisited C. Gilmore Looking at PLS as a Machine Learning Method – Start with Training data (known composition) that include mixtures - important to get number of factors correct for good results – Then move to Validation data (PXRD patterns + known compositions) as independent check of training data– then finally, unknown PXRD patterns – example highlighted: AliteM1 (see slides).
    [Show full text]
  • Sauconite Na0.3Zn3(Si,Al)4O10(OH)2² 4H2O
    Sauconite Na0:3Zn3(Si; Al)4O10(OH)2 ² 4H2O c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: n.d. Clayey, massive; as small micaceous plates in laminated to compact masses. Physical Properties: Cleavage: 001 , perfect. Hardness = 1{2 D(meas.) = n.d. D(calc.) = n.d. Positive identi¯catiofn ofgminerals in the smectite group may need data from DTA curves, dehydration curves, and X-ray powder patterns before and after treatment by heating and with organic liquids. Optical Properties: Translucent. Color: Reddish brown, brown, brownish yellow, mottled. Luster: Dull. Optical Class: Biaxial ({). Orientation: Y = b. ® = 1.55{1.58 ¯ = 1.59{1.62 ° = 1.59{1.62 2V(meas.) = 0±{20± Cell Data: Space Group: n.d. a = 5.2 b = 9.1 c = 15.4 ¯ = n.d. Z = n.d. X-ray Powder Pattern: Coon Hollow mine, Arkansas, USA; air dried sample. 15.4 (100), 2.67 (100), 1.544 (100), 7.77 (90), 4.60 (90), 1.334 (75), 5.58 (50b) Chemistry: (1) (2) SiO2 34.46 33.40 TiO2 0.24 0.15 Al2O3 16.95 7.45 Fe2O3 6.21 1.73 MnO trace CuO 0.13 ZnO 23.10 36.73 MgO 1.11 0.78 CaO 1.92 Na2O 0.22 K2O 0.49 0.27 + H2O 10.67 7.14 H2O¡ 6.72 9.78 Total 99.95 99.70 (1) Friedensville, Pennsylvania, USA. (2) Coon Hollow mine, Arkansas, USA. Mineral Group: Smectite group. Occurrence: Fills vugs and seams in oxidized zinc and copper deposits; may be redeposited at the water table.
    [Show full text]
  • Factors Responsible for Crystal Chemical Variations in The
    American Mineralogist, Volume 95, pages 348–361, 2010 Factors responsible for crystal-chemical variations in the solid solutions from illite to aluminoceladonite and from glauconite to celadonite VICTOR A. DRITS ,1 BELL A B. ZV I A GIN A ,1 DOUGL A S K. MCCA RTY,2,* A N D ALFRE D L. SA LYN 1 1Geological Institute of the Russian Academy of Science, Pyzhevsky per. 7, 119017 Moscow, Russia 2Chevron ETC, 3901 Briarpark, Houston, Texas 77063, U.S.A. AB STR A CT Several finely dispersed low-temperature dioctahedral micas and micaceous minerals that form solid solutions from (Mg,Fe)-free illite to aluminoceladonite via Mg-rich illite, and from Fe3+-rich glauconite to celadonite have been studied by X-ray diffraction and chemical analysis. The samples have 1M and 1Md structures. The transitions from illite to aluminoceladonite and from glauconite to celadonite are accompanied by a consistent decrease in the mica structural-unit thickness (2:1 layer + interlayer) or csinβ. In the first sample series csinβ decreases from 10.024 to 9.898 Å, and in the second from 10.002 to 9.961 Å. To reveal the basic factors responsible for these regularities, struc- tural modeling was carried out to deduce atomic coordinates for 1M dioctahedral mica based on the unit-cell parameters and cation composition. For each sample series, the relationships among csinβ, maximum and mean thicknesses of octahedral and tetrahedral sheets and of the 2:1 layer, interlayer distance, and variations of the tetrahedral rotation angle, α, and the degree of basal surface corruga- tion, ∆Z, have been analyzed in detail.
