Cosmic Ray International Seminar 13-17 September 2010 Catania - Italy
Mass composition results from the Pierre Auger Observatory
Simone Riggi
- n behalf of the Pierre Auger Collaboration
Mass composition results from the Pierre Auger Observatory Simone - - PowerPoint PPT Presentation
Cosmic Ray International Seminar 13-17 September 2010 Catania - Italy Mass composition results from the Pierre Auger Observatory Simone Riggi on behalf of the Pierre Auger Collaboration C.S.F.N.S.M. University of Catania INFN Catania The
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◮ Southern Observatory (Malargüe - Argentina): area ∼3000 km2
◮ Northern Observatory (Colorado - USA): area ∼21000 km2 3 / 43
◮ 12 tonnes of deionized water ◮ 3 Photonis PMTs (diameter 12 cm) ◮ FADC sampling rate 40 MHz ◮ Solar panels for power supply ◮ Time tagging with GPS system (∼8 ns res-
◮ Tank signal calibration in Vertical Equiva-
◮ 5 SD trigger levels, T1&T2 @ PMT and
◮ Tank event rate 3 kHz
trigger
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◮ Signal-weighted barycenter of triggered tanks → core location ◮ Fit to tank timings with a shower front model → shower axis ◮ Fit LDF to tank signals ⇒ S1000 FD calibration
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◮ Signal-weighted barycenter of triggered tanks → core location ◮ Fit to tank timings with a shower front model → shower axis ◮ Fit LDF to tank signals ⇒ S1000 FD calibration
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◮ 6 telescopes/FD site ⇒ 24 telescopes; ◮ Telescope aperture: 30◦×30◦ ◮ Camera: 22×20 Photonis PMTs ◮ FADC sampling rate: 10 MHz ◮ Time tagging with GPS system ◮ Absolute and relative calibration with UV
◮ Atmosphere calibrated with many devices
◮ 3 FD trigger levels, FLT @ PMT level,
◮ Hybrid event rate ∼ 5-10 events/hour 7 / 43
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]
2
slant depth X [g/cm
200 300 400 500 600 700 800 900 1000 1100 )
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Number of charged particles (x 10 1 2 3 4 5 6 7 8 eV
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proton, E=10 eV
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iron, E=10 eV
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gamma, E=10
2
max
500 600 700 800 900 1000 1100 1200
50 100 150 200 250 300 350 400
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◮ signal-weighted fit to PMT directions → Shower Detector Plane (SDP) ◮ signal-weighted fit to PMT timings → shower axis 10 / 43
◮ light profile at the telescope aperture → energy deposit profile ◮ Gaisser-Hillas fit to profiles → Xmax
◮ including rec algorithm, choice of longitudinal fitting function & lateral distribution ◮ systematic uncertainty < 8 g/cm2 (@1018 eV) 11 / 43
◮ CALIBRATION SELECTION
→ no bad pixels
◮ ATMOSPHERE SELECTION
→ small cloud coverage and optimal aerosol conditions
◮ GEOMETRY SELECTION
→ dtank−axis < 2 km, θview>20◦ → precise measurement of the shower axis (∼0.1◦)
◮ PROFILE SELECTION
→ optimal GH fit, small Xmax uncertainties (<40 g/cm2) → no gaps in profiles → Xmax observed in field of view (FoV) → unbiased measurement of Xmax
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[E/eV]
10
log
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10
19
10
Efficiency Ratio
0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2
Fe
/Eff
p
Eff
Fe
/Eff
He
