Investigation of Tho2 As a Structural Analogue for Spent Nuclear Fuel Dissolution Under Repository Conditions
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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 -
The Stability of Lead Isotopes from Thorium
MAY 24, I9I7] NATURE ---------------------------------------------------------245 but I Prof. Stefan lYle:yer may be I .have pointed out the unsuitability of makmg some exammatwn of the radiations of the thonum mmerals for age determination or correlation material, and the results he obtains will therefore be and this is particularly so i.n the case of minerals of very great value in deciding this point. the Palreozoic igneous rocks of Langesundfjord, Nor FREDERICK SoDDY. way. Mr. Lawson and myself based our former con Aberdeen, May 14. that lead could not be the end product of thonum largely on analyses of these minerals. How . PRO.F. SoDDY. having given me the privilege of read e:ver, I have recalculated the ratiQs on the assump mg h1s letter m advance, I should like to take the twn that thonum has one-seventh the lead-producing opportunity of directing attention to the geological age power of uranium, and it is satisfactory to find that :>f the thorium minerals of Ceylon, and to a few further when thorium is less than five times a·s abundant statistics bearing on the suggestion that only 35 per uranium, the ratios agree as closely on th'ts calculation cent. of thorium produces a stable isotope of lead. as do the simple lead-ratios. When thorium is more than five times as abundant as uranium neither set I a!ll to my friend, Mr. E. J. Wayland, late of ratios gives any approach to agreement although of Ceylon, for the follow mg prov1s1onal classdicat10n (in order of age) of the the minerals from anv one locality agree am'ong them older rocks of the island :- selves. -
Stillwellite-(Ce) (Ce, La, Ca)Bsio
Stillwellite-(Ce) (Ce; La; Ca)BSiO5 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Hexagonal. Point Group: 3: As °at rhombohedral crystals, to 4 cm, and massive. Twinning: Observed about [100]. Physical Properties: Cleavage: One imperfect. Fracture: Conchoidal. Hardness = 6.5 D(meas.) = 4.57{4.60 D(calc.) = 4.67 » Optical Properties: Transparent to translucent. Color: Red-brown to pale pink; colorless in thin section. Streak: White. Optical Class: Uniaxial (+) to biaxial (+). ! = 1.765{1.784 ² = 1.780{1.787 2V(meas.) = 0±{6± Cell Data: Space Group: P 31: a = 6.841{6.844 c = 6.700{6.702 Z = 3 X-ray Powder Pattern: Mary Kathleen mine, Australia. 3.43 (s), 2.96 (s), 2.13 (ms), 4.44 (m), 1.864 (m), 2.71 (mw), 2.24 (mw) Chemistry: (1) (2) (1) (2) (1) (2) SiO2 22.40 22.06 La2O3 27.95 19.12 MgO 0.06 UO2 0.22 Ce2O3 33.15 30.82 CaO 0.95 0.34 ThO2 5.41 Pr2O3 1.82 F 0.30 + B2O3 12.23 [13.46] Nd2O3 5.36 H2O 0.85 Al2O3 0.42 Sm2O3 0.34 H2O¡ 0.10 Y2O3 0.74 0.28 Fe2O3 0.18 P2O5 0.67 Total [100.00] [99.26] (1) Mary Kathleen mine, Australia; recalculated to 100.00% after removal of very small amounts of uraninite and apatite determined by separate analysis. (2) Vico volcano, near Vetralla, Italy; by electron microprobe, B2O3 calculated from stoichiometry, original total given as 99.23%; corresponds to (Ce0:50La0:31Nd0:08Th0:05Pr0:03Ca0:02Sm0:01)§=1:00B1:02Si0:97O5: Occurrence: Locally abundant as a metasomatic replacement of metamorphosed calcareous sediments (Mary Kathleen mine, Australia); in alkalic pegmatites in syenite in an alkalic massif (Dara-i-Pioz massif, Tajikistan). -
Radiological Significance of Thorium Processing in Manufacturing
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Thermodynamic Properties of Thorium Dioxide from 298 to 1200 Ok
JO URNAL OF RESEARCH of the National Bureau of Standards-A. Physics and Chemistry Vol. 65, No.2, March- April 1961 Thermodynamic Properties of Thorium Dioxide From 298 to 1,200 oK Andrew C. Victor and Thomas B. Douglas (November 26, 1960) As a step in developing new standards of he.at ca l ~ac i ty applicable up to very h~gh temperatures, t he heat content (enthalpy) of thol'lum dlOxldoe, I h02 , relatn:,e to 2~3 K , was accurately measured at ten temperatures from 323 to 1,173 K . A Bunsen 1.ce ca l ol'l~neter and a drop method were used to make t he mea ~ urements on two samples of ":ldely d Iff erent bulk densities. The corresponding heat-capacity values for the hIgher denSIty sample ~re represented within t heir uncertain ty (estimated to be ± 0.3 to 0.5 %) by the followlI1g empirical equation 1 (cal mole- I deg- I at T OK) : C ~ = 17 . 