Charge excess signature in the CODALEMA data

wosot41348 6 views 36 slides Jun 25, 2024
Slide 1
Slide 1 of 36
Slide 1
1
Slide 2
2
Slide 3
3
Slide 4
4
Slide 5
5
Slide 6
6
Slide 7
7
Slide 8
8
Slide 9
9
Slide 10
10
Slide 11
11
Slide 12
12
Slide 13
13
Slide 14
14
Slide 15
15
Slide 16
16
Slide 17
17
Slide 18
18
Slide 19
19
Slide 20
20
Slide 21
21
Slide 22
22
Slide 23
23
Slide 24
24
Slide 25
25
Slide 26
26
Slide 27
27
Slide 28
28
Slide 29
29
Slide 30
30
Slide 31
31
Slide 32
32
Slide 33
33
Slide 34
34
Slide 35
35
Slide 36
36

About This Presentation

ICRC talk Charge excess signature in the CODALEMA data


Slide Content

Vincent Marin
for the CODALEMA collaboration
SUBATECH
Nantes France
ICRC 2011 Beijing 12/08/2011
China
Charge excess signature in the
CODALEMA data
Interpretation with

CODALEMA, Nançay (France)
Radio detection of air showers above 10
16
eV
Autonomous
station
CODALEMA3
CODALEMA2
1.6 km
CODALEMA2
24 antennas (EW
polarization)
triggered by
an array of 13
scintillators
CODALEMA3
60 dual polarization
antennas,
self-trigger,
in acquisition and
deployment

CODALEMA, Nançay (France)
Radio detection of air showers above 10
16
eV
Autonomous
station
CODALEMA3
CODALEMA2
1.6 km
CODALEMA2
24 antennas (EW
polarization)
triggered by
an array of 13
scintillators
CODALEMA3
60 dual polarization
antennas,
self-trigger,
in acquisition and
deployment
See A.Bellétoile’s talk
on August 15, Monday

CODALEMA, Nançay (France)
Radio detection of air showers above 10
16
eV
Autonomous
station
CODALEMA3
CODALEMA2
1.6 km
CODALEMA2
24 antennas (EW
polarization)
triggered by
an array of 13
scintillators
CODALEMA3
60 dual polarization
antennas,
self-trigger,
in acquisition and
deployment
See A.Bellétoile’s talk
on August 15, Monday
This presentation
focus only on CODALEMA2 data

CODALEMA, Nançay (France)
Direct confirmation of the
geomagnetic origin of
the air shower electric field
CODALEMA Collaboration, Astropart.Phys. 31 (2009)
E α n x B
Sky map of
radio-detected events
EW component of
n X B
Zenith
angular
distribution
Azimuth
angular
distribution
Prediction
data
Prediction
datan x B
n x B

Simulation of ELectric
Field from Air Shower
e
-
e
+
B
•Geomagnetic mechanism contribution
Due to
Lorentz Force
Charge
separation
Transverse current
variation
Maxwell equations
Electric field
e
-e
+

Simulation of ELectric
Field from Air Shower
e
-
e
+
B
•Geomagnetic mechanism contribution
Due to
Lorentz Force
Charge
separation
Transverse current
variation
Maxwell equations
Electric field
•Charge excess contribution
Electrons excess
in the air shower
Residual negative
charge
negative charge
variation
Maxwell equations
Electric field
e
-e
+

Simulation of ELectric
Field from Air Shower
e
-
e
+
B
•Geomagnetic mechanism contribution
Due to
Lorentz Force
Charge
separation
Transverse current
variation
Maxwell equations
Electric field
•Charge excess contribution
Electrons excess
in the air shower
Residual negative
charge
negative charge
variation
Maxwell equations
Electric field
Dominant, already
observed
Second order contribution,
search for its signature in our datae
-e
+

Vertical event at CODALEMA
6
12
18
24
31
37
4349
55
6268
74
80
86
93
99
￿400 ￿200 0 200 400
￿400
￿200
0
200
400
West East￿m￿
South North￿m￿
East￿westpolarization
Θ￿0°
Φ￿0°
￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
￿400 ￿200 0 200 400
￿400
￿200
0
200
400
West East￿m￿
South North￿m￿
Antennapositions
vertical shower, 10
17
eV,
145 antennas
Ground core position in (0,0)
EW electric field absolute
value on the ground
x

