Summary of Uranium Solubility Studies in Concrete Waste Forms and Vadose Zone Environments
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Françoisite-(Ce)
American Mineralogist, Volume 95, pages 1527–1532, 2010 Françoisite-(Ce), a new mineral species from La Creusaz uranium deposit (Valais, Switzerland) and from Radium Ridge (Flinders Ranges, South Australia): Description and genesis NICOLAS MEISSER,1,* JOËL BRUGGER,2,3 STEFA N AN SER M ET ,1 PHILI pp E THÉLI N ,4 A N D FRA N ÇOIS BUSSY 5 1Musée de Géologie and Laboratoire des Rayons-X, Institut de Minéralogie et de Géochimie, UNIL, Anthropole, CH-1015 Lausanne-Dorigny, Switzerland 2South Australian Museum, North Terrace, 5000 Adelaide, Australia 3TRaX, School of Earth and Environmental Sciences, University of Adelaide, 5005 Adelaide, Australia 4Laboratoire des Rayons-X, Institut de Minéralogie et de Géochimie, UNIL, Anthropole, CH-1015 Lausanne-Dorigny, Switzerland 5Laboratoire de la microsonde électronique, Institut de Minéralogie et de Géochimie, UNIL, Anthropole, CH-1015 Lausanne-Dorigny, Switzerland AB STRACT The new mineral françoisite-(Ce), (Ce,Nd,Ca)[(UO2)3O(OH)(PO4)2]·6H2O is the Ce-analog of françoisite-(Nd). It has been discovered simultaneously at the La Creusaz uranium deposit near Les Marécottes in Valais, Switzerland, and at the Number 2 uranium Workings, Radium Ridge near Mt. Painter, Arkaroola area, Northern Flinders Ranges in South Australia. Françoisite-(Ce) is a uranyl- bearing supergene mineral that results from the alteration under oxidative conditions of REE- and U4+- bearing hypogene minerals: allanite-(Ce), monazite-(Ce), ±uraninite at Les Marécottes; monazite-(Ce), ishikawaite-samarskite, and an unknown primary U-mineral at Radium Ridge. The REE composition of françoisite-(Ce) results from a short aqueous transport of REE leached out of primary minerals [most likely monazite-(Ce) at Radium Ridge and allanite-(Ce) at La Creusaz], with fractionation among REE resulting mainly from aqueous transport, with only limited Ce loss due to oxidation to Ce4+ during transport. -
Uraninite Alteration in an Oxidizing Environment and Its Relevance to the Disposal of Spent Nuclear Fuel
TECHNICAL REPORT 91-15 Uraninite alteration in an oxidizing environment and its relevance to the disposal of spent nuclear fuel Robert Finch, Rodney Ewing Department of Geology, University of New Mexico December 1990 SVENSK KÄRNBRÄNSLEHANTERING AB SWEDISH NUCLEAR FUEL AND WASTE MANAGEMENT CO BOX 5864 S-102 48 STOCKHOLM TEL 08-665 28 00 TELEX 13108 SKB S TELEFAX 08-661 57 19 original contains color illustrations URANINITE ALTERATION IN AN OXIDIZING ENVIRONMENT AND ITS RELEVANCE TO THE DISPOSAL OF SPENT NUCLEAR FUEL Robert Finch, Rodney Ewing Department of Geology, University of New Mexico December 1990 This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the author (s) and do not necessarily coincide with those of the client. Information on SKB technical reports from 1977-1978 (TR 121), 1979 (TR 79-28), 1980 (TR 80-26), 1981 (TR 81-17), 1982 (TR 82-28), 1983 (TR 83-77), 1984 (TR 85-01), 1985 (TR 85-20), 1986 (TR 86-31), 1987 (TR 87-33), 1988 (TR 88-32) and 1989 (TR 89-40) is available through SKB. URANINITE ALTERATION IN AN OXIDIZING ENVIRONMENT AND ITS RELEVANCE TO THE DISPOSAL OF SPENT NUCLEAR FUEL Robert Finch Rodney Ewing Department of Geology University of New Mexico Submitted to Svensk Kämbränslehantering AB (SKB) December 21,1990 ABSTRACT Uraninite is a natural analogue for spent nuclear fuel because of similarities in structure (both are fluorite structure types) and chemistry (both are nominally UOJ. Effective assessment of the long-term behavior of spent fuel in a geologic repository requires a knowledge of the corrosion products produced in that environment. -
