Fundamentals of Undervoltage Breakdown Through the Townsend Mechanism
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Study of Memory Effect in an Atmospheric Pressure Townsend
THÈSE En vue de l’obtention du DOCTORAT DE L’UNIVERSITÉ DE TOULOUSE Délivré par l'Université Toulouse 3 - Paul Sabatier Présentée et soutenue par Xi LIN Le 22 février 2019 Study of memory effect in an Atmospheric Pressure Townsend Discharge in the mixture N2/O2 using laser induced fluorescence Ecole doctorale : GEET - Génie Electrique Electronique et Télécommunications : du système au nanosystème Spécialité : Ingénierie des Plasmas Unité de recherche : LAPLACE - Laboratoire PLAsma et Conversion d'Énergie - CNRS-UPS-INPT Thèse dirigée par Simon DAP et Nicolas GHERARDI Jury Mme Svetlana Starikovskaia, Rapporteuse M. Ronny Brandenburg, Rapporteur Mme Françoise Massines, Examinateur M. Frédéric Marchal, Examinateur M. Philippe Teulet, Examinateur M. Simon DAP, Directeur de thèse Acknowledgement I would like to express my deepest thanks to my supervisor, Simon Dap. He has devoted so much time on teaching and leading me into the world of plasma physics. I am very appreciated for his patience and encouragement, also thanks to his support and rich discussion on physics, I finally achieve my thesis. I would also like to express my thanks to Nicolas Naudé for the fruitful discussions and suggestions on electrical characteristics of discharge, and for his knowledge on electrode fabrication and on OES spectroscopy. Thanks to Nicolas Gherardi for his confidence and support on me. Thanks to Prof. Svetlana M Starikovskaia and Prof. Ronny Brandenburg, for reviewing my thesis. I would also like to extend my gratitude to three other jury members, Prof. Françoise Massines, Prof. Feédéric Marchal and Prof. Philippe Teulet, for being the examiners of my work. I appreciate the assistance and advice from the technicians and engineers of Laplace, Benoît Schlegel, Fédéric Sidor, Vincent Bley, Céline Combettes, Cédric Trupin, and Stéphane Martin. -
Evaluation of Monte Carlo Tools for High Energy Atmospheric Physics
Evaluation of Monte Carlo tools for high energy atmospheric physics Casper Rutjes1, David Sarria2, Alexander Broberg Skeltved3, Alejandro Luque4, Gabriel Diniz5,6, Nikolai Østgaard3, and Ute Ebert1,7 1Centrum Wiskunde & Informatica (CWI), Amsterdam, The Netherlands 2Astroparticules et Cosmologie, University Paris VII Diderot, CNRS/IN2P3, France 3Department of Physics and Technology, University of Bergen, 5020 Bergen, Norway 4Instituto de Astrofisica de Andalucia (IAA-CSIC), PO Box 3004, Granada, Spain 5Instituto Nacional de Pesquisas Espaciais, Brazil 6Instituto de Física, Universidade de Brasília, Brazil 7Eindhoven University of Technology, Eindhoven, The Netherlands Correspondence to: Casper Rutjes ([email protected]) Abstract. The emerging field of high energy atmospheric physics (HEAP) includes Terrestrial Gamma-ray Flashes, electron- positron beams and gamma-ray glows from thunderstorms. Similar emissions of high energy particles occur in pulsed high voltage discharges. Understanding these phenomena requires appropriate models for the interaction of electrons, positrons and photons of up to 40 MeV energy with atmospheric air. In this paper we benchmark the performance of the Monte Carlo codes 5 Geant4, EGS5 and FLUKA developed in other fields of physics and of the custom made codes GRRR and MC-PEPTITA against each other within the parameter regime relevant for high energy atmospheric physics. We focus on basic tests, namely on the evolution of monoenergetic and directed beams of electrons, positrons and photons with kinetic energies between 100 keV and 40 MeV through homogeneous air in the absence of electric and magnetic fields, using a low energy cut-off of 50 keV. We discuss important differences between the results of the different codes and provide plausible explanations. -
Experiments and Simulations of an Atmospheric Pressure Lossy Dielectric Barrier Townsend Discharge
