Neutrinos and How to Catch Them 1 Introduction

Total Page:16

File Type:pdf, Size:1020Kb

Neutrinos and How to Catch Them 1 Introduction Neutrinos and how to catch them D. Indumathi, M.V.N. Murthy and G. Rajasekaran The Institute of Mathematical Sciences, Chennai 600 113, India Important developments have occurred recently in neutrino physics. These in- clude the discovery of neutrino mass and the direct experimental proof of the thermonuclear hypothesis for the energy production mechanism in the Sun and other stars. These have led to world-wide plans for new neutrino laboratories. The India-based Neutrino Observatory (INO) is a project aimed at building a world-class underground neutrino laboratory. In this article we describe recent discoveries in neutrino physics as well as the INO project at an elementary level. 1 Introduction Neutrinos are ghostly particles that can penetrate the whole Earth without getting stopped. They are everywhere in the Universe. In fact, trillions of neutrinos are passing through our body every second. All the stars including our Sun produce neutrinos copiously in their core. This is because the nuclear fusion processes that are the source of solar and stellar energy also generate neutrinos. Neutrinos are also produced by exploding stars (supernovae). Other sources of neutrinos include cosmic rays, nuclear reactors, particle accelerators and radioactive ore deep inside the Earth. In addition there are cosmic relic neutrinos from the birth of the Universe. The energy spectrum of the naturally produced neutrinos spans nearly thirty orders of magnitude, from 10−5 eV to 1025 eV. Very important discoveries have been made recently in neutrino physics and neutrino astronomy. Neutrinos, which are the charge-neutral spin-1/2 particle emitted along with electrons (so-called beta-rays) in the radio-active decay of nuclei, were thought to be massless. The new discovery is that they are actually massive, although much lighter than any other particle including the electron. While there is now experimental proof, through the detection of solar neutrinos, that the Sun and other stars are powered by thermonuclear fusion reacions, the same experiments also clearly indicated that neutrinos exhibit the quantum-mechanical phenomenon called oscillation. Impelled by these exciting discoveries, world-wide plans are being made now, for further studies of neutrinos and their properties: their masses, the nature of neutrino oscillation and the nature of the neutrino itself. India was a pioneer in neutrino experiments. In fact, cosmic-ray-produced neutrinos were first detected in the deep mines of Kolar Gold Fields (KGF) in 1965. Although the KGF experiments were closed down because of the closure of the mines, it is now planned to revive underground neutrino experiments in India. The India-based Neutrino Observatory (INO) is a project proposal for an underground laboratory that can house neutrino experiments. We shall give an elementary review of the recent discoveries in neutrino physics and also describe the INO project. The article will attempt to paint an elementary picture of neutrinos and their interactions while highlighting the exciting discoveries that have been made and can yet be made in this field, and to enthuse students, scientists and engineers alike about the vast possibilities in neutrino physics in the world, and, in particular, at the future INO laboratory. The plan of the article is as follows. After a brief history of neutrino physics, we take up solar neutrinos. Because of the historical importance of the solar neutrino problem and its solution, solar neutrinos are discussed in detail. This is followed by brief accounts of 1 atmospheric, reactor and geo-neutrinos. Finally in section 9 we describe the INO project. 2 Brief History of Neutrino Physics The chief landmarks in the history of neutrino physics are given below. We shall describe them in more detail in the rest of the article. • 1930: Wolfgang Pauli proposes the existence of a neutral particle. • 1932: Enrico Fermi gives it the name neutrino and constructs the theory of beta decay. • 1956: Clyde Cowan and Frederick Reines detect the neutrino for the first time. • 1965: The KGF experiment in India observes the neutrinos from atmosphere. • 1967: Raymond Davis’ experiment and the genesis of the solar neutrino problem. • 1998: Discovery of neutrino mass by the Super-Kamioka experiment in Japan. • 2002: Solution of the solar neutrino problem by the SNO detector in Canada. • 2002: The KamLAND experiment in Japan confirms oscillations by a terrestrial ex- periment. • 2005: Detection of geo-neutrinos by KamLAND. Pauli proposed the existence of the neutrino in order to save the principle of conservation of energy in the beta decay of nuclei. He hypothesised that a neutrino is always produced along with the electron in nuclear beta decay. Fermi incorporated the notion of neutrinos into his theory of beta decay. Because of the success of Fermi’s theory in explaining quantitatively all the