Use of Local Minerals in the Treatment of Radioactive Waste

Total Page:16

File Type:pdf, Size:1020Kb

Use of Local Minerals in the Treatment of Radioactive Waste O = 0(0H) •=Si(AI) O = 0(0H) # = AI, Mg, Fe, etc. TECHNICAL REPORTS SERIES No. 136 Use of Local Minerals in the Treatment of Radioactive Waste INTERNATIONAL ATOMIC ENERGY AGENCY, VIENNA, 1972 USE OF LOCAL MINERALS IN THE TREATMENT OF RADIOACTIVE WASTE The following States are Members of the International Atomic Energy Agency: AFGHANISTAN GUATEMALA PAKISTAN ALBANIA HAITI PANAMA ALGERIA HOLY SEE PARAGUAY ARGENTINA HUNGARY PERU AUSTRALIA ICELAND PHILIPPINES AUSTRIA INDIA POLAND BELGIUM INDONESIA PORTUGAL BOLIVIA IRAN ROMANIA BRAZIL IRAQ SAUDI ARABIA BULGARIA IRELAND SENEGAL BURMA ISRAEL SIERRA LEONE BYELORUSSIAN SOVIET ITALY SINGAPORE SOCIALIST REPUBLIC IVORY COAST SOUTH AFRICA CAMEROON JAMAICA SPAIN CANADA JAPAN SUDAN CEYLON JORDAN SWEDEN CHILE KENYA SWITZERLAND CHINA KHMER REPUBLIC SYRIAN ARAB REPUBLIC COLOMBIA KOREA, REPUBLIC OF THAILAND COSTA RICA KUWAIT TUNISIA CUBA LEBANON TURKEY CYPRUS LIBERIA UGANDA CZECHOSLOVAK SOCIALIST LIBYAN ARAB REPUBLIC UKRAINIAN SOVIET SOCIALIST REPUBLIC LIECHTENSTEIN REPUBLIC DENMARK LUXEMBOURG UNION OF SOVIET SOCIALIST DOMINICAN REPUBLIC MADAGASCAR REPUBLICS ECUADOR MALAYSIA UNITED KINGDOM OF GREAT EGYPT, ARAB REPUBLIC OF MALI BRITAIN AND NORTHERN EL SALVADOR MEXICO IRELAND ETHIOPIA MONACO UNITED STATES OF AMERICA FINLAND MOROCCO URUGUAY FRANCE NETHERLANDS VENEZUELA GABON NEW ZEALAND VIET-NAM GERMANY, FEDERAL REPUBLIC OF NIGER YUGOSLAVIA GHANA NIGERIA ZAIRE, REPUBLIC OF GREECE NORWAY ZAMBIA The Agency's Statute was approved on 23 October 1956 by the Conference on the Statute of the IAEA held at United Nations Headquarters, New York; it entered into force on 29 July 1957, The Headquarters of the Agency are situated in Vienna. Its principal objective is "to accelerate and enlarge the contribution of atomic energy to peace, health and prosperity throughout the world". © IAEA, 1972 Permission to reproduce or translate the information contained in this publication may be obtained by writing to the International Atomic Energy Agency. Kärntner Ring 11, P.O. Box 590, A-1011 Vienna, Austria. Printed by the IAEA in Austria June 1972 TECHNICAL REPORTS SERIES No. 136 USE OF LOCAL MINERALS IN THE TREATMENT OF RADIOACTIVE WASTE INTERNATIONAL ATOMIC ENERGY AGENCY VIENNA, 1972 USE OF LOCAL MINERALS IN THE TREATMENT OF RADIOACTIVE WASTE IAEA, VIENNA, 1972 STl/DOC/10/136 FOREWORD A great deal of information has been made available on the various techniques in use for safely managing radioactive waste. The International Atomic Energy Agency periodically convenes panels or other meetings to bring this information up to date and publishes Safety Series, Technical Reports Series and Guidebooks to help disseminate this information. Technical Reports Series No. 78, 'Operation and Control of Ion- Exchange Processes for Treatment of Radioactive Wastes' , published by the Agency in 1967, deals with the use of high capacity organic and in- organic exchange materials. A need has been expressed by developing countries for more information on the use of locally available ion-exchange and sorbent materials. The present publication, which is the outcome of a panel meeting, on the Use of Local Minerals in the Treatment of Radioactive Waste, held at the Agency's Headquarters in Vienna on 5-9 May 1969, presents, for the first time in a single volume, the large amount of practical information available. A list of the panel participants and the advisers appears at the end of the book. These experts kindly provided the material for the publication, which was organized by