Thorium–Ligand Multiple Bonds Via Reductive Deprotection of a Trityl Group† Cite This: Chem
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Th Thorium Compounds with S, Se, Te and B
springer.com Chemistry : Chemistry (general) Brown, David, Wedemeyer, Horst, Buschbeck, Karl-Christian, Keller, Cornelius (Editors-in-chief.) Th Thorium Compounds with S, Se, Te and B The present volume, Thorium C5, deals with the compounds of thorium and sulfur, selenium, tellurium, and boron, as well as with oxoacid compounds of the three chalcogen elements. Thorium borates have already been treated in Thorium C2. In contrast to the corresponding compounds of uranium the thorium sulfides, etc. , do not show any nuclear or other technological application; they are only of academic interest, despite some very interest• ing electronic properties, especially of the 1 : 1 compounds. The thorium-sulfur and the thorium• boron systems in particular were studied in detail, so that we have a clear picture of them, whereas there are still a lot of open questions in the systems Th-Se and Th-Te - not very different from other metal chalcogenide systems. Thorium sulfates are of some technological importance because they are formed in solution during recovery of thorium from monazite by sulfuric acid leaching. The very detailed and critical treatment of the chemical and physical Springer properties of the compounds discussed also enables us to find gaps still remaining in our 8th ed. 1985, XIX, 149 p. knowledge and thus to initiate new research in this field. I want to thank the two authors, Dr. 8th 28 illus., 1 illus. in color. edition Horst Wedemeyer (Karlsruhe) and Dr. David Brown (Harwell), for their excellent contributions, the "Literaturabteilung" of the Karlsruhe Nuclear Research Center for its help in providing reports and other documents difficult to procure, as well as the staff of the Gmelin-Institute, especially to Dr. -
Study of Rare Earth Elements, Uranium and Thorium Migration in Rocks from Espinharas Uranium Deposit, Paraiba - Brazil
2009 International Nuclear Atlantic Conference - INAC 2009 Rio de Janeiro,RJ, Brazil, September27 to October 2, 2009 ASSOCIAÇÃO BRASILEIRA DE ENERGIA NUCLEAR - ABEN ISBN: 978-85-99141-03-8 STUDY OF RARE EARTH ELEMENTS, URANIUM AND THORIUM MIGRATION IN ROCKS FROM ESPINHARAS URANIUM DEPOSIT, PARAIBA - BRAZIL Cirilo C.S. Conceição Instituto de Radioproteção e Dosimetria -IRD Av. salvador Allend, S/N - Jacarepaguá Rio de Janeiro, Brazil CEP.: 22780-160 [email protected] ABSTRACT The determination of Rare Earth Elements as natural analogue in patterns geologic has grown as a tool for predicting the long-term safety of nuclear disposal in geological formation. Migration of natural radionuclides is one of the most serious problems in the waste deposit from nuclear fuel cycle. Rare Earth Elements show the same kinetic behavior in rocks as natural radionuclides. This similar property of the analogues allows perform studies and models on the subject of radionuclides migration. The aim of this study was to determine the distribution of Rare Earth Elements in rocks located at Espinharas – Paraíba – Brazil, uranium deposit. In this work are presented the results from the study above the distribution of rare earth elements in function of the degree of mineralized rocks, composition and the conditions of radioactive equilibrium of the uranium and thorium in some fractures on the rocks from radioactive occurrence of Espinharas-Brazil. The results show that there is a correlation of heavy Rare Earth Elements, uranium and Thorium concentrations to oxidation factor of the rocks. However this correlation was not observed for light Rare Earth Elements. It means that heavy Rare earth Elements follow the natural radionuclides in oxidation process of rocks. -
Radiological Implications of Plutonium Recycle and the Use of Thorium Fuels in Power Reactor Operations
