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Page 1: Atmospheric Neutrinos

Atmospheric Neutrinos

Barry Barish

Bari, Bologna, Boston, Caltech, Drexel, Indiana, Frascati, Gran Sasso,L’Aquila, Lecce, Michigan, Napoli, Pisa, Roma I, Texas, Torino

MACRO

Page 2: Atmospheric Neutrinos

Main features of Macro as detector

• Large acceptance (~10000 m2sr for an isotropic flux)

• Low downgoing rate (~10-6 of the surface rate )

• ~600 tons of liquid scintillator to measure T.O.F. (time resolution ~500psec)

• ~20000 m2 of streamer tubes (3cm cells) for tracking (angular resolution < 1° )

More details in Nucl. Inst. and Meth. A324 (1993) 337.

Page 3: Atmospheric Neutrinos

Neutrino event topologies in MACRO

Detector mass ~ 5.3 kton

Event Rate:(1) up throughgoing (ToF) ~160 /y(2) internal upgoing (ToF) ~ 50/y(3) internal downgoing (no ToF) ~ 35/y(4) upgoing stopping (no ToF) ~ 35/y

Absorber

Streamer

Scintillator

(1) (2)(3)(4)

Page 4: Atmospheric Neutrinos

Energy spectra of events detected in MACRO

<E> ~ 100 GeV for throughgoing <E> ~ 5 GeV for internal upgoing <E> ~ 4 GeV for internal downgoing

and for upgoing stopping

Low energy events allow us to investigate the oscillation parameter space independently of the throughgoing muon data

Page 5: Atmospheric Neutrinos

Neutrino inducedupward-going muons

identified by thetime-of-flight method

scintillator

scintillator

streamertrack

T2-T1) * c / l

Page 6: Atmospheric Neutrinos

Upward throughgoing muons

External -interactions 768 events

upward vs downward muons

Page 7: Atmospheric Neutrinos

Background source for events: pion production by downward ’s (MACRO Collab., Astroparticle Phys. 9(‘98)105)

• rate of downgoing ’s ~105x rate of upgoing ’s

• background mainly pions produced at large angles by interactions in the rock around the detector ( + N + ± + X)

•Estimated background in MACRO: ~ 5% for the stopping muon sample (MACRO Coll., PL B478 (‘00) 5) ~ 1% for the up-throughgoing m (>200 g/cm2 cut) MACRO Coll., PL B434 (‘98) 451)

Page 8: Atmospheric Neutrinos

Pion production at large angle• upgoing charged produced by interactions in the rock under the detector• a background source for upward stopping and throughgoing muons• studied 243 events with downgoing plus upgoing particles

Estimated background - upward throughgoing ’s: ~1%- low energy events: ~5%

Page 9: Atmospheric Neutrinos

Total observed flux and comparison with Monte Carlo

Data number of events: 768 eventsbackground (wrong ) 18 background (’s from muons) 12.5Internal neutrino interactions 14.6

Total 723 events

Prediction (Monte Carlo) 989 ± 17% Bartol neutrino Flux (±14%) GRV-LO-94 cross section (± 9%) Lohmann muon energy loss (± 5%)

data/prediction R = 0.731 ± 0.028stat ± 0.044syst ± 0.124theor

Page 10: Atmospheric Neutrinos

Effects of oscillations on MACRO events

Flux reduction depending on zenith anglefor the upward throughgoing events

0.4

0.5

0.6

0.7

0.8

0.9

1

-1 -0.8 -0.6 -0.4 -0.2 0

Redu

ctio

n fa

ctor

Cos(zenith)

dm2=0.01 eV2

dm2=0.001 eV2

dm2=0.0001 eV2

dm2=0.1 eV2

Upgoing Muons E>1 GeV

Earth

underground detectorL ~ 10 - 104 km

distortion ofthe angulardistribution

Page 11: Atmospheric Neutrinos

Zenith angle distribution

E > 1 GeV

Page 12: Atmospheric Neutrinos

0.001

0.01

0.1

1

10 -5 0.0001 0.001 0.01 0.1 1 m2

Number of events

Angular distribution

Tau Neutrino

Combination

Peak probability from the angular distribution: 26% from the combination: 57%

angular distribution in 10 bins

Probabilities of oscillations (for maximal mixing)

Pro

b ab

il ity

• The peak probability from the angular distribution agrees with the peak probability from the total number of events

• Probability for no-oscillation: ~ 0.4 %

Page 13: Atmospheric Neutrinos

0.001

0.01

0.1

1

10-5 0.0001 0.001 0.01 0.1 1 m2

Number of events

Angular distribution

Sterile Neutrino +

Combination

Peak probability from the angular distribution: 4.1% from the combination: 14.5%

angular distribution in 10 bins

Probabilities for sterile neutrinooscillations with maximum mixing

Peak probabilities lower than that for tau neutrinos:• from the angular distribution: 4.1 %• from combination: 14.5 %

Pro

bab

ility

Page 14: Atmospheric Neutrinos

Probabilities for sterile neutrinooscillations

10-5

10-4

10-3

10-2

10-1

100

0 0.2 0.4 0.6 0.8 1

m2 (

eV2 )

Psterile >=0.1 Pmax tau

sin2(2 )

m > m s

m < m

s

ANGULAR DISTRIBUTION + Normalization

Page 15: Atmospheric Neutrinos

Test of oscillations with the ratiovertical / horizontal

• Ratio (Lipari- Lusignoli, Phys Rev D57 1998) can be statistically more powerful than a 2 test: 1) the ratio is sensitive to the sign of the deviation 2) there is gain in statistical significance

• Disadvantage: the structure in the angular distribution of data can be lost.

