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Atmospheric Neutrinos Barry Barish ologna, Boston, Caltech, Drexel, Indiana, Frascati, Gran a, Lecce, Michigan, Napoli, Pisa, Roma I, Texas, Torino MACRO

Atmospheric Neutrinos

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Atmospheric Neutrinos. Barry Barish. MACRO. Bari, Bologna, Boston, Caltech, Drexel, Indiana, Frascati, Gran Sasso, L’Aquila, Lecce, Michigan, Napoli, Pisa, Roma I, Texas, Torino. Neutrino event topologies in MACRO. Absorber. Streamer. Scintillator. (4). (1). (3). (2). - PowerPoint PPT Presentation

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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