Vertical event at CODALEMA
6
12
18
24
31
37
4349
55
6268
74
80
86
93
99
￿400 ￿200 0 200 400
￿400
￿200
0
200
400
West East￿m￿
South North￿m￿
East￿westpolarization
Θ￿0°
Φ￿0°
￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
￿400 ￿200 0 200 400
￿400
￿200
0
200
400
West East￿m￿
South North￿m￿
Antennapositions
vertical shower, 10
17
eV,
145 antennas
Ground core position in (0,0)
EW electric field absolute
value on the ground
x
east-west asymmetry

Vertical event at CODALEMA
6
12
18
24
31
37
4349
55
6268
74
80
86
93
99
￿400 ￿200 0 200 400
￿400
￿200
0
200
400
West East￿m￿
South North￿m￿
East￿westpolarization
Θ￿0°
Φ￿0°
￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
￿400 ￿200 0 200 400
￿400
￿200
0
200
400
West East￿m￿
South North￿m￿
Antennapositions
vertical shower, 10
17
eV,
145 antennas
Ground core position in (0,0)
EW electric field absolute
value on the ground
x
east-west asymmetry of
the radio signal :
consequence of the
charge excess
contribution

Why?
east-west asymmetry

Vertical event at CODALEMA
6
12
18
24
31
37
4349
55
6268
74
80
86
93
99
￿400 ￿200 0 200 400
￿400
￿200
0
200
400
West East￿m￿
South North￿m￿
East￿westpolarization
Θ￿0°
Φ￿0°
￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
￿400 ￿200 0 200 400
￿400
￿200
0
200
400
West East￿m￿
South North￿m￿
Antennapositions
vertical shower, 10
17
eV,
145 antennas
Ground core position in (0,0)
EW electric field absolute
value on the ground
x
east-west asymmetry of
the radio signal :
consequence of the
charge excess
contribution

Why?
east-west asymmetry
charge
excess
nXB
total
Destructive
Constructive

Consequence of the
charge excess contribution
East-west asymmetry of
the radio signal :
Dependence on arrival direction
West￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
Zenith
North
East
South
B
!B=-27°
!=40°
"=0°
Air Shower
￿200 ￿100 0 100 200
￿200
￿100
0
100
200
West East￿m￿
South North￿m￿
East￿westpolarization

Consequence of the
charge excess contribution
East-west asymmetry of
the radio signal :
Effect on event for different arrival direction
B
West￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
Zenith
North
East
South
!B=-27°
!=0°
"=0°
Air Shower
￿200 ￿100 0 100 200
￿200
￿100
0
100
200
West East￿m￿
South North￿m￿
East￿westpolarization

Consequence of the
charge excess contribution
East-west asymmetry of
the radio signal :
Effect on event for different arrival direction
West￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
Zenith
North
East
South
B
!B=-27°
!=15°
"=180°
Air Shower
￿200 ￿100 0 100 200
￿200
￿100
0
100
200
West East￿m￿
South North￿m￿
East￿westpolarization

Consequence of the
charge excess contribution
East-west asymmetry of
the radio signal :
Effect on event for different arrival direction
West￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
Zenith
North
East
South
B
!B=-27°
!=25°
"=180°
Air Shower
￿200 ￿100 0 100 200
￿200
￿100
0
100
200
West East￿m￿
South North￿m￿
East￿westpolarization

Consequence of the
charge excess contribution
East-west asymmetry of
the radio signal :
Effect on event for different arrival direction
West￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
Zenith
North
East
South
B
!B=-27°
!=30°
"=180°
Air Shower
￿200 ￿100 0 100 200
￿200
￿100
0
100
200
West East￿m￿
South North￿m￿
East￿westpolarization

Consequence of the
charge excess contribution
East-west asymmetry of
the radio signal :
Effect on event for different arrival direction
West￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
Zenith
North
East
South
B
θB=-27°
!=40°
"=180°
Air Shower
￿200 ￿100 0 100 200
￿200
￿100
0
100
200
West East￿m￿
South North￿m￿
East￿westpolarization

Consequence of the
charge excess contribution
East-west asymmetry of
the radio signal :
Effect on event for different arrival direction
West￿￿￿￿￿￿￿￿ ￿￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿￿￿￿￿￿￿￿ ￿￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿￿
￿
￿
￿
￿
￿
Zenith
North
East
South
B
θB=-27°
!=40°
"=180°
Air Shower
￿200 ￿100 0 100 200
￿200
￿100
0
100
200
West East￿m￿
South North￿m￿
East￿westpolarization
Simulation suggests that
the east-west shift of
the apparent radio core
depends on the
arrival direction
of the shower

