16. Fission and Fusion Particle and Nuclear Physics
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Spontaneous Fission of U234, Pu236, Cm240, and Cm244
Lawrence Berkeley National Laboratory Lawrence Berkeley National Laboratory Title Spontaneous Fission of U234, Pu236, Cm240, and Cm244 Permalink https://escholarship.org/uc/item/0df1j1qm Authors Ghiorso, A. Higgins, G.H. Larsh, A.E. et al. Publication Date 1952-04-21 eScholarship.org Powered by the California Digital Library University of California TWO-WEEK LOAN COPY This is a Library Circulating Copy which may be borrowed for two weeks. For a personal retention copy, call Tech. Info. Division, Ext. 5545 UCRL-1772 Unclassified-Chemistry Distribution UNIVEBSITY OF CALIFCEiNIil Radiation Laboratory Contract No, ti-7405-eng-4.8 24.4 SPONTANEOUS FISSION OF' I'Zu6, ~m~~~~ AND Gm A, Ghiorso, G. H, Higgins, A. E. Larsh, Go To Seaborg, and So G, Thompson April 21, 1752 Berkeley, California A. Ghiorso, G. H. Higgins, A. E. Larsh, G. T. Seaborg, and S. Go Thompson Radiation Laboratory and Department of Chemistry Uni versity of California, Berkeley, Californf a April 21, 1952 In a recent communication commenting on the mechanism of fission we called attention to the simple exponential dependence of spontaneous fission rate on Z~/Aand to the effect of an odd nucleon in slowing the fission process.1 Since it is of interest to test further the simple correlation of the spontaneous fission rate for even-even nuclides wfth z~/A~a further number of such rates have been determined, The spontaneous fission rates were measured by pladng the chemically purified samples on one electrode of a parallel plate ionization chamber, filled with a mixture of argon and carbon dioxide, which was connected with an amplifier f ollawed by a register and a stylus recorder. -
Nuclear Energy: Fission and Fusion
CHAPTER 5 NUCLEAR ENERGY: FISSION AND FUSION Many of the technologies that will help us to meet the new air quality standards in America can also help to address climate change. President Bill Clinton 1 Two distinct processes involving the nuclei of atoms can be harnessed, in principle, for energy production: fission—the splitting of a nucleus—and fusion—the joining together of two nuclei. For any given mass or volume of fuel, nuclear processes generate more energy than can be produced through any other fuel-based approach. Another attractive feature of these energy-producing reactions is that they do not produce greenhouse gases (GHG) or other forms of air pollution directly. In the case of nuclear fission—a mature though controversial energy technology—electricity is generated from the energy released when heavy nuclei break apart. In the case of nuclear fusion, much work remains in the quest to sustain the fusion reactions and then to design and build practical fusion power plants. Fusion’s fuel is abundant, namely, light atoms such as the isotopes of hydrogen, and essentially limitless. The most optimistic timetable for fusion development is half a century, because of the extraordinary scientific and engineering challenges involved, but fusion’s benefits are so globally attractive that fusion R&D is an important component of today’s energy R&D portfolio internationally. Fission power currently provides about 17 percent of the world’s electric power. As of December 1996, 442 nuclear power reactors were operating in 30 countries, and 36 more plants were under construction. If fossil plants were used to produce the amount of electricity generated by these nuclear plants, more than an additional 300 million metric tons of carbon would be emitted each year. -
Discovery of the Isotopes with Z<= 10
Discovery of the Isotopes with Z ≤ 10 M. Thoennessen∗ National Superconducting Cyclotron Laboratory and Department of Physics and Astronomy, Michigan State University, East Lansing, MI 48824, USA Abstract A total of 126 isotopes with Z ≤ 10 have been identified to date. The discovery of these isotopes which includes the observation of unbound nuclei, is discussed. For each isotope a brief summary of the first refereed publication, including the production and identification method, is presented. arXiv:1009.2737v1 [nucl-ex] 14 Sep 2010 ∗Corresponding author. Email address: [email protected] (M. Thoennessen) Preprint submitted to Atomic Data and Nuclear Data Tables May 29, 2018 Contents 1. Introduction . 2 2. Discovery of Isotopes with Z ≤ 10........................................................................ 2 2.1. Z=0 ........................................................................................... 