high mass indium detector for low energy solar neutrinos r. s. … · 2004. 2. 23. · eff% bs/in...
TRANSCRIPT
High Mass Indium Detector for Low Energy Solar Neutrinos
R. S. RaghavanBell Labs
NOON ’04, TokyoFeb 11, 2004
New U.S. Opportunities for Astroparticle Science & TechnologyAt Virginia Tech
Phase I: Virginia Tech Kimballton Lab for Underground Science & Engg
in the Kimballton Limestone Mine (1700 mwe)30 min from VT
Phase II: NUSEL @ Kimballton ?Engg. Studies initiated (VT Funded at $1.6 M )
Focus of Phase I
LENS (Low Energy Neutrino Science)Hi Mass Indium Detector of low energy νννν & νννν for Multidisciplinary Astroparticle Discovery
•Particle Physics, Astrophysics--Lo Energy Solar Nu
•High Red Shift Universe — Supernova Relic Nu
•Radiogenic Structure of the Earth — Geo-Nu
•White Paper: http://www.phys.vt.edu/~kimballton/
------MRI Proposal for LENS Supermodule Submitted to NSF
(BNL, INR Moscow, N. Carolina, Princeton, VT, other US…)
∆∆∆∆m2 = 7.1(0.4) eV2
tan2θθθθ12 12 12 12 =0.42(=0.42(=0.42(=0.42(5)Sin2θθθθ13 < 0.07 (3σσσσ)
•Solar Neutrinos Oscillate !
•Boron ????????????flux measured
•Neutrino parameters limited- LMA
Solar Neutrinos--What have we learnt so far?
•Solar Neutrinos Oscillate !
•Boron-8 solar νννν flux measured
•Neutrino parameters limited- LMABahcall & Penya-Garay ‘03
LMA basically from E( ν) ν) ν) ν) > 5 MeV---< 0.1% of total Flux
Parameter values from fit to
5 SN expts (νννν) + KamLand &
Chooz (νννν )
What Next ?•Low energy tests of high energy conclusions•Observe Main Energy Reaction of Sun--pp fusion
Need--Fully Resolved Lo Energy Solar ν ν ν ν spectrum
•Single Experiment•Single Solar Input—pp flux•Only NEUTRINO Data (No ν )ν )ν )ν )•PRECISION data--rates, Lo Nu fluxes•LoNu Discovery potential Goal Minimum loopholes, caveats
Definitive Neutrino, Sun
What‘s NewIn Exptlmethod ?
Bottom Line:
Finally : How does the Sun shine?–Direct Answer in School Books: Lo Nu Spectrum
LENS-Experimental Plan
LENS-SolLiquid scintillator basedCC Solar Nu Experiment at Kimballton (VA USA)(60ton In; 750 ton InLS; 3000 ton In-free LS)CC parameter Known only from (p,n) reactions.Direct measurement integral part of precision experiment.
LENS-Cal
Precision (<3%?) Calibration of In CC (GT) parameter
By MCi υ υ υ υ Source ( 37Ar ?) -- in BAKSAN, Russia
In metal foil/Plastic or LS Scint. Sandwich Detector
(5 ton In; 15 ton Scint)
Eve
nts
per
20
keV
E
ven
ts p
er 2
0 ke
V
Measured energy (MeV) Measured energyMeasured energy (MeV) Measured energy
pp Be
CNO pep
Nov 2003Nov 2003Nov 2003Nov 2003
0.5
Nov 2003Nov 2003Nov 2003Nov 2003
0.5
Be
CNO pep
Tagged electron Spectrum
pp
300 pe/MeV *
0 1.00 1.0
LENS-Sol-Goal
Solar Nu SpectrumAt <2 MeV to probe pp,pep, 7Be, CNO in Sun
ν spectrum e- spectrum
from
ν + Ι+ Ι+ Ι+ Ιn e- + 2 γγγγ +SnE(e-) = E(ν) ν) ν) ν) – 114 keV
e- tagged by isomeric 2 γ γ γ γ cascade decay ( τ ) τ ) τ ) τ )
•Update: Recent values •~ 440pe/MeV
ττττ e1 (prompt)
e/γγγγ2 2 2 2 (115)(115)(115)(115)
γγγγ3333(500)(500)(500)(500)In
Sn
νννν
pp 7Be pep CNO
SSM 29540 9200 480 2050
Practical =SSM x εεεε
7385ε ε ε ε =0.25
7360ε ε ε ε =0.8
380ε ε ε ε =0.8
1640ε ε ε ε =0.8
LMA =Prac x δδδδ
4800δδδδ=0.65
4300δδδδ=0.58
220δδδδ=0.58
930δδδδ=0.58
Design Event Rates for 60 ton Indium; 5y Livetime
Goals for Precision(including CC meas.):
pp: 3%: 7Be: 3%pep: 10% CNO ~6%
Specific expectations from Precision LoNu Results
•Proof of Physics of LMA -- νννν parameters ab initio
•Surprise Discovery? --Subdominant phenomena?
