Geant4 User's Guide for Application Developers Version: geant4 10.0
Geant4 Simulation of Air Showers using Thinning Method€¦ · sources Æ“Charged Particle...
Transcript of Geant4 Simulation of Air Showers using Thinning Method€¦ · sources Æ“Charged Particle...
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Mohammad S. Sabra1
Mark J. Christl1, John W. Watts2 11Marshall Space Flight Center, Huntsville AL
222CSPAR, University of Alabama, Huntsville, AL
14/7/2015
Geant4 Simulation of Air Showers using
Thinning Method
APS April Meeting 2015, Baltimore, MD
https://ntrs.nasa.gov/search.jsp?R=20150006841 2020-07-26T15:04:19+00:00Z
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Cosmic Rays• High-energy protons and heavy
ions• Very broad range of energies• Galactic and Extragalactic• maximum energy predicted at
60 1018 eV (= 60 EeV) (GZK-cutoff)
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p+ cmb+ p + 0
n + +
Proton Horizon~1020 eV
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Extreme Energy Cosmic Rays (EECRs)
• EECRs (E > 60EeV) suffer almost no deflection from magnetic field in extragalactic, galactic, and solar system
• They point back directly to the location of their original sources “Charged Particle Astronomy”
• Detection of EECRs gives us information about their sources
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4
Eleven Science Questions for the New Century*
Question 6:How Do Cosmic Accelerators
Work and What Are They Accelerating?
*”Connecting Quarks with the Cosmos: Eleven Science Questions for the New Century Committee on the Physics of the Universe”, National Research Council , ISBN: 0-309-50569-0 (2003)
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HiRes (Utah) TA (Utah)
Auger (Argentina)
AGASA (Japan)
Yakutsk (Siberia)
Detecting EECR
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Data accumulated
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• EECRs Flux is low of the order of 1 particle/km2/sr/century• At high end of the spectrum reduces to 1 particle/km2/sr/millennium!
Spectra of leading EECRs observations
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Extreme Universe Space Observatory Mission
• A collaboration of 15 countries, 85 institutions and ~ 333 scientists
• It will be the first space-based observatory to use the Earth’s atmosphere to discover the origin of EECRs.
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Extensive Air Showers (EASs)• Studies of the nature of EECRs are based on
the measurement of EASs, • EASs are cascades of secondary particles in
the atmosphere as a result of the interaction of EECRs with the Earth’s atmosphere
• Maximum atmospheric depth Xmax depends on:
primary energy, nature of the primary
particle details of the interactions
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Modeling EAS using Geant4• Atmosphere is modeled as cylinder of radius 0.5 km
and divided into 112 layers of 1 km thickness and varying density
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0
0.25
0.50
0.75
1.00
1.25
0.1 1 10 100
Height (km)
Den
sity
(kg/
m3 )
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Modeling EAS using Geant4
• Using Geant4 model FTF_BICProton and Iron as primaries
• Time and data size are huge!• Simulating 1 event of 1TeV proton:
Time ~ 20 hrsSize ~ 200GB
• Simulation time for EAS scales with energy of primary particle
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Iron
Proton
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Radial distance from core
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Thinning Algorithm• Let Eo be energy of primary particle, and E be
energy of secondary particleThinning level Eth = E / Eo
• All secondaries with energies greater than Ethare followed, BUT if the energy sum of all jsecondaries produced in a certain interaction falls below thinning energy
only one particle is followed 134/7/2015
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100TeV ProtonThinning level 1E-2 1E-4 1E-6
Time (min) 17 66 130
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0
200
400
600
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0 200 400 600 800 1000 1200
Thinning 10-6
Thinning 10-4
Thinning 10-2
Xmax ~ 770 g/cm21 event of 100 TeV Proton
Depth (g/cm2)
Gam
ma
Yie
ld
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100TeV/u IronThinning level 1E-2 1E-4 1E-6
Time (min) 21 120 380
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0
200
400
600
800
1000
1200
0 200 400 600 800 1000 1200
Thinning 10-6
Thinning 10-4
Thinning 10-2
Xmax ~ 370 g/cm2
1 event of 100TeV/u Iron
Depth (g/cm2)
Gam
ma
Yie
ld
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Geant4 vs CORSIKA100TeV Proton
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0 200 400 600 800 1000 1200
0 200 400 600 800 1000 1200
Geant4CORSIKA
100TeV Proton
Depth (g/cm2)
Nor
mal
ized
Gam
ma
Yie
ld
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Geant4 vs CORSIKA100TeV/u Iron
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0.9
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0 200 400 600 800 1000 1200
0 200 400 600 800 1000 1200
Geant4CORSIKA
100TeV/u Iron
Depth (g/cm2)
Nor
mal
ized
Gam
ma
Yie
ld
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Remarks
• Thinning algorithm cuts simulation time significantly
• Xmax is not affected by thinning level• Location of Xmax depends on primary particle• Preliminary calculations show that Geant4
predicts low Xmax compared to CORSIKA:Magnetic FieldGeometry
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Acknowledgement
This work is supported by an appointment to the NASA Postdoctoral Program at Marshall Space
Flight Center, administered by Oak Ridge Associated Universities through a contract with
NASA
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www.orau.org
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Thank You!Questions?