01 RD/B/N3523 Central Electricity Generating Board Research Department Berkeley Nuclear Laboratories RADIOLOGICAL IMPLICATIONS OF PLUTONIUM RECYCLE AND THE USE OF THORIUM FUELS IN POWER REACTOR OPERATIONS By H. F. Macdonald XJ034 January 1976 DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document. Radiological Implications of Plutonium Recycle and the Use of Thorium Fuels in Power Reactor Operations “ by - H.F. Macdonald Approved Head of Health Physics Research Section For inclusion in Nuclear Science Abstracts SUMMARY As economically attractive sources of natural uranium are gradually depleted attention will turn to recycling plutonium or the use of thorium fuels. In this study the radiological implications of these fuel cycles in terms of fuel handling and radioactive waste disposal are investigated in 235 relation to a conventional U enriched oxide fuel. It is suggested that a comparative study of this nature may be an important aspect of the overall optimisation of future fuel cycle strategies. It is shown that the use of thorium based fuels has distinct advan tages in terms of neutron dose rates from irradiated fuels and long term a decay heating commitment compared with conventional uranium/plutonium fuels. However, this introduces a y dose rate problem in the fabrication 233 and handling of unirradiated U fuels. For both plutonium and thorium fuels these radiological problems increase during storage of the fuel prior to reactor irradiation. Finally, the novel health physics problems which arise in the handling and processing of thorium fuels are reviewed in an appendix. -
The Actinide Research Quarterly Is Published Quarterly to Highlight Recent Achievements and Ongoing Programs of the Nuclear Materials Technology Division
1st quarter 2000 TheLos Actinide Alamos National Research Laboratory N u c l e a r M aQuarterly t e r i a l s R e s e a r c h a n d T e c h n o l o g y a U.S. Department of Energy Laboratory Organizers Issue an Invitation to In This Issue Plutonium Futures 1 —The Science Organizers Issue an Invitation to Plutonium Futures —The Science The second of a series of international con- have an exciting collection of some 180 invited ferences on plutonium will be held in Santa Fe, and contributed papers with topics ranging 2 NM, this summer, July 10–13. It follows the very broadly in materials science, transuranic 238Pu Aqueous highly successful 1997 conference, “Plutonium waste forms, nuclear fuels and isotopes, separa- Processing Line Will Futures - The Science,” which attracted over 300 tions, actinides in the environment, detection Provide New NMT participants representing 14 countries. The U.S. and analysis, actinide compounds and com- Capability participants, who made up about 70 percent of plexes, and condensed matter physics of ac- the total participants, came from Department of tinides. These papers, presented in separate 4 Energy national laboratories and a score of uni- oral and poster sessions, will give attendees a Editorial: versities and industries. As in 1997, the confer- chance to learn about current research outside Transactinium ence is sponsored by the Los Alamos National of their particular specialties and provide an Science Needs Laboratory in cooperation with the American opportunity for interdisciplinary discussions Educational Nuclear Society. -
Nature No. 2468, Vol