Mr. E.W. Wiederhold of the IAEA. CONTENTS I. INTRODUCTION 1 II. NATURAL MATERIALS FOR RADIOACTIVE WASTE TREATMENT 3 II. 1. Introduction 3 11.2. Types of reaction mechanism 3 11.2.1. Distribution of the radioactive microcomponent between solid and liquid phases 3 11.2.2. Co-precipitation 3 11.2.3. Coagulation and flocculation of colloids 6 11.2.4. Adsorption from solutions 9 11.2.5. Ion exchange 10 11.2.5.1. Ionic crystals 10 11.2.5.2. Aluminosilicates 12 11.2.6. Mineral replacement reactions 17 11.2.7. Oxidation-reduction mechanisms 19 11.2.7.1. Redox exchangers 19 11.2.7.2. Examples 19 11.2.7.3. Applications 20 11.3. Materials 20 11.3.1. Introduction 20 11.3.2. Mineral classification scheme 21 11.3.3. Minerals of use in waste treatment 21 11.3.4. Oxides and hydroxides 23 11.3.5. Halides 23 11.3.6. Carbonates 24 11.3.7. Phosphates 25 11.3.8. Sulphates 26 11.3.9. Silicates 26 11.3.9.1. Layer silicates 26 11.3.9.2. Zeolites 27 11.3.9.3. Crystal chemistry of the clays and zeolites 27 11.3.9.4. Waste treatment applications — 29 11.3.10. Other naturally occurring substances 30 III. CHARACTERIZATION OF MATERIALS 31 III.l. Sampling 31 III. 1.1. Sampling in the field 31 III.1.2. Laboratory sample preparation 32 III.1.2.1. Microscopic examination 32 111.1.2.2. Crushing 32 111.1.2.3. Sieving 32 111.1.2.4. Separation methods 33 111.2. Identification of the material 33 111.2.1. X-ray diffraction 33 111.2.2. Electron microscopy and electron diffraction 34 111.2.3. Petrographic microscopy 34 111.2.4. Thermal methods 35 111.2.5. Infrared spectrometry 35 111.2.6. Chemical methods of material identification 36 111.3. Physico-chemical characterization 36 111.3.1. General remarks 36 111.3.2. Capacities 36 111.3.2.1. Definitions 36 111.3.2.2. Pure ion exchange capacity (Kr) 37 111.3.2.3. Sorption capacity (K ad) 37 111.3.2.4. Total exchange capacity (Ktot) 38 111.3.2.5. Procedures 38 111.3.2.6. Complications 39 111.3.3. Selectivity 39 111.3.3.1. Ion exchange equilibrium 40 111.3.3.2. Ion exchange isotherm 40 111.3.3.3. Distribution coefficient (K*) 41 41 111.3.3.4. Separation factor (OB ) 111.3.3.5. Selectivity coefficient (NKB) 42 111.3.3.6. Procedures 42 111.3.4. Kinetic properties 42 111.3.4.1. Definitions 43 111.3.4.2. Procedures 43 111.3.5. Swelling properties 44 111.3.5.1. Definitions 44 111.3.5.2. Procedures 45 111.3.6. Reduction-oxidation properties 45 111.3.6.1. Redox capacity 45 Definition 45 Procedure 45 111.3.6.2. Redox potential 46 IV. MATERIALS 47 IV.1. Material preparation 47 IV.1.1. Crushing and grinding 47 IV.1.2. Sieving (screening) 48 IV.1.3. Washing 51 IV.2. Chemical and heat pre-treatment 52 IV.2.1. Chemical pre-treatment 52 IV.2.2. Heat pre-treatment 54 IV.2.3. Pelletizing 56 IV.2.3.1. Heat treatment of bentonites 56 IV.2.3.2. Heat treatment of alumina and clinoptilolite 56 V. PLANT SCALE APPLICATIONS 57 V.l. General 57 V.l.l. Ion exchangers 57 V.l.1.1. Batch process 57 V.l.1.2. Column operation 57 V.l.2. Additives and product conditioners 59 V.2. Operational experience 59 V.2.1. United Kingdom (Harwell) 59 V.2.2. India (Trombay) 61 V.2.3. United States of America 61 V.2.3.1. National Reactor Testing Station (NRTS), Idaho 61 V.2.3.2. O&k Ridge National Laboratory 64 V.2.3.3. Battelle North West Laboratory, Richmond 65 V.2.3.4. Savannah River 65 V.2.4. Federal Republic of Germany 65 V.2.5. Czechoslovak Socialist Republic 66 VI. FINAL PRODUCT CONDITIONING 67 VI.1. Conditioning of exhausted inorganic ion exchangers 67 VI.1.1. Treatment at Idaho Falls 67 VI.1.2. Treatment at Harwell 67 VI. 1.3. Incorporation into bitumen or concrete 67 VI.1.4. Fixation in glasses 68 VI.1.5. Reduction of leachability by heat treatment 68 VI.2. Use of inorganic minerals for improvement of fixed radioactive wastes 68 VII. ECONOMIC ASPECTS 71 VII.1. Capital costs 71 VII.2. Operating costs 72 APPENDIX I: NATURAL MATERIALS FOR USE IN WASTE TREATMENT 73 APPENDIX II: DEFINITION AND DETERMINATION OF CAPACITIES OF NATURAL ION EXCHANGERS .... 