•SSM correct? -- (pp cycle--Be/pp ratio, CNO cycle)
•Nu- Luminosity vs. Photon Luminosity ---
Hidden energy sources in Sun?
Accessible only via Resolved Spectrum of
pp, Be, pep, CNO fluxes
LENS
LMA Favor Conversion
Main Feature :
Low energies: Vac
High energies: Matter
So far only hi energy Data
“ Smoking Gun” at:Low Energy
Schematic LMA ProfileBahcall & Pena-Garay (’03)
pp spectrum—0-420 keVpep line -- 1442 keV
PHYSICS of 2Nu-LMA with only low energy dataab initio measurement of sin22θθθθ & ∆∆∆∆m2
Approach: Measure flavor survival Pee of Individual Lo Nu features
Tools: Use ONLY Standard Candle fluxes: 1% prediction; Variable energy
7
0.75
0.8
0.85
0.9
0.95
1
4 6 8 10 12 14
K=
Pe
e/ [1
-0.5
sin
22
θθ θθ 12]
Sin2 2θθθθ12 =0.95
Sin2 2θθθθ12=0.7
Current LMA 95% c.l. area
7Be pep
pp
∆∆∆∆m2 (x105)eV2
Strategy for direct Measurement of Sin2θθθθ12 and ∆∆∆∆m2
At Low Energy:
pp directly givesSin2θθθθ12independent of ∆∆∆∆m2
Pep, Be lines at Higher energyReveal dependenceOn ∆∆∆∆m2
0.5
0.55
0.6
0.65
0.7
0.75
0.8
0.5 0.6 0.7 0.8 0.9 1
-
3%
Current limits from
7 experimentsLENS-Sol Only
0.5
0.55
0.6
0.65
0.7
0.75
0.8
0.5 0.6 0.7 0.8 0.9 1
-
3%
Current limits from7 expts
pp
flu
x in
LE
NS
-So
l /S
SM
Sin2 2θθθθ12
0.5
0.55
0.6
0.65
0.7
0.75
0.8
0.5 0.6 0.7 0.8 0.9 1
-
3%
Current limits from
7 experimentsLENS-Sol Only
0.5
0.55
0.6
0.65
0.7
0.75
0.8
0.5 0.6 0.7 0.8 0.9 1
-
±±±± 3%
Current limits 95%C.L.From 7 expts
pp
flu
x in
LE
NS
-So
l /S
SM
Sin212
Pee(pp:LMA)=0.985(1-0.5sin22θθθθ12)
Direct Measurement of Sin2θθθθ12 from pp data
0.5
0.55
0.6
0.65
0.7
0.75
4 6 10 12 148
sin22θθθθ =0.95
0.8
0.9
0.7
0.6
0.5
sin22θθθθ =0.95
0.8
0.9
0.7
0.6
0.5
∆∆∆∆m2 (x105)eV2
pep(
LEN
S-S
ol)/p
ep(S
SM
)
Current LMA limits 95% c.l. (7 expts)
Check of LMA with pep signal– Probe of Dm2
∆∆∆∆m2 (x105)eV2
0.4
0.45
0.5
0.55
0.6
0.65
0.7
0.75
4 6 8 10 12 14
sin22θθθθ =0.95
0.8
0.9
0.7
0.6
0.5
sin22θθθθ =0.95
0.8
0.9
0.7
0.6
0.5
Current LMA limits 95% c.l.(7 expts)
P ee(7 B
e)
Measurement of Model-Dependent Be flux using measured 7Be signal and 2νννν LMA determined from Pee of pp and pep stds
Std. Fluxes pp, pep –Assumed.Non-standard fluxes Be, pep, 8 B—derived
using Pee( 2νννν LMA) of pp and pep stds
Final Result: All original solar ν ν ν ν fluxes known.
