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Published byJonathan Dean Modified over 9 years ago
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ARIANNA: A New Concept for Cosmogenic Neutrino Detection
Steven W. Barwick (UC Irvine) A talk in honor of the life and work of Simon Swordy November 19, 2010
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ARIANNA: A New Concept for the Detection of GZK neutrinos
~1 km Steven W. Barwick, UC-Irvine
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Neutrino Telescopes: Agenda
10 years of progress with optical Cherenkov Detectors Extremely Energetic Neutrinos - New Technologies Radio Cherenkov: ARIANNA Teraton -Petaton
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PHOTONS: not deflected, but: reprocessed in sources, absorbed in IR (100 TeV), and CBR
PROTONS: deflection in magnetic fields, GZK cutoff NEUTRINOS: not absorbed or deflected, hard to see
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1997: Unlimited Opportunity
E2 dN/dE (GeVcm-2s-1sr-1) A. Silvestri, PhD Dissertation, 2008 WB Log10(E[GeV])
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13 Years of Diffuse Progress
2010 ~100x improvement E2 dN/dE (GeVcm-2s-1sr-1) A. Silvestri, PhD Dissertation, 2008 Auger x3 ANITA AMANDA-UHE WB Log10(E[GeV])
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Excluding AGN Model Predictions for Diffuse Flux
Excluded Normalization to x-ray or MeV ’s overproduces neutrino flux
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GZK neutrinos [ one of the the most secure predictions in the field ]
New Technologies
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Cosmogenic (or GZK) Neutrinos
Predictions are secure: p + cmb -> -> n + + n -> lower energy protons -> However, -Flux Calculations depend on: Elemental composition (p, Fe, mixed) Cosmology (=0.7) Injection Spectra, E- and Emax Evolution of sources with redshift, (1+z)m Star formation, QSO, GRB, little or no
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GZK Model-Specific limits
all) E dN/dE (cm-2s-1sr-1) 109 GeV ANITA-08 Log10(E[GeV])
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Why Big Detectors? So GZK detection requires > 10 km3
GZK Flux, (E~1018 eV): /km2/yr Interaction Length, : km Event Rate/km3/yr = [/] ~ 0.2 Efficiency, livetime, nice if more than one So GZK detection requires > 10 km3 (aperture > 60 km3sr) Note: ARIANNA has ~ 2400 km3sr
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ARIANNA Sensitivity Greatly increases sensitivity to GZK in E= eV ARIANNA + ESS Flux: 40 events/yr ARIANNA Energy Res: dE/E~1, Angular Res: ~1 deg
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EHE Neutrinos Explore Higher Dimensions
~100sm For GZK E ARIANNA-GZK CC: sm (Anchordoqui, et al, hep-ph/ )
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EHE Neutrinos Explore Lorentz Invariance Violation
ARIANNA (6 mo) ARIANNA (5 yr) No LIV EF(E) (m-2sr-1s-1) ARIANNA-GZK Strong LIV Log E (eV) (Scully, Stecker, arXiv: v1)
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Neutrino Cross-Section
A. Connolly, 2006 ARIANNA - 10 years [ ] = 0.24 If Nev = 400 If =0.5o If =2GQRS GQRS 2 parameter fit: Normalization cross-section
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New Techniques to Observe Cosmogenic Neutrinos
Current Under Development Radio RICE, ANITA ARIANNA, ARA, IceRay, SALSA, etc Air Shower HiRes, Auger TA, Auger N, OWL Acoustic SPATS, AMADEUS
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Askaryan Radio Emission from SLAC beam in Ice
Gorham, Barwick, et al., astro-ph/ Absolute RF power and frequency dependence confirmed Width of cherenkov cone and frequency dependence confirmed
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ARIANNA 31 x 31 array [30 km x 30 km] 1 km 600 m
UCI, LBL, OSU, WashU, KU,UC-London, S.Korea Barwick, astro-ph/
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Satellite Image of Victoria Land and Ross Ice Shelf
Ross Island Dry Valleys wireless internet (2009) ~120 km Minna Bluff ARIANNA 30x30 km2 Ice Thickness ~600m south
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ARIANNA Advantages Straightforward logistics Excellent site properties
not far (~120 km) from main US science station surface deployment (no drilling) Excellent site properties Protected from man-made noise Remarkable attenuation length and reflectivity from bottom Lightweight, robust technologies (so low $$) Internet access 24/7 Array is reconfigurable to follow science
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ARIANNA Characteristics
log(E) eV Zenith Angle Nearly uniform response over the entire sky Peak response at “sweet spot” of GZK spectrum
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ARIANNA “Pointing” Zenith Angle
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Optimal Antenna Gain = 7 LPDA
higher gain restricts viewing of reflected events but accesses lower energy cascades LPDA
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Impact of firn ice on LPDA Antenna (not much, except at f<100MHz)
L. Gerhardt, et al, NIMA, 2010
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Time-domain is rich in information
on-cone off-cone -10 10 Time(ns) -10 10 Time(ns) J. Alvarez-Muniz, A. Romero-Wolf, and E. Zas, arXiv: v1
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Modification by antenna+amp
Interesting structure, well suited to pattern trigger Similar pulse structure for on-cone and off-cone -60 60 Time(ns)
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Camping at Moore’s Bay Site
David Saltzberg
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ARIANNA Site Studies And Radio Quiet!
T. Barrella, et al., J. Glaciology, 2010 Value assumed prior to this work Preliminary Arbitrary amplitude scaling Amazing fidelity of reflected pulse from sea-water bottom -behaves as nearly flawless mirror 1-way attenuation length, averaged over depth and temperature And Radio Quiet!
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ARIANNA Prototype Station (deployed Dec. 2009)
L. Gerhardt, et al, NIMA, 2010 ARIANNA Prototype Station (deployed Dec. 2009) Power Tower Wireless “lab”
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Housekeeping Data Outside Temp windy Wind speed Power Supply Voltage
Jan 1, 2010 Feb 4, 2010
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Trigger rates ~ 10-2 s-1 Randomly distributed in time Trigger: 2 of 3 majority, 5*Vrms
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Prelim. Event Analysis (Jan 5 -Feb 4, 2010)
No events in signal region
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ARIANNA Visualization
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Outlook To probe the GZK neutrino fluxes and particle physics at highest energies, new techniques are being developed based on radio cherenkov , air shower and acoustic detection. ARIANNA has the right combination of size and simplicity of deployment to keep costs down Ice studies in Nov’ 06 astonishingly good Recent protostation studies show low Anthropogenic noise over 1 month periods 7-station engineering array approved by NSF in April 2010
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Air Shower vs Ice Shower (time profiles quite different!)
100MHz-1 GHz
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Electronic Module Schematics
L. Gerhardt, et al, NIMA, 2010
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Solar Panel Power Electronic Module
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GZK Cutoff (Experimentally Confirmed)
arXiv: v1
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