Bianca Keilhauer for the Pierre Auger Collaboration

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Presentation transcript:

Bianca Keilhauer for the Pierre Auger Collaboration XII International Conference on Calorimetry in High Energy Physics Chicago, June 5 - 9, 2006 The Fluorescence Detector of the Pierre Auger Observatory - A Calorimeter for UHECR Bianca Keilhauer for the Pierre Auger Collaboration Forschungszentrum Karlsruhe in der Helmholtz-Gemeinschaft

Cosmic Ray (CR) Spectrum flux (m² sr s GeV) -1 energy (eV) direct measurements KASCADE Grande AUGER 1 particle per m2 • sec Knee 1 particle per m2 • year Ankle 1 particle per km2 • century Cosmic Ray (CR) Spectrum power law over more than 10 orders of magnitude in energy below knee: particles from the Sun and supernova remnants mainly protons and α-particles at knee: γ changes from 2.65 to 3.1 transition to heavier composition at ankle and above: CR of extra-galactic origin again change of γ sources, particle types, GZK-cut off ???

Scientific goals of the Pierre Auger Observatory detection of Extensive Air Showers induced by UHECRs E0 > 5•1018 eV high statistics good understanding of systematics disentangle energy, incoming direction, type of primary particle full sky coverage anisotropy neutrino detection limit on photon flux provide hybrid detection technique

Hybrid Detection Technique longitudinal shower profiles by fluorescence light in atmosphere lateral particle distribution at ground

Why Hybrid Detection Technique ? Surface Detectors 100 % duty cycle acceptance = geometric only last stage of shower development observed energy scale model dependent Fluorescence Detectors ≈ 15 % duty cycle acceptance depends on distance and atmosphere observation of longitudinal shower development (almost) model independent

Location of the Pierre Auger Observatory 2 detection sites: Northern hemisphere, Colorado - USA, construction begin in 2009 Southern hemisphere, Malargüe - Pampa Amarilla - Argentina, construction finished mid 2007

Layout of Southern Observatory 60 km

Auger Fluorescence Detectors 6 telescopes in a station 6 x ( 30° x 28.6° field of view) 4 stations at the boundary of the array 3 stations ready, 4th under construction Los Leones Coihueco

Fluorescence Detector 440 PMT per camera, each 1.5° → resolution better 1° 15% duty cycle 100 ns sampling intervals energy resolution ≤ 10% Fluorescence Detector

Water Cherenkov Tanks ≈ 1100 of 1600 tanks deployed distance 1.5 km to each other 12 m³ ultrapure water duty cycle: 100% angular resolution ≤ 1.1° energy resolution ≈ order (10%) PMT signals: shape and time information 25 ns intervals

Electromagnetic Shower primary particle is electron or positron hadronic interaction yields in π0 → decay into 2 γ Heitler model: γ pair production e+ e- Bremsstrahlung e+ γ e- γ ... ... ... ... ... ... ... ... e+ .... e+ γ .... γ e- .... e- ionization Earth surface

... ... ... ... Hadronic Shower π± π0 K± K0 γ γ π±, π0, μ±, e±, ν primary particle is nucleus for heavier nuclei - superposition of A proton showers π± π0 K± K0 decay ↔ interaction γ γ per generation: ≈ 1/3 of E in em. cascade π±, π0, μ±, e±, ν ... ... ... μ±, ν μ±, ν π±, μ±, ν ... Earth surface < 10 % of E0 in hadr. cascade

Particle Numbers in EAS

Energy Deposit of EAS in the Atmosphere

Shower Maximum

Correction Factor for „Missing Energy“ T. Pierog et al., 29th ICRC, India, 2005

Efforts on reduction of uncertainties balloon launching station absolut "drum" calibration Efforts on reduction of uncertainties central laser facility P. Bauleo et al., 29th ICRC, 2005 F. Arqueros et al., 29th ICRC, 2005 lidar at each telescope fluorescence yield experiment B. K. et al., 29th ICRC, 2005 R. Cester et al., 29th ICRC, 2005 balloon launching station T.Waldenmaier et al., 29th ICRC, 2005

⇒ altitude and time dependent height (km a.s.l.) 10 8 6 5 4 3 2 particle number (x 109) Geometrical Effect atmospheric depth (g/cm²) atmospheric depth: air density: ⇒ altitude and time dependent Fe p 1019eV / 0° US Std. atmosphere