    [Show full text]
  • UNITED STATES DEPARTMENT of AGRICULTURE July
    UNITED STATES DEPARTMENT OF AGRICULTURE SOIL CONSERVATION SERVICE Washington, 0. C. 20250 July 22, 1970 d TECHNICAL RELEASE NOTICE 28-1 Advisory PERS-120 dated May 27, 1970, specified that all use of benzidine in the SCS is prohibited as it may be hazardous to human health. Accordingly, a change in Technical Release No. 28, Clay Minerals is needed to reflect this prohibition. Therefore, please make the following pen and ink change in any copies of the TR you may have: On page 36, fourth paragraph, place an asteriak (*) beside "Benzidine test" and add the follwing to the bottom of the page: *Do not use this test. Benzidine may be hazardous to huw health. Direct or Engineering Division STC . EWP I wo U.S. Department of Agriculture Technical Release No. 28 Soil Conservation Service Geology Engineering Division February 1963 CLAY MINERALS by John N. Holeman, Geologist PREFACE The purpose of this technical release is 1) to assemble some of the published information on clay minerals as related not only to geology but also to chemistry, soil mechanics and physics; '2) to condense and coordinate this information for the use of interested SCS personnel; and 3) to present both theories and basic facts concerning clay min- erals as well as their applicability to engineering geology. It is realized that some aspects of clay minerals are only mentioned sketch- ily while other features are covered in considerable detail; however, this is deemed desirable in the first case for the sake of brevity and in the latter to achieve coherence. The need for assembling data on clay minerals for use within the Soil Conservation Service was first proposed by A.
    [Show full text]
  • List of Abbreviations
    List of Abbreviations Ab albite Cbz chabazite Fa fayalite Acm acmite Cc chalcocite Fac ferroactinolite Act actinolite Ccl chrysocolla Fcp ferrocarpholite Adr andradite Ccn cancrinite Fed ferroedenite Agt aegirine-augite Ccp chalcopyrite Flt fluorite Ak akermanite Cel celadonite Fo forsterite Alm almandine Cen clinoenstatite Fpa ferropargasite Aln allanite Cfs clinoferrosilite Fs ferrosilite ( ortho) Als aluminosilicate Chl chlorite Fst fassite Am amphibole Chn chondrodite Fts ferrotscher- An anorthite Chr chromite makite And andalusite Chu clinohumite Gbs gibbsite Anh anhydrite Cld chloritoid Ged gedrite Ank ankerite Cls celestite Gh gehlenite Anl analcite Cp carpholite Gln glaucophane Ann annite Cpx Ca clinopyroxene Glt glauconite Ant anatase Crd cordierite Gn galena Ap apatite ern carnegieite Gp gypsum Apo apophyllite Crn corundum Gr graphite Apy arsenopyrite Crs cristroballite Grs grossular Arf arfvedsonite Cs coesite Grt garnet Arg aragonite Cst cassiterite Gru grunerite Atg antigorite Ctl chrysotile Gt goethite Ath anthophyllite Cum cummingtonite Hbl hornblende Aug augite Cv covellite He hercynite Ax axinite Czo clinozoisite Hd hedenbergite Bhm boehmite Dg diginite Hem hematite Bn bornite Di diopside Hl halite Brc brucite Dia diamond Hs hastingsite Brk brookite Dol dolomite Hu humite Brl beryl Drv dravite Hul heulandite Brt barite Dsp diaspore Hyn haiiyne Bst bustamite Eck eckermannite Ill illite Bt biotite Ed edenite Ilm ilmenite Cal calcite Elb elbaite Jd jadeite Cam Ca clinoamphi- En enstatite ( ortho) Jh johannsenite bole Ep epidote
    [Show full text]
  • Mineralogy in Geotechnical Engineering
    JOURNAL OF Engineering Science and Journal of Engineering Science and Technology Review 3 (1) (2010) 108-110 Technology Review Research Article www.jestr.org Mineralogy in Geotechnical Engineering A. Namdar Mysore University, India. Received 5 December 2009; Revised 24 March 2010; Accepted 30 April 2010 Abstract The several investigations on soils by different researchers have been executed, but research on soil mechanical properties based on mineralogy is very meager, in this regard the author intention is employee of natural minerals for evaluation of soil cohesion, it may leads to developments of a soil with appropriates characteristics in permeability, transmitting load, resisting against deformation and settlement. This paper deals with analysis of soil cohesion based on mineralogy. The result revealed cohesion of a plastic soil could be improve by mineral presented in an non plastic soil, and also carbonate has negative affect on soil cohesion and some other soil minerals also have same affect on cohesion that required to be more investigate. Keywords: Mixed Soil; Soil mineralogy; Carbonate. 1. Introduction It is require analysis of soil cohesion based on consideration of ing C, Φ and density values and adopting Terzaghi’s method, the soil mineralogy result. The soil cohesion is an element in control- safe bearing capacity of the soil mixed models were calculated. ling soil bearing capacity. In calculation of safe bearing capacity at all models has been as- The soil bearing capacity could be determined by several sumed of 1.5m depth and 2.5m*2.5m widths for square footing, methods like bearing capacity tables in various building codes, to improvement of site characteristics by select of different types analytical methods, and plate bearing test, penetration test, model of soils, which are consist of natural mineral, attempt was to find test, prototype tests and laboratory test [1-2].
    [Show full text]