057 + 1 8. 06 ( 10 -4) T - 2.5166 (1 05)/1'2 At 298 oK t his equation agrees with previously reported low-temperatu.re measurements made with an adiabatic calorimeter. Values of heat content, heat capaelty, entropy, and Gibb's free energy function are tabulated from 298.15 t o 1,200 oK. 1. Introduction measll remen ts arc soon to be extended up to ap proximately 1,800 OK. Current practical and theoretical developm~l!ts However, at higher temperatures aluminum oxide have increased the need for accurate heat capaCltlOs is impractical as a heat standard, for it becomes and related thermal properties at high temp ~rature s, increasingly volatile, and melts at approximately yet the values reported for the same mat~nal from 2,300 OK. -
Extraction of Thorium Oxide from Monazite Ore
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Supervised Undergraduate Student Research Chancellor’s Honors Program Projects and Creative Work 5-2019 Extraction of Thorium Oxide from Monazite Ore Makalee Ruch University of Tennessee, Knoxville, [email protected] Chloe Frame University of Tennessee, Knoxville Molly Landon University of Tennessee, Knoxville Ralph Laurel University of Tennessee, Knoxville Annabelle Large University of Tennessee, Knoxville Follow this and additional works at: https://trace.tennessee.edu/utk_chanhonoproj Part of the Environmental Chemistry Commons, Geological Engineering Commons, and the Other Chemical Engineering Commons Recommended Citation Ruch, Makalee; Frame, Chloe; Landon, Molly; Laurel, Ralph; and Large, Annabelle, "Extraction of Thorium Oxide from Monazite Ore" (2019). Chancellor’s Honors Program Projects. https://trace.tennessee.edu/utk_chanhonoproj/2294 This Dissertation/Thesis is brought to you for free and open access by the Supervised Undergraduate Student Research and Creative Work at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Chancellor’s Honors Program Projects by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. Extraction of Thorium Oxide from Monazite Ore Dr. Robert Counce Department of Chemical and Biomolecular Engineering University of Tennessee Chloe Frame Molly Landon Annabel Large Ralph Laurel Makalee Ruch CBE 488: Honors -
Fabrication of Thorium and Thorium Dioxide
Natural Science, 2015, 7, 10-17 Published Online January 2015 in SciRes. http://www.scirp.org/journal/ns http://dx.doi.org/10.4236/ns.2015.71002 Fabrication of Thorium and Thorium Dioxide Balakrishna Palanki (Retired) Nuclear Fuel Complex, Hyderabad, India Email: [email protected] Received 10 November 2014; revised 9 December 2014; accepted 28 December 2014 Copyright © 2015 by author and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract Thorium based nuclear fuel is of immense interest to India by virtue of the abundance of Thorium and relative shortage of Uranium. Thorium metal tubes were being cold drawn using copper as cladding to prevent die seizure. After cold drawing, the copper was removed by dissolution in ni- tric acid. Thorium does not dissolve being passivated by nitric acid. Initially the copper cladding was carried out by inserting copper tubes inside and outside the thorium metal tube. In an inno- vative development, the mechanical cladding with copper was replaced by electroplated copper with a remarkable improvement in thorium tube acceptance rates. Oxalate derived thoria powder was found to require lower compaction pressures compared to ammonium diuranate derived urania powders to attain the same green compact density. However, the green pellets of thoria were fragile and chipped during handling. The strength improved after introducing a ball milling step before compaction and maintaining the green density above the specified value. Alternatively, binders were used later for greater handling strength. Magnesia was conventionally being used as dopant to enhance the sinterability of thoria. -
Crystallographic Study of Uranium-Thorium Bearing Minerals in Tranomaro, South-East Madagascar