3 2.2. Hydrogen . 5 2.3. Helium .......................................................................................... 7 2.4. Lithium ......................................................................................... 9 2.5. Beryllium . 11 2.6. Boron ........................................................................................... 13 2.7. Carbon.......................................................................................... 15 2.8. Nitrogen . 18 2.9. Oxygen.......................................................................................... 21 2.10. Fluorine . 24 2.11. Neon........................................................................................... -
Spontaneous Fission Half-Lives of Heavy and Superheavy Nuclei Within a Generalized Liquid Drop Model
Spontaneous fission half-lives of heavy and superheavy nuclei within a generalized liquid drop model Xiaojun Bao1, Hongfei Zhang1,∗ G. Royer2, Junqing Li1,3 June 4, 2018 1. School of Nuclear Science and Technology, Lanzhou University, Lanzhou 730000, China 2. Laboratoire Subatech, UMR: IN2P3/CNRS-Universit´e-Ecole des Mines, 4 rue A. Kastler, 44 Nantes, France 3. Institute of Modern Physics, Chinese Academy of Science, Lanzhou 730000, China Abstract We systematically calculate the spontaneous fission half-lives for heavy and superheavy arXiv:1302.7117v1 [nucl-th] 28 Feb 2013 nuclei between U and Fl isotopes. The spontaneous fission process is studied within the semi-empirical WKB approximation. The potential barrier is obtained using a generalized liquid drop model, taking into account the nuclear proximity, the mass asymmetry, the phenomenological pairing correction, and the microscopic shell cor- rection. Macroscopic inertial-mass function has been employed for the calculation of the fission half-life. The results reproduce rather well the experimental data. Rela- tively long half-lives are predicted for many unknown nuclei, sufficient to detect them if synthesized in a laboratory. Keywords: heavy and superheavy nuclei; half-lives; spontaneous fission ∗Corresponding author. Tel.: +86 931 8622306. E-mail address: [email protected] 1 1 Introduction Spontaneous fission of heavy nuclei was first predicted by Bohr and Wheeler in 1939 [1]. Their fission theory was based on the liquid drop model. Interestingly, their work also con- tained an estimate of a lifetime for fission from the ground state. Soon afterwards, Flerov and Petrzak [2] presented the first experimental evidence for spontaneous fission. -
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Photofission Cross Sections of 238U and 235U from 5.0 Mev to 8.0 Mev Robert Andrew Anderl Iowa State University
Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1972 Photofission cross sections of 238U and 235U from 5.0 MeV to 8.0 MeV Robert Andrew Anderl Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Nuclear Commons, and the Oil, Gas, and Energy Commons Recommended Citation Anderl, Robert Andrew, "Photofission cross sections of 238U and 235U from 5.0 MeV to 8.0 MeV " (1972). Retrospective Theses and Dissertations. 4715. https://lib.dr.iastate.edu/rtd/4715 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]. INFORMATION TO USERS This dissertation was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction, 1. The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity, 2. -
Compilation and Evaluation of Fission Yield Nuclear Data Iaea, Vienna, 2000 Iaea-Tecdoc-1168 Issn 1011–4289
IAEA-TECDOC-1168 Compilation and evaluation of fission yield nuclear data Final report of a co-ordinated research project 1991–1996 December 2000 The originating Section of this publication in the IAEA was: Nuclear Data Section International Atomic Energy Agency Wagramer Strasse 5 P.O. Box 100 A-1400 Vienna, Austria COMPILATION AND EVALUATION OF FISSION YIELD NUCLEAR DATA IAEA, VIENNA, 2000 IAEA-TECDOC-1168 ISSN 1011–4289 © IAEA, 2000 Printed by the IAEA in Austria December 2000 FOREWORD Fission product yields are required at several stages of the nuclear fuel cycle and are therefore included in all large international data files for reactor calculations and related applications. Such files are maintained and disseminated by the Nuclear Data Section of the IAEA as a member of an international data centres network. Users of these data are from the fields of reactor design and operation, waste management and nuclear materials safeguards, all of which are essential parts of the IAEA programme. In the 1980s, the number of measured fission yields increased so drastically that the manpower available for evaluating them to meet specific user needs was insufficient. To cope with this task, it was concluded in several meetings on fission product nuclear data, some of them convened by the IAEA, that international co-operation was required, and an IAEA co-ordinated research project (CRP) was recommended. This recommendation was endorsed by the International Nuclear Data Committee, an advisory body for the nuclear data programme of the IAEA. As a consequence, the CRP on the Compilation and Evaluation of Fission Yield Nuclear Data was initiated in 1991, after its scope, objectives and tasks had been defined by a preparatory meeting. -