Journal of Physics D: Applied Physics PAPER Related content - Atmospheric pressure glow discharge Experiments and simulations of an atmospheric plasma A A Garamoon and D M El-zeer pressure lossy dielectric barrier Townsend - Diffuse barrier discharges discharge Z Navrátil, R Brandenburg, D Trunec et al. - Nonlinear phenomena in dielectric barrier discharges: pattern, striation and chaos To cite this article: S Im et al 2014 J. Phys. D: Appl. Phys. 47 085202 Jiting OUYANG, Ben LI, Feng HE et al. Recent citations View the article online for updates and enhancements. - Radial structures of atmospheric-pressure glow discharges with multiple current pulses in helium Zhanguo Bai et al This content was downloaded from IP address 128.12.245.233 on 22/09/2020 at 18:06 Journal of Physics D: Applied Physics J. Phys. D: Appl. Phys. 47 (2014) 085202 (10pp) doi:10.1088/0022-3727/47/8/085202 Experiments and simulations of an atmospheric pressure lossy dielectric barrier Townsend discharge S Im, M S Bak1, N Hwang2 and M A Cappelli Mechanical Engineering Department, Stanford University, Stanford, California 94305-3032, USA E-mail: [email protected] Received 25 September 2013, revised 7 January 2014 Accepted for publication 9 January 2014 Published 7 February 2014 Abstract A diffuse discharge is produced in atmospheric pressure air between porous alumina dielectric barriers using low-frequency (60 Hz) alternating current. To study its formation mechanism, both the discharge current and voltage are measured while varying the dielectric barrier porosity (0%, 48% or 85%) and composition (99% Al2O3 ,99% SiO2 or 75% Al2O3 + 16% SiO2 + 9% other oxides). -
The Physics of Streamer Discharge Phenomena
The physics of streamer discharge phenomena Sander Nijdam1, Jannis Teunissen2;3 and Ute Ebert1;2 1 Eindhoven University of Technology, Dept. Applied Physics P.O. Box 513, 5600 MB Eindhoven, The Netherlands 2 Centrum Wiskunde & Informatica (CWI), Amsterdam, The Netherlands 3 KU Leuven, Centre for Mathematical Plasma-astrophysics, Leuven, Belgium E-mail: [email protected] Abstract. In this review we describe a transient type of gas discharge which is commonly called a streamer discharge, as well as a few related phenomena in pulsed discharges. Streamers are propagating ionization fronts with self-organized field enhancement at their tips that can appear in gases at (or close to) atmospheric pressure. They are the precursors of other discharges like sparks and lightning, but they also occur in for example corona reactors or plasma jets which are used for a variety of plasma chemical purposes. When enough space is available, streamers can also form at much lower pressures, like in the case of sprite discharges high up in the atmosphere. We explain the structure and basic underlying physics of streamer discharges, and how they scale with gas density. We discuss the chemistry and applications of streamers, and describe their two main stages in detail: inception and propagation. We also look at some other topics, like interaction with flow and heat, related pulsed discharges, and electron runaway and high energy radiation. Finally, we discuss streamer simulations and diagnostics in quite some detail. This review is written with two purposes in mind: First, we describe recent results on the physics of streamer discharges, with a focus on the work performed in our groups. -
Simulations of the Propagation of Streamers in Electrical Discharges in a 5Mm Water Filled Gap
Research Article Curr Trends Biomedical Eng & Biosci Volume 9 Issue 4 -september 2017 Copyright © All rights are reserved by Duaa A Uamran DOI: 10.19080/CTBEB.2017.09.555767 Simulations of the Propagation of Streamers in Electrical Discharges in a 5mm Water Filled Gap Thamir H Khalaf1 and Duaa A Uamran1,2* 1Department of Physics, College of Science, University of Baghdad, Iraq 2Department of Physics, College of Science, University of Kerbala, Iraq Submission: August 09, 2017; Published: September 27, 2017 *Corresponding author: Duaa A Uamran, Department of Physics, College of Science, University of Baghdad, Iraq, Email: Abstract This work is devoted to the modeling of streamer discharge, propagation in liquid dielectrics (water) gap using the bubble theory. This of the electrical discharge (streamer) propagating within adielectric liquid subjected to a divergent electric, using finite element method (in thetwo dielectric dimensions). liquid Solution gap and of indicates Laplace’s the equation minimum governs breakdown the voltage voltage andrequired electric for fielda 5mm distributions atmospheric within pressure the dielectricconfiguration, liquid the gap electrode as 22KV. configuration a point (pin) - plane configuration, the plasma channels were followed, step to step. That shows the streamer discharge bridges shown agreement with the streamer growth, according to the simulation development time. The initiated streamer grows and branches toward all elements that satisfy the required conditions. The electric potential and field distributions Keywords: Herbal; Phytochemical; Cytotoxic; Formulations Introduction and slow, heavy ions alter the propagation of discharge channels The breakdown of insulating liquids is not simple to explain [7-9]. and the mechanism responsible for the initiation of breakdown is still open to controversy. -