experimental data on nuclear beta decays, there was hardly any doubt (at least in theorists’ minds) that neutrinos existed; however, a direct detection of the neutrino came only in 1956. This achievement was due to Cowan and Reines who succeeded in detecting the antineutrinos produced from fission fragments in a nuclear reactor. In 1965, neutrinos produced from cosmic-ray interactions with Earth’s atmosphere were detected at KGF in India and later in many other experiments in the world. Solar neu- trinos were detected by Davis et al. in 1967 in the U.S.A. and later by other detectors. The Kamioka detector in Japan and other detectors also observed neutrinos from the su- pernova explosion SN1987A. The Super-Kamioka detector discovered neutrino mass through the study of cosmic-ray-produced neutrinos in 1998, while the Sudbury Neutrino Observa- tory (SNO) in Canada solved the solar neutrino problem in 2002. The KamLAND detector in Japan confirmed the neutrino oscillation in a purely terrestrial experiment, using an- tineutrinos from nuclear reactors, in 2002 and the same detector detected geo-neutrinos in 2005. 3 Solar Neutrinos In the 19th century, the source of the energy in the Sun and the stars remained a major puzzle in science, which led to many controversies. The answer to this question held the key to several related questions: • What is the age of the Sun? 2 • This in turn is intimately related to the origin of life on Earth, since the ultimate source of energy for everything that happens on Earth is derived from the Sun. Charles Darwin had a crude estimate of the age of the Earth as about 300 million years old, based on the rate of erosion of the Wealds in the South of England. This seemed to Darwin long enough to produce the varied species on Earth through natural selection. This was contradicted by the physicists, most notably William Thomson, Lord Kelvin, at that time. Kelvin gave an estimate of 30 million years as the age of the Sun by calculating its gravitational energy divided by the rate at which the energy is radiated. Obviously the age of the Earth could not have been larger than the age of Sun. Certainly life on Earth could not have existed before the Sun! Finally the problem was solved only after the discovery of the atomic nucleus and the tremendous energy locked up inside the nucleus. It was Arthur Eddington who, in 1920, suggested nuclear energy as the source of solar and stellar energy. It took many more years for the development of nuclear physics to advance to the stage when Hans Bethe, the Master Nuclear Physicist, analysed all the relevant facts and solved the problem completely in 1939. A year earlier, Carl von Weizs¨acker had given a partial solution. Bethe’s paper is a masterpiece. It gave a complete picture of the thermonuclear reactions that power the Sun and the stars. However, a not-so-well-known fact is that Bethe omitted the neutrino that is emitted along with the electron, in the reactions enumerated by him. The neutrino, which became a part of Fermi’s theory for beta decay, was already a well- known entity in nuclear physics. So it is rather inexplicable why Bethe ignored the neutrinos in his famous paper. The authority of Bethe’s paper was so great that astronomers and astrophysicists who followed him in subsequent years failed to note the presence of neutrinos. Even many textbooks in Astronomy and Astrophysics written in the 1940s and 1950s did not mention neutrinos! This was unfortunate, since we must realize that, in spite of the great success of Bethe’s theory, it is nevertheless only a theory. Observation of neutrinos from the Sun is the only direct experimental evidence for Eddington’s thermonuclear hypothesis and Bethe’s theory of energy production. Herein lies the importance of detecting solar neutrinos. The basic process of thermonuclear fusion in the Sun and stars is four protons combining into an alpha particle and releasing two positrons, two neutrinos and 26.7 MeV of energy. However, the probability of four protons meeting at a point is negligibly small even at the large densities existing in the solar core. Hence the actual series of nuclear reactions occurring in the solar and stellar cores are given by the so-called pp chain (see Box 1) and the carbon- cycle (see Box 2). In the carbon cycle the four protons are successively absorbed in a series of nuclei, starting and ending with carbon. In the pp-chain two protons combine to form the deuteron and further protons are added. In the Sun, the dominant process is the pp-chain. In heavier stars, it is the carbon cycle. 3 Box 1: The pp chain. + + p+p → D + e + νe p+p+e → D+ νe Eν ≤ 0.423 MeV Eν = 1.442 MeV 99.77% 0.23% D+p → He3 + γ 3 3 4 3 4 7 3 4 + He + He → He + p + p He + He → Be + γ He +p → He + e + νe 84.92% 15.08% 10−5% Eν ≤ 18.77 MeV 7 − 7 7 8 Be + e → Li + νe Be +p → B + γ 15.07% 0.01% Eν = 0.861 MeV (90%) Eν = 0.383 MeV (10%) 7 4 4 8 4 + Li +p → He + He B → 2He + e + νe Eν ≤ 15 MeV 4 + In all branches of the pp chain, the net process is 4p → He + 2e + 2νe.
