Quantum-Mechanical Evaluation of the Thermodynamics and Kinetics of Environmentally-Relevant Actinide Reactions
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Oct. 14, 1958 J. M. CARTER ET AL 2,856,263 PROCESS for the RECOVERY and PURIFICATION of URANIUM DEPOSITS Original Filed April 21, 1944 ‘7 Sheets-Sheet 1
Oct. 14, 1958 J. M. CARTER ET AL 2,856,263 PROCESS FOR THE RECOVERY AND PURIFICATION OF URANIUM DEPOSITS Original Filed April 21, 1944 ‘7 Sheets-Sheet 1 IN VEN TORS James M Car/‘er Mar?n D. ?ame/7 BY ATTORNEY Oct. 14, 1958 J. M. CARTER ET AL 2,856,263 PROCESS FOR THE RECOVERY AND PURIFICATION OF URANIUM DEPOSITS Original Filed April 21, 1944 7 Sheets-Sheet 55 QQOUMM,vRMmG w.9386mmE IN VEN TORS James M. Car fer By Marfin 0 Home/7 W4 W ATTORNEY Oct. 14,1958 J. M. CARTER ET AL 2,856,263 PROCESS FOR THE RECOVERY AND PURIFICATION _ OF URANIUM DEPOSITS Origlnal Filed April 21, 1944 7 Sheets-Sheet 4 SCRUBBYING. AND WASHING PARTS OF CALUTRON ' WITH HOT WATER Lf- WASH WATER :FCONDENSATE ' \WATERANDMAKE UP snevmc SOL/D IMPUR/ TIES — WASH WA TER -—p>- CONDENSING To DISCARD I OXIDIZING ORSALVAGE SOLUTION U02” Cu?! Few’! Cr!!! Ni“ FILTERING‘ - '3 PREC/P/TATE 0* |——‘———/ F/LTRA TE _ U024!- TO DISCARD __ EVAPORATING gel”,++ OR SALVAGE PRECIPITATING Z/VH OH AND F'LTER'NG gFlLTRA TE TO FURTHER T REATMENT Fig. 4 I INVENTORS ‘James M Cor fer, BY Mar/7'0 D. Kama/7 ' @ M A TTORNEY Oct. 14,1958 J. M. CARTER ET AL . 2,356,263 PROCESS FOR THE RECOVERY AND PURIFICATION 0F URANIUM DEPOSITS Original Filed April 21, 1944 7 Sheets-Sheet s DISSOLVING URANIUM METAL DEPOSITED ON COPPER COLLECTOR IN COLD HNo3 (8N) CONDENSATE I AND MAKE UP SOLUTION HNO3 U02" ' Cu ** 7—>— CONDENSING ' HN03 . EVAPORATI NG CONCENTRA TED \ soburj'o/v _ F/LTRA TE C35 cu {NHJLF H PRECIPITATING ‘ -[—-~’—NH4OH A ND F ILTERING ' f/RECIP/ TA TES *Cu/‘OHZH4 :0 01 ORTO SALVAGEDISCARD *Trace T__>_ DISSOLVING HN 0 3 ' - SOLUTION U02 +4 *cuvf *Tme F/LTRA TE PRECIPITATING _l—_'_NH OH AND FILTERING 4 { PREClP/TATE NH U 0 TO DISCARD ( ‘)2 2 ’ OR SALVAGE , r---‘“—? TO FURTHER TREATMENT 5 I N V EN TORS' James M Car/‘er ' Mar/"in D. -
ORGANOMETAT,T,TC CHEMISTRY of URANIUM a Thesis Submitted By
ORGANOMETAT,T,TC CHEMISTRY OF URANIUM A thesis submitted by R1TN R. SIGURDSON, B.Sc. for the DEGREE of DOCTOR of PHILOSOPHY of the UNIVERSITY of LONDON Royal College of Science Imperial College of Science and Technology London, SW7 ?AY August 1976 TO MY PARENTS 3 ACKNOWLEDGEMENTS I would like to express my gratitude to Professor Geoffrey Wilkinson, F.R.S. for his guidance and enthusiastic support throughout the course of this work. Many thanks are also extended to Drs. Dick Andersen, Ernesto Carmona-Guzman and David Cole-Hamilton for their suggestionS, encouragement and advice, and to Dr. Kostas Mertis for his patient help during the first months. I am indebted to the Canadian Research Council of Canada for financial support during the past three years. 4 CONTENTS ABSTRACT 6 INTRODUCTION I. The Chemistry of Uranium(IV) 8 .II. The Chemistry of Uranium(V) 15 III. The Chemistry of Uranium(VI) 16 CHAPTER I. DILITHIUMHEXAALKYLURANATE(IV) COMPLEXES I. Introduction 19 II. Results and Discussion 27 III. Experimental 35 CHAPTER II. TRILITHIUMOCTAALKYLURANATE(V) COMPLEXES I. Introduction 54 II. Results and Discussion 55 III. Experimental 60 CHAPTER III. ADDITION COMPOUNDS OF URANIUM(VI) HEXAISO-PROPDXIDE WITH LITHIUM, MAGNESIUM AND ALUMINIUM ALKYLS I. Introduction 70 II. Results and Discussion 71 III. Experimental 77 CHAPTER IV. ORGANOMETALLIC CHEMISTRY OF ADAMANTANE I. Introduction 84 II. Results and Discussion 85 III. Experimental 87 REFERENCES 92 5 ABBREVIATIONS Me - methyl Et - ethyl Prn- normal-propyl Pri- iso-propyl Bun- normal-butyl But- iso-butyl But- tertiary-butyl Ph - phenyl CP cyclopentadienyl DME - dimethoxyethane tmed - N,N,NI,N'-tetramethylethylenediamine pmdt - N,N,Nt,N",N"-pentamethyldiethylenetriamine g.l.c. -
