Download presentation
Presentation is loading. Please wait.
Published byJovani Mullins Modified over 9 years ago
1
GZK ’s and their Detection with IceCube Interactions Interactions Results Results Implications for the IceCube Implications for the IceCube Summary Summary Shigeru Yoshida Dept. of Physics CHIBA Univ. CHIBA Univ. Chiba/Nagoya 2003
2
IceCube 1400 m 2400 m AMANDA South Pole IceTop Skiway 80 Strings 80 Strings 4800 PMT 4800 PMT Instrumented volume: 1 km3 (1 Gt) Instrumented volume: 1 km3 (1 Gt) IceCube is designed to detect neutrinos of all flavors at energies from 10 7 eV (SN) to 10 20 eV IceCube is designed to detect neutrinos of all flavors at energies from 10 7 eV (SN) to 10 20 eV
3
1.4 km 1km Upward Ice Rock ν ± π γ ν + e - e 1km lepton ν
4
UHE (EeV or even higher) Neutrino Events Arriving Extremely Horizontally Needs Detailed Estimation Limited Solid Angle Window ( N A ) -1 ~ 600 ( /10 -32 cm 2 ) -1 ( /2.6g cm -3 ) -1 [km] Involving the interactions generating electromagnetic/hadron cascades NN X e + e - Chiba/Naoya 2003
5
e e e/ Weak Incoming Products Weak Cascades Decay Weak Pair/decay Bremss Pair PhotoNucl. Decay Pair Pair Bremss Decay Weak Decay
6
Chiba/Nagoya 2003 Cross Sections and the Energy Loss Term CTEQ5 Parton Distribution for the evaluation
7
Chiba/Nagoya 2003
9
Muon(Neutrinos) from Nadir Angle
10
e e e/ Weak Incoming Products Weak Cascades Decay Weak Pair/decay Bremss Pair PhotoNucl. Decay Pair Pair Bremss Decay Weak Decay
11
Chiba/Nagoya 2003 Tau(Neutrinos) from Suppression By decay pair contribution
12
GZK Neutrino Production 2.725 K 411 photons / cm 3 0.6 x 10 -27 cm 2 γ p n p π + μ + ν e + ν γ E = 10 20 eV E 0.8 x 10 20 eV ~ Conventional Mechanism of EHE neutrinos!!
13
Chiba/Nagoya 2003
15
1.4 km 1km Upward Ice Rock ν ± π γ ν + e - e 1km lepton ν
16
Chiba/Nagoya 2003 A factor of 2 enhancement Due to the heavier lepton production
17
Chiba/Nagoya 2003
18
e e e/ Weak Incoming Products Weak Cascades Decay Weak Pair/decay Bremss Pair PhotoNucl. Decay Pair Pair Bremss Decay Weak Decay
19
Chiba/Nagoya 2003 Upward-going
20
Chiba/Nagoya 2003 Downward going!!
21
1.4 km 1km Upward Ice Rock ν ± π γ ν + e - e 1km Downward ν γ γ + e - e lepton
22
Chiba/Nagoya 2003
23
Down-going events dominates… 1400 m 2800 m 11000m UpDown
24
1.4 km 1km Downward Upward Ice Rock ν ν ± π γ γ γ ν + e - e 1km + e - e lepton EHE events!
25
Chiba/Nagoya 2003 Downward going!! 1 km 2 year
26
Energy Spectrum Diffuse Search Blue: after downgoing muon rejection Red: after cut on N hit to get ultimate sensitivity
27
Chiba/Nagoya 2003 Intensity of EHE and GZK model I (E>10PeV) I (E>10PeV) RATE [/yr/ km 2 ] m=4 Z max =4 Down 5.90 10 -19 5.97 10 -19 0.37 Up 3.91 10 -20 6.63 10 -20 0.03 m=7 Z max =5 Down 8.88 10 -17 9.10 10 -17 53.4 Up 5.72 10 -19 9.73 10 -18 4.64 [cm -2 sec -1 ]
28
Chiba/Nagoya 2003 GZK model dependence
29
Chiba/Nagoya 2003 Findings… appeared in EeV-10EeV is our prime target on UHE detection. 1/100-1/500 of primary intensity! Downward and make main contributions in EeV Energy Estimation would be a key for the bg reduction GZK is DETECTABLE by IceCube 0.4-50 events/year
30
Chiba/Nagoya 2003 We still need… IceCube Sensitivity on energy-deposit basis -Simulation of the EHE energy deposit profile -Smart Background rejection
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.