Recommended publications
  • Updated Geoneutrino Measurement with Borexino
    UPDATED GEONEUTRINO MEASUREMENT WITH BOREXINO LIVIA LUDHOVA FOR BOREXINO COLLABORATION IKP-2, FORSCHUNGSZENTRUM JÜLICH AND RWTH AACHEN UNIVERSITY, GERMANY SEPTEMBER 10TH, 2019 TAUP 2019, TOYAMA, JAPAN OUTLINE (OR WHERE IS THIS ENERGY COMING FROM?) • What are geoneutrinos and why to study them • Expected geoneutrino signal at LNGS (Italy) • Borexino and antineutrino detection • Borexino geoneutrino measurement: fresh new results • Geological interpretation EARTH’S HEAT BUDGET Radiogenic heat & Integrated surface heat flux: Geoneutrinos can help! Htot = 47 + 2 TW Lithosphere Mantle Heat production in lithosphere “well” known Big uncertainty Mantle cooling 7 - 9 TW Heat production in mantle 1 – 27 TW 4 – 27 TW Core cooling 9 – 17 TW Core cooling Mantle cooling Geoneutrinos: antineutrinos/neutrinos from the decays of long-lived radioactive isotopes naturally present in the Earth 238U (99.2739% of natural U) à 206Pb + 8 α + 8 e- + 6 anti-neutrinos + 51.7 MeV 232Th à 208Pb + 6 α + 4 e- + 4 anti-neutrinos + 42.8 MeV 235U (0.7205% of natural U) à 207Pb + 7 α + 4 e- + 4 anti-neutrinos + 46.4 MeV 40K (0.012% of natural K) à 40Ca + e- + 1 anti-neutrino + 1.32 MeV (BR=89.3 %) 40K + e- à 40Ar + 1 neutrino + 1.505 MeV (BR=10.7 %) q the only direct probe of the deep Earth q released heat and geoneutrino flux in a well fixed ratio q to measure geoneutrino flux = (in principle) = to get radiogenic heat q in practice (as always) more complicated….. Earth shines in geoneutrinos: flux ~106 cm-2 s-1 leaving freely and instantaneously the Earth interior (to
    [Show full text]
  • Review Article Geoneutrinos
    Hindawi Publishing Corporation Advances in High Energy Physics Volume 2012, Article ID 235686, 34 pages doi:10.1155/2012/235686 Review Article Geoneutrinos Ondrejˇ Srˇ amek,´ 1 William F. McDonough,1 and John G. Learned2 1 Department of Geology, University of Maryland, College Park, MD 20742, USA 2 Department of Physics and Astronomy, University of Hawaii, Honolulu, HI 96822, USA Correspondence should be addressed to Ondrejˇ Srˇ amek,´ [email protected] Received 9 July 2012; Accepted 20 October 2012 Academic Editor: Arthur B. McDonald Copyright q 2012 Ondrejˇ Srˇ amek´ et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Neutrino geophysics is an emerging interdisciplinary field with the potential to map the abundances and distribution of radiogenic heat sources in the continental crust and deep Earth. To date, data from two different experiments quantify the amount of Th and U in the Earth and begin to put constraints on radiogenic power in the Earth available for driving mantle convection and plate tectonics. New improved detectors are under construction or in planning stages. Critical testing of compositional models of the Earth requires integrating geoneutrino and geological observations. Such tests will lead to significant constraints on the absolute and relative abundances of U and Th in the continents. High radioactivity in continental crust puts limits on land-based observatories’ capacity to resolve mantle models with current detection methods. Multiple-site measurement in oceanic areas away from continental crust and nuclear reactors offers the best potential to extract mantle information.