Final tests of consistency of neutrino & solar physics: 3 neutrino mixing: θθθθ13 13 13 13 ????For solar Neutrinos: Pee (3nu) = Pee(2nu) cos4 θθθθ13
Derivation of SN fluxes from measured signals must use Pee(3νννν) rather than Pee(2νννν). If NOT,
all SN fluxes could be off by 10%since sin2θθθθ13 < 5% (3σσσσ) (Chooz).
To Explore Pee(3νννν):Use Measured Optical Luminosity L( γγγγ)& compare with Neutrino Luminosity L(νννν) derived from solar νννν Fluxes fromLENS-Sol using Pee(2νννν)
L(νννν) = L(γγγγ)[0.914φφφφp+ 0.07φφφφBe+ 0.014φφφφCNO] =cos4 θθθθ13 0.998L(γγγγ)ΦΦΦΦi from LENS (Pee(2νννν))δδδδ(φφφφpp) ~ ±±±± 3%;3%;3%;3%; δ(δ(δ(δ(L)<<1% δ(δ(δ(δ(φφφφΒεΒεΒεΒε) ∼) ∼) ∼) ∼±±±± 6%; 6%; 6%; 6%; δ(δ(δ(δ(φφφφCNO)∼)∼)∼)∼±±±± 10%10%10%10%
Equation anchored by L(γ γ γ γ ) to high precision. LHS precision determined basically by LENS δδδδ(φφφφpp) ±±±± 3%;3%;3%;3%; Inferences 1) Assume: L (ν)ν)ν)ν) ≡≡≡≡ L (γγγγ) → cos4 θθθθ13 < 0.03 → sin2 θθθθ13 < 0.015 (Particle phys)
2) Take sin2 θθθθ13 << 0.015 from future measurement → L(ν) = L(γ) tο ±±±± 3%;3%;3%;3%; (Solar Phys) Experimental Proof of solar energy = nuclear energy only ±±±±3%;
Final precision consistency of Neutrino and Solar Physics
Check other questions: Be/pp- ratio for Surprise Neutrino physics phenomenology?
Nunokowa: hep-ph/See also Smirnov ( )for low energy sterile conversion
Solar Astrophysics
Knowledge of Conversion Parameters implies Knowledge of solar Neutrino Fluxes correctedFor Conversion:All Fluxes known with high precision for the first timeCheck1) Solar Model Critically by individual predicted fluxes2) Check consistency of SSM using
Be/pp ratio = (3,3)/(3,4) He reaction ratio---backbone of SSM
3) Neutrino Luminosity Are there sources of Energy Of the sun BESIDES nuclear reactions?