Weeksite K2(UO2)2(Si5o13)·4H2O
Weeksite K2(UO2)2(Si5O13)·4H2O Crystal Data: Monoclinic. Point Group: 2/m: As bladed or acicular crystals, flattened on {010} and elongated along [001], and as flat plates; also as spherulites and radiating fibrous clusters. - Twinning: By two-fold rotation around [401 ]. Physical Properties: Cleavage: Two good prismatic cleavages noted. Hardness = < 2 D(meas.) = ~ 4.1 D(calc.) = 3.80 Radioactive. Optical Properties: Transparent to translucent. Color: Yellow. Luster: Waxy to silky. Optical Class: Biaxial (-). α = 1.596 β = 1.603 γ = 1.606 2V(meas.) = ~ 60° 2V(calc.) = 66° Pleochroism: X = colorless, Y = pale yellow-green, Z = yellow-green. Dispersion: r > v, strong. Orientation: X = b, Y = c, Z = a. Cell Data: Space Group: C2/m. a = 14.26(2) b = 35.88(10) c = 14.20(2) β = 111.578(3)° Z = 4 X-ray Powder Pattern: Thomas Range, Utah, USA. 7.11 (10), 5.57 (9), 8.98 (8), 3.55 (7), 3.30 (7), 2.91 (6), 3.20 (5) Chemistry: (1) (1) Na2O 0.53 Al2O3 0.6 K2O 4.73 SiO2 29.44 CaO 0.67 UO3 55.78 BaO 3.11 H2O [7.02] MgO 0.18 Total 101.28 SrO 0.20 (1) Anderson mine, Arizona, USA; average of 8 electron microprobe analyses, supplemented by TGA, H2O calculated from structure, corresponds to (K1.031Na0.176Ca0.123Ba0.208)Σ=1.537(UO2)2.002 (Si5.030O13)·4H2O. Occurrence: In “opal" veinlets in rhyolite, agglomerates, sandstones and limestones. Association: “Opal," “chalcedony," calcite, gypsum, fluorite, uraninite, thorogummite, uranophane, boltwoodite, carnotite, margaritasite. Distribution: In the USA, in Utah, at the Autunite No. -
Uranium Dioxide Is Voluminous
r>r 19 i o% ORNL-4755 UC-25 - Metals, Ceramics, and Materials s <-;. CONVERSIOH OF V&&4VWA NITRATE TO i aRAMlC-OR^Dt OXIDE>fs6t THE U&HT W4TBT J- -« .•'--• "" * -„ -' r J* - J * \ ^ --; f % ;~, <r- 4>- >» N< DMSICH0F DAfE -,i M\OH CAR6IDE COft^0tATtOR. U.S. ATOMIC *N**0T COMMAS»OIV 9>f & ^ima®tf»T^^*tB iwww® 1 PH^sarf in «*£ Uf9t«t Stress e* America. A vatfatt» from ---Sri*; -3K- >f ~ - - i ,43^>*£«* «^ ixn^ar»# ac «*, mts&mf of work {passaged b? tfw Lhnw XtitNr tfgr *}~ti$*i $**m «ar t!» untod Soto* Aflymic ^ «^ awy ^ iftw^r itT»i&y*OT« nor mf sd ihev canifiesscs.. ^iU- >*• ^H^ **•-» *-*• V .24, i *~ eta* -4-T" * iL - - IBS kfiE- r-„- 2 • «. "« J" '»' i - ^r'-s^j. •NOTICt ORNL-4755 Contract No. W-7405-eng-26 METAI5 AND CERAMICS DIVISION CONVERSION OF URANIUM NITRATE TO CERAMIC-GRADE OXIDE FOR THE LIGHT WATER ESEEDER REACTOR: PROCESS DEVELOPMENT J. M. Leitnaker M. L. Smith C. M. Fitzpatrick APRIL 1972 OAK RIDGE NATIONAL LABORATORY Oak Ridge, Tennessee 37830 operated by UNION CARBIDE CORPORATIOJN for the U.S. ATOMIC ENERGY COMMISSION W5TWBUTI0N OF THIS DOCUMENT IS UftUMflli iii CONTENTS Page Abstract 1 Introduction 1 Previous Investigations - 3 Stabilisation 4 Behavior of IXfe in Dry Air or Oxygen at Lev Tenpera&ures . 5 Behavior of UCfe in Dry Air or Oxygen at High Temperatures . 5 Behavior of DC^ in Hoist Air 7 Stabilisation of UO2 by Control of Surface Area 7 Stabilization by Addition of Moisture 11 Stabilization of UO2 with Dry Ice 12 Mechanical Stabilization of UO2 13 Reduction of Uranate to UO2 14 General Process Description . -
The Reduced Uraniferous Mineralizations Associated with the Volcanic Rocks of the Sierra Pena Blanca (Chihuahua, Mexico)
