KISTI 2013 달 토양에서 지하 깊이에 따른 고에너지 우주선 환경 영향 분석 Jongdae Sohn, Yu Yi Dept. of Astronomy & Space Science, Chungnam National University.

Slides:



Advertisements
Similar presentations
Introduction to Ionizing Radiation
Advertisements

DOSE SPECTRA FROM ENERGETIC PARTICLES AND NEUTRONS (DoSEN) S. Smith 1, N. A. Schwadron 1 C. Bancroft 1, P. Bloser 1, J. Legere 1, J. Ryan 1, H. E. Spence.
Analysis of Mercury’s X-ray fluorescence M. Laurenza, M. Storini and A. Gardini IFSI-INAF, Via del Fosso del Cavaliere, 100, Rome 00133, Italy Joint SERENA.
Parameterized Shower Simulation in Lelaps: a Comparison with Geant4 Daniel Birt, Amy Nicholson.
S. Guatelli IEEE 2004 – NSS - Rome Dosimetry for Interplanetary Missions: the Geant4 REMSIM application S. Guatelli 1, P. Nieminen 2, M.G. Pia 1 IEEE NSS,
Charged Particle Radiation
Cosmic rays in solar system By: Tiva Sharifi. Cosmic ray The earth atmosphere is bombarded with the energetic particles originating from the outer space.
The Cosmic R A y Telescope for the Effects of Radiation.
Danish Space Research Institute Danish Small Satellite Programme FH Space_Environment.ppt Slide # 1 Flemming Hansen MScEE, PhD Technology Manager.
Space radiation dosimetry and the fluorescent nuclear track detector Nakahiro Yasuda National Institute of Radiological Sciences.
Effects of Solar Energetic Particle Events on the Martian Surface and Atmosphere F Leblanc, DA Brain, JG Luhmann, GT Delory, RA Mewaldt, CM Cohen 2004.
What are the Forms of Hazardous Radiation? Stanley B. Curtis Fred Hutchinson Cancer Research Center, ret. & Dept. of Environmental Health University of.
14 User Documents and Examples II SLAC Geant4 Tutorial 17 May 2007 Dennis Wright Geant4 V8.3.
EFFECTS of the TERRESTRIAL MAGNETOSPHERE on RADIATION HAZARD on MOON MISSIONS R. Koleva, B. Tomov, T. Dachev, Yu. Matviichuk, Pl. Dimitrov, Space and Solar-Terrestrial.
LIGHT IN THE SKY. What are the light bulbs of our universe?
Stopping Power The linear stopping power S for charged particles in a given absorber is simply defined as the differential energy loss for that particle.
PLANETOCOSMICS L. Desorgher, M. Gurtner, E.O. Flückiger, and P. Nieminen Physikalisches Institut, University of Bern ESA/ESTEC.
Workshop on Physics on Nuclei at Extremes, Tokyo Institute of Technology, Institute for Nuclear Research and Nuclear Energy Bulgarian Academy.
Centre de Toulouse Radiation interaction with matter 1.
Radiation conditions during the GAMMA-400 observations:
NEEP 541 Radiation Interactions Fall 2003 Jake Blanchard.
GRAS Validation and GEANT4 Electromagnetic Physics Parameters R. Lindberg, G. Santin; Space Environment and Effects Section, ESTEC.
P. Scampoli - 24th ICNTS Bologna, September 4,
System for Radiation Environment characterization (fluxes, doses, dose equivalents at Earth, Moon and Mars) on hourly thru yearly time frame Example: Snapshots.
Single Event Effects in microelectronic circuits Author: Klemen Koselj Advisor: Prof. Dr. Peter Križan.
NUCLEAR VS. CHEMICAL CHEMICAL reactions involve rearranging of atoms: e.g., H 2 +O 2  H 2 O No new atoms are created. Chemistry involves electrons only.
GCR Primaries (See Wilson et al. poster for latest CRaTER proton albedo map) RELATIVE CONTRIBUTIONS OF GALACTIC COSMIC RAYS AND LUNAR PARTICLE ALBEDO TO.
REMSIM Radiation Exposure and Mission Strategies for Interplanetary Manned Missions Susanna Guatelli, 9 th March 2004, Genova, Italy
Mars images courtesy of ESA Portal Multimedia Gallery Mars Radiation Environment Characterization Results, previous and ongoing activities Ana Keating.
The PLANETOCOSMICS Geant4 application L. Desorgher Physikalisches Institut, University of Bern.