R-Process: Observations, Theory, Experiment
r-process: observations, theory, experiment H. Schatz Michigan State University National Superconducting Cyclotron Laboratory Joint Institute for Nuclear Astrophysics 1. Observations: do we need s,r,p-process and LEPP? 2. r-process (and LEPP?) models 3. r-process experiments SNR 0103-72.6 Credit: NASA/CXC/PSU/S.Park et al. Origin of the heavy elements in the solar system s-process: secondary • nuclei can be studied Æ reliable calculations • site identified • understood? Not quite … r-process: primary • most nuclei out of reach • site unknown p-process: secondary (except for νp-process) Æ Look for metal poor`stars (Pagel, Fig 6.8) To learn about the r-process Heavy elements in Metal Poor Halo Stars CS22892-052 (Sneden et al. 2003, Cowan) 2 1 + solar r CS 22892-052 ) H / X CS22892-052 ( g o red (K) giant oldl stars - formed before e located in halo Galaxyc was mixed n distance: 4.7 kpc theya preserve local d mass ~0.8 M_sol n pollutionu from individual b [Fe/H]= −3.0 nucleosynthesisa events [Dy/Fe]= +1.7 recall: element number[X/Y]=log(X/Y)-log(X/Y)solar What does it mean: for heavy r-process? For light r-process? • stellar abundances show r-process • process is not universal • process is universal • or second process exists (not visible in this star) Conclusions depend on s-process Look at residuals: Star – solar r Solar – s-process – p-process s-processSimmerer from Simmerer (Cowan et etal.) al. /Lodders (Cowan et al.) s-processTravaglio/Lodders from Travaglio et al. -0.50 -0.50 -1.00 -1.00 -1.50 -1.50 log e log e -2.00 -2.00 -2.50 -2.50 30 40 50 60 70 80 90 30 40 50 60 70 80 90 Element number Element number ÆÆNeedNeed reliable reliable s-process s-process (models (models and and nu nuclearclear data, data, incl. -
VII. Nuclear Fission and Fusion Lorant Csige
VII.VII. NuclearNuclear FissionFission andand FusionFusion LorantLorant CsigeCsige LaboratoryLaboratory forfor NuclearNuclear PhysicsPhysics HungarianHungarian AcademyAcademy ofof SciencesSciences NuclearNuclear bindingbinding energy:energy: possibilitypossibility ofof energyenergy productionproduction NuclearNuclear FusionFusion ● Some basic principles: ─ two light nuclei should be very close to defeat the Coulomb repulsion → nuclear attraction: kinetic energy!! ─ not spontenious, difficult to achieve in reality ─ advantage: large amount of hydrogen and helium + solutions without producing any readioactive product NuclearNuclear fusionfusion inin starsstars ● proton-proton cycle: ~ mass of Sun, many branches ─ 2 + ν first step in all branches (Q=1.442 MeV): p+p → H+e +νe ● diproton formation (and immediate decay back to two protons) is the ruling process ● stable diproton is not existing → proton – proton fusion with instant beta decay! ● very slow process since weak interaction plays role → cross section has not yet been measrued experimentally (one proton „waits” 9 billion years to fuse) ─ second step: 2H+1H → 3He + γ + 5.49 MeV ● very fast process: only 4 seconds on the avarage ● 3He than fuse to produce 4He with three (four) differenct reactions (branches) ─ ppI branch: 3He + 3He → 4He + 1H + 1H + 12.86 MeV ─ ppII branch: ● 3He + 4He → 7Be + γ 7 7 ● 7 7 ν Be + e- → Li + νe ● 7Li + 1H → 4He + 4He ─ ppIII branch: only 0.11% energy of Sun, but source of neutrino problem ● 3He + 4He → 7Be + γ 7 1 8 8 + 4 4 ● 7 1 8 γ 8 + ν 4 4 Be + H → -
Uses of Isotopic Neutron Sources in Elemental Analysis Applications