115In ( 95.7%)ττττ = 6.4x1014 y
115Sn
B(GT) = 0.17; Qνννν=114
e1
(e/γγγγ)2 115.6 (e/γγγγ = 0.96)
γγγγ3 497.3
115 In(p,n)100.8 (e/γ =5.7)
ττττ = 4.76 µµµµs
ββββmax = 498.8
ττττ = 16 ps
τ = 231µs
9/2+
1/2+
3/2+
7/2+
11/2-
0
497.3
612.8
713.6
7/2+ 1857
B(GT) ~0.01; Qν =1362
e
115In ( 95.7%)ττττ = 6.4x1014 y
115Sn
B(GT) = 0.17; Qνννν=114
e1
(e/γγγγ)2 115.6 (e/γγγγ = 0.96)
γγγγ3 497.3
115 In(p,n)100.8 (e/γ =5.7)
ττττ = 4.76 µµµµs
ββββmax = 498.8
ττττ = 16 ps
τ = 231µs
9/2+
1/2+
3/2+
7/2+
11/2-
0
497.3
612.8
713.6
7/2+ 1857
B(GT) ~0.01; Qν =1362
e
The Indium Low Energy Neutrino Tag
115In ( 95.7%)ττττ = 6.4x1014 y
115Sn
B(GT) = 0.17; Qνννν=114
e1
(e/γγγγ)2 115.6 (e/γγγγ = 0.96)
γγγγ3 497.3
115 In(p,n)100.8 (e/γ =5.7)
ττττ = 4.76 µµµµs
ββββmax = 498.8
ττττ = 16 ps
τ = 231µs
9/2+
1/2+
3/2+
7/2+
11/2-
0
497.3
612.8
713.6
7/2+ 1857
B(GT) ~0.01; Qν =1362
e
115In ( 95.7%)ττττ = 6.4x1014 y
115Sn
B(GT) = 0.17; Qνννν=114
e1
(e/γγγγ)2 115.6 (e/γγγγ = 0.96)
γγγγ3 497.3
115 In(p,n)100.8 (e/γ =5.7)
ττττ = 4.76 µµµµs
ββββmax = 498.8
ττττ = 16 ps
τ = 231µs
9/2+
1/2+
3/2+
7/2+
11/2-
0
497.3
612.8
713.6
7/2+ 1857
B(GT) ~0.01; Qν =1362
e
The Indium Low Energy Neutrino Tag
random
νννν signal + Bgd at short delays
Bgd only at long delays (mostly 115In ββββ’s)
In
Hybrid In-Detector
Built-in live background measurement
BASIC METHODOLOGY
Foundations Laid by work of LENS R&D group 200-2003
In
In-free
Dcell
Dmin
Conceptual Hybrid Design to suppress In Bgd
Design parameters
• In =4t• Theor. Signal 1/d
• In betas >450 keV2.5x107
• pe/MeV=310
• DL (s) = 14 cm(@100 keV)
• Primary Cell???? 2s = 60 cm
• ????E (s) = 18 keV(@100 keV)
• Module Dim.10x10x300 (In)
Designparameters
In =4t•Theor. Signal 1/d
•In β β β β >450 keV: 2.5x1077
• pe/ /MeV =310∆∆∆∆L (σ)(σ)(σ)(σ)= 14 cm
@ 100 keV
• Primary Cell±2σ±2σ±2σ±2σ = 60 cm
• ∆∆∆∆E (σ)(σ)(σ)(σ)= 18 keV(@100 (keV)
•Module Dim.
10x10x300 (In)
Simulation
Sim. Results• hνννν = 6500/ MeV
Simulation of Spectroscopy in (old) Hybrid design
????????????(115 keV)γγγγ 3(500) γγγγ2 (115)
In
ττττ e1 (prompt)e/γγγγ2 2 2 2 (115)(115)(115)(115)
γγγγ 3333(500)(500)(500)(500)10x10x400 (with buffer)
Design parameters
• In =4t• Theor. Signal 1/d
• In betas >450 keV2.5x107
• pe/MeV=310
• DL (s) = 14 cm(@100 keV)
• Primary Cell???? 2s = 60 cm
• ????E (s) = 18 keV(@100 keV)
• Module Dim.10x10x300 (In)
Designparameters
In =4t•Theor. Signal 1/d
•In β β β β >450 keV: 2.5x1077
• pe/ /MeV =310∆∆∆∆L (σ)(σ)(σ)(σ)= 14 cm
@ 100 keV
• Primary Cell±2σ±2σ±2σ±2σ = 60 cm
• ∆∆∆∆E (σ)(σ)(σ)(σ)= 18 keV(@100 (keV)
•Module Dim.
10x10x300 (In)
Simulation
Sim. Results• hνννν = 6500/ MeV
Design parameters
• In =4t• Theor. Signal 1/d
• In betas >450 keV2.5x107
• pe/MeV=310
• DL (s) = 14 cm(@100 keV)
• Primary Cell???? 2s = 60 cm
• ????E (s) = 18 keV(@100 keV)
• Module Dim.10x10x300 (In)
Designparameters
In =4t•Theor. Signal 1/d
•In β β β β >450 keV: 2.5x1077•In β β β β >450 keV: 2.5x1077
• pe/ /MeV =310∆∆∆∆L (σ)(σ)(σ)(σ)= 14 cm
@ 100 keV
• Primary Cell±2σ±2σ±2σ±2σ = 60 cm
• ∆∆∆∆E (σ)(σ)(σ)(σ)= 18 keV(@100 (keV)
•Module Dim.
