Extraction of Thorium Oxide from Monazite Ore
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Monazite Trumps Zircon: Applying SHRIMP U–Pb Geochronology To
Contrib Mineral Petrol (2017) 172:63 DOI 10.1007/s00410-017-1386-5 ORIGINAL PAPER Monazite trumps zircon: applying SHRIMP U–Pb geochronology to systematically evaluate emplacement ages of leucocratic, low-temperature granites in a complex Precambrian orogen Agnieszka M. Piechocka1 · Courtney J. Gregory1 · Jian-Wei Zi1 · Stephen Sheppard1 · Michael T. D. Wingate2 · Birger Rasmussen1 Received: 13 January 2017 / Accepted: 24 June 2017 / Published online: 7 July 2017 © The Author(s) 2017. This article is an open access publication Abstract Although zircon is the most widely used geochro- U–Pb zircon dating of these leucocratic granites either yielded nometer to determine the crystallisation ages of granites, it can ages that were inconclusive (e.g., multiple concordant ages) or be unreliable for low-temperature melts because they may not incompatible with other geochronological data. To overcome crystallise new zircon. For leucocratic granites U–Pb zircon this we used SHRIMP U–Th–Pb monazite geochronology to dates, therefore, may refect the ages of the source rocks rather obtain igneous crystallisation ages that are consistent with the than the igneous crystallisation age. In the Proterozoic Cap- geological and geochronological framework of the orogen. ricorn Orogen of Western Australia, leucocratic granites are The U–Th–Pb monazite geochronology has resolved the time associated with several pulses of intracontinental magmatism interval over which two granitic supersuites were emplaced; a spanning ~800 million years. In several instances, SHRIMP Paleoproterozoic supersuite thought to span ~80 million years was emplaced in less than half that time (1688–1659 Ma) and a small Meso- to Neoproterozoic supersuite considered to Communicated by Franck Poitrasson. -
Llallagua Tin Ore Deposit (Bolivia)
resources Article Speculations Linking Monazite Compositions to Origin: Llallagua Tin Ore Deposit (Bolivia) Elizabeth J. Catlos * and Nathan R. Miller Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, 1 University Sta. C9000, EPS 1.130, Austin, TX 78712, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-512-471-4762 Received: 3 May 2017; Accepted: 25 July 2017; Published: 29 July 2017 Abstract: Monazite [(Ce,Th)PO4] from the Llallagua tin ore deposit in Bolivia is characterized by low radiogenic element contents. Previously reported field evidence and mineral associations suggest the mineral formed via direct precipitation from hydrothermal fluids. Monazite compositions thus may provide insight into characteristics of the fluids from which it formed. Chemical compositions of three Llallagua monazite grains were obtained using Electron Probe Microanalysis (EPMA, n = 64) and laser ablation mass spectrometry (LA-ICP-MS, n = 56). The mineral has higher amounts of U (123 ± 17 ppm) than Th (39 ± 20 ppm) (LA-ICP-MS, ±1σ). Grains have the highest amounts of fluorine ever reported for monazite (0.88 ± 0.10 wt %, EPMA, ±1σ), and F-rich fluids are effective mobilizers of rare earth elements (REEs), Y, and Th. The monazite has high Eu contents and positive Eu anomalies, consistent with formation in a highly-reducing back-arc environment. We speculate that F, Ca, Si and REE may have been supplied via dissolution of pre-existing fluorapatite. Llallagua monazite oscillatory zoning is controlled by an interplay of low (P + Ca + Si + Y) and high atomic number (REE) elements. -
Inelastic Collisions of Atomic Thorium and Molecular Thorium Monoxide with Cold Helium-3