Journal of Minerals and Materials Characterization and Engineering, 2013, 1, 347-352 Published Online November 2013 (http://www.scirp.org/journal/jmmce) http://dx.doi.org/10.4236/jmmce.2013.16053 Crystallographic Study of Uranium-Thorium Bearing Minerals in Tranomaro, South-East Madagascar Frank Elliot Sahoa1, Naivo Rabesiranana1*, Raoelina Andriambololona1, Nicolas Finck2, Christian Marquardt2, Hörst Geckeis2 1Institut National des Sciences et Techniques Nucléaires (Madagascar-INSTN), Antananarivo, Madagascar 2Institute of Nuclear Waste and Disposal (INE), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany Email: *[email protected] Received September 20, 2013; revised October 21, 2013; accepted November 5, 2013 Copyright © 2013 Frank Elliot Sahoa et al. This is an open access article distributed under the Creative Commons Attribution Li- cense, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. ABSTRACT Studies are undertaken to characterize the uranium and thorium minerals of south-east Madagascar. Seven selected uranothorianite bearing pyroxenites samples from old abandoned uranium quarries in Tranomaro, south Amboasary, Madagascar (46˚28'00"E, 24˚36'00"S) have been collected. To determine the mineral micro-structure, they were inves- tigated for qualitative identification of crystalline compounds by using X-ray powder diffraction analytical method (XRD). Results showed that the uranium and thorium compounds, as minor elements, were present in various crystal- line structures. Thorium, as thorianite, is present in a simple ThO2 cubic crystalline system, whereas the uranium com- ponent of the Tranomaro uranothorianite samples is oxide-based and is a mixture of complex oxidation states and crys- talline systems. Generally called uraninite, its oxide compounds are present in more than eight phases. -
Aec-Nasa Tech Brief
March 1969 Brief 69-10079 sty C AEC-NASA TECH BRIEF YES AEC-NASA Tech Briefs describe innovations resulting from the research and development program of the U.S. AEC or from AEC-NASA interagency efforts. They are issued to encourage commercial application. Tech Briefs are published by NASA and may be purchased, at 15 cents each, from the Clearinghouse for Federal Scientific and Technical Information, Springfield, Virginia 22151. Preparation of Thorium by Magnesium—Zinc Reduction Stirring Motor Ball Valve Stuffing Box Assembly Sampling Port - Water Annulus Graphitar Bearing 1___._Hea t Shields SST Shaft Ta Thermowell Graphite Secondary Crucible Heated Ta Shaft Graphite Pouring Mold Baffled Crucible^v I SST Shell Ta Paddle THORIUM DIOXIDE REDUCTION APPARATUS A technique for the preparation of thorium metal success of the process. by magnesium—zinc reduction of thorium dioxide has The present method for commercial production of been investigated on a laboratory scale. The extent thorium metal involves metallothermic reduction of of reduction was determined as a function of time, thorium tetrafluoride with calcium in the presence of amount and composition of flux, temperature, agita- zinc chloride. However, calcium is expensive as a re- tion, particle size of the oxide, and magnesium con- ductant and the process requires a prior hydro-fluo- centration in the alloy. It was found that the use of rination step. Using magnesium—zinc alloy for the a flux of the proper composition is essential to the reduction of thorium dioxide has potential economic (continued overleaf) This document was prepared under the sponsorship of the Atomic liability resulting from the use of the information contained in this Energy Commission and/or the National Aeronautics and Space document, or warrants that the use of any information, apparatus, Administration. -
Chemical Compatibility Storage Group
CHEMICAL SEGREGATION Chemicals are to be segregated into 11 different categories depending on the compatibility of that chemical with other chemicals The Storage Groups are as follows: Group A – Compatible Organic Acids Group B – Compatible Pyrophoric & Water Reactive Materials Group C – Compatible Inorganic Bases Group D – Compatible Organic Acids Group E – Compatible Oxidizers including Peroxides Group F– Compatible Inorganic Acids not including Oxidizers or Combustible Group G – Not Intrinsically Reactive or Flammable or Combustible Group J* – Poison Compressed Gases Group K* – Compatible Explosive or other highly Unstable Material Group L – Non-Reactive Flammable and Combustible, including solvents Group X* – Incompatible with ALL other storage groups The following is a list of chemicals and their compatibility storage codes. This is not a complete list of chemicals, but is provided to give examples of each storage group: Storage Group A 94‐75‐7 2,4‐D (2,4‐Dichlorophenoxyacetic acid) 94‐82‐6 2,4‐DB 609-99-4 3,5-Dinitrosalicylic acid 64‐19‐7 Acetic acid (Flammable liquid @ 102°F avoid alcohols, Amines, ox agents see SDS) 631-61-8 Acetic acid, Ammonium salt (Ammonium acetate) 108-24-7 Acetic anhydride (Flammable liquid @102°F avoid alcohols see SDS) 79‐10‐7 Acrylic acid Peroxide Former 65‐85‐0 Benzoic acid 98‐07‐7 Benzotrichloride 98‐88‐4 Benzoyl chloride 107-92-6 Butyric Acid 115‐28‐6 Chlorendic acid 79‐11‐8 Chloroacetic acid 627‐11‐2 Chloroethyl chloroformate 77‐92‐9 Citric acid 5949-29-1 Citric acid monohydrate 57-00-1 Creatine 20624-25-3 -
