Β-Particle Energy-Summing Correction for Β-Delayed Proton Emission Measurements
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Arxiv:1901.01410V3 [Astro-Ph.HE] 1 Feb 2021 Mental Information Is Available, and One Has to Rely Strongly on Theoretical Predictions for Nuclear Properties
Origin of the heaviest elements: The rapid neutron-capture process John J. Cowan∗ HLD Department of Physics and Astronomy, University of Oklahoma, 440 W. Brooks St., Norman, OK 73019, USA Christopher Snedeny Department of Astronomy, University of Texas, 2515 Speedway, Austin, TX 78712-1205, USA James E. Lawlerz Physics Department, University of Wisconsin-Madison, 1150 University Avenue, Madison, WI 53706-1390, USA Ani Aprahamianx and Michael Wiescher{ Department of Physics and Joint Institute for Nuclear Astrophysics, University of Notre Dame, 225 Nieuwland Science Hall, Notre Dame, IN 46556, USA Karlheinz Langanke∗∗ GSI Helmholtzzentrum f¨urSchwerionenforschung, Planckstraße 1, 64291 Darmstadt, Germany and Institut f¨urKernphysik (Theoriezentrum), Fachbereich Physik, Technische Universit¨atDarmstadt, Schlossgartenstraße 2, 64298 Darmstadt, Germany Gabriel Mart´ınez-Pinedoyy GSI Helmholtzzentrum f¨urSchwerionenforschung, Planckstraße 1, 64291 Darmstadt, Germany; Institut f¨urKernphysik (Theoriezentrum), Fachbereich Physik, Technische Universit¨atDarmstadt, Schlossgartenstraße 2, 64298 Darmstadt, Germany; and Helmholtz Forschungsakademie Hessen f¨urFAIR, GSI Helmholtzzentrum f¨urSchwerionenforschung, Planckstraße 1, 64291 Darmstadt, Germany Friedrich-Karl Thielemannzz Department of Physics, University of Basel, Klingelbergstrasse 82, 4056 Basel, Switzerland and GSI Helmholtzzentrum f¨urSchwerionenforschung, Planckstraße 1, 64291 Darmstadt, Germany (Dated: February 2, 2021) The production of about half of the heavy elements found in nature is assigned to a spe- cific astrophysical nucleosynthesis process: the rapid neutron capture process (r-process). Although this idea has been postulated more than six decades ago, the full understand- ing faces two types of uncertainties/open questions: (a) The nucleosynthesis path in the nuclear chart runs close to the neutron-drip line, where presently only limited experi- arXiv:1901.01410v3 [astro-ph.HE] 1 Feb 2021 mental information is available, and one has to rely strongly on theoretical predictions for nuclear properties. -
Two-Proton Radioactivity 2
Two-proton radioactivity Bertram Blank ‡ and Marek P loszajczak † ‡ Centre d’Etudes Nucl´eaires de Bordeaux-Gradignan - Universit´eBordeaux I - CNRS/IN2P3, Chemin du Solarium, B.P. 120, 33175 Gradignan Cedex, France † Grand Acc´el´erateur National d’Ions Lourds (GANIL), CEA/DSM-CNRS/IN2P3, BP 55027, 14076 Caen Cedex 05, France Abstract. In the first part of this review, experimental results which lead to the discovery of two-proton radioactivity are examined. Beyond two-proton emission from nuclear ground states, we also discuss experimental studies of two-proton emission from excited states populated either by nuclear β decay or by inelastic reactions. In the second part, we review the modern theory of two-proton radioactivity. An outlook to future experimental studies and theoretical developments will conclude this review. PACS numbers: 23.50.+z, 21.10.Tg, 21.60.-n, 24.10.-i Submitted to: Rep. Prog. Phys. Version: 17 December 2013 arXiv:0709.3797v2 [nucl-ex] 23 Apr 2008 Two-proton radioactivity 2 1. Introduction Atomic nuclei are made of two distinct particles, the protons and the neutrons. These nucleons constitute more than 99.95% of the mass of an atom. In order to form a stable atomic nucleus, a subtle equilibrium between the number of protons and neutrons has to be respected. This condition is fulfilled for 259 different combinations of protons and neutrons. These nuclei can be found on Earth. In addition, 26 nuclei form a quasi stable configuration, i.e. they decay with a half-life comparable or longer than the age of the Earth and are therefore still present on Earth. -
2.3 Neutrino-Less Double Electron Capture - Potential Tool to Determine the Majorana Neutrino Mass by Z.Sujkowski, S Wycech
