Y2 Neutrino Physics - University of...
Transcript of Y2 Neutrino Physics - University of...
Y2 Neutrino Physics (spring term 2017)
Dr E Goudzovski [email protected]
http://epweb2.ph.bham.ac.uk/user/goudzovski/Y2neutrino
Lecture 7
Atmospheric neutrino experiments
Previous lecture
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The most precise neutrino “absolute” mass measurements
come from studies of the 3H beta-decay spectrum near the endpoint.
The absolute neutrino mass scale: unknown but below 2 eV/c2.
Neutrino mixing leads to the flavour oscillations phenomenon.
Oscillations have been observed. Therefore the neutrinos are
massive, and lepton flavour is not conserved at large distances.
Two-flavour oscillations are described by two fundamental
parameters: the mass splitting m2 and the mixing angle .
Principal concepts: oscillation length, oscillation maxima,
appearance and survival probabilities.
Three-flavour oscillations are described by the
neutrino mixing matrix.
This lecture
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Atmospheric neutrinos and their flavour composition.
The Cherenkov effect.
Water Cherenkov neutrino detectors; Super-Kamiokande.
Observables sensitive to atmospheric neutrino oscillations.
Evidence of atmospheric neutrino oscillations.
Cherenkov neutrino telescopes.
Reading list:
K. Kleinknecht. Detectors for particle radiation. Chapter 5.3.
D. Perkins. Introduction to high energy physics. Chapter 9.7.2.
“Atmospheric neutrinos” in Soler et al.
Journal articles: see course webpage.
Cosmic rays
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Primary cosmic rays:
mainly high energy protons and 4He
from astrophysical sources
(including supernovae).
Secondary cosmic rays (air showers):
light particles produced in
inelastic interactions with air
(N, O nuclei).
Main source of atmospheric neutrinos:
decays of secondary pions and kaons
p
Atmospheric neutrinos
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Main source of atmospheric neutrinos:
At energies E<1 GeV, most and decay:
Highly energetic muons reach the ground
(and even penetrate deep underground):
(relativistic time dilation) Mean free path:
E=1 GeV muons:
E=1 GeV pions: (atmosphere thickness: ~10 km)
Atmospheric neutrino properties
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Computed muon (anti)neutrino flux
1 10 102 103
E, GeV
0.1
Flavour composition
Neutrino flux: ~10 cm2 s1.
Directionality: roughly isotropic, up-down symmetric.
Typical energy: ~1 GeV, wide energy range.
Typical uncertainty on the calculated atmospheric neutrino flux: ±20%.
Uncertainty of the /e ratio: ±3%.
E, GeV
Insufficient time
for muon decay
Atmospheric neutrino detection
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Charged current reactions (inverse beta decays)
Thresholds are not crucial for atmospheric neutrinos:
E(e)=1.8 MeV, E()=110 MeV, E()=3.5 GeV.
A possibility: multi-kilotonne water Cherenkov detectors
Comparison with reactor experiments (see lecture 4)
Larger cross-section than for reactor neutrinos:
(E=1GeV)~1038 cm2 vs (E=1MeV)~1043 cm2.
Lower neutrino flux than in reactor experiments:
ATM~10 cm2 s1 vs REACTOR~1013 cm2 s1.
Therefore neutrino interaction rates per nucleon (~) are ~107 lower:
FATM~0.1/year/tonne vs FREACTOR~100/hour/tonne.
W
Requirement to oscillation experiments:
flavour identification of the charged leptons produced.
Cherenkov effect
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Cherenkov radiation is emitted when a charged particle
passes through a dielectric medium at a speed greater than
the speed of light in that medium (>1/n).
Emission angle wrt particle direction
is fixed (the “Cherenkov angle”):
Threshold velocity:
Example: water (n=1.33).
Threshold velocity: min = 1/n = 0.75; maximum angle: max = 41o.
Measurement of velocity . If momentum known, compute mass:
Cherenkov particle identification. Not sensitive to particle charge (+/–).
