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UNIVERSITA’ DEL SALENTOUNIVERSITA’ DEL SALENTOFacoltà di Scienze MM.FF.NNFacoltà di Scienze MM.FF.NN
TIME MEASUREMENTS WITH THE ARGO-YBJ DETECTORTIME MEASUREMENTS WITH THE ARGO-YBJ DETECTOR
Dott.ssa Anna Karen Calabrese MelcarneDott.ssa Anna Karen Calabrese Melcarne
Dottorato di Ricerca in Fisica XIX ciclo
Settore scientifico FIS/04
22
OUTLINE
ARGO-YBJ as a ground-based detector
Timing calibration in EAS experiments (Characteristic Plane Method)
Characteristic Plane (CP) correction applied to ARGO-YBJ data
Physics results after calibration
33
Cosmic Ray SpectrumCosmic Ray Spectrum
44
Observation of Extensive Air Showers produced in the atmosphere by primary ’s
and nuclei
55
High Altitude Cosmic Ray Laboratory @ YangBaJingSite Altitude: 4300 m a.s.l. , ~ 600 g/cm2
Site Coordinates: longitude 90° 31’ 50” E, latitude 30° 06’ 38” N
66
Cosmic ray physics
• anti-p / p ratio at TeV energy• spectrum and composition (Eth few TeV)• study of the shower space-time structure
VHE -Ray Astronomy Search for point-like (and diffuse) galactic and extra-galactic sources at few hundreds GeV energy threshold
Search for GRB’s (full GeV / TeV energy range)
Sun and Heliosphere physics (Eth few GeV)
Main Physics GoalsMain Physics Goals
77
Layer (92% active surface) of Resistive Plate Chambers (RPC), covering a large area (5600 m2)
+ sampling guard ring+ 0.5 cm lead converter
time resolution ~1 nsspace resolution = strip
10 Pads (56 x 62 cm2)for each RPC
1 CLUSTER = 12 RPC
78 m
111 m
99 m
74 m
BIGPAD
ADC
RPC
(43 m2)
ARGO-YBJ layoutARGO-YBJ layout
88
RPC is suited to be used as element of a surface RPC is suited to be used as element of a surface detectordetector
RPC
PAD
Resistive Plate ChamberLow cost , high efficiency, highspace & time resolution (1 ns),easy access to any part of detector,robust assembling, easy to achieve>90% coverage, mounting withoutmechanical supports.
2850x1258mm2
99
Detector performancesDetector performances
good pointing accuracy (less than 0.5°)
detailed space-time image of the shower front
capability of small shower detection ( low E threshold)
large FoV (2) and high “duty-cycle” (100%)
continuous monitoring of the sky (-10°< <70°)Impossible for Atmospheric Cherenkov telescopes
1010
Full space-time reconstruction
Shower topology
Structure of the shower front
A unique way
to study EAS
74 m
60 m
90 m
150 ns
50 m
1111
Study of the EAS space-time structureStudy of the EAS space-time structure
The High space-time granularity of the ARGO-YBJ detector allows a deep study of shower phenomenology
with unique performance
Example 1: Very energetic shower
1212
Arrival Direction ReconstructionArrival Direction Reconstruction
Conical Fit
2E
PE
PE0
PP
2 )mc
yl
c
xtt(
EEEEEE sinsinm and cossinl
2PE
PE
PE0
PP
2 )c
Rm
c
yl
c
xtt(
Planar Fit
In EAS experiments for an event E the time tEP can be measured on each fired detector unit P, whose position (xP,yP) is well known
Primary direction cosines
angle azimuth
angle zenith
E
E
This quantity is not a proper 2 . Indeed the measurement unit is ns2
1313
Timing CalibrationTiming Calibration
P= residual correction + systematic correction
•Residuals correction reduces the differences between fit time and measured time
•Systematic correction guarantees the removal of the complete offset
Taking into account the time offset P typical of the detector unit
PEPEE0PEP ymxl)tΔt(c Plane-equation
1414
The air shower arrival directions have the following distribution:
.constd
dN
The systematic offset introduces a quasi-sinusoidal modulation in azimuth distribution
l0=sin0cos0 and m0=sin0cos0 disform the original angular distribution
1515
Characteristic Plane (CP) Definition
Fake Plane (FP)
PEPEE0PEP ymxl)tΔt(c Real Plane (RP)
P'EP
'E
'E0
resPEP ymxl)tt(c
resPE0
PPP c
yb
c
xaΔ On average
E0'
E0E0E'EE
'E tt mmb lla
Assuming uniform azimuth distribution
'E
'E mb and la
1616
CP Method Checks (Fast MC simulation)
Azimuth distribution before calibration Azimuth distribution after calibration
Time offsets introduced in the time measurement CP correction removes the time offsets
1717
CP method works also when a pre-modulation on primary azimuth angle is present
The CP method annulls <l> and <m> leaving a sinusoidal modulation on the distribution of the new ’’ azimuth angle
1818
Residual correction has been applied twice and systematic correction has been
applied according to the values:
A Gaussian fit is applied in the range ±10 ns around the bin with maximum number of entries
ARGO-YBJ DATA(ARGO-42, ARGO-104, ARGO-
130)
4'4' 1067m and 10304l
c
ym
c
xlΔ P'
EP'
EresPP
1919
Correction
Residuals after correction
2020
Effect of conical shape of the shower front
planar fit
Conical shape
FULL SIMULATION
Corsika+ARGOG codes
2121
CP method with conical correction
PE0
pE
PEEP
resP R
ct
c
ym
c
xlt
t
Planar residual after CP conical correction
Conical residual after CP conical correction
2222
Geomagnetic field effect
In the geomagnetic field, the secondary charged particles generated in EAS are stretched by the Lorentz force
2e
2
cosE2
sinBhd Average shift in the shower
plane for a secondary electron
electrons ofenergy average E
North) magnetic 0(shower theof angleazimuth
shower theof anglezenith
ninclinatio cgeomagneti
cos sinsincoscosacos
field cgeomagneti B
rajectoryelectron t theofheight verticalaverage h
e
H
HH
2323
θcos
χsing
2
YBJ - the geomagnetic effect is stronger for showers from North than for showers from South
This difference is more evident for larger zenith angles
H = 45° at ARGO-YBJ
15°
35°
45°
55°
cos sinsincoscos acos HH
=
=
North South
=
=
2424
Estimate of South-North asymmetry: MC
)]4p2cos(3p)2pcos(1p1[0pd
dN
N events from North (161.5º < Φ < 341.5º )
S events from South (161.5º >Φ and Φ >341.5º)
%1NS
NS2
Tibet AS estimate 2.5% higher rate from South direction with respect to North direction (geomagnetic field effect + slope of the hill where the array is located)
2525
Estimate of South-North asymmetry: Data
As expected CP method annulls the mean values of the primary direction cosines but a small sinusoidal modulation is still present in azimuth distribution
The mean values of direction cosines after CP correction are
1.0% 0.9%
2626
TDC peaks distribution
Before correction
After correction
2727
TDC method to update the calibration
TDC peak distribution after calibration has a regular concave shape
Without hardware change and with the same trigger, the concave surface should remain unvaried
On the other hand ….