Numerical Simulation of Townsend Discharge, Paschen Breakdown and Dielectric Barrier Discharges Napoleon Leoni, Bhooshan Paradkar
Numerical Simulation of Townsend Discharge, Paschen Breakdown and Dielectric Barrier Discharges Napoleon Leoni, Bhooshan Paradkar HP Laboratories HPL-2009-234 Keyword(s): Townsend Discharge, Paschen Breakdown, Dielectric Barrier Discharges, Corona. Numerical Simulation Abstract: Practical understanding of electrical discharges between conductors or between conductors and dielectrics is instrumental for the development of novel charging devices for Digital Printing Applications. The work presented on this paper focuses on fundamental aspects related to the inception of electrical discharges and breakdown in the initial stages (few 100's of ?s) to a detail hard to match with experimental techniques. Numerical simulations of 1-D Townsend and Dielectric Barrier Discharges (DBDs) are performed using a commercial Finite Element package (COMSOL). A combined fluid model for the electron and Ion fluxes is used together with a local field approximation on a 1-D domain comprised of Nitrogen gas. The renowned Paschen breakdown result is successfully predicted numerically. Results are shown for the transient Townsend discharge that leads to this breakdown offering insight into the positive feedback mechanism that enables it. These transient results show how impact ionization combined with cathode secondary emission generate increasing waves of positive ions that drift towards the cathode again self feeding the discharge process. The simulation is then extended to predict the nature of a DBD in the case of a single voltage pulse. External Posting Date: September 6, 2009 [Fulltext] Approved for External Publication Internal Posting Date: September 6, 2009 [Fulltext] To be published and presented at NIP 2009, Loiusville, KY, September, 20-24, 2009 © Copyright NIP 2009 Numerical Simulation of Townsend Discharge, Paschen Breakdown and Dielectric Barrier Discharges Napoleon Leoni; Hewlett Packard Laboratories, Palo Alto, CA. -
Relativistic Runaway Electrons Above Thunderstorms
Relativistic Runaway Electrons above Thunderstorms Nikolai G. Lehtinen Physics Department STAR Laboratory Stanford University Advisers: Umran S. Inan, EE Department, Timothy F. Bell, EE Department, Roger W. Romani, Physics Department Plan 1. Introduction 2. Monte Carlo model of runaway electron avalanche 3. Fluid model of runaway electrons above thunderstorms 4. Effects of runaway electrons in the conjugate hemisphere Lightning-mesosphere interaction phenomena ~ 2000 cm-3 Electron density Β 100 km THERMOSPHERE Elves 80 km Sprites MESOSPHERE γ-rays 60 km Runaway ~100 MV 40 km E ~ 103 V/m electrons STRATOSPHERE at 40 km Blue Jet 20 km Cameras + + + + + TROPOSPHERE +CG 0 km - --- - γ-ray flash Red Sprites (BATSE observation) 40 Elves 30 20 Sprites 10 Rate (counts/0.1ms) 0 015205 10 1996.204.07.17.38.792 Time (ms) Red Sprites Red Sprites: - altitude range ~50-90 km - lateral extent ~5-10 km - occur ~1-5 ms after +CG discharge - last up to several 10 ms Aircraft view Ground View 90-95 km horizon Space Shuttle View sprite sprite thunderstorm Examples of Terrestrial Gamma Ray Flashes (BATSE Data) Terrestrial Gamma Rays: - time duration ~1 ms - energies 20 keV—2 MeV - hard spectrum (bremsstrahlung) Rate (counts/0.1ms) Rate (counts/0.1ms) Rate (counts/0.1ms) Time (ms) Time (ms) Time (ms) Time (ms) C. T. R. Wilson, 1925 While the electric force due to the thundercloud falls off rapidly, ... the electric force required to cause sparking ... falls off still more rapidly. Thus, ... there will be a height above which the electric force due to the cloud exceeds the sparking limit .. -
Electrical Breakdown in Gases