For highly relativistic particles (1),
C
C
(n: refractive index)
Cherenkov photon spectrum
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Wavelength, nm
Typical Cherenkov photon spectrum
FrankTamm spectrum
with chromatic dispersion
Dispersion
neglected
“red” “violet”
(a gas Cherenkov detector co-developed by the Birmingham group
for the NA62 experiment at CERN)
FrankTamm formula:
(Dispersion: the refractive index n depends on wavelength)
Cherenkov light emission
near a nuclear reactor:
(www.spectrum.ieee.org/image/37182)
dx: path; d: wavelength interval; Dominated by low wavelength; Integrated intensity is determined by the Cherenkov angle C.
Arb
itra
ry s
cale
Water Cherenkov detectors
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41°
Neutrino detection in WCD
Highly relativistic charged leptons (max)
produce ~40 photons/cm.
Ionization energy loss by a muon: ~2 MeV/cm.
Dimension of the largest detector: 40 m.
Charged lepton traverses it in ~100 ns,
emitting ~105 Cherenkov photons.
Photons detected by PMTs along the walls (time resolution ~1 ns). a series of “Cherenkov rings”
Measurement of speed & direction
of the charged lepton. e,
Neutrino and charged lepton directions
are correlated. Typical angular resolution:
25° at E = 1 GeV; 0 for higher E.
e,
(application for atmospheric neutrinos)
(GeV energy range)
Inverse beta decays:
Light sensitive detectors (PMTs)
Lig
ht
sensi
tive d
ete
cto
rs (
PM
Ts)
Lig
ht
sensi
tive d
ete
cto
rs (
PM
Ts)
Super-Kamiokande
10 Photos: © Kamioka Observatory, ICRR (Institute for Cosmic Ray Research), The University of Tokyo
The largest water Cherenkov detector built so far
Cosmic ray shield (Mt. Ikeno,
Japanese Alps): 1000 m below surface.
50k tonnes of pure H2O.
In operation since 1996.
inner detector,
“fiducial volume”
outer detector to
veto external activity
Super-K (1)
11 World’s largest 20’’ diameter PMTs
Super-K (2)
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© Kamioka Observatory,
ICRR (Institute for Cosmic Ray Research),
The University of Tokyo
Super-K Cherenkov images
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603 MeV muon:
sharply defined
ring edge
Super-K Cherenkov images
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492 MeV electron:
diffused ring edge
due to multiple
scattering
NB: leptons
are not observable
due to the short lifetime
Lepton flavour
identification
(e vs )
Atmospheric : observables
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(1) Oscillation is the change of neutrino flavour.
The /e flux ratio in the absence of oscillations is known.
Therefore, the simplest observable is the measured /e flux ratio.
(2) Oscillations depend on the travelled path L.
Downward-going : ~10 km path.
Upward-going : ~ 2REarth ~ 13000 km path.
Observables: up-down asymmetries of and e fluxes.
Generalization: zenith angle (z) distribution of and e.
(3) Oscillations depend on the path-to-energy ratio.
Observable: path-to-energy ratio (L/E) distribution of and e.
Appearance probability
(two-favour case):
The goal: search for neutrino oscillations
(1) Muon/electron flux ratio
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Measured/expected ratio
Muon/electron neutrino flux ratio
Experi
ment
The “atmospheric neutrino anomaly”: deficit of atmospheric
muon neutrinos (), an early hint for oscillations (1980s).
Inconclusive: could be e.g. proton decays in the detector ( )
(lepton number violation; emission of a ~300 MeV positron)
(2a) Up-down asymmetry
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Oscillation length for a 1 GeV atmospheric neutrino:
L0 ≫ atmosphere thickness (~10 km).
L0 ≪ Earth diameter (~13000 km).
Therefore the Earth is an ideally sized lab!
Downward-going neutrinos do not oscillate: survival prob.