Mineral Formation and Sorption Mechanisms in Marine Ferromanganese-Rich Sediments
Mineral Formation and Sorption Mechanisms In Marine Ferromanganese-rich Sediments Amy Leanne Atkins Submitted in accordance with the requirements for the degree of Doctor of Philosophy The University of Leeds School of Earth and Environment October 2014 The candidate confirms that the work submitted is her own, except where work, which has formed part of jointly authored publications has been included. The contributions of the candidate and the other authors to this work have been indicated overleaf. The candidate confirms that appropriate credit has been given where reference has been made to the work of others. This copy has been supplied on the understanding that it is copyright material and that no quotation from this thesis may be published without proper acknowledgement. ii Declaration Chapter 4 is a reproduction of a peer-reviewed publication in the journal Geochimica et Cosmochimica Acta as: Atkins A. L., Shaw S., Peacock C. L. (2014) Nucleation and growth of todorokite: Implications for trace-metal cycling in marine sediments. Geochim. Cosmochim. Acta. 144, 109-125. TEM images presented in chapter 4 were collected by Michael Ward at the Leeds Electron Microscopy and Spectroscopy centre with the guidance of the candidate. All other experimental work has been conducted by the candidate. The interpretation of the experimental data, and preparation of the manuscript has been undertaken by the candidate with the help and guidance of her supervisors: Caroline L. Peacock and Sam Shaw. Chapter 5 is a reproduction of a manuscript currently in the final stages of preparation for submission to the journal Geochimica et Cosmochimica Acta as: Atkins A. -
Crystallographic Determination of Wild Type, Mutant and Substrate
Copyright is owned by the Author of the thesis. Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only. The thesis may not be reproduced elsewhere without the permission of the Author. Crystallographic Determination of Wild Type, Mutant and SubstrateSubstrate---- Analogue Inhibited Structures of Bacterial Members of a Family of Superoxide Dismutases bybyby Simon Hardie Oakley Submitted as part of the requirements for the degree of Doctor of Philosophy Institute of Fundamental Sciences, Chemistry Massey University, New Zealand 2009 i "Part of the inhumanity of the computer is that, once it is competently programmed and working smoothly, it is completely honest." Isaac Asimov (1920-92), author, inventor of the word “robotics”. ii 0.1 Abstract Crystallographic Determination of Wild Type, Mutant and Substrate-Analogue Inhibited Structures of Bacterial Members of a Family of Superoxide Dismutases The iron and manganese superoxide dismutases are a family of metallo-enzymes with highly conserved protein folds, active sites and dimer interfaces. They catalyse the elimination of the cytotoxic free radical superoxide to molecular oxygen and hydrogen peroxide by alternate reduction then oxidation of the active- site with the concomitant transfer of protons from the solvent. There are many key aspects of enzymatic function that lack a structural explanation. The focus of this study is on three crystal structures. The iron-substituted manganese superoxide dismutase from Escherichia coli complexed with azide, a substrate-mimicking inhibitor, was solved to 2.2 Å. This “wrong” metal form shows a binding pattern seen previously in the manganese superoxide dismutase from Thermus thermophilus. -