American Mineralogist, Volume 70, pages 1290-1297, 1985 The reduced uraniferous mineralizations associated with the volcanic rocks of the Sierra Pena Blanca (Chihuahua, Mexico) BRtcIrrn ANru, Centre de Recherchessur la Giologie de I'Urqnium BP 23, 54 5 0 1, V andoeuure-les-Nancy C6dex, F rance ,lwo hcquns LERoY Centre de Recherchessur la Giologie de l'Uranium BP 23,54501, Vaniloeuure-les-Nancy Cidex, France and Ecole Nationale Supirieure ile Gdologie Appliquie et de Prospection Miniire ile Nancy, BP 452,54001, Nancy Cidex, France Abstrect The uraniferousmineralizations of the Nopal I deposit (Sierra Pena Blanca, Chihuahua, Mexico) are related to a breccia pipe in a tertiary vitroclastic tuff (Nopal Formation). De- tailed mineralogicaland fluid inclusion studies led to the discovery of a primary mineral- ization stageof tetravalenturanium as part of an ilmenite-hematitephase. This stageoccurs soon after the depositionof the tuff and is relatedto H2O-CO, N, fluids, similar to those of the vapor phase,under temperaturesranging from 300 to 350'C. The well developedkaolini- zation of the Nopal tuff is associatedwith a secondtetravalent uranium stage(pitchblende- pyrite association).Fluids are aqueousand their temperatureranges from 250 to 200'C. The precipitation of pitchblende with pyrite within the pipe is due to a HrS activity increase strictlylimited to this structure.The remainderof mineralizingevents, either hydrothermal or supergene,led to the hexavalenturanium minerals that prevailtoday. Introduction of Chihuahua city. This Sierra -
Iidentilica2tion and Occurrence of Uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals from the Colorado Plateaus
IIdentilica2tion and occurrence of uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals From the Colorado Plateaus c By A. D. WEEKS and M. E. THOMPSON A CONTRIBUTION TO THE GEOLOGY OF URANIUM GEOLOGICAL S U R V E Y BULL E TIN 1009-B For jeld geologists and others having few laboratory facilities.- This report concerns work done on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE- INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan. Director Reprint, 1957 For sale by the Superintendent of Documents, U. S. Government Printing Ofice Washington 25, D. C. - Price 25 cents (paper cover) CONTENTS Page 13 13 13 14 14 14 15 15 15 15 16 16 17 17 17 18 18 19 20 21 21 22 23 24 25 25 26 27 28 29 29 30 30 31 32 33 33 34 35 36 37 38 39 , 40 41 42 42 1v CONTENTS Page 46 47 48 49 50 50 51 52 53 54 54 55 56 56 57 58 58 59 62 TABLES TABLE1. Optical properties of uranium minerals ______________________ 44 2. List of mine and mining district names showing county and State________________________________________---------- 60 IDENTIFICATION AND OCCURRENCE OF URANIUM AND VANADIUM MINERALS FROM THE COLORADO PLATEAUS By A. D. WEEKSand M. E. THOMPSON ABSTRACT This report, designed to make available to field geologists and others informa- tion obtained in recent investigations by the Geological Survey on identification and occurrence of uranium minerals of the Colorado Plateaus, contains descrip- tions of the physical properties, X-ray data, and in some instances results of chem- ical and spectrographic analysis of 48 uranium arid vanadium minerals. -
Journal of Luminescence 210 (2019) 425–434