EG0600081 3rd Conference on Nuclear & Particle Physics (NUPPAC 01) 20 - 24 Oct., 2001 Cairo, Egypt USES OF ISOTOPIC NEUTRON SOURCES IN ELEMENTAL ANALYSIS APPLICATIONS A. M. Hassan Department of Reactor Physics Reactors Division, Nuclear Research Centre, Atomic Energy Authority. Cairo-Egypt. ABSTRACT The extensive development and applications on the uses of isotopic neutron in the field of elemental analysis of complex samples are largely occurred within the past 30 years. Such sources are used extensively to measure instantaneously, simultaneously and nondestruclively, the major, minor and trace elements in different materials. The low residual activity, bulk sample analysis and high accuracy for short lived elements are improved. Also, the portable isotopic neutron sources, offer a wide range of industrial and field applications. In this talk, a review on the theoretical basis and design considerations of different facilities using several isotopic neutron sources for elemental analysis of different materials is given. INTRODUCTION In principle there are two ways to use neutrons for elemental and isotopic abundance analysis in samples. One is the neutron activation analysis which we call it the "off-line" where the neutron - induced radioactivity is observed after the end of irradiation. The other one we call it the "on-line" where the capture gamma-rays is observed during the neutron bombardment. Actually, the sequence of events occurring during the most common type of nuclear reaction used in this analysis namely the neutron capture or (n, gamma) reaction, is well known for the people working in this field. The neutron interacts with the target nucleus via a non-elastic collision, a compound nucleus forms in an excited state. -
Uranium (Nuclear)
Uranium (Nuclear) Uranium at a Glance, 2016 Classification: Major Uses: What Is Uranium? nonrenewable electricity Uranium is a naturally occurring radioactive element, that is very hard U.S. Energy Consumption: U.S. Energy Production: and heavy and is classified as a metal. It is also one of the few elements 8.427 Q 8.427 Q that is easily fissioned. It is the fuel used by nuclear power plants. 8.65% 10.01% Uranium was formed when the Earth was created and is found in rocks all over the world. Rocks that contain a lot of uranium are called uranium Lighter Atom Splits Element ore, or pitch-blende. Uranium, although abundant, is a nonrenewable energy source. Neutron Uranium Three isotopes of uranium are found in nature, uranium-234, 235 + Energy FISSION Neutron uranium-235, and uranium-238. These numbers refer to the number of Neutron neutrons and protons in each atom. Uranium-235 is the form commonly Lighter used for energy production because, unlike the other isotopes, the Element nucleus splits easily when bombarded by a neutron. During fission, the uranium-235 atom absorbs a bombarding neutron, causing its nucleus to split apart into two atoms of lighter mass. The first nuclear power plant came online in Shippingport, PA in 1957. At the same time, the fission reaction releases thermal and radiant Since then, the industry has experienced dramatic shifts in fortune. energy, as well as releasing more neutrons. The newly released neutrons Through the mid 1960s, government and industry experimented with go on to bombard other uranium atoms, and the process repeats itself demonstration and small commercial plants. -
An Introduction to the IAEA Neutron-Gamma Atlas Ye Myint1, Sein Htoon2
MM0900107 Jour. Myan. Aca<L Arts & Sa 2005 Vol. in. No. 3(i) Physics An Introduction to the IAEA Neutron-Gamma Atlas Ye Myint1, Sein Htoon2 Abstract NG-ATLAS is the abbreviation of Neutron-Gamma Atlas. Neutrons have proved to be especially effective in producing nuclear transformations, and gamma is the informer of nucleus. In nuclear physics, observable features or data are determined externally such as, energy, spin and cross section, where neutron and gamma plays dominant roles. (Neutron, gamma) (n,y) reactions of every isotope are vital importance for nuclear physicists. Introduction Inside the nucleus, protons and neutrons are simply two different states of a single particle, the nucleon. When neutron leaves the.nucleus, it is an unstable particle of half life 11.8 minutes, beta decay into proton. It is not feasible to describe beta decay without the references to Dirac 's hole theory; it is the memorandum for his hundred-birth day . The role of neutrons in nuclear physics is so high and its radiative capture by elements (neutron, gamma) reaction i.e, (n,y ) or NG-ATLAS is presented. The NG-Atlas. data file contains nuclear reaction cross section data of induced capture reaction for targets up to Z =96 . It comprises more than seven hundred isotopes, if the half lives are above half of a day. Cross sections are listed separately for ground , first and second excited states .And if the isomers have half life longer than 0.5 days , they are also include as targets .So the information includes a total of about one thousand reactions on different channels and the incident neutron energy ranging fromlO"5 eV to 20 MeV.