High-voltage Pulsed Power Engineering, Fall 2018 Electrical Breakdown in Gases Fall, 2018 Kyoung-Jae Chung Department of Nuclear Engineering Seoul National University Gas breakdown: Paschen’s curves for breakdown voltages in various gases Friedrich Paschen discovered empirically in 1889. Left branch Right branch Paschen minimum F. Paschen, Wied. Ann. 37, 69 (1889)] 2/40 High-voltage Pulsed Power Engineering, Fall 2018 Generation of charged particles: electron impact ionization + Proton Electron + + Electric field Acceleration Electric field Slow electron Fast electron Acceleration Electric field Acceleration Ionization energy of hydrogen: 13.6 eV 3/40 High-voltage Pulsed Power Engineering, Fall 2018 Behavior of an electron before ionization collision Electrons moving in a gas under the action of an electric field are bound to make numerous collisions with the gas molecules. 4/40 High-voltage Pulsed Power Engineering, Fall 2018 Electron impact ionization Electron impact ionization + + Electrons with sufficient energy (> 10 eV) can remove an electron+ from an atom and produce one extra electron and an ion. → 2 5/40 High-voltage Pulsed Power Engineering, Fall 2018 Townsend mechanism: electron avalanche = Townsend ionization coefficient ( ) : electron multiplication : production of electrons per unit length along the electric field (ionization event per unit length) = = exp( ) = = 푒 푒 6/40 High-voltage Pulsed Power Engineering, Fall 2018 Townsend 1st ionization coefficient When an electron travels a distance equal to its free path in the direction of the field , it gains an energy of . For the electron to ionize, its gain in energy should be at least equal to the ionization potential of the gas: 1 1 = ≥ st ∝ The Townsend 1 ionization coefficient is equal to the number of free paths (= 1/ ) times the probability of a free path being more than the ionizing length , 1 1 exp exp ∝ − ∝ − = ⁄ − A and B must be experimentally⁄ determined for different gases. -
Ball Lightning Caused by a Semi-Relativistic Runaway Electron Avalanche
Journal of Atmospheric and Solar-Terrestrial Physics 120 (2014) 36–40 Contents lists available at ScienceDirect Journal of Atmospheric and Solar-Terrestrial Physics journal homepage: www.elsevier.com/locate/jastp Ball lightning caused by a semi-relativistic runaway electron avalanche Geron S. Paiva a,n, Carlton A. Taft a, Nelson C.C.P. Furtado a, Marcos C. Carvalho a, Eduardo N. Hering a, Marcus Vinícius b, F.L. RonaldoJr.c, Neil M. De la Cruz a a Centro Brasileiro de pesquisas Físicas, Rua Dr. Xavier Sigaud, 150, 22290-180 Rio de Janeiro, Brazil b Departamento de Química Fundamental, Universidade Federal de Pernambuco, 50740-540 Recife, Pernambuco, Brazil c Universidade Católica de Pernambuco, Rua do Principe, 526, 50050-900, Recife, Pernambuco, Brazil article info abstract Article history: Ball lightning (BL) is observed as a luminous sphere in regions of thunderstorm activity. There are many Received 11 June 2013 reports of BL forming in total absence of thunderclouds, associated with earthquakes and volcanoes. In Received in revised form this latter case, BL has been known to appear out of “nowhere”. In this work, a hypothesis on BL 13 August 2014 formation is presented involving the interaction between very low frequency (VLF) radio waves and Accepted 14 August 2014 atmospheric plasmas. High-velocity light balls are produced by ionic acoustic waves (IAWs) interacting Available online 20 August 2014 with a stationary plasma. Several physical properties (color, velocity, and fragmentation) observed in the Keywords: BL phenomenon can be explained through this model. Ball lightning & 2014 Elsevier Ltd. All rights reserved. Rock piezoelectricity Semi-relativistic runaway electron avalanche 1. -
A 3-Stage Gated UV-Photon Gaseous Detector with Optical Imaging
INJS DOCUMINT WIS-89|9/March-PH A 3-Stage Gated UV-Photon Gaseous Detector with Optical Imaging A. Breskin, R. Chechik* and D. Sauvage Department of Nuclear Physics The Weizmann Institute of Science Rehovot 76100, Israel Abstract UV-Photons are detected by a low-pressure photosensitive multistep gaseous de tector. Photoelectrons are multiplied in two charge amplification stages. A third, light amplification stage operating in a scintillation mode, provides light yields >5.107 vis ible photons per single photoelectron avalanche, in Argon-CjHe-TMAE gas mixture. We present results or. absolute photon yields in various TMAE gas mixtures, at low gas pressures and at low charge gains. We describe the operation mechanism and some ba sic properties of the gated 3-stage detectors, such as stability of operation at high back ground