Journal of Luminescence 210 (2019) 425–434 Contents lists available at ScienceDirect Journal of Luminescence journal homepage: www.elsevier.com/locate/jlumin Insight into the effect of A-site cations on structural and optical properties of T RE2Hf2O7:U nanoparticles ∗ Maya Abdoua, Santosh K. Guptaa,b, Jose P. Zunigaa, Yuanbing Maoa,c, a Department of Chemistry, University of Texas Rio Grande Valley, 1201 West University Drive, Edinburg, TX, 78539, USA b Radiochemistry Division, Bhabha Atomic Research Centre, Trombay, Mumbai, 400085, India c School of Earth, Environmental, and Marine Sciences, University of Texas Rio Grande Valley, 1201 West University Drive, Edinburg, TX, 78539, USA ARTICLE INFO ABSTRACT Keywords: A2B2O7 type pyrochlores have been recently proposed as a potential nuclear waste host due to their many Uranium interesting properties. To assess and understand the performance of these compounds as nuclear waste hosts, the Pyrochlore speciation and structural investigations on actinide-doped RE2Hf2O7 are needed since both are imperative from Phase-transition their application perspective. In this work, we investigated the effect of uranium doping at different con- Luminescence centrations in the range of 0–10% on the structural and optical properties of RE Hf O :U (RE = Y, Gd, Nd, and Cotunnite 2 2 7 Lu) nanoparticles (NPs). The Y2Hf2O7 NPs exist in slightly disordered pyrochlore structure and the extent of disordering increases as a function of uranium doping while the structure reaches a cotunnite phase at 10.0% doping level. The Nd2Hf2O7 NPs also exist in a distorted pyrochlore structure and their distortion increases with increasing uranium doping inducing a phase transition into a disordered fluorite structure at 10.0% uranium doping. -
Revision 1 Manuscript Submitted To
This is a preprint, the final version is subject to change, of the American Mineralogist (MSA) Cite as Authors (Year) Title. American Mineralogist, in press. (DOI will not work until issue is live.) DOI: http://dx.doi.org/10.2138/am.2013.4295 10/3 1 Revision 1 2 3 Manuscript submitted to the Special Section: 4 "Mineralogy and the Nuclear Industry: Actinides in 5 Geology, Energy, and the Environment" 6 7 8 9 10 Evidence for nanocrystals of vorlanite, a rare uranate mineral, in the Nopal I low- 11 temperature uranium deposit (Sierra Peña Blanca, Mexico) 12 Guillaume Othmane,1,* Thierry Allard,1 Nicolas Menguy,1 Guillaume Morin,1 Imène Esteve,1 13 Mostafa Fayek,2 and Georges Calas1 14 15 1 Institut de Minéralogie et de Physique des Milieux Condensés (IMPMC), UMR 7590 16 CNRS-UPMC/Paris VI-IRD, Case 115, 4 place Jussieu, 75252 Paris Cedex 05, France 17 18 2 Dept. of Geological Sciences, University of Manitoba, Winnipeg, MB, Canada R3T 2N2 19 20 * E-mail: [email protected] 21 1 Always consult and cite the final, published document. See http://www.minsocam.org or GeoscienceWorld This is a preprint, the final version is subject to change, of the American Mineralogist (MSA) Cite as Authors (Year) Title. American Mineralogist, in press. (DOI will not work until issue is live.) DOI: http://dx.doi.org/10.2138/am.2013.4295 10/3 22 ABSTRACT 23 The occurence of vorlanite, cubic CaUO4, is reported in the Nopal I uranium deposit 24 (Sierra Peña Blanca, Mexico). This is the first time this rare calcium uranate has been found 25 displaying a cubic morphology, in agreement with its crystal structure. -
Thn Auertcan M Rlueralocrsr