    [Show full text]
  • Experimental Aspects of Geoneutrino Detection: Status and Perspectives
    Experimental Aspects of Geoneutrino Detection: Status and Perspectives O. Smirnov,1 1JINR, Joint Institute for Nuclear Research, Dubna, Russian Federation October 22, 2019 Abstract Neutrino geophysics, the study of the Earth's interior by measuring the fluxes of geologically produced neutrino at its surface, is a new interdisciplinary field of science, rapidly developing as a synergy between geology, geophysics and particle physics. Geoneutrinos, antineutrinos from long- lived natural isotopes responsible for the radiogenic heat flux, provide valuable information for the chemical composition models of the Earth. The calculations of the expected geoneutrino signal are discussed, together with experimental aspects of geoneutrino detection, including the description of possible backgrounds and methods for their suppression. At present, only two detectors, Borexino and KamLAND, have reached sensitivity to the geoneutrino. The experiments accumulated a set of ∼190 geoneutrino events and continue the data acquisition. The detailed description of the experiments, their results on geoneutrino detection, and impact on geophysics are presented. The start of operation of other detectors sensitive to geoneutrinos is planned for the near future: the SNO+ detector is being filled with liquid scintillator, and the biggest ever 20 kt JUNO detector is under construction. A review of the physics potential of these experiments with respect to the geoneutrino studies, along with other proposals, is presented. New ideas and methods for geoneutrino detection are reviewed. Contents 1 Introduction 2 2 Geoneutrinos and the Earth's heat 4 2.1 Long-lived radiogenic elements . 4 2.2 Radiogenic heat and geoneutrino luminosity of the Earth . 9 arXiv:1910.09321v1 [physics.geo-ph] 21 Oct 2019 3 Geoneutrino flux calculation 11 3.1 Neutrino oscillations .
    [Show full text]
  • Neutrino Oscillations: the Rise of the PMNS Paradigm Arxiv:1710.00715
    Neutrino oscillations: the rise of the PMNS paradigm C. Giganti1, S. Lavignac2, M. Zito3 1 LPNHE, CNRS/IN2P3, UPMC, Universit´eParis Diderot, Paris 75252, France 2Institut de Physique Th´eorique,Universit´eParis Saclay, CNRS, CEA, Gif-sur-Yvette, France∗ 3IRFU/SPP, CEA, Universit´eParis-Saclay, F-91191 Gif-sur-Yvette, France November 17, 2017 Abstract Since the discovery of neutrino oscillations, the experimental progress in the last two decades has been very fast, with the precision measurements of the neutrino squared-mass differences and of the mixing angles, including the last unknown mixing angle θ13. Today a very large set of oscillation results obtained with a variety of experimental config- urations and techniques can be interpreted in the framework of three active massive neutrinos, whose mass and flavour eigenstates are related by a 3 3 unitary mixing matrix, the Pontecorvo- × Maki-Nakagawa-Sakata (PMNS) matrix, parameterized by three mixing angles θ12, θ23, θ13 and a CP-violating phase δCP. The additional parameters governing neutrino oscillations are the squared- mass differences ∆m2 = m2 m2, where m is the mass of the ith neutrino mass eigenstate. This ji j − i i review covers the rise of the PMNS three-neutrino mixing paradigm and the current status of the experimental determination of its parameters. The next years will continue to see a rich program of experimental endeavour coming to fruition and addressing the three missing pieces of the puzzle, namely the determination of the octant and precise value of the mixing angle θ23, the unveiling of the neutrino mass ordering (whether m1 < m2 < m3 or m3 < m1 < m2) and the measurement of the CP-violating phase δCP.
    [Show full text]
  • Exploring the Earth's Mantle with Geoneutrinos
    IL NUOVO CIMENTO Vol. 36 C, N. 1 Gennaio-Febbraio 2013 DOI 10.1393/ncc/i2013-11446-1 Colloquia: IFAE 2012 Exploring the Earth’s mantle with geoneutrinos ∗ G. Fiorentini(1)(2)(3),G.L.Fogli(4)(5),E.Lisi(5), F. Mantovani(1)(3)( ), A. M. Rotunno(4)andG. Xhixha(2) (1) Dipartimento di Fisica, Universit`a di Ferrara - Via Saragat 1, 44100 Ferrara, Italy (2) INFN, Laboratori Nazionali di Legnaro - Via dell’Universit`a 2 - 35020 Legnaro (PD), Italy (3) INFN, Sezione di Ferrara - Via Saragat 1, 44100 Ferrara, Italy (4) Dipartimento Interateneo di Fisica “Michelangelo Merlin” Via Amendola 173, 70126 Bari, Italy (5) INFN, Sezione di Bari - Via Orabona 4, 70126, Bari, Italy ricevuto il 31 Agosto 2012 Summary. — The KamLAND and Borexino experiments have observed, each at ∼ 4σ level, signals of electron antineutrinos produced in the decay chains of thorium and uranium in the Earth’s crust and mantle (Th and U geoneutrinos). Various pieces of geochemical and geophysical information allow an estimation of the crustal geoneutrino flux components with relatively small uncertainties. The mantle component may then be inferred by subtracting the estimated crustal flux from the measured total flux. On the base of this approach we find that crust- subtracted signals show hints of a residual mantle component, emerging at ∼ 2.4σ level by combining the KamLAND and Borexino data. The inferred mantle flux slightly favors scenarios with relatively high Th and U abundances, within ±1σ uncertainties comparable to the spread of predictions from recent mantle models. PACS 95.55.Vj – Neutrino, muon, pion, and other elementary particle detectors; cosmic ray detectors.