2828
TDC peak dependence on temperature (night-day difference)
A collective shift (~3 ns) is observed.
Method odd-even events
The main effect of the TDC dependence on temperature is a shift of all TDC peaks, negligible for calibration and a minor effect is present but it is of the order of 0.2 ns
C4ΔT
2929
TDC dependence on offline CLUSTERs
The effect of offline CLUSTERs is visible only in peculiar conditions, thus this effect on the TDC calibration is negligible
3030
Angular Resolution
MC/data
Chess board method
72 parameter : the value in the angular distribution which contains ~72 % of the events
The residual correction improves the angular resolution
Even/Odd
3131
Moon shadow: absolute pointing
The systematical correction improves the absolute pointing
Significance map of the Moon shadow selecting events with a number of fired pads > 500 (~ 5 TeV median energy) and with zenith angle of the incident direction < 45°. 558 hours of observation.
)TeV(E
Z1.5Δ
3232
Time structure of EAS front
The curvature (Td) of the shower front as the mean of time residuals with respect to a planar fit
The thickness (TS) of the shower front as RMS of time residuals with respect to a conical fit
Shower curvature
3333
COMPARISON DATA-simulation
SIMULATION
COMPARISON proton-photon
Shower thickness
Shower thickness
3434
Conclusions
Characteristic Plane calibration has been defined and studied
Calibration with planar and conical fit for ARGO-42, ARGO-104, ARGO-130
Fast TDC calibration
South-North azimuthal asymmetry studied with full simulation
Improvements in the angular resolution and absolute pointing
Study on time structure of the shower front
3737
Papers
• G.Aielli et al., Nucl.Instr. And Meth., A562 (2006) 92• H.H.He, P.Bernardini, A.K.Calabrese Melcarne, S.Z.Chen, ”Detector Time
Offset and Off-line Calibration in EAS Experiments”, Astroparticle Physics 27 (2007) 528-531
Conferences and proceedings
• A.K.Calabrese Melcarne, “Time Calibration of the ARGO-YBJ detector”, *Cividale 2005 High Energy Gamma Ray Experiments*, 183-187
• P.Bernardini et al., “Time Calibration of the ARGO-YBJ experiment”, 29th International Cosmic Ray Conference, Pune 2005, 5-147
• A.K.Calabrese Melcarne, “Calibrazione del rivelatore ARGO-YBJ”, XCII Congresso Nazionale Societa’ Italiana di Fisica, atticon3408 III-C-39
• B.Wang et al., “Preliminary results on the Moon shadow with ARGO-YBJ”, 30th International Cosmic Ray Conference, Merida 2007, Mexico
• A.K.Calabrese Melcarne, I.De Mitri, G.Marsella, L.Perrone, G.Petronelli,A.Surdo, G.Zizzi , “Study of cosmic ray shower front and time structure with ARGO-YBJ”, 30th International Cosmic Ray Conference, Merida 2007, Mexico
3838
ARGO internal notes
Note 2004/02 • P.Bernardini, A.K.Calabrese Melcarne, C.Pino, “Time calibration of six Cluster”
Note 2005/02• P.Bernardini, A.K.Calabrese Melcarne, C.Pino, “Time-Calibration of the ARGO-YBJ detector (42 Clusters)”
Note 2006/03• P.Bernardini, A.K.Calabrese Melcarne, I.De Mitri, G.Mancarella, “Study of the arrival times of cosmic rays”
Note 2006/04• S.Z.Chen, A.K.Calabrese Melcarne, H.H.He, P.Bernardini, B.G.Sun, F.R.Zhu,”Characteristic Plane Method with Conical Correction”
Note 2006/05• P.Bernardini, A.K.Calabrese Melcarne, G.Mancarella, M.Khakian Ghomi, “Analysis of shower clusters”
Note 2007/03• A.K.Calabrese Melcarne, S.Z.Chen, P.Bernardini, H.H.He, “Conical Calibration for 130 Clusters and automatic updating”