Inelastic collisions of atomic thorium and molecular thorium monoxide with cold helium-3 The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Au, Yat Shan. 2014. Inelastic collisions of atomic thorium and molecular thorium monoxide with cold helium-3. Doctoral dissertation, Harvard University. Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:12274226 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA Inelastic Collisions of Atomic Thorium and Molecular Thorium Monoxide with Cold Helium-3 A dissertation presented by Yat Shan Au to The Department of Physics in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the subject of Physics Harvard University Cambridge, Massachusetts November 2013 c 2013 - Yat Shan Au All rights reserved. Dissertation advisor Author Professor John Morrissey Doyle Yat Shan Au Inelastic Collisions of Atomic Thorium and Molecular Thorium Monoxide with Cold Helium-3 Abstract We measure inelastic cross sections for atomic thorium (Th) and molecular thorium monoxide (ThO) in collisions with 3He at temperatures near 1 K. We determine the 3 −17 −2 Zeeman relaxation cross section for Th ( F2) to be ∼ 2 × 10 cm at 800 mK. 3 We study electronic inelastic processes in Th ( P0) and find no quenching even after 106 collisions at 800 mK. We measure the vibrational quenching cross section for ThO (X, ν = 1) to be (7:9 ± 2:7) × 10−19 cm−2 at 800 mK. -
1 REVISION #3 Generalizations About Monazite: Implications For
1 1 REVISION #3 2 Generalizations about monazite: Implications for geochronologic studies 3 Elizabeth J. Catlos 4 University of Texas at Austin, Jackson School of Geosciences, Dept. of Geological Sciences, 1 5 University Sta. C9000 EPS 1.130, Austin, TX 78712, USA 6 Abstract. With the advent of techniques that preclude mineral separation, ages from specific 7 compositional domains in monazite [(Ce, La, Th)PO4] have provided a wealth of information 8 regarding the timing of the geologic evolution of numerous regions. However, confusion can 9 arise when single grains show large differences in age that fail to correlate to chemistry or 10 location within the monazite. Generalizations that lead to incorrect age interpretations include 11 that monazite zoning in Y, Th, and/or the rare earth elements (REE) always identify (1) distinct 12 tectonic events, (2) environment of crystallization, and (3) provenance of detrital grains. 13 Increasing Th contents in monazite do not always reflect (1) increasing grade in metamorphic 14 grains, (2) changes in silicate melt composition in igneous grains, (3) make the mineral more 15 susceptible to alteration, nor (4) control the mineral’s uptake of REE. Metamorphic monazites 16 from Himalayan garnet-bearing rocks with co-existing allanite show no relationship between Th 17 content and REE. Instead, chondrite-normalized REE patterns of the allanite mirror those of the 18 monazite, indicating the variations are related to the reactant that formed the mineral. 19 Generalizations about Pb behavior in monazite remain problematic. Incorporation of Pb into 20 monazite has thus far been precluded by experimental studies, yet common Pb has been 21 measured in many studies of natural monazite. -
Radiological Significance of Thorium Processing in Manufacturing
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Alteration of Magmatic Monazite In
Title: Alteration of magmatic monazite in granitoids from the Ryoke belt (SW Japan): processes and consequences Manuscript Number: 7025R - CORRECTION Authors: Etienne Skrzypek, University of Graz Shuhei Sakata, Gakushuin University Dominik Sorger, University of Graz 1 Alteration of magmatic monazite in granitoids from the Ryoke belt (SW Japan): 2 processes and consequences 3 4 REVISION 1 st 5 Corrected October 31 2019 6 1,2* 3 2 7 ETIENNE SKRZYPEK , SHUHEI SAKATA AND DOMINIK SORGER 8 1Department of Geology and Mineralogy, Graduate School of Science, Kyoto University, 9 Kitashirakawa-Oiwakecho, Sakyo-ku, Kyoto 606-8502, Japan 10 2Department of Petrology and Geochemistry, NAWI Graz Geocenter, University of Graz, 11 Universitätsplatz 2, 8010 Graz, Austria 12 3Department of Chemistry, Faculty of Science, Gakushuin University, 1-5-1 Mejiro, Toshima- 13 ku, Tokyo 171-8588, Japan 14 * E-mail: [email protected] 15 16 Running title: Alteration of magmatic monazite 17 18 With 7 figures and 2 tables 19 1 1 20 ABSTRACT 21 The alteration of magmatic monazite and its consequences for monazite geochronology are 22 explored in granitoids from the western part of the Ryoke belt (Iwakuni-Yanai area, SW 23 Japan). Biotite-granite samples were collected in two plutons emplaced slightly before the 24 main tectono-metamorphic event: one, a massive granite (Shimokuhara) adjoins schistose 25 rocks affected by greenschist facies metamorphism; and the second, a gneissose granite 26 (Namera) adjoins migmatitic gneiss that experienced upper-amphibolite facies conditions. 