Prediction for the CODALEMA statistics
Simulation with SELFAS2 of
10
17
eV proton air showers
following the CODALEMA stat:
We need:
•arrival directions
•ground core positions

Prediction for the CODALEMA statistics
Simulation with SELFAS2 of
10
17
eV proton air showers
following the CODALEMA stat:
We need:
•arrival directions
•ground core positions
CODALEMA
Obtained with
particle detectors data
Density map
Sky maps of observed
radio events.
Monte Carlo sim. : (!,") and (Xcore,Ycore)

Prediction for the CODALEMA statistics
Simulation with SELFAS2 of
10
17
eV proton air showers
following the CODALEMA stat:
CODALEMA array
Simulation
with
SELFAS2.2
using
￿
￿￿￿
￿
￿
￿
￿￿￿￿￿￿￿ ￿￿￿
￿
￿
￿
￿
￿
￿
￿￿
￿
￿
￿
￿
￿
￿
￿
￿300￿200￿1000100200300
￿200
￿100
0
100
200
300
West East￿m￿
South North￿m￿
We need:
•arrival directions
•ground core positions
CODALEMA
Obtained with
particle detectors data
Density map
Sky maps of observed
radio events.
Monte Carlo sim. : (!,") and (Xcore,Ycore)

Prediction for the CODALEMA statistics
Simulation with SELFAS2 of
10
17
eV proton air showers
following the CODALEMA stat:
Event reconstruction
with the CODALEMA
analysis software
Lateral profile E0.exp(-d/d0)
4 free parameters:
E0, d0, XRcore, YRcore
CODALEMA array
Simulation
with
SELFAS2.2
using
￿
￿￿￿
￿
￿
￿
￿￿￿￿￿￿￿ ￿￿￿
￿
￿
￿
￿
￿
￿
￿￿
￿
￿
￿
￿
￿
￿
￿
￿300￿200￿1000100200300
￿200
￿100
0
100
200
300
West East￿m￿
South North￿m￿
We need:
•arrival directions
•ground core positions
CODALEMA
Obtained with
particle detectors data
Density map
Sky maps of observed
radio events.
Monte Carlo sim. : (!,") and (Xcore,Ycore)

For each simulated event, the reference frame is
centered on the ground particles shower core
Reconstructed radio cores from simulation

For each simulated event, the reference frame is
centered on the ground particles shower core
Reconstructed radio cores from simulation
#20 m
Global shift
of radio cores
toward the east

For each simulated event, the reference frame is
centered on the ground particles shower core
Reconstructed radio cores from simulation
#20 m
Global shift
of radio cores
toward the east

For each simulated event, the reference frame is
centered on the ground particles shower core
Reconstructed radio cores from simulation
#20 m
Global shift
of radio cores
toward the east
Without charge
excess in SELFAS2
No radio cores shift

Particle
shower cores
Particle detector
scintillators
EW polarized
antenna arrays
Radio
shower core
= Scintillator
T
= Antenna EW
T
TT TTT T T
T
T
T
T
T T
T
T
T
T
T
T
T
For each event, the reference frame is centered on the
ground particles shower core
What about the CODALEMA data...
315 reconstructed radio
cores with respect to the
particle shower core

Particle
shower cores
Particle detector
scintillators
EW polarized
antenna arrays
Radio
shower core
= Scintillator
T
= Antenna EW
T
TT TTT T T
T
T
T
T
T T
T
T
T
T
T
T
T
For each event, the reference frame is centered on the
ground particles shower core
What about the CODALEMA data...
315 reconstructed radio
cores with respect to the
particle shower core
CODALEMA
data
CODALEMA

Particle
shower cores
Particle detector
scintillators
EW polarized
antenna arrays
Radio
shower core
= Scintillator
T
= Antenna EW
T
TT TTT T T
T
T
T
T
T T
T
T
T
T
T
T
T
For each event, the reference frame is centered on the
ground particles shower core
What about the CODALEMA data...
315 reconstructed radio
cores with respect to the
particle shower core
CODALEMA
data
CODALEMA
good agreement!!!