81 1. Introduction 81 2. Elementary principles 82 3. Definitions of ion exchange capacity 83 4. General methods of determination 92 References to Appendix II 95 APPENDIX III: COMMUNICATIONS CONCERNING NATIONAL EXPERIENCE IN VARIOUS COUNTRIES 97 1. France 97 2. Germany, Federal Republic of 97 3. Italy 98 4. Korea 99 5. Union of Soviet Socialist Republics 99 Special communication by V.M. Sedov, USSR: Research in the USSR on the use of natural sorbents for radioactive waste treatment 99 REFERENCES 107 LIST OF PARTICIPANTS 113 I. INTRODUCTION In 1962 the Agency convened an ad hoc panel on Radioactive Waste Disposal into the Ground. This panel was primarily concerned with the rate of movement of ground water and radioactive isotopes through soil. Ion exchange with and sorption by naturally occurring zeolites and clays were discussed. Replacement reactions, in which a slightly soluble mineral in the soil is gradually replaced by a less soluble species by reacting with an appropriate ion in the solution, were also discussed. In 1964 the Agency convened another panel relating to the use of minerals in the treatment of radioactive wastes. This panel was on the Application of Mineral Reactions in Radioactive Waste Treatment. Much useful information was presented and a variety of mineral reactions were discussed. Among the topics discussed were mineral species used as aids in flocculation, as sorbents or exchange media in beds or columns, as sorbents or exchange media which remove the activity from discharges to the ground and those species which tend to concentrate activity in the sediments of streams, lakes and oceans. Much work had been done on the various clays, vermiculite, zincite, pyrolusite and zeolites.
Recommended publications
  • Mineral Processing
    Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19
    [Show full text]
  • The Thermal Dehydration of Natural Zeolites
    549.67:536.4 MEDEDELINGEN LANDBOUWHOGESCHOOL WAGENINGEN • NEDERLAND • 74-9 (1974) THE THERMAL DEHYDRATION OF NATURAL ZEOLITES (with a summary in Dutch) L. P. VAN REEUWIJK Department of Soil Science and Geology, Agricultural University, Wageningen, The Netherlands (Received 11-11-1974) H. VEENMAN & ZONEN B.V. - WAGENINGEN - 1974 Ml Mededelingen Landbouwhogeschool Wageningen 74-9 (1974) (Communications Agricultural University) is also published as a thesis CONTENTS 1. INTRODUCTION 1 1.1. History 1 1.2. Genesis and occurrence of natural zeolites 2 1.3. Structural classification 4 1.4. Practical applications of zeolites 8 2. THE DEHYDRATION OF ZEOLITES - A CRITICAL REVIEW 11 2.1. Introduction 11 2.2. DTA and TG 12 2.3. High temperature X-ray analysis 13 2.4. Vapour pressure 14 2.5. The reaction mechanism 15 2.6. Rehydration 16 3. THE COMPLEXITY OF THE DEHYDRATION PROCESS 17 3.1. Types of dehydration 17 3.2. Examples 18 3.3. Effect of pressure on dehydration 22 3.3.1. Qualitative aspect 22 3.3.2. Quantitative aspect - Calibration of pressure 25 3.4. Dehydration equilibrium and hysteresis 26 3.5. Internal and external adsorption 28 4. DEHYDRATION OF ZEOLITES OF THE NATROLITE GROUP 30 4.1. Materials and procedures 30 4.2. Results and discussion 31 4.2.1. Natrolite 31 4.2.2. Mesolite 33 4.2.3. Scolecite 36 4.2.4. Thomsonite 37 4.2.5. Gonnardite 37 4.2.6. Edingtonite 38 4.3. Conclusions 39 5. PRESSURE-TEMPERATURE RELATIONS 40 5.1. The Clausius-Clapeyron equation 41 5.2. Experimental 43 5.3.