27 Despite contrasting textures, the granite samples have similar mineral modes and 28 compositions. Monazite in the massive granite is dominated by primary domains with limited 29 secondary recrystallization along cracks and veinlets. -
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. -
Redox-Controlled Dissolution of Monazite in Fluids and Implications
1 2 submitted to American Mineralogist 3 4 5 Redox-controlled dissolution of monazite in 6 fluids and implications for phase stability 7 in the lithosphere 8 9 10 11 Dustin Trail1,2*, 12 13 1Department of Earth & Environmental Sciences 14 University of Rochester, Rochester, NY 14627, USA 15 16 2Department of Earth, Planetary and Space Sciences, 17 University of California, Los Angeles, CA, USA 18 19 20 * [email protected]; ph 585 276 7182 21 22 23 24 Submitted 9/6/2017 25 26 Revision 1, ms #6296, revised 11/26/17 27 28 29 30 31 32 33 34 35 36 37 38 Keywords: monazite, solubility, incongruent dissolution, oxygen fugacity 39 40 1 41 Abstract 42 Monazite is an important host of rare earth elements in the lithosphere, including redox-sensitive 43 Ce, which may occur as trivalent and tetravalent in terrestrial environments. Here, monazite 44 solubility is explored as a function of oxygen fugacity through a series of dissolution experiments o 45 in alkali-rich and H2O fluids at 925 C and 1.5 GPa. The oxygen fugacity was controlled with 7 46 different solid-state buffers, and ranged from about the iron-wüstite to above the magnetite- 47 hematite equilibrium reactions. The solubility of natural monazite increases monotonically at 48 oxygen fugacities equal to or higher than the fayalite-magnetite-quartz equilibrium. Electron 49 microscopy reveals incongruent dissolution at Ni-NiO and above, where Ce-oxide is observed with 50 monazite as a stable phase. Solubility experiments were also conducted with synthetic crystals 51 (CePO4, LaPO4, Th+Si-doped monazite). -
Thorium Substitution in Monazite: Case Studies and Forward Modelling
Thorium substitution in monazite: case studies and forward modelling Megan A. Williams Department of Earth Sciences School of Physical Sciences University of Adelaide This Thesis is submitted in fullfi llment of the requirements for the degree of Doctor of Philosophy December 2019 Table of Contents Abstract vii Declaration viii Publications arising from this thesis ix Acknowledgements xi Chapter 1: Signifi cance and aims of this thesis xv Chapter outlines xviii Chapter 2: Thorium distribution in the crust: outcrop and grain scale perspectives 3 Abstract 3 1 Introduction 3 2 Geological background 3 3 Sample selection 5 4 Methods 5 4.1 Whole rock geochemistry 5 4.2 In fi eld Gamma ray Spectrometry (in fi eld GRS) 5 4.3 Mineral Liberation Analysis (MLA) 6 4.4 Electron Probe Microanalysis (EPMA) 6 5 Results 7 5.1 Whole rock geochemistry 7 5.2 In fi eld GRS 7 5.4 EPMA 12 6 Discussion 15 6.1 Melt loss and the preservation of monazite 15 6.2 Bulk rock trends in thorium distribution 15 6.3 Monazite distribution at Mt Staff ord 16 6.4 Monazite forming reactions 17 6.5 Grain scale trends in thorium distribution 18 6.6 Retention of thorium in granulite facies terranes 19 7 Conclusions 20 Acknowledgements 20 Supporting Information 20 References 20 Appendix S2.1: Whole rock geochemistry for Mt Staff ord samples. 22 Chapter 3: Thorium zoning in monazite: a case study from the Ivrea Verbano Zone, NW Italy 29 i Abstract 29 1 Introduction 29 2 Geological setting 30 3 Mineral assemblages and textures in metapelites 32 4 Sample selection 32 5 Methods 33 5.1 Whole -
