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利用 ARGO-YBJ 的月亮阴影数据对能标的讨论. 查 敏 中科院高能物理研究所. Motivation: constructing an energy “anchor”. normalization and absolute energy calibration and reference for indirect measurements. Important progress on elemental CR energy spectrum from satellite/balloon-born experiments. ISS-CREAM. - PowerPoint PPT Presentation
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利用 ARGO-YBJ的月亮阴影数据对能标的讨论查敏中科院高能物理研究所
Motivation: constructing an energy “anchor”
Important progress on elemental CR energy spectrum from satellite/balloon-born experiments
normalization and absolute energy calibration and reference for indirect measurements
ISS-CREAM
ISS-CREAM is planned for launch in 2014
Direct experiment: CREAM example
Few TeV region few 100 TeV (MC )
first suggestion by Clark 1957
Deficit of CR as looking at the moonSize of the deficit --> actual angular resolutionPositon of the deficit pointing errorDisplacement of moon shadow energy calibration ( size.vs. E)
Selected MOON data
Using moon shadow East-West displacement to calibration Erec:The relation between Erec and Nstrip
利用地磁场的磁谱仪的作用,再加上 ARGO高海拔、低阈能得特点,挑选阴影数据通过对宇宙线轻成分在低能端能谱的测量,建立“能标”。
Summary of notable experiments
82MAGIC
The energy scale error is estimated to be smaller than 13% in the energy range 1 – 30 (TeV/Z).
Two systematic uncertainties may affect the Multiplicity-Energy relation:• the assumed primary CR chemical composition (7%)• the uncertainties of different hadronic models (6%)
55 s.d.
ARGO coll., Phys.Rev. D 84 (2011) 022003 / ARGO coll., Phys.Rev. D 85 (2012) 022002
Energy calibrtion
From Menjo Hiroaki ICRC2013 (LHCf coll.)
Geomagnetic field
International Geomagnetic Reference Field (IGRF) coefficients by IAGA
Trigger: 20 pads Rate ~3.5 kHz Dead time 4% First data in July 2006 Stop operation in February 2013
ARGO-YBJ Detector
Low energy with digital signal High energy with analog readout
High altitude location ( 4300 m + 606g/cm2)Full coverage with RPC (92% covering factor)
analysis details• Shower production
– Zenith angle range: 0-40°• Moon shadow statistics. Vs. shower attenuation effect
• Moon shadow statistics
• Data Selection– Add more inclined showers– detailed shower information
θ ≤15° ≤25° ≤30° ≤40° ≤46° ≤50°
Moon T 6% 25% 35% 63% 83% 1 (105276.)
Sec(θ) 1.04 1.1 1.15 1.3 1.44 1.55
1 month moon shadow -9 sigma;Theta< 30 deg + |xc|<31 + |yc|<31 + Ns>300
--continued
<R> < 22 m Non-light contamination ratio: 4-6%
Proton showers steeper and narrower lateral distribution
--continued• Moon shadow analysis
– Direct Integration method – 0-35 °light data– LGRF model
• Shower production– CORSIKA package– Hadronic models:
• EPOS-LHC + Fluka & QGSJETII-3 + QHEISHA;– Zenith angle range: 0-40° + uniform azimuth angle;– 5 groups composition
• P /He /CNO/MgAlSi/Iron• Detector response simulation: G4ARGO package
– Core sampling 1500 x 15000 m2;• Data Selection
– Core: |Xc|<31 + |Yc|<31 m;– Good contained data: r + Rp70 <50 m;– Zenith < 35 deg– <R> <22 m
Moon shadow result
400-800 800-1000
1000-2000 >2000
Preliminary result:
Summary and Outlook
• ARGO-YBJ is a good candidate to construct an “energy anchor”;
• Selection of light component is OK;• Moon shadow measurement offers cross check;• Preliminary result is encouraging;• To finish work and understand systematic
uncertainty;
backup
Moon shadow: an important tool to check the detector performances and offer energy calibration
10 standard deviations /month
ARGO coll., Phys.Rev. D 84 (2011) 022003 / ARGO coll., Phys.Rev. D 85 (2012) 022002
Energy calibration
West displacement of the shadow caused by the geomagnetic field
Bending ≈ 1.58°Z/E (TeV)