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Neutrino Physics - Double-Beta Decay
Steve ElliottLos Alamos National
Laboratory
June 2007 Steve Elliott, FNAL Neutrino Summer School 2
Lecture Outline
• Double Beta Decay– Basic physics– General experimental techniques– The various experiments
June 2007 Steve Elliott, FNAL Neutrino Summer School 3
Example Decay Scheme
2+
0+
0+
0+
2-
Ge76
As76
Se76
!!
In many even-even nuclei, β decay is energetically forbidden. This leaves ββ
as the allowed decay mode.
EndpointEnergy
June 2007 Steve Elliott, FNAL Neutrino Summer School 4
ββ(2ν): Allowed weak decay
!
2n" 2p+ 2e#
+ 2$ e
e-
e-
Z+2Z+1
Zνe
νe
June 2007 Steve Elliott, FNAL Neutrino Summer School 5
ββ(0ν): requires massive Majorana νOnly practical way to address the particle-antiparticle question
e-
e-
Z+2
Z+1
Z νe
n! p + e"+ #e
!e + n" p + e#
!
(RH "e )
!
(LH "e)
June 2007 Steve Elliott, FNAL Neutrino Summer School 6
Energy Spectrum for the 2 e-
2.01.51.00.50.0
Sum Energy for the Two Electrons (MeV)
Two Neutrino Spectrum Zero Neutrino Spectrum
1% resolution!(2") = 100 * !(0")
EndpointEnergy
June 2007 Steve Elliott, FNAL Neutrino Summer School 7
ββ History
• ββ(2ν) rate first calculated by Maria Goeppert-Mayer in 1935.
• First observed directly in 1987.• Why so long? Background
τ1/2(U, Th) ~ Tuniverse
τ1/2(ββ(2ν)) ~ 1010 Tuniverse
• But next we want to look for a process with:
τ1/2(ββ(0ν)) ~ 1017 Tuniverse
June 2007 Steve Elliott, FNAL Neutrino Summer School 8
ββ Candidates
There are a lot of them!
June 2007 Steve Elliott, FNAL Neutrino Summer School 9
How to choose a ββ isotope?
• Detector technology exists
• High isotopic abundance or an enrichedsource exists.
• High energy = fast rate
• High energy = above background
June 2007 Steve Elliott, FNAL Neutrino Summer School 10
ββ CandidatesAbundance > 5%,Trans. Energy > 2 MeV
Frequently studied isotope.
June 2007 Steve Elliott, FNAL Neutrino Summer School 11
ββ Decay Rates
!2" = G2" M2"
2
!0" = G0"M0"
2
m"2
G are calculable phase space factors.G0ν ~ Q5
|M| are nuclear physics matrix elements.Hard to calculate.
mν is where the interesting physics lies.
June 2007 Steve Elliott, FNAL Neutrino Summer School 12
“Because Its Not There”
Larson
June 2007 Steve Elliott, FNAL Neutrino Summer School 13
Neutrino Mass: What do we want to know?
Mas
sAbsolute
MassScale
RelativeMassScale
!"
!#
!#
!"
$
%
& & & & &
'
(
) ) ) ) )
or
!"
!#
$
% & &
'
( ) )
Dirac or Majoranaνe ν1 ν2 ν3
Ue1
2Ue2
2Ue3
2
Mixing
June 2007 Steve Elliott, FNAL Neutrino Summer School 14
Neutrino Mass: How do we learn what we want toknow?
Absolute Mass Scale
Relative Mass Scale
Mixing Matrix
Elements
CP nature
of
, cosm. Oscil.
Need all 3 types of experiments.
June 2007 Steve Elliott, FNAL Neutrino Summer School 15
Neutrino Masses: What do we know?
• The results of oscillation experiments indicate νdo have mass!, set the relative mass scale, and aminimum for the absolute scale.
• β decay experiments set a maximum for theabsolute mass scale.
50 meV < mν < 2200 meV
June 2007 Steve Elliott, FNAL Neutrino Summer School 16
We also know ν mix.
!e!µ
!"
#
$
% %
&
'
( ( =
Ue1 Ue2 Ue3
Uµ1 Uµ2 Uµ3
U"1 U"2 U"3
#
$
% %
&
'
( (
!1!2!3
#
$
% %
&
'
( (
The weak interaction produces νe, νµ, ντ.
These are not pure mass states but a linearcombination of mass states.
Oscillation experiments indicate that ν mix and constrain Uαi.