rates and localization resolutions particularly at large TMAE concentration and high temperature operation conditions. Further applications are discussed. (Submitted to Nuclear Instruments and Methods in Physics Research) * The Hettie H. Heineman Research Fellow 1. Introduction Single UV-photons, in the wavelength range of 120-220 nm can be efficiently de tected and imaged with gaseous detectors filled with photosensitive vapours. Several UV-imaging techniques have been developed, mostly motivated by the application to Cerenkov Ring Imaging (RICH)1' in particle physics. There exist many other appli cations of UV-detectors such as in particle calorimetry2', nuclear medicine3-, plasma diagnostics'1', and UV astronomy5'. -
Gas Breakdown and Gas-Filled Detectors
Gas Breakdown and Gas-filled Detectors Fall, 2017 Kyoung-Jae Chung Department of Nuclear Engineering Seoul National University Paschen’s curves for breakdown voltages in various gases Friedrich Paschen discovered empirically in 1889. Left branch Right branch Paschen minimum 2/28 Radiation Source Engineering, Fall 2017 Generation of charged particles: electron impact ionization + Proton Electron + + Electric field Acceleration Electric field Slow electron Fast electron Acceleration Electric field Acceleration 3/28 Radiation Source Engineering, Fall 2017 Townsend mechanism: electron avalanche Cathode Electric Field Anode e- ……. e- e- N e- N e- ……. = + + Townsend ionization coefficient ( ) : electron multiplication : production of electrons per unit length along the electric field (ionization event per unit length) = = exp( ) = = 푒 푒 4/28 Radiation Source Engineering, Fall 2017 Townsend 1st ionization coefficient Townsend related the ionization mean free path (λi = 1/ ) to the total scattering mean free path (λ) by treating it as being a process activated by drift energy gained from the field (Eλ), with an activation energy eVi. 1 1 = exp ∝ − Semi-empirical expression for Townsend first ionization coefficient = ⁄ − A and C must be experimentally⁄ determined for different gases Gas A(ion pairs/mTorr) C(V/mTorr) He 182 5000 Ne 400 10000 H2 1060 35000 N2 1060 34200 Air 1220 36500 5/28 Radiation Source Engineering, Fall 2017 Townsend’s avalanche process is not self-sustaining A - - - - - - - - N N N N p Voltage + - + - + - + - N N d = = + - + - 푒 N UV + - x K Townsend’s avalanche process cannot be sustained without external sources for generating seed electrons. 6/28 Radiation Source Engineering, Fall 2017 Breakdown: Paschen’s law Secondary electron emission by ion impact: When heavy positive ions strike the cathode wall, secondary electrons are released from the cathode material. -
The Main Features of the Streamer Discharge Mode in Coordinate Gas Detector
The main features of the streamer discharge mode in coordinate gas detector V.I.Razin Institute for Nuclear Researches, Russian Academy of Sciences, Moscow Abstract. In work the results of the analysis are presented relating to the status of a streamer discharge mode in different gas detectors developed at the moment in laboratories and nuclear‐physics installations. Thanks to new representations from a scope of high‐speed narrow gas detectors together with the settle technique of a multiwire devices there are the possibility to undertake the next attempts to know a nature of this phenomenon. Studying prebreakdown and postbreakdown states in such detectors with the objective to rise their operation reliability under conditions of a high counting rate is a pressing issue. Introduction. Since opening by G.Charpak and F.Sauli [1] of a strong current operating mode of multiwire proportional chambers which later became know as self‐quenched streamer (SQS) mode[2], passed more than 40 years. Nevertheless the nature of this physical phenomenon in gases at normal pressure has a number few the studied features. If before SQS‐mode associated with large gap chambers, big percentage of extinguishing additives as hydrocarbons and methylal, thick anode wires etc. in modern wireless narrow –gap position‐sensitivity devices of type RPC, GEM, MICROMEGAS [3‐5], the existence of a large signal is also revealed. The most typical feature of the transition of a gas‐discharge detector to the streamer mode is a jump in the signal amplitude. In the transition region simultaneously small and large signals caused by the avalanche amplification mechanism and the streamer formation respectively exist.