Particle
shower cores
Particle detector
scintillators
EW polarized
antenna arrays
Radio
shower core
= Scintillator
T
= Antenna EW
T
TT TTT T T
T
T
T
T
T T
T
T
T
T
T
T
T
For each event, the reference frame is centered on the
ground particles shower core
What about the CODALEMA data...
315 reconstructed radio
cores with respect to the
particle shower core
CODALEMA
data
CODALEMA
good agreement!!!
What about arrival direction
dependence???

￿0.5 0.0 0.5 1.0
￿200
￿100
0
100
200
￿v￿B￿East￿West
￿
c
West￿east
￿m￿
—SELFAS2
￿￿SELFAS2￿Σ
Simulation SELFAS2
Dependence on
arrival direction
!
core
West-east
v x B

￿0.5 0.0 0.5 1.0
￿200
￿100
0
100
200
￿v￿B￿East￿West
￿
c
West￿east
￿m￿
—SELFAS2
￿￿SELFAS2￿Σ
Simulation SELFAS2
Dependence on
arrival direction
￿
￿
￿
￿
￿
￿
￿
￿￿￿
￿0.5 0.0 0.5 1.0
￿200
￿100
0
100
200
￿v￿B￿East￿West
￿
c
West￿east
￿m￿
￿Internalevents
—SELFAS2
￿￿SELFAS2￿Σ
!
core
West-east
v x B
•Passing usual quality cuts
•Internal to radio and particles array
Internal events
vs CODALEMA data

￿0.5 0.0 0.5 1.0
￿200
￿100
0
100
200
￿v￿B￿East￿West
￿
c
West￿east
￿m￿
—SELFAS2
￿￿SELFAS2￿Σ
Simulation SELFAS2
Dependence on
arrival direction
￿
￿
￿
￿
￿
￿
￿
￿￿￿
￿0.5 0.0 0.5 1.0
￿200
￿100
0
100
200
￿v￿B￿East￿West
￿
c
West￿east
￿m￿
￿Internalevents
—SELFAS2
￿￿SELFAS2￿Σ
￿
￿
￿
￿
￿￿
￿
￿￿
￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿
￿0.5 0.0 0.5 1.0
￿200
￿100
0
100
200
￿v￿B￿East￿West
￿
c
West￿east
￿m￿
￿￿Externalevents
￿Internalradiocore,
statisticx2￿
￿Internalevents
—SELFAS2
￿￿SELFAS2￿Σ
!
core
West-east
v x B
•Passing usual quality cuts
•Internal to radio and particles array
Internal events
vs CODALEMA data
External events

Passing usual quality cuts

Internal to radio array

￿0.5 0.0 0.5 1.0
￿200
￿100
0
100
200
￿v￿B￿East￿West
￿
c
West￿east
￿m￿
—SELFAS2
￿￿SELFAS2￿Σ
Simulation SELFAS2
Dependence on
arrival direction
￿
￿
￿
￿
￿
￿
￿
￿￿￿
￿0.5 0.0 0.5 1.0
￿200
￿100
0
100
200
￿v￿B￿East￿West
￿
c
West￿east
￿m￿
￿Internalevents
—SELFAS2
￿￿SELFAS2￿Σ
￿
￿
￿
￿
￿￿
￿
￿￿
￿￿￿
￿
￿
￿
￿
￿
￿
￿
￿
￿
￿￿￿
￿0.5 0.0 0.5 1.0
￿200
￿100
0
100
200
￿v￿B￿East￿West
￿
c
West￿east
￿m￿
￿￿Externalevents
￿Internalradiocore,
statisticx2￿
￿Internalevents
—SELFAS2
￿￿SELFAS2￿Σ
!
core
West-east
v x B
•Passing usual quality cuts
•Internal to radio and particles array
Internal events
vs CODALEMA data
External events

Passing usual quality cuts

Internal to radio array
close to GeoMag.
Field (<15°)
>80%
of the statistics

Conclusion
CODALEMA
•a new observable has been identified as being an evidence of the charge
excess mechanism in the air showers electric field in the MHz frequency
domain
•two different mechanims ! two different polarization patterns !
interferences ! displacement $c at the ground level of the maximum electric
field location with respect to the maximum particle density location
•$c depends on the shower arrival direction (checked for the EW polarization):
good agreement between simulations with SELFAS2 and the CODALEMA
data
•this new observable should be measurable in AERA at the Pierre Auger
observatory.
•the charge excess fraction depends on the arrival direction and on the antenna
location; for instance, for a vertical shower, the charge excess signal represents
20% of the total electric field
Tags