Eff
Fe
/Eff
O
Eff
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◮ The resolution deteriorates towards low energies (less light) ◮ 1018 eV: ∼27 g/cm2, 1019 eV: <20 g/cm2 ◮ Cross-checked with stereo data 15 / 43
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19
2
max
QGSJET01 QGSJETII Sibyll 2.1 EPOS 1.99
syst
proton iron
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18
19
max
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t [25 ns]
60 65 70 75 80 85 90 95 100 105
Signal [VEM peak]
20 40 60 80 100 120
t [25 ns]
60 65 70 75 80 85 90 95 100 105
Signal [VEM peak]
20 40 60 80 100 120
±
µ γ
±
e total
◮ t1/2 sensitive to shower development
◮ t1/2 sensitive to electron/muon content
◮ t1/2 linearly correlates with Xmax
N
1/2 − t1/2(r, θ, Eref )
1/2(r, θ, S)
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◮ em component absorption in late region
◮ em absorption increases with zenith θ
◮ Asymmetry profile maximum as
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◮ Independent measurement of composition with 2 detectors ◮ Parameter reconstruction and selection under control ◮ Different sources of systematics studied
◮ increasing statistics ◮ composition from Xmax distributions ◮ low energy enhancements (→ 1017 eV) ◮ composition with muons counters and radio antennas 25 / 43
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◮ PRE-SELECTION
→ hybrids (1 tank at least); → E>1019 eV (photon analysis), E>1018 eV (ER);
◮ GEOMETRY SELECTION
→ "HottestTank"-axis distance<2 km; → Minimum viewing angle>20◦;
◮ PROFILE SELECTION
→ Xmax observed; → optimal Gaisser-Hillas fit: χ2
GH/Ndf <2.5, χ2 GH/χ2 linear <0.9;
→ σstat (Xmax )< 40 g/cm2, σstat (E)/E < 20%; → no gaps in profile (ProfileGap/TrackLength< 20%;
◮ CALIBRATION SELECTION
→ good cal period; → no bad pixels;
◮ ATMOSPHERE SELECTION
→ Aerosol MieDB; → VAOD@3km ≤ 0.1; → Cloud Coverage ≤ 25%;
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◮ PRE-SELECTION
→ hybrids (1 tank at least); → E>1019 eV (photon analysis), E>1018 eV (ER);
◮ GEOMETRY SELECTION
→ "HottestTank"-axis distance<2 km; → Minimum viewing angle>20◦;
◮ PROFILE SELECTION
→ Xmax observed; → optimal Gaisser-Hillas fit: χ2
GH/Ndf <2.5, χ2 GH/χ2 linear <0.9;
→ σstat (Xmax )< 40 g/cm2, σstat (E)/E < 20%; → no gaps in profile (ProfileGap/TrackLength< 20%;
◮ CALIBRATION SELECTION
→ good cal period; → no bad pixels;
◮ ATMOSPHERE SELECTION
→ Aerosol MieDB; → VAOD@3km ≤ 0.1; → Cloud Coverage ≤ 25%;
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◮ PRE-SELECTION
→ hybrids (1 tank at least); → E>1019 eV (photon analysis), E>1018 eV (ER);
◮ GEOMETRY SELECTION
→ "HottestTank"-axis distance<2 km; → Minimum viewing angle>20◦;
◮ PROFILE SELECTION
→ Xmax observed; → optimal Gaisser-Hillas fit: χ2
GH/Ndf <2.5, χ2 GH/χ2 linear <0.9;
→ σstat (Xmax )< 40 g/cm2, σstat (E)/E < 20%; → no gaps in profile (ProfileGap/TrackLength< 20%;
◮ CALIBRATION SELECTION
→ good cal period; → no bad pixels;
◮ ATMOSPHERE SELECTION
→ Aerosol MieDB; → VAOD@3km ≤ 0.1; → Cloud Coverage ≤ 25%;
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Event with maximum outside FOV
◮ PRE-SELECTION
→ hybrids (1 tank at least); → E>1019 eV (photon analysis), E>1018 eV (ER);
◮ GEOMETRY SELECTION
→ "HottestTank"-axis distance<2 km; → Minimum viewing angle>20◦;
◮ PROFILE SELECTION
→ Xmax observed; → optimal Gaisser-Hillas fit: χ2