June 2007 Steve Elliott, FNAL Neutrino Summer School 17
Oscillations and HierarchyPossibilities
mass
Normal Invertedmsmallest1
2
312
3
49 meV
9 meV
νe is composed of a large fraction of ν1.
June 2007 Steve Elliott, FNAL Neutrino Summer School 18
What about mixing, mν & ββ(0ν)?
m!! = Uei
2
mi
i=1
3
" #i
ε = ±1, CP cons.
Compare to β decay result:
m! = Uei
2
mi
2
i=1
3
"
virtual νexchange
real νemission
No mixing: m!! = m"e= m
1
June 2007 Steve Elliott, FNAL Neutrino Summer School 19
Why does the CP parity appear in <mββ>?
Look at the critical part of this diagram.
A0ν ∼ Σin
n
p
p
W-
W-
νi
e-
Uei
Uei
e-
June 2007 Steve Elliott, FNAL Neutrino Summer School 20
The crossed channel.
e+ e-
W- W+
νi
A! Uei
2e+W
"HSM
#i
i
$ #iHSMe"W
+
The 1st vertex creates the CP partnerof the particle needed by the 2nd vertex.
But CP !i= "
i!i
Upon substitution, the factor εi appears.
Vertex 1
Vertex 2
June 2007 Steve Elliott, FNAL Neutrino Summer School 21
What can be learned from Oscillations & ββ?
• From oscillations, we have:Information on UeiInformation on δm2
• With <mββ> constraints, we can constrain m1:(2 flavor example)
!
m"" = Ue1
2m1+#
21Ue2
2m
1
2+$m
21
2
June 2007 Steve Elliott, FNAL Neutrino Summer School 22
Min. <mββ> as a vector sum.General Case
m!! = Ue1
2
m1+ e
i!Ue2
2
m2+ e
i"Ue3
2
m3
!
"
Ue3
2m3
Ue2
2m2
Ue1
2m1
<mββ>
<mββ> is the modulus of the resultant.In this example, <mββ> has a min. It cannot be 0.
min
June 2007 Steve Elliott, FNAL Neutrino Summer School 23
PlotThanks toPetr Vogel
More General: 3 ν
50 meV orfew x 1027 yr
msmallest
<mββ
>
June 2007 Steve Elliott, FNAL Neutrino Summer School 24
More General
PlotThanks toPetr Vogel
50 meV orfew x 1027 yr
June 2007 Steve Elliott, FNAL Neutrino Summer School 25
50 meVOr ~ 1027 yr
Normal
Inverted
0.1
1
10
100
1000Eff
ecti
ve !! M
ass
(m
eV
)
12 3 4 5 6 7
102 3 4 5 6 7
1002 3 4 5 6 7
1000
Minimum Neutrino Mass (meV)
Ue1
= 0.866 "m2
sol = 70 meV
2
Ue2
= 0.5 "m2
atm = 2000 meV
2
Ue3 = 0
Inverted
Normal
Degenerate
Solar Scale
Atmospheric Scale
KKDC Claim
An exciting time for ββ!
< mββ > in the range of10 - 50 meV is very interesting.
For the next experiments:
For at leastone
neutrino:
!
mi > "matmos2
# 50meV
!
m"" # 50meV
June 2007 Steve Elliott, FNAL Neutrino Summer School 27
The 1st Observation
June 2007 Steve Elliott, FNAL Neutrino Summer School 28
The Heidelberg-Moscow Experiment
Foun
datio
ns o
f Phy
sics
, 32,
(200
2)
8”
~10 kg of 76Ge13 years of data
June 2007 Steve Elliott, FNAL Neutrino Summer School 29
Elliott & VogelAnnu. Rev. Part. Sci. 2002 52:115
102
103
104
105
Mass L
imit
(m
eV
)
20202000198019601940
Year
Ge-76Ge-76
Te-128
Te-128
Se-82
Ge-76
Ge-76
Ca-48Nd-150
Nd-150
EXO-200
GERDA
MJ-120
CUORE
>3.6x1021 y150Nd
<(0.8-5.6) eV>4.5x1023 y136Xe
<(0.41-1.) eV>3.0x1024 y130Te
<(1.1-1.5) eV>7.7x1024 y128Te
<1.7 eV>1.7x1023 y116Cd
<(0.6-2.7) eV>5.8x1023 y100Mo
<(1.2-3.2) eV>2.1x1023 y82Se
=0.44 eV=1.2x1025 y76Ge
<(0.33-1.35) eV>1.6x1025 y76Ge
<0.35 eV>1.9x1025 y76Ge
<(7.2-44.7) eV>1.4x1022 y48Ca
m!! "1
M G0#$1 / 2
%
& ' '
(
) * *
June 2007 Steve Elliott, FNAL Neutrino Summer School 30
An Ideal ExperimentMaximize Rate/Minimize Background
• Large Mass (~ 1 ton)• Good source radiopurity
• Demonstrated technology• Natural isotope
• Small volume, source = detector• Good energy resolution
• Ease of operation• Large Q value, fast ββ(0ν)
• Slow ββ(2ν) rate• Identify daughter
• Event reconstruction• Nuclear theory
m!! "b#E
Mtlive
$
% & &
'
( ) )
1
4
June 2007 Steve Elliott, FNAL Neutrino Summer School 31
Great Number of Proposed Experiments
• Calorimeter– Semi-conductors– Bolometers– Crystals/nanoparticles immersed in scintillator
• Tracking– Liquid or gas TPCs– Thin source with wire chamber or scintillator
“Found” PeaksPR
D45
, 254
8 (1
992)
A 2527-keV Ge-det. peak that was an electronic artifact.