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. -
Shocked Monazite Chronometry: Integrating Microstructural and in Situ Isotopic Age Data for Determining Precise Impact Ages
Contrib Mineral Petrol (2017) 172:11 DOI 10.1007/s00410-017-1328-2 ORIGINAL PAPER Shocked monazite chronometry: integrating microstructural and in situ isotopic age data for determining precise impact ages Timmons M. Erickson1 · Nicholas E. Timms1 · Christopher L. Kirkland1 · Eric Tohver2 · Aaron J. Cavosie1,3 · Mark A. Pearce4 · Steven M. Reddy1 Received: 30 August 2016 / Accepted: 10 January 2017 © Springer-Verlag Berlin Heidelberg 2017 Monazite is a robust geochronometer and {110}, {212}, and type two (irrational) twin planes with Abstract ̄ ̄ ̄ ̄ occurs in a wide range of rock types. Monazite also records rational shear directions in [011] and [110]. SIMS U–Th– shock deformation from meteorite impact but the effects Pb analyses of the plastically deformed parent domains of impact-related microstructures on the U–Th–Pb sys- reveal discordant age arrays, where discordance scales with tematics remain poorly constrained. We have, therefore, increasing plastic strain. The correlation between discord- analyzed shock-deformed monazite grains from the central ance and strain is likely a result of the formation of fast uplift of the Vredefort impact structure, South Africa, and diffusion pathways during the shock event. Neoblasts in impact melt from the Araguainha impact structure, Brazil, granular monazite domains are strain-free, having grown using electron backscatter diffraction, electron microprobe during the impact events via consumption of strained par- elemental mapping, and secondary ion mass spectrometry ent grains. Neoblastic monazite from the Inlandsee leu- (SIMS). Crystallographic orientation mapping of monazite cogranofels at Vredefort records a 207Pb/206Pb age of grains from both impact structures reveals a similar com- 2010 ± 15 Ma (2σ, n = 9), consistent with previous impact bination of crystal-plastic deformation features, includ- age estimates of 2020 Ma. -
Actinide Arene-Metalates: Ion Pairing Effects on the Electronic Structure of Unsupported Uranium- Arene Sandwich Complexes
Actinide Arene-Metalates: Ion Pairing Effects on the Electronic Structure of Unsupported Uranium- Arene Sandwich Complexes Jesse Murillo,† Rina Bhowmick,‡ Katie L. M. Harriman,ǁ Alejandra Gomez-Torres,† Joshua Wright,¥ Robert W. Meulenberg,± Pere Miró,‡ Alejandro Metta-Magaña,† Muralee Murugesu,ǁ Bess Vlaisavljevich,*,‡ and Skye Fortier*,† †Department of Chemistry and Biochemistry, University of Texas at El Paso, El Paso, Texas 79968, United States ‡Department of Chemistry, University of South Dakota, Vermillion, South Dakota 57069, United States ǁDepartment of Chemistry and Biomolecular Sciences, University of Ottawa, Ottawa, Ontario K1N 6N5, Canada ¥ Department of Physics, Illinois Institute of Technology, Chicago, IL, 60616, United States ± Department of Physics and Astronomy and Frontier Institute for Research in Sensor Technologies, University of Maine, Orono, ME, 04469, United States ABSTRACT: Chatt reaction methods were employed to synthesize the first well characterized actinide-arene sand- wich complexes. Namely, addition of [UI2(THF)3(μ-OMe)]2⸱THF (2⸱THF) to THF solutions containing 6 equiv. 6 4 of K[C14H10] generates the dimeric complexes [K(18-crown-6)(THF)2]2[U(η -C14H10)(η -C14H10)(μ-OMe)]2⸱4THF 18C6 6 4 THF (1 ⸱4THF) and {[K(THF)3][U(η -C14H10)(η -C14H10)(μ-OMe)]}2 (1 ) upon crystallization of the products in THF in the presence or absence of 18-crown-6, respectively. Both 118C6⸱4THF and 1THF are thermally stable in the solid-state at room temperature; however, after crystallization, they become insoluble in THF or DME solutions and instead gradually decompose upon standing. X-ray diffraction analysis reveals 118C6⸱4THF and 1THF to be structurally similar, possessing uranium centers sandwiched between anthracene ligands of mixed tetrahapto and hexahapto ligation modes.