DEPARTMENT OF NUCLEAR SPECTROSCOPY AND TECHNIQUE 39 The above conservatively large systematic hypothesis. TIle quoted uncertainties will be soon uncertainty reflects the fact that we did not finish reduced as our analysis progresses. evaluating the corrections fully in the current analysis We are simultaneously recording a large set of at the time of this writing, a situation that will soon radiative decay events for the processes t e'v y change. This result is to be compared with 1he and pi-+eN v y. The former will be used to extract previous most accurate measurement of McFarlane the ratio FA/Fv of the axial and vector form factors, a et al. (Phys. Rev. D 1984): quantity of great and longstanding interest to low BR = (1.026 ± 0.039)'1 I 0 energy effective QCD theory. Both processes are as well as with the Standard Model (SM) furthermore very sensitive to non- (V-A) admixtures in prediction (Particle Data Group - PDG 2000): the electroweak lagLangian, and thus can reveal BR = (I 038 - 1.041 )*1 0-s (90%C.L.) information on physics beyond the SM. We are currently analyzing these data and expect results soon. (1.005 - 1.008)* 1W') - excl. rad. corr. Tale 1 We see that even working result strongly confirms Current P1IBETA event sxpelilnentstatistics, compared with the the validity of the radiative corrections. Another world data set. interesting comparison is with the prediction based on Decay PIBETA World data set the most accurate evaluation of the CKM matrix n >60k 1.77k element V d based on the CVC hypothesis and ihce >60 1.77_ _ _ results -
Problem Set 3 Solutions
22.01 Fall 2016, Problem Set 3 Solutions October 9, 2016 Complete all the assigned problems, and do make sure to show your intermediate work. 1 Activity and Half Lives 1. Given the half lives and modern-day abundances of the three natural isotopes of uranium, calculate the isotopic fractions of uranium when the Earth first formed 4.5 billion years ago. Today, uranium consists of 0.72% 235U, 99.2745% 238U, and 0.0055% 234U. However, it is clear that the half life of 234U (245,500 years) is so short compared to the lifetime of the Earth (4,500,000,000 years) that it would have all decayed away had there been some during the birth of the Earth. Therefore, we look a little closer, and find that 234U is an indirect decay product of 238U, by tracing it back from its parent nuclides on the KAERI table: α β− β− 238U −! 234T h −! 234P a −! 234U (1) Therefore we won’t consider there being any more 234U than would normally be in equi librium with the 238U around at the time. We set up the two remaining equations as follows: −t t ;235 −t t ;238 = 1=2 = 1=2 N235 = N0235 e N238 = N0238 e (2) Using the current isotopic abundances from above as N235 and N238 , the half lives from n 9 t 1 1 the KAERI Table of Nuclides t =2;235 = 703800000 y; t =2;238 = 4:468 · 10 y , and the lifetime of the earth in years (keeping everything in the same units), we arrive at the following expressions for N0235 and N0238 : N235 0:0072 N238 0:992745 N0235 =−t = 9 = 4:307N0238 =−t = 9 = 2:718 (3) =t1 ;235 −4:5·10 =7:038·108 =t1 ;238 −4:5·10 =4:468·109 e =2 e e =2 e Finally, taking the ratios of these two relative abundances gives us absolute abundances: 4:307 2:718 f235 = = 0:613 f238 = = 0:387 (4) 4:307 + 2:718 4:307 + 2:718 235U was 61.3% abundant, and 238U was 38.7% abundant. -
Nuclear Glossary
NUCLEAR GLOSSARY A ABSORBED DOSE The amount of energy deposited in a unit weight of biological tissue. The units of absorbed dose are rad and gray. ALPHA DECAY Type of radioactive decay in which an alpha ( α) particle (two protons and two neutrons) is emitted from the nucleus of an atom. ALPHA (ααα) PARTICLE. Alpha particles consist of two protons and two neutrons bound together into a particle identical to a helium nucleus. They are a highly ionizing form of particle radiation, and have low penetration. Alpha particles are emitted by radioactive nuclei such as uranium or radium in a process known as alpha decay. Owing to their charge and large mass, alpha particles are easily absorbed by materials and can travel only a few centimetres in air. They can be absorbed by tissue paper or the outer layers of human skin (about 40 µm, equivalent to a few cells deep) and so are not generally dangerous to life unless the source is ingested or inhaled. Because of this high mass and strong absorption, however, if alpha radiation does enter the body through inhalation or ingestion, it is the most destructive form of ionizing radiation, and with large enough dosage, can cause all of the symptoms of radiation poisoning. It is estimated that chromosome damage from α particles is 100 times greater than that caused by an equivalent amount of other radiation. ANNUAL LIMIT ON The intake in to the body by inhalation, ingestion or through the skin of a INTAKE (ALI) given radionuclide in a year that would result in a committed dose equal to the relevant dose limit . -