FEBRUARY IS, 1917J NATURE LETTERS TO THE EDITOR. and in Paris, several of them fam l-us for their atomic- weight determinations, doubt has lingered with r-egard [The Editor does not hold himself responsible for to our results for the very much more difficult case of opinions expressed by his correspondents. Neither thorium lead. In the first place, no one but myself can he undertake to return, or to correspond with has been able to obtain a suitable material by which the writers of, rejected manuscripts intended for to test the question, and I, of course, can claim no this or any other part of NATURE. No notice is previous experience of atomic-weight work. In the taken of anonymous communications.] second place, there has been an unfortunate confusion The Atomic Weight of "Thorium" Lead. between my material, Ceylon thorite, and thorianite, IN continuation of preliminary work published by a totally distinct mixed thorium and uranium Ceylon Mr. H. Hyman and myself (Trans. Chern. Soc., 1914, mineral. Lastly, there has been the widespread view, due :v., 1402) I gave an account in NATURE, February 4, to Holmes and Lawson, Fajans, and others, mainly 1915, p. 615, of the preparation of 80 grams of lead derived from geological evidence, that thorium-E, the from Ceylon thorite and of the determination of its isotope of lead resulting from the ultimate change of density in comparison with that of ordinary lead, thorium, was not sufficiently stable to accumulate over which proved the thorite lead to be 0'26 per cent. geological periods of time. -
Separation of Radioactive Elements from Rare Earth Element-Bearing Minerals
metals Review Separation of Radioactive Elements from Rare Earth Element-Bearing Minerals Adrián Carrillo García 1, Mohammad Latifi 1,2, Ahmadreza Amini 1 and Jamal Chaouki 1,* 1 Process Development Advanced Research Lab (PEARL), Chemical Engineering Department, Ecole Polytechnique de Montreal, C.P. 6079, Succ. Centre-ville, Montreal, QC H3C 3A7, Canada; [email protected] (A.C.G.); mohammad.latifi@polymtl.ca (M.L.); [email protected] (A.A.) 2 NeoCtech Corp., Montreal, QC H3G 2N7, Canada * Correspondence: [email protected] Received: 8 October 2020; Accepted: 13 November 2020; Published: 17 November 2020 Abstract: Rare earth elements (REE), originally found in various low-grade deposits in the form of different minerals, are associated with gangues that have similar physicochemical properties. However, the production of REE is attractive due to their numerous applications in advanced materials and new technologies. The presence of the radioactive elements, thorium and uranium, in the REE deposits, is a production challenge. Their separation is crucial to gaining a product with minimum radioactivity in the downstream processes, and to mitigate the environmental and safety issues. In the present study, different techniques for separation of the radioactive elements from REE are reviewed, including leaching, precipitation, solvent extraction, and ion chromatography. In addition, the waste management of the separated radioactive elements is discussed with a particular conclusion that such a waste stream can be -
United States Patent Office 2,988,421
United States Patent Office Patented June2,988,421 13, 196 heavailaaaar 1 2 contain more than 200 gms. alkali metal and chloride ions 2,988,421 per litre. The following tables show the loss of thorium PROCESS FOR THE SEPARATION OF THORUM and lanthanons under various conditions in the presence WilliamANDRARE Palmer Kemp, EARTHS Shenfield, FROM and MONAZTE James Johnston, 5 of sodium and potassium chloride. Hainault, England, assignors to Thorium Limited, Lon don, England, a corporation of Great Britain NaCl, ThO Ln2O No Drawing. Filed Aug. 20, 1957, Ser. No. 679,126 Acidity gm.fl. loss, loss, Claim priority, application Great Britain Aug. 24, 1956 gm.fl. gm.fl. 9 Claims. (C. 23-145) -ror-rm-m-m------- 10 : 122 This invention relates to a process for separating thori- 4.5 8: um and lanthanon salts from other materials present in : g monazite. The invention is particularly useful in that it 55 i. provides a process for separating salts of thorium and the : 8. lanthanons from phosphate and impurities present in 1655 400 6.65 ground mineral monazite. The term lanthanon in this specification includes the elements with atomic numbers KC ThO Ln2O from 57-71; this group is also known as the rare earth Acidity fi. is is elements. gm.fl. gm.fl. Monazite sand is a mineral phosphate containing thori- .am-m-m-m-m-m-m-wn um and the lanthanon phosphates to the extent of about 38 o' 95-98% by weight. Another source is ground mineral 300 0.005 1.0 monazite which is far less pure than monazite sand and contains only about 75% of the thorium and lanthanon In a preferred form of the process the filtered extract phosphates. -