Measured value ~ 2 (and one sided) from the expectedvalue for sterile neutrino

0.9

1

1.1

1.2

1.3

1.4

1.5

10-5 0.0001 0.001 0.01 0.1

Ratio nsterile max mixingRatio ntau max mixingDATA MAR 2000

-

1 <

co

s (

)

<-0

.6

-0.6

< c

os

(

) <

0

P best Tau/ P best Sterile = 15 (5% systematic in each bin )

m2 (eV2)

MACRO UPMU

Page 16: Atmospheric Neutrinos

Internal Downgoing ’s and

Upward Going Stopping ’s

from MC simulation:• E ~ 4 GeV• mixture

upward going stopping ~ 50% internal downgoing

• ~ 87% from –charged current events

DATA - Background = 229 events

Upward going stopping

Internal downgoing

Page 17: Atmospheric Neutrinos

Data vs Monte Carlo Predictions

• : Bartol flux with geomagnetic cutoffs (error ~ 20%)

• = Q.E. + 1 (Lipari et al., PRL74 (1995) 4384)+ DIS (GRV-LO-94 PDF) (error ~ 15%)

• (E,zenith): detector response and acceptance (systematic error ~ 10 %)

MC: 247 25sys 62theo

DATA: 135 12stat

MC: 329 33sys 82theo

DATA: 229 15stat

Internal down + Upgoing stop

Internal upward going ’s

Low Energy Neutrino Events

Page 18: Atmospheric Neutrinos

Internal upward events

maximum mixingm2= 2.5 x 10-3 eV 2

thsysstatIUMC

Data14.006.004.055.0

)(

expected 247 ± 62thor

real data 135 ± 12stat

- - - 146 events

• Data consistent with a constant deficit in all zenith angle bins ( 2 /d.o.f. = 3.1/4 on shape)• Probability for NO oscillations: ~ 4.3% (one side)

Page 19: Atmospheric Neutrinos

Internal downward + Upward stopping events

thsysstatUGSIDMC

Data18.007.004.070.0

)(

expected 329 ± 82th

real data 229 ± 15stat

- - - 252 events

maximum mixingm2= 2.5 x 10-3 eV 2

• Data consistent with a constant deficit in all zenith angle bins• Probability for NO oscillations: ~ 12% (one side)

Page 20: Atmospheric Neutrinos

(Internal upward) / (Internal downward + Upward stopping)

• Most of the theor. uncertainties canceled (<5%)• Systematic errors reduced (~6%)

Data: R = 0.59 ± 0.07stat

Expected (No oscillations): R = 0.75 ± 0.04sys ± 0.04th

compatibility ~ 2.7%

Expected oscillations R = 0.58 ± 0.03sys ± 0.03th

(maximal mixing and m2 = 2.5 x 10-3 eV2 )

Ratio of event types at low energy

Page 21: Atmospheric Neutrinos

Ratio of event types at low energy

+

upgoing internal

upgoing stopinternal downgoing

• Most of the theor. uncertainties canceled < 5%

• Systematic errors reduced ~ 6%

Data: R = 0.59 ± 0.07stat

Expected (No oscillations): R = 0.75 ± 0.04sys ± 0.04th

Expected oscillations R = 0.58 ± 0.03sys ± 0.03th

maximal mixing

m2 = 2.5 x 10-3 eV2

Page 22: Atmospheric Neutrinos

10-5

10-4

10-3

10-2

10-1

0 0.2 0.4 0.6 0.8 1

m2 (

eV2 )

sin2(2 )

Low Energies

UPMU

MACRO March 2000 Data90% Confidence Level

MACRO events:confidence level regions for

oscillation

Page 23: Atmospheric Neutrinos

Summary and Conclusions

High energy events:

oscillation favoured with large mixing angle and m2 ~ 2.5x10-3 eV2

sterile disfavoured at ~ 2 level

Low energy events:

event deficit with respect to expectation different for Internal upward, and internal downward + Uuward going stopping

no zenith angle distortion

compatibility between result and expectation (no oscillations) with a probability < 3 %

agreement with hypothesis of oscillation with large mixing angle and 10-3 < m2 < 2x10-2 eV2

A consistent scenario arises from both high and low energy MACRO events


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