Recent Developments in Radioactive Charged-Particle Emissions
Recent developments in radioactive charged-particle emissions and related phenomena Chong Qi, Roberto Liotta, Ramon Wyss Department of Physics, Royal Institute of Technology (KTH), SE-10691 Stockholm, Sweden October 19, 2018 Abstract The advent and intensive use of new detector technologies as well as radioactive ion beam facilities have opened up possibilities to investigate alpha, proton and cluster decays of highly unstable nuclei. This article provides a review of the current status of our understanding of clustering and the corresponding radioactive particle decay process in atomic nuclei. We put alpha decay in the context of charged-particle emissions which also include one- and two-proton emissions as well as heavy cluster decay. The experimental as well as the theoretical advances achieved recently in these fields are presented. Emphasis is given to the recent discoveries of charged-particle decays from proton-rich nuclei around the proton drip line. Those decay measurements have shown to provide an important probe for studying the structure of the nuclei involved. Developments on the theoretical side in nuclear many-body theories and supercomputing facilities have also made substantial progress, enabling one to study the nuclear clusterization and decays within a microscopic and consistent framework. We report on properties induced by the nuclear interaction acting in the nuclear medium, like the pairing interaction, which have been uncovered by studying the microscopic structure of clusters. The competition between cluster formations as compared to the corresponding alpha-particle formation are included. In the review we also describe the search for super-heavy nuclei connected by chains of alpha and other radioactive particle decays. -
Abundance and Radioactivity of Unstable Isotopes
5 RADIONUCLIDE DECAY AND PRODUCTION This section contains a brief review of relevant facts about radioactivity, i.e. the phenomenon of nuclear decay, and about nuclear reactions, the production of nuclides. For full details the reader is referred to textbooks on nuclear physics and radiochemistry, and on the application of radioactivity in the earth sciences (cited in the list of references). 5.1 NUCLEAR INSTABILITY If a nucleus contains too great an excess of neutrons or protons, it will sooner or later disintegrate to form a stable nucleus. The different modes of radioactive decay will be discussed briefly. The various changes that can take place in the nucleus are shown in Fig.5.1 In transforming into a more stable nucleus, the unstable nucleus looses potential energy, part of its binding energy. This energy Q is emitted as kinetic energy and is shared by the particles formed according to the laws of conservation of energy and momentum (see Sect.5.3). The energy released during nuclear decay can be calculated from the mass budget of the decay reaction, using the equivalence of mass and energy, discussed in Sect.2.4. The atomic mass determinations have been made very accurately and precisely by mass spectrometric measurement: 2 E = [Mparent Mdaughter] P mc (5.1) with 1 amu V 931.5 MeV (5.2) Disintegration of a parent nucleus produces a daughter nucleus which generally is in an excited state. After an extremely short time the daughter nucleus looses the excitation energy through the emittance of one or more (gamma) rays, electromagnetic radiation with a very short wavelength, similar to the emission of light (also electromagnetic radiation , but with a longer wavelength) by atoms which have been brought into an excited state. -
Two-Proton Decay Energy and Width of 19Mg(G.S.)