Upward-going neutrinos undergo many oscillation cycles.
(except for the minority at extremely high energies above ~100 GeV)
Survival probability for the upward-going neutrinos:
Averaged over L/E
(the effect of “solar” oscillations, L0~104 km, cancels accidentally)
(m2 known from
experiment)
Upward-going neutrinos
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(Half of the original flavour neutrinos survive even at maximal mixing)
Indefinite integral of f(x) = sin2x:
Mean value of a function:
Mean value of f(x) = sin2x over a period (0<x<):
Survival probability for upward-going neutrinos:
(2b) Zenith angle z
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Distance between neutrino
production point and detector L
depends on zenith angle z
Uncertainty on the production point
(~atmosphere thickness): L=5km.
A non-assessed problem: obtain the L = f(cosz) dependence
Earth
Detector
Atmosphere
local vertical axis
Downward-going :
z = 0
Upward-going:
z = 180°
Horizontal :
z = 90°
Generalization of the “up/down” approach
–1 –0.5 0 0.5 1
104
103
102
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Distance vs zenith angle
cosz
L ,k
m
L = f(cosz)
downward-
going
upward-
going
0º z 180º
+1 ≥ cos z ≥ 1
~10 km L 13000 km
The expected oscillation pattern
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Horizontal neutrinos Upward-going neutrinos
z measurements at Super-K
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Data and best fit
to oscillations
Prediction:
no oscillations
Up-down flux asymmetry.
Deficit of upward-going .
No excess or deficit of e.
The data are compatible
to oscillations
“Sub-GeV” = low energy and worse directional correlation
downward-
going upward-
going
downward-
going upward-
going
(3) L/E analysis at Super-K
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L/E (km/GeV)
Muon (anti)neutrino counts:
data/(expectation for no oscillations)
The dip = first oscillation maximum.
Higher maxima not visible due to insufficient resolution.
Fits to decay and decoherence
models fail to explain the data
Fit to oscillations
No oscillations 400 km/GeV
Oscillation parameters
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Atmospheric neutrinos: disappearance experiments
(MINOS and T2K accelerator experiments will be discussed later)
Maximum mixing:
sin2(223) 1
(almost complete
disappearance
at oscillation maxima)
Experimentally, m2atm = (2.40.1)×103 eV2 and atm = (457)°
R. Nichol @ Neutrino 2012, Kyoto, Japan
Megatonne & gigatonne detectors
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Megatonne water Cherenkov experiments:
Hyper-Kamiokande in Japan might be operational by 2023
(~25 times Super-Kamiokande mass; several identical water tanks).
Gigatonne neutrino telescopes using natural Cherenkov radiators:
WATER ICE
Large PMT arrays operate in the
Mediterranean Sea and at Lake Baikal
IceCube neutrino telescope
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World’s largest neutrino detector:
1 km3 (0.9 Gigatonne) of
Antarctic ice instrumented with PMTs.
IceCube location at the South Pole
Photodetector module
~100 m spacing between PMTs: sensitive mainly to
high-energy astrophysical neutrinos (100 GeV<E<1 PeV).
DeepCore: atmospheric neutrinos (1 GeV<E<100 GeV).
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Neutrino detection via
Cherenkov light emitted by a muon
A PeV (1015 eV) energy neutrino event
Excellent angular resolution:
moon shadow in the cosmic rays
seen with TeV (=1012 eV) muons
IceCube neutrino telescope
Summary
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Atmospheric energy spectrum: wide, GeV range; flavour
composition: /e2 at GeV energy, /e>2 at higher energy.
The leading atmospheric (and astrophysical) neutrino detection
technology: water and ice Cherenkov detectors.
Observables sensitive to oscillations: muon/electron ratio,
up-down asymmetries, zenith angle (z) and L/E distributions.
Atmospheric neutrino observations are consistent with
oscillations with m2=2.4×103 eV2 and
near-maximal mixing (atm 45o). [Oscillations established in 1998]