    [Show full text]
  • THE CRYSTAL STRUCTURE of CAHNITE, Cabaso4 (OH)4
    THE CRYSTAL STRUCTURE OF CAHNITE, CaBAsO4 (OH)4 by Charles T. Prewitt S.B., M.I.T.AAT.rc (1955) SUBMITTED IN PARTIAL YULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY (1960) Signature of Author .,. ..... .. ... .... Department of>Geolgy nd Geophysics, May 20, 1960 Certified by . t -.. 4-w.Vi 4 ... .. ... , . Thesis Supervisor Accepted by . .* . .... ... Chairman, Departmental Committee on Graduate Students THE CRYSTAL STRUCTURE OF CAHNITE, Ca2 BAs04 (OH)4 Charles T. Prewitt Submitted to the Department of Geology on May 20, 1960 in partial fulfillment of the requirements for the degree of Master of Science. Cahnite is one of the few crystals which had been assigned to crystal class 4. A precession study showed that its diffraction sphol is 4/m I-/-, which contains space groups I4, I4E, and14/. Because of the known 4 morphology, it must be assigned to space group I4. The unit cell, whose dimensions are a = 7.11A, o = 6.201, contains two formula weights of Ca BAsO (OH)L. The structure was studied with the aid of in ensity medsurements made with a single-crystal diffractometer. Patterson s ntheses were first made for projections along the c, a, and 110 directions. The atomic numbers of the atoms are in the ratio As:Ca.0:B = 33:20:8:5, so that the Patterson peaks are dominated by the atom pairs containing arsenic as one member of the pair. Since there are only two arsenic atoms in a body-centered cell, one As can be arbitrarily assigned to the origin.
    [Show full text]
  • The Picking Table Volume 50, No. 2 – Fall 2009
    2009FallPT:Layout 1 8/27/2009 10:21 AM Page 1 JOURNAL OF THE FRANKLIN-OGDENSBURG MINERALOGICAL SOCIETY Volume 50, No. 2 – Fall 2009 $20.00 U.S. SPECIAL EDITION TH 50 ANNIVERSARY The contents of The Picking Table are licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. 2009FallPT:Layout 1 8/27/2009 10:21 AM Page 2 The Franklin-Ogdensburg Mineralogical Society, Inc. OFFICERS and STAFF 2009 PRESIDENT SLIDE COLLECTION CUSTODIAN Bill Truran Edward H. Wilk 2 Little Tarn Court, Hamburg, NJ 07419 202 Boiling Springs Avenue (973) 827-7804 E. Rutherford, NJ 07073 [email protected] (201) 438-8471 VICE-PRESIDENT TRUSTEES Richard Keller C. Richard Bieling (2009-2010) 13 Green Street, Franklin, NJ 07416 Richard C. Bostwick (2009-2010) (973) 209-4178 George Elling (2008-2009) [email protected] Steven M. Kuitems (2009-2010) Chester S. Lemanski, Jr. (2008-2009) SECOND VICE-PRESIDENT Lee Lowell (2008-2009) Joe Kaiser Earl Verbeek (2008-2009) 40 Castlewood Trail, Sparta, NJ 07871 Edward H. Wilk (2008-2009) (973) 729-0215 Fred Young (2008-2009) [email protected] LIAISON WITH THE EASTERN FEDERATION SECRETARY OF MINERALOGICAL AND LAPIDARY Tema J. Hecht SOCIETIES (EFMLS) 600 West 111TH Street, Apt. 11B Delegate Joe Kaiser New York, NY 10025 Alternate Richard C. Bostwick (212) 749-5817 (Home) (917) 903-4687 (Cell) COMMITTEE CHAIRPERSONS [email protected] Auditing William J. Trost Field Trip Warren Cummings TREASURER Historical John L. Baum Denise Kroth Mineral Exchange Richard C. Bostwick 240 Union Avenue Nominating William Kroth Wood-Ridge, NJ 07075 Program Fred Young (201) 933-3029 Swap & Sell Chester S.