University of Pennsylvania ScholarlyCommons Department of Physics Papers Department of Physics 7-30-2007 Two-Proton Decay Energy and Width of 19Mg(g.s.) H. Terry Fortune University of Pennsylvania, [email protected] Rubby Sherr Princeton University Follow this and additional works at: https://repository.upenn.edu/physics_papers Part of the Physics Commons Recommended Citation Fortune, H. T., & Sherr, R. (2007). Two-Proton Decay Energy and Width of 19Mg(g.s.). Retrieved from https://repository.upenn.edu/physics_papers/171 Suggested Citation: H.T. Fortune and R. Sherr. (2007). Two-proton decay energy and width of 19Mg(g.s.). Physical Review C 76, 014313. © 2007 The American Physical Society http://dx.doi.org/10.1103/PhysRevC.76.014313 This paper is posted at ScholarlyCommons. https://repository.upenn.edu/physics_papers/171 For more information, please contact [email protected]. Two-Proton Decay Energy and Width of 19Mg(g.s.) Abstract We use a weak-coupling procedure and results of a shell-model calculation to compute the two-proton separation energy of 19Mg. Our result is at the upper end of the previous range, but 19Mg is still bound for single proton decay to 18Na. We also calculate the 2p decay width. Disciplines Physical Sciences and Mathematics | Physics Comments Suggested Citation: H.T. Fortune and R. Sherr. (2007). Two-proton decay energy and width of 19Mg(g.s.). Physical Review C 76, 014313. © 2007 The American Physical Society http://dx.doi.org/10.1103/PhysRevC.76.014313 This journal article is available at ScholarlyCommons: https://repository.upenn.edu/physics_papers/171 PHYSICAL REVIEW C 76, 014313 (2007) Two-proton decay energy and width of 19Mg(g.s.) H. -
Radioactive Decay & Decay Modes
CHAPTER 1 Radioactive Decay & Decay Modes Decay Series The terms ‘radioactive transmutation” and radioactive decay” are synonymous. Many radionuclides were found after the discovery of radioactivity in 1896. Their atomic mass and mass numbers were determined later, after the concept of isotopes had been established. The great variety of radionuclides present in thorium are listed in Table 1. Whereas thorium has only one isotope with a very long half-life (Th-232, uranium has two (U-238 and U-235), giving rise to one decay series for Th and two for U. To distin- guish the two decay series of U, they were named after long lived members: the uranium-radium series and the actinium series. The uranium-radium series includes the most important radium isotope (Ra-226) and the actinium series the most important actinium isotope (Ac-227). In all decay series, only α and β− decay are observed. With emission of an α particle (He- 4) the mass number decreases by 4 units, and the atomic number by 2 units (A’ = A - 4; Z’ = Z - 2). With emission β− particle the mass number does not change, but the atomic number increases by 1 unit (A’ = A; Z’ = Z + 1). By application of the displacement laws it can easily be deduced that all members of a certain decay series may differ from each other in their mass numbers only by multiples of 4 units. The mass number of Th-232 is 323, which can be written 4n (n=58). By variation of n, all possible mass numbers of the members of decay Engineering Aspects of Food Irradiation 1 Radioactive Decay series of Th-232 (thorium family) are obtained. -
CHAPTER 2 the Nucleus and Radioactive Decay
1 CHEMISTRY OF THE EARTH CHAPTER 2 The nucleus and radioactive decay 2.1 The atom and its nucleus An atom is characterized by the total positive charge in its nucleus and the atom’s mass. The positive charge in the nucleus is Ze , where Z is the total number of protons in the nucleus and e is the charge of one proton. The number of protons in an atom, Z, is known as the atomic number and dictates which element an atom represents. The nucleus is also made up of N number of neutrally charged particles of similar mass as the protons. These are called neutrons . The combined number of protons and neutrons, Z+N , is called the atomic mass number A. A specific nuclear species, or nuclide , is denoted by A Z Γ 2.1 where Γ represents the element’s symbol. The subscript Z is often dropped because it is redundant if the element’s symbol is also used. We will soon learn that a mole of protons and a mole of neutrons each have a mass of approximately 1 g, and therefore, the mass of a mole of Z+N should be very close to an integer 1. However, if we look at a periodic table, we will notice that an element’s atomic weight, which is the mass of one mole of its atoms, is rarely close to an integer. For example, Iridium’s atomic weight is 192.22 g/mole. The reason for this discrepancy is that an element’s neutron number N can vary. -
Proton Decay at the Drip-Line Magic Number Z = 82, Corresponding to the Closure of a Major Nuclear Shell
NEWS AND VIEWS NUCLEAR PHYSICS-------------------------------- case since it has one proton more than the Proton decay at the drip-line magic number Z = 82, corresponding to the closure of a major nuclear shell. In Philip Woods fact the observed proton decay comes from an excited intruder state configura WHAT determines whether a nuclear ton decay half-life measurements can be tion formed by the promotion of a proton species exists? For nuclear scientists the used to explore nuclear shell structures in from below the Z=82 shell closure. This answer to this poser is that the species this twilight zone of nuclear existence. decay transition was used to provide should live long enough to be identified The proton drip-line sounds an inter unique information on the quantum mix and its properties studied. This still begs esting place to visit. So how do we get ing between normal and intruder state the fundamental scientific question of there? The answer is an old one: fusion. configurations in the daughter nucleus. what the ultimate boundaries to nuclear In this case, the fusion of heavy nuclei Following the serendipitous discovery existence are. Work by Davids et al. 1 at produces highly neutron-deficient com of nuclear proton decay4 from an excited Argonne National Laboratory in the pound nuclei, which rapidly de-excite by state in 1970, and the first example of United States has pinpointed the remotest boiling off particles and gamma-rays, leav ground-state proton decay5 in 1981, there border post to date, with the discovery of ing behind a plethora of highly unstable followed relative lulls in activity. -
RIA, Beta Decay and the R-Process
Preliminaries So Far Future Beta Decay, the R Process, RIA J. Engel April 4, 2006 Preliminaries So Far Future 1 Beta Decay is Important, Hard 2 What’s Been Done So Far 3 Future Work Preliminaries So Far Future Beta-Decay Far From Stability is Important 126 Limits of nuclear existence Half-lives are particularly 82 important at the r-process r-process “ladders” (N=50, 82, 126) 50 protons 82 ry where abundances peak. These d 28 rp-process 20 ctional Theo half-lives determine the 50 t Mean Fiel 8 28 neutrons Density Fun r-process time scale. 2 20 Selfconsisten 2 8 A=10 A~60 A=12 But others are also important; 0Ñω Shell Towards a unified affect abundances between Ab initio Model description of the nucleus few-body peaks. calculations No-Core Shell Model G-matrix Yes, uncertainties in astrophysics dwarf those in nuclear physics, but we won’t really understand the nucleosynthesis until both are reduced. 5 Preliminaries So Far Future Calculating Beta Decay is Hard. (though it gets easier in neutron-rich nuclei). To calculate beta decay between two states, you need: an accurate value for the decay energy ∆E (since −5 T1/2 ∝ ∆E ) matrix elements of the GT operator ~στ− and (sometimes) “forbidden” operators ~r~στ− between the two states .[Most of the strength of is above threshold, btw]. So your nuclear structure model must do a good job with nuclear masses, spectra, and wave functions, and to simulate the r process it must do the job in almost all isotopes.