10x10x300 (In)
Simulation
Sim. Results• hνννν = 6500/ MeV
Simulation of Spectroscopy in (old) Hybrid design
????????????(115 keV)γγγγ 3(500) γγγγ2 (115)
In
ττττ e1 (prompt)e/γγγγ2 2 2 2 (115)(115)(115)(115)
γγγγ 3333(500)(500)(500)(500)
Simulation of Spectroscopy in (old) Hybrid design
????????????(115 keV)γγγγ 3(500) γγγγ2 (115)
In
ττττ e1 (prompt)e/γγγγ2 2 2 2 (115)(115)(115)(115)
γγγγ 3333(500)(500)(500)(500)
ττττ e1 (prompt)e/γγγγ2 2 2 2 (115)(115)(115)(115)
γγγγ 3333(500)(500)(500)(500)10x10x400 (with buffer)
J.P.Meyer (LENS Notes 2002-03
10x10x300 cm module; pp signal onlyEff% BS/In ββββ S N S/N
(10µµµµs)23 1.3x10-9 0.24 0.14 1.7
21 <0.7x10-9 0.22 <0> >3
Optimum Design Area
Eff. Be, CNO, pep signals
>80%; S/N >>1
Cell Size (cm)
εff.
4 6 8 10 12 14
10x10x300 cm module; pp signal onlyEff% BS/In ββββ S N S/N
(10µµµµs)23 1.3x10-9 0.24 0.14 1.7
21 <0.7x10-9 0.22 <0> >3
Optimum Design Area
Eff. Be, CNO, pep signals
>80%; S/N >>1
10x10x300 cm module; pp signal onlyEff% BS/In ββββ S N S/N
(10µµµµs)23 1.3x10-9 0.24 0.14 1.7
21 <0.7x10-9 0.22 <0> >3
Optimum Design Area
Eff. Be, CNO, pep signals
>80%; S/N >>1
Cell Size (cm)
εff.
4 6 8 10 12 14
J.P.Meyer, LENS Notes 2000-03
• · Hybrid strategy effective in solving the In -radioactivity background completely.
• · Granularity required of 60x10x10 cm vertex cell moderate and practical for high quality low energy nuclear spectroscopy
Conclusions of Analysis of Hybrid Design
• · Hybrid strategy effective in solving the In -radioactivity background completely.
• · Granularity required of 60x10x10 cm vertex cell moderate and practical for high quality low energy nuclear spectroscopy
Next Challenge: Design Hi-Mass Detector Next Challenge: Design Hi-Mass Detector
Conclusions of Analysis of Hybrid Design
• 1. High transparency InLS technology---optical length L(1/e) ~10m ---fewer InLS modules-- data channels—lower cost
• 2. Multi-layer reflecting foils ----New light pipe technology
- ----New design possibilities compatible to 1)
• 3. New hybrid design----Exploits 1) & 2)
Keystones to Hi-Mass In DetectorNew Developments 2003-04 (US-Russia)
0.01
0
0.004
0.008
0.012
0.016
0.02
0.024
0.028
370 400 430 460 490 520 550 580 610 640 670 700
Abso
rban
ce in
10
cm c
ell
Solvent PCInLS 7% In--No fluors
A(430) ~0.003→→→→L(1/e)(430) ~14m
Wavelength (nm)
0
0.004
0.008
0.012
0.016
0.02
0.024
0.028
370 400 430 460 490 520 550 580 610 640 670 700
Abso
rban
ce in
10
cm c
ell
Solvent PCInLS 7% In--No fluors
A(430) ~0.003→→→→L(1/e)(430) ~14m
Wavelength (nm)
In Liq. Scint.Solvent PCScint Yield 42% @7% wt InL(1/e)(430 nm)= 10 m
UpdateNew Safe Solvent:PhenylcyclohexaneF.P. 100CNon-toxicInLS/PCH Scint Yield 42% ofSolvent @ 7% InTransparency Same as PC