Upper Limit of the Periodic Table and the Future Superheavy Elements
CLASSROOM Rajarshi Ghosh Upper Limit of the Periodic Table and the Future Department of Chemistry The University of Burdwan ∗ Superheavy Elements Burdwan 713 104, India. Email: [email protected] Controversy surrounds the isolation and stability of the fu- ture transactinoid elements (after oganesson) in the periodic table. A single conclusion has not yet been drawn for the highest possible atomic number, though there are several the- oretical as well as experimental results regarding this. In this article, the scientific backgrounds of those upcoming super- heavy elements (SHE) and their proposed electronic charac- ters are briefly described. Introduction Totally 118 elements, starting from hydrogen (atomic number 1) to oganesson (atomic number 118) are accommodated in the mod- ern form of the periodic table comprising seven periods and eigh- teen groups. Total 92 natural elements (if technetium is consid- ered as natural) are there in the periodic table (up to uranium hav- ing atomic number 92). In the actinoid series, only four elements— Keywords actinium, thorium, protactinium and uranium—are natural. The Superheavy elements, actinoid rest of the eleven elements—from neptunium (atomic number 93) series, transactinoid elements, periodic table. to lawrencium (atomic number 103)—are synthetic. Elements after actinoids (i.e., from rutherfordium) are called transactinoid elements. These are also called superheavy elements (SHE) as they have very high atomic numbers. Prof. G T Seaborg had Elements after actinoids a very distinct contribution in the field of transuranium element (i.e., from synthesis. For this, Prof. Seaborg was awarded the Nobel Prize in rutherfordium) are called transactinoid elements. 1951. -
Revisiting the Thorium-Uranium Nuclear Fuel Cycle
s e r u t Revisiting the a e f thorium-uranium nuclear fuel cycle [DOI: 10.1051/EPN:2007007 ] Sylvain David a, Elisabeth Huffer b and Hervé Nifenecker b, Energy Panel of the French Physics Society a Institut de Physique Nucléaire d’Orsay • France b Laboratoire de Physique Subatomique et de Cosmologie (IN2P3, Grenoble) • France thorium-uranium nuclear fuel cycle, in which the main amounts of uranium 233 available remained tiny, insufficient to HE fissile nucleus is uranium 233 and fuel regeneration is allow the rapid development of a thorium-uranium concept. ensured through neutron capture on thorium 232 offers many It appears today that the growth rate of nuclear power Tpotential advantages as compared to the better known urani - worldwide does not require the fast development of breeder re - um-plutonium fuel cycle. These include, in particular, reduced actor concepts. It is then possible, as we show in this paper, to high activity long lived waste production and less likelihood of constitute a stockpile of uranium 233 that could allow the nuclear proliferation. A brief description of the nuclear reactors development of a fleet of thorium-uranium reactors. We show being considered for this fuel cycle is given. We show also that a also that such a concept has many major advantages, in partic - strategy can be put together to constitute the initial uranium ular concerning the disposal of radioactive waste and the risks 233 supply for such reactors, using today’s pressurized water of nuclear proliferation. We give a brief description of the types reactors and a thorium and plutonium mixed oxide fuel. -