Surface Geochemistry of the Clay Minerals
Proc. Natl. Acad. Sci. USA Vol. 96, pp. 3358–3364, March 1999 Colloquium Paper This paper was presented at the National Academy of Sciences colloquium ‘‘Geology, Mineralogy, and Human Welfare,’’ held November 8–9, 1998 at the Arnold and Mabel Beckman Center in Irvine, CA. Surface geochemistry of the clay minerals GARRISON SPOSITO*†,NEAL T. SKIPPER‡,REBECCA SUTTON*, SUNG-HO PARK*, ALAN K. SOPER§, AND JEFFERY A. GREATHOUSE¶ *Earth Sciences Division, Mail Stop 90y1116, Ernest Orlando Lawrence Berkeley National Laboratory, University of California, Berkeley, CA 94720; ‡Department of Physics and Astronomy, University College, Gower Street, London WC1E 6BT, United Kingdom; §ISIS Facility, Rutherford Appleton Laboratory, Chilton, Didcot, Oxfordshire OX11 0QX, United Kingdom; and ¶Department of Chemistry, University of the Incarnate Word, 4301 Broadway, San Antonio, TX 78209 ABSTRACT Clay minerals are layer type aluminosilicates (6) and in the construction of environmental liners (7). Major that figure in terrestrial biogeochemical cycles, in the buff- impact on industrial organic synthesis comes in the many ering capacity of the oceans, and in the containment of toxic designed catalysts developed from clay minerals with adsorbed waste materials. They are also used as lubricants in petroleum polymeric cations (8). extraction and as industrial catalysts for the synthesis of many Certain clay minerals are isostructural with mica (1, 2) but organic compounds. These applications derive fundamentally are not as well crystallized because of random isomorphic from the colloidal size and permanent structural charge of cation substitutions in their structure (9, 10). These cation clay mineral particles, which endow them with significant substitutions lead to a negative net surface charge that induces surface reactivity. -
1214 Final Report SF 10 03 06-CS
AN ASSESSMENT OF SOURCES, PATHWAYS, MECHANISMS AND RISKS OF CURRENT AND POTENTIAL FUTURE POLLUTION OF WATER AND SEDIMENTS IN GOLD-MINING AREAS OF THE WONDERFONTEINSPRUIT CATCHMENT Report to the WATER RESEARCH COMMISSION Compiled by Henk Coetzee Council for Geosience Reference to the whole of the publication should read: Coetzee, H. (compiler) 2004: An assessment of sources, pathways, mechanisms and risks of current and potential future pollution of water and sediments in gold-mining areas of the Wonderfonteinspruit catchment WRC Report No 1214/1/06, Pretoria, 266 pp. Reference to chapters/sections within the publication should read (example): Wade, P., Winde, F., Coetzee, H. (2004): Risk assessment. In: Coetzee, H (compiler): An assessment of sources, pathways, mechanisms and risks of current and potential future pollution of water and sediments in gold-mining areas of the Wonderfonteinspruit catchment. WRC Report No 1214/1/06, pp 119-165 WRC Report No 1214/1/06 ISBN No 1-77005-419-7 MARCH 2006 Executive summary 1. Introduction and historical background The eastern catchment of the Mooi River, also known as the Wonderfonteinspruit, has been identified in a number of studies as the site of significant radioactive and other pollution, generally attributed to the mining and processing of uraniferous gold ores in the area. With the establishment of West Rand Consolidated in 1887 gold mining reached the Wonderfonteinspruit catchment only one year after the discovery of gold on the Witwatersrand. By 1895 five more gold mines had started operations in the (non-dolomitic) headwater region of the Wonderfonteinspruit as the westernmost part of the West Rand goldfield. -