    [Show full text]
  • Carbonatites of the World, Explored Deposits of Nb and REE—Database and Grade and Tonnage Models
    Carbonatites of the World, Explored Deposits of Nb and REE—Database and Grade and Tonnage Models By Vladimir I. Berger, Donald A. Singer, and Greta J. Orris Open-File Report 2009-1139 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2009 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod/ Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov/ Telephone: 1-888-ASK-USGS Suggested citation: Berger, V.I., Singer, D.A., and Orris, G.J., 2009, Carbonatites of the world, explored deposits of Nb and REE— database and grade and tonnage models: U.S. Geological Survey Open-File Report 2009-1139, 17 p. and database [http://pubs.usgs.gov/of/2009/1139/]. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. ii Contents Introduction 1 Rules Used 2 Data Fields 2 Preliminary analysis: —Grade and Tonnage Models 13 Acknowledgments 16 References 16 Figures Figure 1. Location of explored Nb– and REE–carbonatite deposits included in the database and grade and tonnage models 4 Figure 2. Cumulative frequency of ore tonnages of Nb– and REE–carbonatite deposits 14 Figure 3 Cumulative frequency of Nb2O5 grades of Nb– and REE–carbonatite deposits 15 Figure 4 Cumulative frequency of RE2O3 grades of Nb– and REE–carbonatite deposits 15 Figure 4 Cumulative frequency of P2O5 grades of Nb– and REE–carbonatite deposits 16 Tables Table 1.
    [Show full text]
  • B Clifford Frondel
    CATALOGUE OF. MINERAL PSEUDOMORPHS IN THE AMERICAN MUSEUM -B CLIFFORD FRONDEL BU.LLETIN OF THEAMRICANMUSEUM' OF NA.TURAL HISTORY. VOLUME LXVII, 1935- -ARTIC-LE IX- NEW YORK Tebruary 26, 1935 4 2 <~~~~~~~~~~~~~7 - A~~~~~~~~~~~~~~~, 4~~~~~~~~~~~~~~~~~~~~~~~~~~~~~4 4 4 A .~~~~~~~~~~~~~~~~~~~~~~~~~~4- -> " -~~~~~~~~~4~~. v-~~~~~~~~~~~~~~~~~~t V-~ ~~~~~~~~~~~~~~~~ 'W. - /7~~~~~~~~~~~~~~~~~~~~~~~~~~7 7-r ~~~~~~~~~-A~~~~ ~ ~ ~ ~ ~ ~ ~ ~ ~ -'c~ ~ ~ ' -7L~ ~ ~ ~ ~ 7 54.9:07 (74.71) Article IX.-CATALOGUE OF MINERAL PSEUDOMORPHS IN THE AMERICAN MUSEUM OF NATURAL HISTORY' BY CLIFFORD FRONDEL CONTENTS PAGE INTRODUCTION .................. 389 Definition.389 Literature.390 New Pseudomorphse .393 METHOD OF DESCRIPTION.393 ORIGIN OF SUBSTITUTION AND INCRUSTATION PSEUDOMORPHS.396 Colloidal Origin: Adsorption and Peptization.396 Conditions Controlling Peptization.401 Volume Relations.403 DESCRIPTION OF SPECIMENS.403 INTRODUCTION DEFINITION.-A pseudomorph is defined as a mineral which has the outward form proper to another species of mineral whose place it has taken through the action of some agency.2 This precise use of the term excludes the regular cavities left by the removal of a crystal from its matrix (molds), since these are voids and not solids,3 and would also exclude those cases in which organic material has been replaced by quartz or some other mineral because the original substance is here not a mineral. The general usage of the term is to include as pseudomorphs both petrifactions and molds, and also: (1) Any mineral change in which the outlines of the original mineral are preserved, whether this surface be a euhedral crystal form or the irregular bounding surface of an embedded grain or of an aggregate. (2) Any mineral change which has been accomplished without change of volume, as evidenced by the undistorted preservation of an original texture or structure, whether this be the equal volume replacement of a single crystal or of a rock mass on a geologic scale.