Position of Shower Maximum both EAS in US-Std, 60°, 1019eV: → Δhmax= 770 m vertical difference in altitude 7.63 8.40 Fe p Fluorescence Yield in photons/m height in m a.s.l. EAS , 60°, 1019eV, p summer (Argentina) Fe winter (Arg.) → Δhmax= 120 m vertical difference in altitude 8.03 8.15 Fe p Fluorescence Yield in photons/m B. K. et al., Astropart.Phys.22, 249, 2004

Fluorescence Light mainly e± of EAS excites N2 molecules in air 18 strong emission bands in 2P system between 300 and 400 nm 1 strong emission band in 1N system between 300 and 400 nm Fluorescence Yield with assumption

Fluorescence Yield at sea level for a 0.85 MeV electron in US Std. Atmosphere B. K. et al., Astropart.Phys.25, 259, 2006

Real EAS Event from Auger R. Engel, Forschungszentrum Karlsruhe

Energy determination from hybrid events 93 events above 1018 eV take S38 value from SD vs. energy from FD fit line through data Log (E) = -0.79 + 1.06 Log(S38) energy conversion factor E = 0.16 S381.06 (E in EeV, S38 in VEM) Uncertainty: 15% at 3 EeV 40% at 100 EeV P. Sommers, Auger Collab. 29th ICRC, 2005

Cosmic Ray Spectrum „before Auger“ R. Engel, Forschungszentrum Karlsruhe

Cosmic Ray Spectrum with estimated „Auger Flux“ R. Engel, Forschungszentrum Karlsruhe

Estimated Spectrum R. Engel, Forschungszentrum Karlsruhe

Uncertainties on the reconstructed energy from FD signal in the PMTs light collection 5 % detector calibration 12 % photons at the FD geometry reconstruction (hybrid) 2 % aerosol levels 10 % fluorescence photons emitted at the shower axis atmospheric density profile 2 % fluorescence yield 15 % energy deposit per slant depth correction for missing energy 3 % primary cosmic ray energy < 25 % Inprovements in the near future J. Bellido, Auger Collab. 29th ICRC, 2005

Summary Southern detector near completion First cosmic ray spectrum Multiple efforts on atmospheric monitoring and calibration 36 presentation and 1 highlight talk at the 29th International Cosmic Ray Conference, Pune, India, 2005 ⇒ just brief overview about science results presented

That‘s also working for Auger

First estimate of the cosmic ray spectrum data set from January 1st 2004 - June 5th 2005 all events with zenith angle between 0° and 60° time average area = 660 km² ( 22 % of final size) Quality cuts: core surrounded by equilateral triangle of working stations station with highest signal has ≥ 5 working nearest neighbours full efficiency above 3 EeV 3525 SD events above 1018.5 eV Procedure calculate energy from SD signal → time-integrated water Cherenkov signal S(1000) zenith angle correction - Constant Intensity Cut method use hybrid events for conversion of SD value to energy calculate exposure of the growing array P. Sommers, Auger Collab. 29th ICRC, 2005

Estimated Spectrum vs. Log(E) Error bars on points indicate Poisson statistical uncertainty (or 95% CL upper limit) based on the number of events. Systematic uncertainty is indicated by double arrows at two different energies. Horizontal: Systematic E Vertical: Exposure uncertainty ΔE/E ≈ 50 % ΔE/E ≈ 30 % P. Sommers, Auger Collab. 29th ICRC, 2005

Reconstruction of measured EAS profiles Malargüe Monthly Models vs. US standard atmosphere Änderung der rekonstruierten Primärenergie < 1% Verschiebung der Position des Schauermaximums ≈ -15 g/cm² B.K. et al., Auger Collab. 29th ICRC, 2005

Remaining Uncertainties within monthly models Malargüe Monthly Models modified by applying an 1σ error (day-to-day variations) uncertainty of depth of maximum ≈ 6 g/cm² uncertainty of primary energy ≈ 0.5 % B.K. et al., Auger Collab. 29th ICRC, 2005

Auger Shower Profiles proton photons iron M. Risse, astro-ph/0512434, 2005 photons iron

Seasonal and Altitude dependence for Auger for a 0.85 MeV electron B. K. et al., Astropart.Phys.25, 259, 2006

Energy Resolution of the Atmosphere - Energy Deposit at Shower Maximum - T. Pierog et al., 29th ICRC, India, 2005