The Elements.Pdf
A Periodic Table of the Elements at Los Alamos National Laboratory Los Alamos National Laboratory's Chemistry Division Presents Periodic Table of the Elements A Resource for Elementary, Middle School, and High School Students Click an element for more information: Group** Period 1 18 IA VIIIA 1A 8A 1 2 13 14 15 16 17 2 1 H IIA IIIA IVA VA VIAVIIA He 1.008 2A 3A 4A 5A 6A 7A 4.003 3 4 5 6 7 8 9 10 2 Li Be B C N O F Ne 6.941 9.012 10.81 12.01 14.01 16.00 19.00 20.18 11 12 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 3 Na Mg IIIB IVB VB VIB VIIB ------- VIII IB IIB Al Si P S Cl Ar 22.99 24.31 3B 4B 5B 6B 7B ------- 1B 2B 26.98 28.09 30.97 32.07 35.45 39.95 ------- 8 ------- 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 4 K Ca Sc Ti V Cr Mn Fe Co Ni Cu Zn Ga Ge As Se Br Kr 39.10 40.08 44.96 47.88 50.94 52.00 54.94 55.85 58.47 58.69 63.55 65.39 69.72 72.59 74.92 78.96 79.90 83.80 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 5 Rb Sr Y Zr NbMo Tc Ru Rh PdAgCd In Sn Sb Te I Xe 85.47 87.62 88.91 91.22 92.91 95.94 (98) 101.1 102.9 106.4 107.9 112.4 114.8 118.7 121.8 127.6 126.9 131.3 55 56 57 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 6 Cs Ba La* Hf Ta W Re Os Ir Pt AuHg Tl Pb Bi Po At Rn 132.9 137.3 138.9 178.5 180.9 183.9 186.2 190.2 190.2 195.1 197.0 200.5 204.4 207.2 209.0 (210) (210) (222) 87 88 89 104 105 106 107 108 109 110 111 112 114 116 118 7 Fr Ra Ac~RfDb Sg Bh Hs Mt --- --- --- --- --- --- (223) (226) (227) (257) (260) (263) (262) (265) (266) () () () () () () http://pearl1.lanl.gov/periodic/ (1 of 3) [5/17/2001 4:06:20 PM] A Periodic Table of the Elements at Los Alamos National Laboratory 58 59 60 61 62 63 64 65 66 67 68 69 70 71 Lanthanide Series* Ce Pr NdPmSm Eu Gd TbDyHo Er TmYbLu 140.1 140.9 144.2 (147) 150.4 152.0 157.3 158.9 162.5 164.9 167.3 168.9 173.0 175.0 90 91 92 93 94 95 96 97 98 99 100 101 102 103 Actinide Series~ Th Pa U Np Pu AmCmBk Cf Es FmMdNo Lr 232.0 (231) (238) (237) (242) (243) (247) (247) (249) (254) (253) (256) (254) (257) ** Groups are noted by 3 notation conventions. -
Compounds of the Metals Beryllium, Magnesium
C01F COMPOUNDS OF THE METALS BERYLLIUM, MAGNESIUM, ALUMINIUM, CALCIUM, STRONTIUM, BARIUM, RADIUM, THORIUM, OR OF THE RARE-EARTH METALS (metal hydrides [N: monoborane, diborane or addition complexes thereof] C01B6/00; salts of oxyacids of halogens C01B11/00; peroxides, salts of peroxyacids C01B15/00; sulfides or polysulfides of magnesium, calcium, strontium, or barium C01B17/42; thiosulfates, dithionites, polythionates C01B17/64; compounds containing selenium or tellurium C01B19/00; binary compounds of nitrogen with metals C01B21/06; azides C01B21/08; [N: compounds other than ammonia or cyanogen containing nitrogen and non-metals and optionally metals C01B21/082; amides or imides of silicon C01B21/087]; metal [N: imides or] amides C01B21/092, [N: C01B21/0923]; nitrites C01B21/50; [N: compounds of noble gases C01B23/0005]; phosphides C01B25/08; salts of oxyacids of phosphorus C01B25/16; carbides C01B31/30; compounds containing silicon C01B33/00; compounds containing boron C01B35/00; compounds having molecular sieve properties but not having base-exchange properties C01B37/00; compounds having molecular sieve and base-exchange properties, e.g. crystalline zeolites, C01B39/00;cyanides C01C3/08; salts of cyanic acid C01C3/14; salts of cyanamide C01C3/16; thiocyanates C01C3/20; [N: double sulfates of magnesium with sodium or potassium C01D5/12; with other alkali metals C01D15/00, C01D17/00]) Definition statement This subclass/group covers: All compounds of Be,Mg,Al,Ca,Sr,Ba,Ra,Th or rare earth metals except those compounds which are classified in C01G because of application of the last appropriate place rule. So, in principle does this subclass comprise all Al-compounds with elements as such being part of C01B-C01D, e.g. -