    [Show full text]
  • Ferricerite-(La) (La, Ce, Ca)9Fe (Sio4)3(Sio3oh)4(OH)3
    3+ Ferricerite-(La) (La, Ce, Ca)9Fe (SiO4)3(SiO3OH)4(OH)3 Crystal Data: Hexagonal. Point Group: 3m. Forms boxwork-like aggregates of equant to tabular crystals flattened on [00*1] to 2 mm with dominant rhombohedral and pinacoidal faces, as pseudomorphs after an unidentified hexagonal prismatic mineral. Physical Properties: Cleavage: None. Tenacity: Brittle. Fracture: Conchoidal. Hardness = 5 D(meas.) = 4.7(1) D(calc.) = 4.74 Optical Properties: Translucent. Color: Light yellow to pinkish brown. Streak: White. Luster: Vitreous. Optical Class: Uniaxial (+). ω = 1.810(5) ε = 1.820(5) Cell Data: Space Group: R3c. a = 10.7493(6) c = 38.318(3) Z = 6 X-ray Powder Pattern: Mt. Yuksporr, Khibina massif, Kola Peninsula, Russia. 2.958 (100), 3.47 (40), 3.31(38), 2.833 (37), 2.689 (34), 1.949 (34), 3.53 (26) Chemistry: (1) (2) La2O3 37.57 CaO 5.09 Ce2O3 23.67 Fe2O3 1.40 Pr2O3 0.61 MgO 0.51 Nd2O3 1.48 SiO2 22.38 Sm2O3 0.10 P2O5 0.63 Gd2O3 0.24 H2O 3.20 SrO 1.97 Total 98.85 (1) Mt. Yuksporr, Khibina massif, Kola Peninsula, Russia; average electron microprobe analysis supplemented by IR spectroscopy, H2O by Penfield method; corresponds to (La4.23Ce2.65Ca1.37Sr0.35 Nd0.16Pr0.07Gd0.02Sm0.01)Σ=8.86(Fe0.32Ca0.30Mg0.23)Σ=0.85[SiO4]3[(Si0.84P0.16)Σ=1.00O3(OH)]4(OH)2.78. Mineral Group: Cerite supergroup, cerite group. Occurrence: A late-stage, low-temperature secondary phase in a symmetrically zoned, aegirine- natrolite-microcline vein in gneissose foyaite.
    [Show full text]
  • Mineralogy and Crystal Structures of Barium Silicate Minerals
    MINERALOGY AND CRYSTAL STRUCTURES OF BARIUM SILICATE MINERALS FROM FRESNO COUNTY, CALIFORNIA by LAUREL CHRISTINE BASCIANO B.Sc. Honours, SSP (Geology), Queen's University, 1998 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE in THE FACULTY OF GRADUATE STUDIES (Department of Earth and Ocean Sciences) We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA December 1999 © Laurel Christine Basciano, 1999 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department of !PcX,rU\ a^/icJ OreO-^ Scf&PW The University of British Columbia Vancouver, Canada Date OeC S/79 DE-6 (2/88) Abstract The sanbornite deposits at Big Creek and Rush Creek, Fresno County, California are host to many rare barium silicates, including bigcreekite, UK6, walstromite and verplanckite. As part of this study I described the physical properties and solved the crystal structures of bigcreekite and UK6. In addition, I refined the crystal structures of walstromite and verplanckite. Bigcreekite, ideally BaSi205-4H20, is a newly identified mineral species that occurs along very thin transverse fractures in fairly well laminated quartz-rich sanbornite portions of the rock.
    [Show full text]
  • The Genesis of Zeolites
    Eur. J. Mineral. 1989,1,479-487 The genesis of zeolites GLAUCoGOTTARDIt* Istituto di Mineralogia e Petrologia, Università di Modena, via S. Eufemia 19,1-41100 Modena, Italy Abstract: The equilibrium diagrams of zeolites and the different possibilities of synthesizing zeolites starting from chemicals, minerals, and natural glasses are reviewed so to have a general picture of the conditions of crystallization of these minerals. Subsequently, a description and interpretation is given of the geological environments where zeolites crystallize in nature. Key-words: zeolite, diagenesis, very-low-grade metamorphism, hydrothermalism, volcanic glass. 1. Introduction and heulandite generally contain some M+ ca­ tions, which are almost absent in laumontite, yu­ This topic has been the subject of so many publi­ gawaralite and wairakite, so the alkali metal con­ cations (e.g. Hay, 1978, 1986; Iijima, 1978, 1980; centration in the system may influence the given Kastner & Stonecipher, 1978; Surdam & Shep- boundaries. Additional diagrams on these zeolites pard, 1978) over the last ten years, that one may can be found in the literature, but none is known wonder "Why another one?". As a matter of fact, to the author for zeolites other than those men­ all these previous studies give detailed informa­ tioned here. Field and laboratory evidence suggests tion on rock-forming zeolites, generally crystal­ that some other alkali zeolites may have a stabil­ lized from natural glasses during diagenesis, but ity field; this is certainly true for clinoptilolite, they omit any consideration of zeolites in veins the siliceous alkali-rich variant of heulandite, and and vugs of massive rocks. The author also aims is also probably true for natrolite and mordenite.