    [Show full text]
  • 100208 Mcdonough Ext
    PERSPECTIVES GEOPHYSICS Neutrinos created by nuclear decay may allow geoscientists to measure the distribution of Mapping the Earth’s Engine radioactive elements in the Earth. William F. McDonough article physicists and geophysicists optimal location for measuring the rarely meet to compare notes, but ear- Continental crust (>50%) distribution of heat-producing ele- lier this year researchers from these two Proposed Mantle (<50%) ments in the ancient core of a P geoneutrino disciplines gathered to discuss antineutrinos continent. Here, the antineutrino detectors (the antiparticle of the neutrino) (1). These signal will be dominated by the fundamental particles are a by-product of crustal component at about the reactions occurring in nuclear reactors and 80% level. This experiment will pass easily through Earth, but they are also SNO+ provide data on the bulk composi- generated deep inside Earth by the natural tion of the continents and place radioactive decay of uranium, thorium, and Core (~0%) limits on competing models of the potassium (in which case they are called continental crust’s composition. geoneutrinos). Particle physicists have re- The Boron Solar Neutrino experi- cently shown that it is possible to detect Hanohano ment (Borexino) detector, situated geoneutrinos and thus establish limits on the in central Italy (and hence some- amount of radioactive energy produced in the what removed from the regions of interior of our planet (2). This year’s joint France with many reactors), has meeting was aimed at enhancing communica- begun counting (5). This detector tion between the two disciplines in order to will accumulate a geoneutrino sig- on August 31, 2007 better constrain the distribution of Earth’s nal from a younger continental radioactive elements.
    [Show full text]
  • 40K Geoneutrino Detection
    40K Geoneutrino Detection Mark Chen Queen’s University and the Canadian Institute for Advanced Research Neutrino Geoscience 2015, Paris, France June 15, 2015 Why Potassium Geoneutrinos? n ~16% of Earth’s radiogenic heat is from 40K q would be good to quantify after 238U and 232Th n K/U ratio in chondrites > in the crust q would measurement help pin down abundances of other moderate volatiles in the Earth? n K may reside in the Earth’s core?? q e.g. Murthy, Lee and Jeanloz, Ohtani q does this help solve some core energetics issues (e.g. geodynamo, heat flow at CMB)? Th & U Volatility trend @ 1AU from Sun slide from Bill McDonough 40K Decay 40K→40Ca + e− +ν n 89.28% Qβ=1.311 MeV e 40 − 40 n 10.72% QEC=1.505 MeV K + e → Ar +ν e q 10.67% to 1.461 MeV state (Eν = 44 keV) q 0.05% to g.s. (Eν = 1.5 MeV) 0.0117% isotopic abundance 40K Spectrum + threshold for ν e + p → e + n [figure from KamLAND Nature paper] Potassium Geoneutrino Fluxes n (5-15) × 106 cm−2 s−1 for the antineutrinos 5 −2 −1 n (5-15) × 10 cm s for the 44 keV νe 3 −2 −1 n (2-6) × 10 cm s for the 1.5 MeV νe n compare to 1.44 MeV pep solar νe 8 −2 −1 1.42 × 10 cm s (and also CNO solar neutrinos at 1.5 MeV) You can probably forget about detecting the –5 1.5 MeV νe … only 63 keV away and 10 less intense! 40 K ν e Detection n ν e -e scattering q requires electron recoil directionality due to large flux of solar neutrinos (could imagine giant TPC) n 1/3 event per ton per year n NC nuclear excitation q not distinctive from νe or γ nuclear excitation n NC coherent neutrino-nucleus scattering
    [Show full text]
  • Expected Geoneutrino Signal at JUNO