-0.005
0.005
0.015
0.025
0.035
470
Abs
orb
ance
in
10cm
cel
l
-0.005
0.005
0.015
0.025
0.035
370 420 520 570
Wavelength (nm)
InLS 7 wt % In/ PC solvent
No Fluors L(1/e) = 14 m
Fluors (pTP/MSB)L(1/e) (430) = 10 m
-0.005
0.005
0.015
0.025
0.035
470
Abs
orb
ance
in
10cm
cel
l
-0.005
0.005
0.015
0.025
0.035
370 420 520 570
Wavelength (nm)
InLS 7 wt % In/ PC solvent
No Fluors L(1/e) = 14 m
Fluors (pTP/MSB)L(1/e) (430) = 10 m
Data from BNL
Data from Bell Labs
Cage structure ofDouble sided 3M reflector foil 10x10cm Sq
Back reflector
Refl. foil light concentrator
End Buffer
20” PMT
3” PMT
InLS (8% In)400x10x10cm
InFree LS
Optical window
End Buffer50cm
z- Event coordinate fromTOF delay betweenfwd & bwd light
Back reflector
500 400
1010
Cage structure ofDouble sided 3M reflector foil 10x10cm Sq
Back reflector
Refl. foil light concentrator
End Buffer
20” PMT
3” PMT
InLS (8% In)400x10x10cm
InFree LS
Optical window
End Buffer50cm
z- Event coordinate fromTOF delay betweenfwd & bwd light
Back reflector
500 400
1010
Cage structure ofDouble sided 3M reflector foil 10x10cm Sq
Back reflector
Refl. foil light concentrator
End Buffer
20” PMT
3” PMT
InLS (8% In)400x10x10cm
InFree LS
Optical window
End Buffer50cm
z- Event coordinate fromTOF delay betweenfwd & bwd light
Back reflector
InLS (8% In)400x10x10cm
InFree LS
Optical window
End Buffer50cm
z- Event coordinate fromTOF delay betweenfwd & bwd light
Back reflector
500 400
1010
2 ton Supermodule)LENS-Sol (Phase I-- )LENS-Sol (Phase I-- )
Hi Mass In Detector: In Mass 60 tonsIn LS (8% In) 750tonIn Free LS 3000 tonPMT:3” : 19000; 20” : 2100
50 100 150 200 250 300
Sig
ma
/ E (
keV
)
E,keV50 100 150 200 250 300
R=250 cm from PMT
E,keV
Performance Simulation of 1 –PMT Spectroscopy 500 cm
PMT Reflector
pe/MeV
50 100 150 200 250 300
E,keV50 100 150 200 250 300
00,000,020,040,060,080,100,120,140,160,180,200,22
00,000,020,040,060,080,100,120,140,160,180,200,22
0,000,020,040,060,080,100,120,140,160,180,200,22
00,000,020,040,060,080,100,120,140,160,180,200,22
0,000,020,040,060,080,100,120,140,160,180,200,22
00,000,020,040,060,080,100,120,140,160,180,200,22
0,000,020,040,060,080,100,120,140,160,180,200,22
R=250 cm from PMT
E,keV
Performance Simulation of 1 –PMT Spectroscopy 500 cm
PMT Reflector
σσσσ/ E =0.15
440 pe/MeV
LENS probe of other celestial bodies and phenomenaVia Antineutrino Spectroscopy via (ννννe bar,p)
LENS ideal device•Target Mass: 3750 tons•In content excellent n-detector (3000b)•Background suppressed because of short
time window for event search•Reactor background low (Preliminary estimate= ~300/3750 tons/y•Ideal combination of Hi Mass, Low bgd-----Likely the most powerful LOW ENERGYAntineutrino detector