    [Show full text]
  • Chemical Composition of Ferrierite WILLIAM S. WISE 93/06
    American Mineralogist, Volume 61, pa ges 60-66, 1976 Chemical composition of ferrierite WILLIAM S. WISE Department of Geological Sciences, University of California Santa Barbara, California 93/06 AND R. W. TSCHERNICH 532 Avenue A, Snohomish, Washington 98920 Abstract Ferrierite specimens from localities at Altoona, Washington; Silver Mountain, Alpine County, California; and Pinaus Lake, Monte Lake, and Francois Lake, British Columbia, have been analyzed by microprobe methods. These new analyses are combined with available data to delineate the compositional range for this zeolite. The frame work composition ranges from (Al7•5Si27 5072) to (Al,Sia,072). The a cell dimension varies linearly with the Si content. There are between 3 and 5 exchangeable cations (univalent and divalent) per unit cell of 72 oxygens, but with wide variations; the amount of univale11t ions ranges from 21 to 85 percent. There is no clear parititioning of the univalent ions, as the Na/(Na+K) ratio is highly variable. Mg is clearly fractionated in all ferrierites (Ca/(Ca + Mg) < 0.40), regardless of the amount of divalent ions. The highest known amounts of BaO (2.54%) and SrO (0.40%) are in the Silver Mountain ferrierite. Associated zeolites commonly include clinoptilolite or heulandite, although mordenite and dachiardite also occur with ferrierite at Altoona. The broad compositional range of ferrierite indicates that it can crystallize from solutions with a wide variety of alkali and alkaline earth cations, none of which are essential to the zeolite. If present, Mg ions are fractionated into the zeolite. Ferrierite crystallizes in response to high silica activities. However, to account for the range in silica contents, the a810, must be coupled with other variables, such as temperature or aH,o, in order to prevent crystallization of other high silica zeolites.
    [Show full text]
  • A Specific Gravity Index for Minerats
    A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951).
    [Show full text]
  • ZINCIAN AEGIRINE-AUGITE and JEFFERSONITE from FRANKLIN, NEW JERSEY Cr.Rrnonofnonnbr Enn Jux Ho, Departmentof Geolog,Icalsciences, H Arsaril [] Niaer Sity Cambrid
    THE AMERICAN MINERALOGIST, VOL 51, SEPTEMBER_OCTOBER, 1966 ZINCIAN AEGIRINE-AUGITE AND JEFFERSONITE FROM FRANKLIN, NEW JERSEY Cr.rrnonoFnoNnBr eNn Jux ho, Departmentof Geolog,icalSciences, H arsaril [] niaer sity Cambrid. ge, M as s a chu s e tt s.r Agsrnect A coarsely crystallized dark colored monoclinic pyroxene found abundantly in skarn zones at Franklin and Sterling Hill, New Jersey, has long been known under the name jefiersonite. It has been classed as a diopsidic pyroxene, but four new chemical analyses (with accompanying r-ray and optical data) establish that it comprises highly zincian and manganoan members of a series from aegirine-augite to sodian and ferrian augite. Both Mn2+ and Zn are much in excess of Fe2f, with almost 40 atomic per cent Mn in the B position in one analysis. As Fea+and Na decrease the color changes from reddish brown and mahogany brown to dark olive green and greenish black. The original jefiersonite of Vanuxem and Keating (1822) probably referred to the latter material; the name lacks species or varietal significance and may be set aside. INtnooucuoN Three different types of pyroxene have been found in the so-called skarn zones in the orebodiesat Franklin and Sterling Hill, New Jersey. The most common type is a manganoan and sometimes also zincian variety of diopside. It generally contains NInO in the range from 4 to 10 weight per cent (Table 1, anal. 1 to 5). If little or Lo Zn is present,this material has been called schefierite,following the varietal name originally proposedby Michaelson(1863) for manganoandiopside of similar com- position from Langban, Sweden.
    [Show full text]