Arsenic Adsorption Onto Minerals: Connecting Experimental Observations with Density Functional Theory Calculations
Minerals 2014, 4, 208-240; doi:10.3390/min4020208 OPEN ACCESS minerals ISSN 2075-163X www.mdpi.com/journal/minerals Article Arsenic Adsorption onto Minerals: Connecting Experimental Observations with Density Functional Theory Calculations Heath D. Watts 1,*, Lorena Tribe 2 and James D. Kubicki 1,3,* 1 Department of Geosciences, The Pennsylvania State University, University Park, PA 16802, USA 2 Division of Science, The Pennsylvania State University, Berks, Reading, PA 19610, USA; E-Mail: [email protected] 3 Earth and Environmental Systems Institute, The Pennsylvania State University, University Park, PA 16802, USA * Authors to whom correspondence should be addressed; E-Mails: [email protected] (H.D.W.); [email protected] (J.D.K.); Tel.: +1-814-865-3951 (J.D.K.); Fax: +1-814-867-2378 (J.D.K). Received: 24 December 2013; in revised form: 25 February 2014 / Accepted: 6 March 2014 / Published: 27 March 2014 Abstract: A review of the literature about calculating the adsorption properties of arsenic onto mineral models using density functional theory (DFT) is presented. Furthermore, this work presents DFT results that show the effect of model charge, hydration, oxidation state, and DFT method on the structures and adsorption energies for AsIII and AsV onto Fe3+-(oxyhydr)oxide cluster models. Calculated interatomic distances from periodic planewave and cluster-model DFT are compared with experimental data for AsIII and AsV adsorbed to Fe3+-(oxyhydr)oxide models. In addition, reaction rates for the adsorption of AsV on α-FeOOH (goethite) (010) and Fe3+ (oxyhydr)oxide cluster models were calculated using planewave and cluster-model DFT methods. Keywords: arsenic; density functional theory (DFT); kinetics; thermodynamics; adsorption; computational chemistry; planewave DFT; reaction rates; As—Fe bond distances Minerals 2014, 4 209 1. -
Kinetics and Mechanisms of Electron Transfer Reactions of Metal Complexes Ormond Jerry Parker Iowa State University
Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1968 Kinetics and mechanisms of electron transfer reactions of metal complexes Ormond Jerry Parker Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Physical Chemistry Commons Recommended Citation Parker, Ormond Jerry, "Kinetics and mechanisms of electron transfer reactions of metal complexes " (1968). Retrospective Theses and Dissertations. 4619. https://lib.dr.iastate.edu/rtd/4619 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. This dissertation has been microfihned exactly as received 69-9882 PARKER, Ormond Jerry, 1939- KINETICS AND MECHANISMS OF ELECTRON TRANSFER REACTIONS OF METAL COMPLEXES. Iowa State University, Ph.D., 1968 Chemistry, physical University Microfilms. Inc., Ann Arbor, Michigan KINETICS AND MECHANISMS OF ELECTRON TRANSFER REACTIONS OF METAL COMPLEXES by Ormond Jerry Parker A Dissertation Submitted to the Graduate Faculty in Partial Fulfillment of The Requirements for the Degree of DOCTOR OF PHILOSOPHY Major Subject: Physical Chemistry Approved: Signature was redacted for privacy. IffyCharge of Maj<6r Work Signature was redacted for privacy. -
April 24-27, 2007