Currently the Solar Energetic Particle Environment Models (SEPEM) system treats only protons within the interplanetary environment, and the shielding analysis.
Alpha and Beta Interactions
Dose Predictions for Moon Astronauts Image Source: Nicholas Bachmann, Ian Rittersdorf Department of Nuclear Engineering and Radiological.
Regolith Materials Sheila A. Thibeault1, Richard L. Kiefer2, Myung-Hee Y. Kim2, Janet L. Chapman2, J. Adam Weakley2, and D. Ryan McGlothlin2 1NASA Langley.
LIP & ESA 18121/04/NL/CH MarsREC An integrated tool for Mars Radiation Environment Characterization and Effects 5º longitude.
Earth-Moon-Mars Radiation Environment Model N. A. Schwadron, K. Kozarev, L. Townsend, M. Desai, M. A. Dayeh, F. Cucinotta, D. Hassler, H. Spence, M. Pourars,
Assessment of radiation shielding materials for protection of space crews using CR-39 plastic nuclear track detector J. M. DeWitt 1, E. R. Benton 1, Y.
Horizon Observations Hydrogen in the top 10 cm of lunar regolith should enhance the flux of albedo protons ejected at grazing (horizontal) angles relative.
Daniel Matthiä(1)‏, Bernd Heber(2), Matthias Meier(1),
Solar Storm Radiation Model (SStoRM) Prepared by: Joshua Lande–Marlboro College, VT and Ron Turner–ANSER, 2900 South Quincy Street, Suite 800, Arlington,
3/2003 Rev 1 II.2.9a – slide 1 of 25 IAEA Post Graduate Educational Course Radiation Protection and Safe Use of Radiation Sources Part IIQuantities and.
Dose Predictions for Moon Astronauts Image Source: Nicholas Bachmann, Ian Rittersdorf Nuclear Engineering and Radiological Sciences.
Approaches to forecasting radiation risk from Solar Energetic Particles Silvia Dalla (1), Mike Marsh (2) & Timo Laitinen (1) (1) University of Central.
© The Aerospace Corporation 2010 Use of Geant4 Simulations to Understand LRO/CRaTER Observations M. D. Looper, J. E. Mazur, J. B. Blake, The Aerospace.
Pedro Brogueira 1, Patrícia Gonçalves 2, Ana Keating 2, Dalmiro Maia 3, Mário Pimenta 2, Bernardo Tomé 2 1 IST, Instituto Superior Técnico, 2 LIP, Laboratório.
Encontro com a Ciência e a Tecnologia em Portugal 4-7 Julho 2010.
Gyeongbok Jo 1, Jongdae Sohn 2, KyeongWook Min 2, Yu Yi 1, Suk-bin Kang 2 1 Chungnam National University 2 Korea Advanced Institute of Science.
J. Helsby, P. Ford, R. Hoch, K. Gnanvo, R. Pena, M. Hohlmann, D. Mitra
Solar gamma-ray and neutron registration capabilities of the GRIS instrument onboard the International Space Station Yu. A. Trofimov, Yu. D. Kotov, V.
INTERACTION OF PARTICLES WITH MATTER
and 9 February 2000 CHEP2000 ESA Space Environment &
Martian Radiation Env. Modelling Tools (QinetiQ)
Dose Equivilant Rad Pro III NUCP 2331.
Ideas for Martian environment models and further G4 development : input from L.Desorgher Building of a user friendly and modular magnetic shielding tool.
Geant4 REMSIM application
(Or, How Dirty is Your Water?)
Lunar Reconnaissance Orbiter CRaTER Critical Design Review
Results of ion simulations
N. Stoffle University of Houston
Gamma-ray Albedo of the Moon Igor V. Moskalenko (Stanford) & Troy A
and 9 February 2000 CHEP2000 ESA Space Environment &
Radioprotection for interplanetary manned missions
Outside the nucleus, the beta decay {image} will not occur because the neutron and electron have more total mass than the proton. This process can occur.
P. Nieminen, E. Daly, A. Mohammadzadeh, H.D.R. Evans, G. Santin
Gamma Ray Satellites Simulations with Geant4
CRaTER Science Requirements
Recent, undergoing and planned ESA-supported activities concerning development, use and promotion of the Geant4 toolkit E. Daly, R. Nartallo, P. Nieminen.
Short Course Siena, 5-6 October 2006
G4GeneralParticleSource Class:
Presentation transcript:

KISTI 2013 달 토양에서 지하 깊이에 따른 고에너지 우주선 환경 영향 분석 Jongdae Sohn, Yu Yi Dept. of Astronomy & Space Science, Chungnam National University

Motivation Introduction – Geant 4 (for Geometry And Tracking) – Geant 4 for Space Science – Lunar Surface Structure Simulation and Analysis Summary Contents

Many countries of the world including the United States, China, Japan and India explore the moon and Mars. We have to prepare the moon exploration here and now. When the human being explores and lives on the Moon, the Human being is influenced by a lot of the high-energy particles in lunar environment ; galactic cosmic ray (GCR), solar energetic proton (SEP). Thus, we must consider the environmental impact of high-energy cosmic radiation. Motivation

A toolkit for the simulation of the passage of particles through matter Developed by a world-wide Collaboration of approximately 100 scientists Its areas of application  High Energy Physics  Astrophysics and nuclear physics  Experiments, Medical, Accelerator and Space Science Introduction: Geant 4 (for Geometry And Tracking)

Space electronics and Space Science detector systems Simulations of astronaut radiation hazards Planetary exploration applications Interfaces and tools to space environment analysis tools such as SPENVIS Cosmic ray magnetospheric propagation analyses Micro-dosimetry Large-scale simulations requiring event biasing and GRID capabilities General shielding optimization applications Introduction: Geant 4 for Space Science 5º5º 5º 5º

Introduction: Lunar Surface Structure Geological structure of the Lunar soil [cited by Lunar Sourcebook: a user’s guide to the moon]

Introduction: The energy spectrum for cosmic rays Composition of cosmic rays (1 ~ 20 GeV) [cited by : protons (89%), helium nuclei (10%), the nuclei of heavier elements (1%)

Introduction: Composition of Lunar Soil Chemical compositions of average Apollo 15 soils samples used in the radiation experiments. Mean soil density: 3.39g/cm 3 [Wieczorek et al. (2006)] [Soil in Mare][Soil in Highland]

Introduction: Linear Energy Transfer Linear energy transfer (LET)  A measure of the energy transferred to material as an ionizing particle travels through it.  This measure is used to quantify the effects of ionizing radiation on biological specimens or electronic devices.  An average energy for a given path length traveled.  An average path length for a given deposited energy. t: an thickness of material (-dE/dx): Energy imparted to matter

Simulation: Deposited energy of protons Deposited energy of proton beam (1 ~ 6500 MeV) after passing through the Lunar soil of 10m depth

Simulation: Residual LET for Lunar Soil (Linear Scale) Residual energy deposition in Soil for 1, 5, 10, 15, 20 GeV/nucleon Proton beam after passing through Lunar Soil (Linear Scale)

Simulation: Residual LET for Lunar Soil (Log Scale) Residual energy deposition in Soil for 1, 5, 10, 15, 20 GeV/nucleon Proton beam after passing through Lunar Soil (Log Scale)

Analysis: Effective Dose Effective Dose (H E ) :

Analysis: Effective Dose for Lunar Soil (Linear Scale) Effective Dose for the depth [0 ~ 10 m] of the Lunar soil. Natural Background is based on the Atlantic Seaboard value [0.6 mSv/year]. [National Council on Radiation Protection and Measurements, NCRP Report 116]

Analysis: Effective Dose for Lunar Soil (Log Scale) Effective Dose for the depth [0 ~ 40 m] of the Lunar soil. Natural Background is based on the Atlantic Seaboard value [0.6 mSv/year].

Analysis: Effective Dose for Lunar Soil (Log Scale) Effective Dose for the depth [0 ~ 10 m] of the Lunar soil. Natural Background is based on the Atlantic Seaboard value [0.6 mSv/year].

Summary Using Geant4, we examine the environmental impact of high-energy cosmic radiation for the range of 1, 5, 10, 15, and 20 GeV for Lunar soil depth [1 ~ 40 m] of Lunar soil chemical compositions (3.39 g/cm 3 ). At the result, under the Lunar soil of 4.5 m depth, there is less impact of high-energy environment in Lunar radiation environment compared with the natural background radiation on the Earth [0.6 mSv/year]. We will also examine the environmental impact of high-energy cosmic radiation on the Martian and Lunar surface using other composition of cosmic rays.