GH/Ndf <2.5, χ2 GH/χ2 linear <0.9;
→ σstat (Xmax )< 40 g/cm2, σstat (E)/E < 20%; → no gaps in profile (ProfileGap/TrackLength< 20%;
◮ CALIBRATION SELECTION
→ good cal period; → no bad pixels;
◮ ATMOSPHERE SELECTION
→ Aerosol MieDB; → VAOD@3km ≤ 0.1; → Cloud Coverage ≤ 25%;
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Event with bad pixels
◮ PRE-SELECTION
→ hybrids (1 tank at least); → E>1019 eV (photon analysis), E>1018 eV (ER);
◮ GEOMETRY SELECTION
→ "HottestTank"-axis distance<2 km; → Minimum viewing angle>20◦;
◮ PROFILE SELECTION
→ Xmax observed; → optimal Gaisser-Hillas fit: χ2
GH/Ndf <2.5, χ2 GH/χ2 linear <0.9;
→ σstat (Xmax )< 40 g/cm2, σstat (E)/E < 20%; → no gaps in profile (ProfileGap/TrackLength< 20%;
◮ CALIBRATION SELECTION
→ good cal period; → no bad pixels;
◮ ATMOSPHERE SELECTION
→ Aerosol MieDB; → VAOD@3km ≤ 0.1; → Cloud Coverage ≤ 25%;
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Event with bad aerosol conditions
◮ PRE-SELECTION
→ hybrids (1 tank at least); → E>1019 eV (photon analysis), E>1018 eV (ER);
◮ GEOMETRY SELECTION
→ "HottestTank"-axis distance<2 km; → Minimum viewing angle>20◦;
◮ PROFILE SELECTION
→ Xmax observed; → optimal Gaisser-Hillas fit: χ2
GH/Ndf <2.5, χ2 GH/χ2 linear <0.9;
→ σstat (Xmax )< 40 g/cm2, σstat (E)/E < 20%; → no gaps in profile (ProfileGap/TrackLength< 20%;
◮ CALIBRATION SELECTION
→ good cal period; → no bad pixels;
◮ ATMOSPHERE SELECTION
→ Aerosol MieDB; → VAOD@3km ≤ 0.1; → Cloud Coverage ≤ 25%;
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Event with cloudy conditions
◮ ANTIBIAS CUTS
→ requiring Xmax in FOV reject very deep and shallow showers → bias the event selection; → use MC to determine a range of detectable depths, given the shower geometry; → the viewable depths depend on shower geometry (telescope FOV, distance from the FD), energy, atmosphere; → guarantee an unbiased selection;
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GH/Ndf < 2.5
linear-χ2 GH) > 4
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HotTankAxisDist < 750 833 × log10(E/EeV) 2000 log10(E/EeV) < 0 0 ≤ log10(E/EeV) < 1.5 log10(E/EeV) ≥ 1.5
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max
max − Xmax)2
max − Xmax)2
N
N−1 V 2
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◮ SD spectrum
⇒ zenith angles < 60◦; ⇒ energy > 3×1018 eV; ⇒ energy calibrated with a subset of high quality hybrid events; ⇒ exposure ε from number of active detector stations over time;
◮ FD spectrum
⇒ energy > 1018 eV; ⇒ exposure from dedicated time-dependent MC simulations describing real data-taking conditions;
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◮ Test null hypothesis (isotropy)
⇒ Prob. P to observe at least k correlated events out of N (isotropic p=0.21), likelihood ratio R: P =
N
N j
R = 1
p pk (1 − p)N−k dp
pk (1 − p)N−k+1
◮ Find correlation scale
⇒ Scan P minima vs θ, z, Ethr
◮ Confirm/reject the signal with independent data samples
prescription: α=1%, β=5%, R>95% ⇒ reject isotropy @ 99% level
◮ Running the prescription
⇒ Data period II (06/2006-08/2007) k/N=9/13 (kiso=2.7), P=2×10−4 ⇒ ANISOTROPY CLAIM ⇒ Data period II+III (06/2006-03/2009) k/N=17/44 (kiso=9.2), P=6×10−3 ⇒ ANISOTROPY CLAIM. . . but reduced correlation signal
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◮ SD limits
◮ FD limits
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