    Expected geoneutrino signal at JUNO Virginia STRATI1,2,*, Marica BALDONCINI1,3, Ivan CALLEGARI2, Fabio MANTOVANI1,3, William F. McDONOUGH4, Barbara RICCI1,3, Gerti XHIXHA2 1 Department of Physics and Earth Sciences, University of Ferrara, Via Saragat 1, 44121 - Ferrara, Italy 2 INFN, Legnaro National Laboratories, Viale dell’Università, 2 - 35020 Legnaro (Padua) Italy 3 INFN, Ferrara Section, Via Saragat 1, 44121 - Ferrara, Italy 4 Department of Geology, University of Maryland, 237 Regents Drive, College Park, MD 20742, USA. *Corresponding author Email: [email protected] Abstract Constraints on the Earth’s composition and on its radiogenic energy budget come from the detection of geoneutrinos. The KamLAND and Borexino experiments recently reported the geoneutrino flux, which reflects the amount and distribution of U and Th inside the Earth. The JUNO neutrino experiment, designed as a 20 kton liquid scintillator detector, will be built in an underground laboratory in South China about 53 km from the Yangjiang and Taishan nuclear power plants, each one having a planned thermal power of approximately 18 GW. Given the large detector mass and the intense reactor antineutrino flux, JUNO aims to collect high statistics antineutrino signals from reactors but also to address the challenge of discriminating the geoneutrino signal from the reactor background. 6.5 The predicted geoneutrino signal at JUNO is 39.75.2 TNU, based on the existing reference Earth model, with the dominant source of uncertainty coming from the modeling of the compositional variability in the local upper crust that surrounds (out to ~500 km) the detector. A special focus is dedicated to the 6° × 4° Local Crust surrounding the detector which is estimated to contribute for the 44% of the signal.
    [Show full text]
  • Partial Radiogenic Heat Model for Earth Revealed by Geoneutrino Measurements
    ARTICLES PUBLISHED ONLINE: 17 JULY 2011 | DOI: 10.1038/NGEO1205 Partial radiogenic heat model for Earth revealed by geoneutrino measurements The KamLAND Collaboration* The Earth has cooled since its formation, yet the decay of radiogenic isotopes, and in particular uranium, thorium and potassium, in the planet’s interior provides a continuing heat source. The current total heat flux from the Earth to space is 44:2 ± 1:0 TW, but the relative contributions from residual primordial heat and radiogenic decay remain uncertain. However, radiogenic decay can be estimated from the flux of geoneutrinos, electrically neutral particles that are emitted during radioactive decay and can pass through the Earth virtually unaffected. Here we combine precise measurements of the geoneutrino flux from the Kamioka Liquid-Scintillator Antineutrino Detector, Japan, with existing measurements from the C8:8 Borexino detector, Italy. We find that decay of uranium-238 and thorium-232 together contribute 20:0−8:6 TW to Earth’s heat flux. The neutrinos emitted from the decay of potassium-40 are below the limits of detection in our experiments, but are known to contribute 4 TW. Taken together, our observations indicate that heat from radioactive decay contributes about half of Earth’s total heat flux. We therefore conclude that Earth’s primordial heat supply has not yet been exhausted. he Kamioka Liquid-Scintillator Antineutrino Detector mantle, outer core and inner core. Although the mechanical (KamLAND) Collaboration reported the results of the first properties and bulk composition of the shells are well established, Tstudy of electron antineutrinos (νe s) produced within the their detailed composition, including the abundances of radiogenic Earth in 2005 (ref.