THn AUERTcANM rluERALocrsr JOURNAL OF TIIE MINDRALOGICAL SOCIETY OF ANIERICA vbl.41 JULY-AUGUST, 1956 Nos. 7 and 8 MTNERAL COMPOSTTTON OF G'UMMTTE*f Crrllonl FnoNonr, H artard Llniaersity,Cambrid,ge, M ass., and. U. S. GeologicalSurwy, Washington, D.C. ABSTRACT The name gummite has been wideiy used for more than 100 years as a generic term to designate fine-grained yellow to orange-red alteration products of uraninite whose true identity is unknown. A study of about 100 specimens of gummite from world-wide localities has been made by r-ray, optical, and chemical methods. rt proved possible to identify almost all of the specimens with already known uranium minerals. Gummite typicalty occurs as an alteration product of uraninite crystals in pegmatite. Such specimensshow a characteristic sequenceof alteration products: (1) A central core of black or brownish-black uraninite. (2) A surrounding zone, yellow to orange-red, composed chiefly of hydrated lead uranyl oxides. This zone constitutes the traditional gummite. It is principally composed of fourmarierite, vandendriesscheite and two unidentified phases (Mineral -4 and Mineral c). Less common constituents are clarkeite, becquerelite, curite, and schoepite. (3) An outer silicate zone. This usually is dense with a greenish-yellow color and is composed of uranophane or beta-uranophane; it is sometimes soft and earthy with a straw-yellow to pale-brown color and is then usually composed of kasolite or an unidenti- fied phase (Minerat B). Soddyite and sklodowskite occur rarely. There are minor variations in the above general sequence. rt some specimens the core may be orange-red gummite without residual uraninite or the original uraninite crystal may be wholly converted to silicates. -
CNWRA Paper Element Mobility in Uranium Deposits of the Sierra
Elemental Mobility in Uranium Deposits of the Sierra Peiia Blanca as a Natural Analog of Radionuclide Migration in a High-Level Nuclear Waste Repository English C. Pearcy and M. Murphy Southwest ResearchWilliam Institute San Antonio, Texas Phillip C. Goodell University of Texas El Paso, Texas For many years research interest in uranium ore deposits was mainly directed toward understanding the mechanisms and processes of formation of the deposits. Motivation for these studies derived from the economic value of the uranium as fuel for nuclear reactors. More recently, concern with disposal of the spent nuclear fuel has prompted research on uranium deposits because they can provide information on the behavior of nuclear waste in geologic repositories. Because high-level nuclear waste (HLW) will constitute a threat to public safety for many thousands of years, it is necessary to attempt to predict the performance of a HLW repository far into the future. Although such times are short on a geologic scale, they are far in excess of experimental capabilities. In addition, the size of a geologic repository greatly exceed that of laboratory facilities. One approach to theseHLW problems of large timewill and space scales is to study natural systems. For example, natural materials which approximate components of a repository may be studied to gain a better understanding of the behavior to be expected from the repsirory marerial. Similarly, a process which occurs (or has occurred) in nature and which may be significant to the performance of a repository may be investigated to learn of possible effects on a repository system. By studying such natural analogs, which have existed for time spans comparable to radionuclide isolation requirements and which are of comparable scale to a repository, the uncertainty inherent in projecting such large scale processes far into the future can be reduced. -
Kinetic Study of the Oxidative Dissolution of UO2 in Aqueous Carbonate Media