A ~2528-keV Te-det.peak that was a 2σStatistical flucuation. N
P B3
5 (P
roc.
Sup
p.),
366
(199
4).
Need more thanone experiment
June 2007 Steve Elliott, FNAL Neutrino Summer School 33
A Recent Claim for ββ(0ν)
Mod
. Phy
s. Le
tt. A
16, 2
409
(200
1)
20
15
10
5
0
Counts
20802060204020202000
Energy (keV)
June 2007 Steve Elliott, FNAL Neutrino Summer School 34
The ROI
The “feature” at 2038keV is arguablypresent. This willprobably requireexperimental testing.
Background leveldepends on intensity fitto other peaks.
June 2007 Steve Elliott, FNAL Neutrino Summer School 35
Future Data Requirements
Why wasn’t this claim sufficient to avoidcontroversy?
• Low statistics of claimed signal - hard torepeat measurement• Background model uncertainty• Unidentified lines• Insufficient auxiliary handles
Result needs confirmation or repudiation
June 2007 Steve Elliott, FNAL Neutrino Summer School 36
Various Levels of Confidence
• A preponderance of the evidence: a combination of– Correct peak energy– Single-site energy deposit– Proper detector distributions (spatial, temporal)– Rate scales with isotope fraction
• Beyond a reasonable doubt: include the following– Observe the two-electron nature of the event– Measure kinematic dist. (energy sharing, opening angle)– Observe the daughter– Observe the excited state decay
• Open and shut case: the smoking gun– See the process in several isotopes
June 2007 Steve Elliott, FNAL Neutrino Summer School 37
Classes of Background for ββ(0ν)
• ββ(2ν) tailNeed good energy resolution.
• Natural U, Th in source and shieldingPure materials, segmentation, pulse shape.
• Cosmic ray activationStore and prepare materials underground.
June 2007 Steve Elliott, FNAL Neutrino Summer School 38
ββ(2ν) as a Background.Sum Energy Cut Only
next generationexperimentalgoal
10-4
10-3
10-2
10-1
100
101
102
103
<m
!!>
Sen
siti
vity
(meV
)
54321Resolution (%)
100Mo
136Xe
76Ge
130Te
2.0
1.5
1.0
0.5
0.0
dN
/d(K
e/Q
)
1.00.80.60.40.20.0Ke/Q
30
20
10
0
x1
0-6
1.101.000.90
Ke/Q
!
S
B=me
7Q" 6T1/ 2
2#
T1/ 2
0#
June 2007 Steve Elliott, FNAL Neutrino Summer School 39
Natural Activity
• The Problem: τ(U, Th) ~ 1010 yearsGoal: τ(ββ(0ν)) ~ 1027 years
• Detector: Intrinsic Ge is very pure• Cryostat: Electro-formed Cu• Shielding: Roman Pb• Front End Electronics: behind shield
June 2007 Steve Elliott, FNAL Neutrino Summer School 40
Cosmic Ray Induced Activity
• Material dependent.Lots of experience with Ge.
• Need for depth to avoid activation.
• Need for storage to allow activationto decay.
June 2007 Steve Elliott, FNAL Neutrino Summer School 41
Pb(n,n’γ) and 76Ge: an example
206Pb 207Pb
3744 keV 3633 keV
1703 keV1467 keV1167 keV
803 keV
g.s.571 keV
g.s.
2041 keV
3062 keV
DEP of 3062line is at 2040
keV!!
Am
Be
stud
y at
LA
NL
n,n’
stu
dy a
t TU
NL