    [Show full text]
  • Updated Geoneutrino Measurement with the Borexino Detector
    Updated Geoneutrino Measurement with the Borexino Detector Aktualisierte Geoneutrino-Messung mit dem Borexino-Detektor von Sindhujha Kumaran Master arbeit in Physik vorgelegt der Fakultat¨ fur¨ Mathematik, Informatik und Naturwissenschaften der RWTH AACHEN September 2018 angefertigt im Physikalischen Institut III. B Erstgutachter und Betreuer Zweitgutachter Prof. Dr. Livia Ludhova Prof. Dr. Achim Stahl Physikalischen Institut III. B Physikalischen Institut III. B RWTH Aachen RWTH Aachen Ich versichere, dass ich die Arbeit selbstst¨andigverfasst und keine anderen als die angegebenen Quellen und Hilfsmittel benutzt sowie Zitate kenntlich gemacht habe. Aachen, den To my dearest brother, Aswin. \That you are here|that life exists and identity, That the powerful play goes on, and you may contribute a verse." -O Me! O Life!, Walt Whitman Abstract Geoneutrinos are electron antineutrinos and neutrinos emitted in the radioactive decays from the Earth's interior. Due to the intrinsic dependence of the geoneutrino flux and the heat produced in the radioactive decays, geoneutrinos contribute uniquely to our knowledge about the Earth. The main goal of neutrino geophysics is to use the obtained geoneutrino signals in estimating the abundance and distribution of the heat producing elements such as 238U, 235U, 232Th and 40K. The radiogenic heat contribution, especially the mantle contribution to the total surface heat flux and the nature of the mantle still remain as open questions. The combination of the total geoneu- trino flux (≈106 cm−2s−1) and the weak interaction cross section (≈10−42 cm−2s−1) lead to huge statistical uncertainties in the current measurements. This has made the study of geoneutrinos quite challenging and so far, only two detectors, namely KamLAND and Borexino, have measured geoneutrinos.
    [Show full text]
  • Geoneutrinos and the Heat Budget of the Earth
    Geoneutrinos and the heat budget of the Earth Ondřej Šrámek University of Maryland presented at Department of Geophysics, Charles University in Prague on 14 November 2012 Collaboration with Bill McDonough (UMD), Steve Dye (HPU), Shijie Zhong (UCB), Edwin Kite (Caltech), Vedran Lekić (UMD) Seismology Geodynamics Mineral physics Experimental Geochemistry particle physics ......... Geoneutrinos “Geoneutrinos” = electron anti-neutrinos emitted in β− decays of naturally occurring radionuclides geo-ν’s now detectable ... and have been detected Measuring radioactivity of the Earth! How much radiogenic heating in the mantle?? What is the Earth made of?? Chemical reservoirs in the mantle?? 1. geophysical motivation 2. neutrino history 3. antineutrino production, propagation, detection 4. observations of geoneutrinos 5. predictions of geoneutrinos flux 6. perspectives Radiogenic heating rate in the mantle...? How do we know it...? heat output (surface heat flux) 238U primordial heat + 232 radiogenic heating Th 40K ? How much radiogenic heating in the Earth? How is it spatially distributed? ... implications for geodynamics U Th K Composition of Silicate Earth • U, Th, K are lithophile elements, strong arguments against presence in the core • Composition of “Silicate Earth” (BSE) of interest, Silicate Earth = whole Earth minus the core • [But: some unorthodox models even predicting natural nuclear reactor in Earth’s deep interior] • Cosmochemistry and geochemistry: BSE compositional estimates • Difficult. Usual problem in geophysics: rock samples only
    [Show full text]
  • Editorial Neutrino Masses and Oscillations
    Hindawi Publishing Corporation Advances in High Energy Physics Volume 2014, Article ID 823127, 4 pages http://dx.doi.org/10.1155/2014/823127 Editorial Neutrino Masses and Oscillations Elisa Bernardini,1 Leslie Camilleri,2 Vincenzo Flaminio,3 Srubabati Goswami,4 and Seon-Hee Seo5 1 DESY, Platanen Allee 6, 15738 Zeuthen, Germany 2 Columbia University 435 W. 116th Street, New York, NY 10027-7201, USA 3 Physics Department and INFN, Largo Bruno Pontecorvo, 56127 Pisa, Italy 4 Physical Research Laboratory, Navrangpura, Ahmedabad 380009, India 5 Department of Physics and Astronomy, Seoul National University, Republic of Korea Correspondence should be addressed to Vincenzo Flaminio; [email protected] Received 17 December 2013; Accepted 17 December 2013; Published 30 March 2014 Copyright © 2014 Elisa Bernardini et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The publication of this article was funded by SCOAP3. The year 2013 marks the 100th anniversary of the birth of originated a vast number of both experimental and theoreti- Bruno Pontecorvo, who first suggested the possibility that cal developments. neutrinos might have a nonzero mass such that oscillations The original ideas (1957-58) are first considered in this among different neutrino states might occur. Pontecorvo paper. This is followed by the consideration of a later paper constantly pursued this idea, after the discovery of other by Pontecorvo on neutrino oscillations (1967) and by the neutrino flavours, until his death. anticipation of the solar neutrino problem.
    [Show full text]