Program and Abstracts Separations Program Heavy Element Chemistry Program Contractors’ Meeting O’Callaghan Annapolis Hotel, Annapolis, MD April 24-27, 2007 Chemical Sciences, Geosciences, and Biosciences Division Office of Basic Energy Sciences Office of Science U.S. Department of Energy Program and Abstracts Separations Program Heavy Element Chemistry Program Contractors’ Meeting O’Callaghan Annapolis Hotel Annapolis, MD April 24-27, 2007 Chemical Sciences, Geosciences, and Biosciences Division Office of Basic Energy Sciences Office of Science U.S. Department of Energy Cover Graphics: The cover artwork is a metaphor of DMDOHEMA dragging down Am3+ into the organic layer, while HDHP tugs at Yb3+. The “teeth” illustrate a stretched “adhesive,” a metaphor for the difficulty in separating 4f from 5f trivalent ions. For more detail see abstract P1-2, Mark R. Antonio, “Structural Chemistry of Lanthanide and Americium Complexes in Solvent Extraction,” p 25. Image reproduced by permission of Mark R. Antonio and The Royal Society of Chemistry from Benoît Gannaz, Mark R. Antonio, Renato Chiarizia, Clément Hill and Gérard Cote, Dalton Trans., 2006, 4553, DOI: 10.1039/b609492a. i This document was produced under contract number DE-AC05-06OR23100 between the U.S. Department of Energy and Oak Ridge Associated Universities. The research grants and contracts described in this document are supported by the U.S. DOE Office of Science, Office of Basic Energy Sciences, Chemical Sciences, Geosciences and Biosciences Division. ii Foreword This abstract booklet provides a record of the seventh U.S. Department of Energy contractors’ meeting in separations sciences and the fourth in heavy element chemistry. The Chemical Sciences, Geosciences and Biosciences Division of the Office of Basic Energy Sciences and its predecessors have sponsored research in heavy element chemistry and separations sciences for some sixty years. -
The Chemical Complexities of Plutonium David L
The Chemical Complexities of Plutonium David L. Clark ew people have ever seen plutonium, and far fewer have actually handled or manipu- lated it. Yet this manmade element has arguably altered the course of civilization as Fmuch as copper, bronze, iron, or steel. Within five years of its synthesis, the primary use of plutonium was for the release of nuclear energy in weapons of mass destruction, and it seemed that the new element might lead the human race to the brink of self-annihilation. But instead, plutonium has become a stabilizing agent in global politics, forcing the human race to govern itself without resorting to nuclear war. Never before has a simple chemical element had such a profound impact on the consciousness of mankind. Plutonium has had a similarly humbling impact in the more circumscribed arena of science. Incredibly, it displays physicochemical behaviors that are among the most complex of any element in the periodic table. The pure element exhibits seven distinct crystal phases, is highly reactive, and is known to form compounds, complexes, or alloys with virtually every other element. Molten plutonium is highly corrosive and will slowly react with its container, causing difficulties for handling. When elemental plutonium reacts to give up its valence electrons, it can form a wide variety of positively charged ions with the ability to form up to twelve chemical bonds to other ions or molecules in solution. The element can exhibit five oxidation states, and under certain chemical conditions, four different oxidation states can be present in appreciable amounts simultaneously! No other element displays such a complex chemistry. -
Adsorption of Selenite on Heat Treated Sea Nodule Residue
