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SHENIE : S imulation of H igh E nergy N eutrino I nteracting with the E arth
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Transcript of SHENIE : S imulation of H igh E nergy N eutrino I nteracting with the E arth
VHENTW, 4/25/206 M.A. Huang
SHENIE: Simulation of High Energy Neutrino
Interacting with the EarthM.A. Huanga, Y.L. Hongb, C.H. Iongbc, G.L. Linb
(a) General Education Center, National United University,
1, Lien-da, Kung-ching Li, Miao-Li, 36003, TAIWAN(b) Institute of Physics, National Chiao-Tung University,
1001 Ta Hsueh Rd., Hsin-chu, 300, TAIWAN (c) Current Address: Institute of Physics, Academia Sinica,
Nankang, Taipei, 105, TAIWAN
Presenter: M.A. Huang ([email protected]),
VHENTW, 4/25/206 M.A. Huang
What is SHENIE
SHENIE means
goddess in Mandarin!
VHENTW, 4/25/206 M.A. Huang
UHE- fluxes
So many UHE- fluxes, how to detect them?
Traditional detector technologyNuTel & CRTNT
New techniquesRadioSound wave
Need MC simulation for
neutrino interacting with
the Earth!
VHENTW, 4/25/206 M.A. Huang
Target: Mauna Loa, Hawaii Big Island, USA http://hep1.phys.ntu.edu.tw/nutel/P. Yeh, et al., Modern Physics Lett. A.19, 1117-1124, (2004).
Mauna Loa
View from Hualalai
See NuTel talk by Bob Y. Hsiung
VHENTW, 4/25/206 M.A. Huang
Target: Mt. Wheeler, Nevada, USA. (prototype in construction)
Z. Cao, M.A. Huang, P. Sokolsky, Y. Hu, J. Phys. G, 31, 571-582, (2005)
Highlight of the year 2005 by J PG
See CRTNT talk by Zhen Cao
VHENTW, 4/25/206 M.A. Huang
Radio array in salt dome
Radio signal from EAS Large
Cherenkov angle!
Underground salt dome. Higher density
than water/ice Good
transparency to radio signal
Free of artificial noise
1
2
3
4
5
6
7
Dep
th (
km
)Halite (rock salt)• L(<1GHz) > 500 m w.e.• Depth to >10km• Diameter: 3-8 km• Veff ~ 100-200 km3 w.e.• No known background• >2 steradians possible
Antenna array
Figure comes from Peter Gorham, talk in SLAC SalSA workshop, 2005.
VHENTW, 4/25/206 M.A. Huang
Previous version of SHENIE Monte-Carlo simulation for all processes except energy
loss, which use deterministic method.
where decay length = E.
Publications based on this version: M.A. Huang, J.J. Tseng, and G.L. Lin (7/31- 8/7, 2003) Proc. of the 28
th ICRC, Tsukuba, Japan, p.1427, (2003) M.A. Huang, Proc. of the 21th International Conference on Neutrino
Physics and Astrophysics (ν-2004) at Paris, French, Nucl. Phys. B (Proc. Suppl.), 143, 546, (2005); astro-ph/0412642
P. Yeh, et al., Proc. of CosPA 2003, Modern Physics Lett. A.19, 1117-1124, (2004)
Z. Cao, M.A. Huang, P. Sokolsky, Y. Hu, J. Phys. G, 31, 571-582, (2005)
2
E
dE
E
dx
P
dPEE
dx
dE
VHENTW, 4/25/206 M.A. Huang
Current SHENIE structure
CC/NC
leptons
hadronse
New event
N
Y
Propagation thru. Earth
Tauola
Enter DSR E
e
h
N
Y
EnterDSR Y
shower Esh
N
Exit DSRYN
CC :
decay
dE/dx
dE/dx
EDirection,position
E
VHENTW, 4/25/206 M.A. Huang
Coordinate system
Global : Isotropic distribution
of & path length L and tot
al depth
Local :User supplied
topological map• Altitude (East, North)
X: geometric EastY: geometric NorthZ: Vertical
(geodetic) outward
L
R
L=2Rsin
VHENTW, 4/25/206 M.A. Huang
Earth ModelSpherical Earth, R =
6371.2 KmDensity/composition
profileMaterial around
detector can be selected from 4 materials.
VHENTW, 4/25/206 M.A. Huang
DSR
DSR: Detector Sensitive RegionFor SalSA simulation:
Sphere of 5 km radius, under 1km of rock.
For ES telescope: DSR set on top of Earth and local topological map must be supplied.
Salt dome
1 km
5 km
Std. rock
VHENTW, 4/25/206 M.A. Huang
-N interaction
CC/NC total cross-section determine interaction probability.W–resonance can be
added by usersNon-Standard model
cross-section can be implemented as external data file
• G.L. Lin, M.A. Huang, C.H. Iong, work in progress
VHENTW, 4/25/206 M.A. Huang
Materials 4 materials: std. rock,
water (ice), salt, iron Input particles:
e/e , / , /
Energy loss of and in 4 materials Ionization (). Pair Production, Photo-
Nuclear, Bressmstrlung Soft energy loss cut at 0.