8188 Ind. Eng. Chem. Res. 2004, 43, 8188-8193 Kinetic Study of the Oxidative Dissolution of UO2 in Aqueous Carbonate Media Shane M. Peper,† Lia F. Brodnax,† Stephanie E. Field,† Ralph A. Zehnder,† Scott N. Valdez,‡ and Wolfgang H. Runde*,† Chemistry and Nuclear Materials Technology Divisions, Los Alamos National Laboratory, Los Alamos, New Mexico 87545 The oxidative dissolution of uranium(IV) dioxide powder at room temperature in aqueous carbonate media has been investigated. Kinetic studies evaluating the efficacy of various oxidants, including K2S2O8, NaOCl, and H2O2, for dissolving UO2 in alkaline solution have been performed, with H2O2 exhibiting the most rapid initial dissolution at 0.1 M oxidant concentrations. This result is due in part to the ability of peroxide to act as both an oxidant and a ligand under alkaline conditions. A spectrophotometric titration was used to confirm peroxide coordination to the U(VI) metal center. The disappearance of characteristic absorbance maxima associated 4- with UO2(CO3)3 (e.g., 448.5 nm) and a subsequent change in solution coloration upon titration with hydrogen peroxide indicated a change in speciation. Optimization of the hydrogen peroxide concentration indicated that the initial rate of uranium oxidation increased with increasing peroxide concentration, with a maximum reaction rate estimated at about 0.9 M peroxide. In addition, the effects of both the carbonate countercation and the carbonate concentration were also studied. It was determined that for 40 mg UO2 0.5MNa2CO3 was the most propitious choice, exhibiting both a high initial dissolution rate and the highest UO2 dissolution capacity among the systems studied. -
SIMPLE URANIUM OXIDES, HYDROXIDES U4+ + U6+, SIMPLE and COMPLEX URANYL HYDROXIDES in ORES Andrey A
New Data on Minerals. 2011. Vol. 46 71 SIMPLE URANIUM OXIDES, HYDROXIDES U4+ + U6+, SIMPLE AND COMPLEX URANYL HYDROXIDES IN ORES Andrey A. Chernikov Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, [email protected], [email protected] The review of published and new own data of simple uranium oxides revealed that the formation of five simple oxides is probable: nasturan, sooty pitchblende, uraninite, uranothorianite, and cerianite. Among simple oxides, nasturan, sooty pitchblende, and uraninite are the most abundant in ores varied in genesis and mineralogy. Uranothorianite or thorium uraninite (aldanite) is occasional in the ores, while cerianite is believed in U-P deposits of Northern Kazakhstan. Hydrated nasturan is the most abundant among three uranium (IV+VI) hydroxides in uranium ores. Insignificant ianthinite was found in few deposits, whereas cleusonite was indentified only in one deposit. Simple uranyl hydroxides, schoepite, metaschoepite, and paraschoepite, are widespread in the oxidized ores of the near-surface part of the Schinkolobwe deposit. They are less frequent at the deeper levels and other deposits. Studtite and metastudtite are of insignificant industrial importance, but are of great inter- est to establish genesis of mineral assemblages in which they are observed, because they are typical of strongly oxidized conditions of formation of mineral assemblages and ores. The X-ray amorphous urhite associated with hydrated nasturan and the X-ray amorphous hydrated matter containing ferric iron and U6+ described for the first time at the Lastochka deposit, Khabarovsk krai, Russia are sufficiently abundant uranyl hydroxides in the oxidized uranium ores. Significant complex uranyl hydroxides with interlayer K, Na, Ca, Ba, Cu, Pb, and Bi were found basically at a few deposits: Schinkolobwe, Margnac, Wölsendorf, Sernyi, and Tulukuevo, and are less frequent at the other deposits, where quite large monomineralic segregations of nasturan and crystals of uraninite were identified.