International Journal of Advanced Chemical Science and Applications (IJACSA) ________________________________________________________________________ Adsorption of Selenite on Heat Treated Sea Nodule Residue 1P.K.Satapathy, 2T.R.Mohanta, 3A.K.Sahoo 1P.G. Department of Chemistry, North Orissa University, Baripada 2Department of Chemistry, F.M. Junior College, Balasore Email: [email protected] Adsorption of selenite/selenate on hydrous oxides of ABSTRACT: - The present study was carried out to investigate the adsorption characteristics of sea nodule iron, manganese, and aluminum [2, 3-6] appears to be an efficient and inexpensive method for removing trace residue (SNR) heated at 400°C towards aqueous selenite. contaminants. Selenite adsorption on manganese nodule Physico-chemical characterization revealed that the leached residue was a complex mixture of oxides of mainly surface was also studied by Parida et al[7]. However adsorption of selenite has not yet been studied using heat manganese and iron along with MnCO3. Adsorption studies were carried out at varying the pH, selenite ion treated sea nodule residue. So the present study is an concentration, SNR dosage and in presence of competitive attempt to use 400°C heated sea nodule residue sample ions. It was found that the selenite adsorption increased as adsorbent towards adsorption of selenium. with pH reaches maximum at pH 5.0 and then decreased. Further it was found that the percentage of selenite II. EXPERIMENTAL adsorption increased with increasing amount of adsorbent Materials (SNR) and decreased with increasing initial concentration of selenite. It was observed that the percentage of Leached residue sample (SNR), generated after adsorption of selenite decreased with increasing reduction roast-ammoniacal leaching process were concentration of externally added ions. -
The Radiochemistry of Plutonium
National v Academy of Sciences National1Research Council . E The Radiocheunistry of Plutonium ,“. m COMMlllEE ON NUCLEAR SCIENCE ~. A. Bromley, Chainmm R. D. Evans, Vice Cluri7man Yale University Massachusetts Institute of Technology Lewis Slack, Secrekq National Rese=ch COunCtl E. C. Anderson Jerry B. Marion Los Afamo6 Scientific Laboratory University of Maryland N. E. Baflou R. L. PLatman U. S. Naval Radiological Defense Argonne National Laboratory Labomto~ Ernest C. Pollard Martin J. Barger Pennsylvania State University , National Bureau of Standards Katharine Way C. J. Borkowski Oak Ridge National Laboratory Oak Ridge National Laboratory George W. Wetherill Herbert Goldstein University of California Columbia Uoivereity Marvin E. Wyman Bemd Kahn University of Illinois Taft Sanitary Engineering Center Harold Glsser William S. Rodney Office of Navsl Reeearch National Science Foundation George A. Kolstad Atomic Energy Commission SllWllMMITIEEON RADIOCNEMiSTSY Nathao E. Ballou, Chaivman Julian M. Nielsen U. S. Naval Radiolostcal Defense Battefle Pacific Northwest Lain-atow G. D. O’Ke!.ley G. R. Chq@n Oak Ridge National Laboratory Florida State University E. P. Steinberg Herbert M. Clark Argonne Nationaf Laboratory Rensselaer Polytechnic Institute D. N. Sunderman Richard M. Diamond Battelle Memoriel Institute IJmrence Radiation Laboratory John W. Winchester Jerome Hudla Massachusetts Institute of Technology Brookhaven National Laboratory R. P. Schuman, Consultant Jere D. Knight Sri Venkateswara University Los Alsmos Scientific Laboratow Tirupati, AndhI= Pradesh, India W. E. Nervik Lawrence Radiation Laborstory The Radiochemistry of Plutonium. George” H. Coleman September 1, 1965 UN17JERSITY OF CALIFORNIA Lawrence Radiation Laboratory Livermore, California AEC Contract No. W-7405 -eng-48 Subcommittee on Radiochemistry National Academy of Sciences—National Reaearcb Council Prfmtedin USA.