01 (can be changed)
XX Tau loss by
~ 0.16% at E > 2.51017 eV.
VHENTW, 4/25/206 M.A. Huang
decay
decay simulated by Randomly choose one event from
a data bank of pre-simulated events • current version
Link to TAUOLA • in near future
TAUOLA simulation Fully polarized
• Tauola have 22 decay modes, while PDB have 37 modes
TAUOLA gives 4 momentum in CM of all decay particles Define E’cm = P║ + M
Boost to lab by = E-lab / M
Secondary particle energy in lab frame E’lab = E’cm
VHENTW, 4/25/206 M.A. Huang
Shower energy If decay inside Earth, E-lab is calculated and are re-pro
pagated thru the rest of journey. If decay in atmosphere, shower energy Esh is sum over
Elab of hadrons or electron / gamma. The mean energy per particles is calculated by Esh/M, where M i
s number of secondary particles which generate shower.
Esh-CM
Mean energy~ 0.5
VHENTW, 4/25/206 M.A. Huang
Consistence check Use several methods to calculate tau flux passing throug
h 100km of standard rock for two different source spectrum (AGN and GZK). MC: Use SHENIE, this work
• M.A. Huang, et al., paper in preparation. Semi-MC: MC in all processes except dE/dX
• M.A. Huang, Proc. of ν-2004 at Paris, Nucl. Phys. B, 143, 546, (2005)
Analytical calculation: Solve and transport eq.• J.J. Tseng et al., Phys. Rev. D 68, 063003, (2003).
Source spectrum:• AGN: A. Neronov, et al., Phys. Rev. Lett., 89, 051101 (2002)• GZK: R. Engel, D. Seckel and T. Stanev, Phys. Rev. D 64, 093010
(2001).
Typical Earth skimming event, =90.5, cord length ~100 km.
VHENTW, 4/25/206 M.A. Huang
AGN fluxes MC method produce results si
milar to analytical method. Conditions used in MC:
105 GeV < E < 1010 GeV N=3107
~1.10 1020 cm-2 s-1 sr-1
N=2979 (at E > 105 GeV) Mean conversion efficiency 9.
9310-5
Total fluxes 2.710-17 (cm2 sr s)-1 ; Equivalent to 8.5 events/(km2 sr yr) Should multiply trigger effici
ency and acceptance to get event rate.
• Both energy-dependent
energy peak at around 5~63 PeV, shower energy will peak around 10 PeV.
VHENTW, 4/25/206 M.A. Huang
GZK fluxes For GZK neutrinos, Slightly move to lower en
ergy due to large energy loss.
MC simulation conditions: 105 GeV < E < 1012 GeV N=508294 ~1.521022 cm-2 s-1 sr-1
N=5969 (at E > 105 GeV) Mean conversion efficienc
y 1.1710-2
Total fluxes 3.910-19 (cm2 sr s)-1 ; Equivalent to 0.12 events/(km2 sr yr)
energy peak at around 0.04 PeV ~1.6 EeV, Shower energy will peak around 0.1 EeV.
VHENTW, 4/25/206 M.A. Huang
Underground salt dome detector
Strawman array: 12 x 12 strings, 12 nodes per string (8 shown), 225 m spacing. Total volume (2.475km)3 = 15.16 km3 = 32.83 km3 of w.e. Figure and specification come from Peter Gorham, talk in SLA
C SalSA workshop, Mar. 2005.
VHENTW, 4/25/206 M.A. Huang
Results -1cos vs. shower energy: all events
VHENTW, 4/25/206 M.A. Huang
SalSA tau events
Showers come from several processes: decay, energy loss, CC and reverse CC.
For each event, the maximum energy of sub-showers were used to identify this event.
VHENTW, 4/25/206 M.A. Huang
FWHM of cos distribution: -0.05 < cos < 1, i.e. 0< < 93
FWHM of Esh: 1016.5 eV < Esh < 1018 eV.
(Eth=1015 eV)
VHENTW, 4/25/206 M.A. Huang
Conclusion SHENIE simulation code is “almost” finish!
Still need some cosmetic works on user friendly I/O.• Especially, need to work on output to ntuple.
No manual or any documentation yet! For Earth skimming events:
AGN tau flux ~ 8.5 events/(km2 sr yr), need detector ~ 1 km2 sr • Shower spectrum peak around 1016 eV.
GZK tau flux ~ 0.12 events/(km2 sr yr), need detector ~ 100 km2 sr • Shower spectrum peak around 1017 eV.
For underground detector such as SalSA: Shower spectrum peak around 1017 eV. -0.1 < cos <1. In a radius of 5km salt dome, tau event rate could reach ~ 2.5 events
/year• Highly depend on detector simulation, which is highly simplified in this study.