A Brief Overview Including Uses, Worldwide Resources, and Known Occurrences in Alaska
A brief overview including uses, worldwide resources, and known occurrences in Alaska Information Circular 61 David J. Szumigala and Melanie B. Werdon STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES Division of Geological & Geophysical Surveys (DGGS) 3354 College Road, Fairbanks, AK 99709-3707 www.dggs.alaska.gov COVER PHOTO CAPTIONS: TOP: Sheeted REE-bearing veins, Dotson Trend, Bokan Mountain property, Alaska. Photo from http://www.ucoreraremetals.com/docs/SME_2010_Keyser.pdf BOTTOM: Rare-earth-element-bearing quartz vein exposed in granite, Bokan Mountain, Alaska. Photo from http://www.ucoreraremetals.com/docs/SME_2010_Keyser.pdf RARE-EARTH ELEMENTS: A brief overview including uses, worldwide resources, and known occurrences in Alaska David J. Szumigala and Melanie B. Werdon GGS Minerals Program The Alaska Division of Geological & Geophysical Surveys (DGGS), part of the Department of Natural Resources, is charged by statute with determining the potential of Alaska’s land for production of metals, minerals, fuels, and geothermal resources; the locations and supplies of groundwater and construction Dmaterial; and the potential geologic hazards to buildings, roads, bridges, and other installations and structures. The Mineral Resources Section at DGGS collects, analyzes, and provides information on the geological and geophysical framework of Alaska as it pertains to the state’s mineral resources. The results of these studies include reports and maps, which are used by scientists for various associated studies, by mining company geologists as a basis for their more focused exploration programs, and by state and federal agency personnel in resource and land-use management decisions. This paper provides a brief overview of rare-earth elements, their uses, and current worldwide sources of their production. -
Uranothorite from Eastern Ontario1
URANOTHORITEFROM EASTERN ONTARIO1 S. C. ROBINSON2 eno SYDNEY ABBEYB Geol,og'ical, Survey of Canadn, Ottawa ABSTRACT Uranothorite is found in manydeposits of the Grenville sub-province in Ontario and Quebec, and in some mines.is an important ore mineral of uranium. Its occurrence, habit, and physical properties are reviewed. Analyses for eleven specimens of uran- othorite are presented and variations in analysesand physical properties are discussed. For chemical analysis, silica was separated by perchloric dehydration and lead by sulphide and sulphate precipitation. Uranium was determined by a cupferron-oxine method, thorium and rare eartfrs via oxalate and "thorin", iron with o-phenanthroline, and calcium by oxalate precipitation. Water was determined by a modified Penfield metJrod, carbon dioxide by acid evolution and total carbon by combustion, each on a separate sample. Panr I: OccunnBxcE AND DBscnrprroN (S.C.R.) Intrad,uction Uranoth5rite was first identified and analysed in Canada by H. V. Ellsworth (L927)4 in specimens from the MacDonald feldspar mine, near Hybla, Ontario. Since that time, it has been identified in many other deposits of the Grenville sub-province of the Canadian Shield, both in eastern Ontario and in southwestern Quebec. In the past four years uranothorite has emerged as a minor ore mineral of uranium in mines of the Bancroft-Wilberforce camp where uraninite is the principal source of uranium. Few additional data on uranothorite in Canada have been published since Ellsworth's original paper. In the course of a field project on the mineralogy of uranium deposits in the Bancroft-Wilberforce region by one of us (S.C.R.), it became obvious that although uranothorite is an important contributor of uranium in ores of some mines, knowledge of its occurrence and com- position was inadequate.