Geo-Neutrinos:Global Measure ofU/Th in the Earth’s Crust:
Geo-Neutrinos:Global Measure ofU/Th in the
Detect Via antineutrinosEmitted in ββββ- decayOf U and Th
ννννe bar +p→→→→e+ +n
LENS-Sol 3.75kT(Lower ReactorBgd)
1kTLENS-Sol 3.75kT(Lower ReactorBgd)
1kTLENS-Sol 3.75kT(Lower ReactorBgd)
1kT
Super Nova Relic (Anti) Neutrino Sensitivity (Strigari et al)
VT Muon Telescope TentVT Muon Telescope Tent
Extra View Graphs
115In ( 95.7%)
115Sn
e1
115.6
497.3
1/2+
3/2+
7/2+
0
497.3
612.8
115In ( 95.7%)
115Sn
e1
497.3
1/2+
3/2+
7/2+
0
497.3
612.8
115In ( 95.7%)
115Sn
e1
497.3
1/2+
3/2+
7/2+
0
497.3
612.8
115In ( 95.7%)
115Sn
e1
497.3
1/2+
3/2+
7/2+
0
497.3
612.8
νp
nττττ = 4.76= 4.76= 4.76= 4.76µµµµs
ττττ = 231 = 231 = 231 = 231 µµµµs
µµµµ100
11/2-
p
115In ( 95.7%)
115Sn
e1
115.6
497.3
1/2+
3/2+
7/2+
0
497.3
612.8
115In ( 95.7%)
115Sn
e1
497.3
1/2+
3/2+
7/2+
0
497.3
612.8
115In ( 95.7%)
115Sn
e1
497.3
1/2+
3/2+
7/2+
0
497.3
612.8
115In ( 95.7%)
115Sn
e1
497.3
1/2+
3/2+
7/2+
0
497.3
612.8
νp
nττττ = 4.76= 4.76= 4.76= 4.76µµµµs
ττττ = 231 = 231 = 231 = 231 µµµµs
µµµµ100
11/2-
p
Cosmogenic production of In(p,n)Sn :
Rejectable via p recoil, n tagsRate @ 1600 mwe depth (Kimballton): I= 2x100/y/60t In;Tagged Background in solar runs = Iεεεε = ~50/y/60t
50-300
0
30
40
50
0.05 0.1 0.15 0.2 0.25 0.3
Energy, MeV
Sig
nal R
ate
20
10
LWO: ???? m 2 77x10 -12 eV2; sin22???? = 0.55
0
30
40
50
0.05 0.1 0.15 0.2 0.25 0.3
Energy, MeV
Sig
nal R
ate
20
10
LWO:
0
50
0.05 0.1 0.15 0.2 0.25 0.3
Energy, MeV
Sig
nal R
ate
0
50
0.05 0.1 0.15 0.2 0.25 0.3
Energy, MeV
Sig
nal R
ate
LWO:
400pe/ MeV
77x10 -12 eV2; sin22 = 0.55
30
40
20
10
30
40
20
10
∆∆∆∆m2 77x10 -12 eV2; sin22θ = 0.55400pe/ MeV
0
0.04
0.08
0.12
0 2 4 6 8 10 12 14Neutrino Energy (MeV)
Re
l. I
nte
ns
ity
SSM
LMA
LWO
LWO: Example ofSurpr ise scenar io.Energy spectrum and Pee>7 MeV identical to LMA
Revealed only byStrong oscillations ofpp spectrum
In-LS (5.5wt% In) PMTPMT
100 cm
5cm Source
241AmSum Coinc
57CoSum coinc
60 keV
26 keV
122 keV
Pb X-ray 136 keV
Borexino
Eurasian Crust
American Crust Pacific Crust
Atlantic Crust Kamland
Continental crust 35kmU 1.8ppm; Th 7.2ppm
Oceanic crust 6.5kmU 0.1ppm; Th 0.4 ppm
Total Heat 40TW(U+Th)Heat = 15TWNew: GeoReactor=3-10TW ?
Overall Geo Model: U,Th (Mantle) = U, Th (Crust);
HomestakeHawaii
2900 km
6400 km
South PoleGeomanda
R
CORE
MANTLEU 0.01ppmTh 0.04ppm
Total U: 8.2x1019 gTotal Th: 33x1019 g
Internal Energy Sources in the Ear th and their Distr ibution
Borexino
Eurasian Crust
American Crust Pacific Crust
Atlantic Crust Kamland
Continental crust 35kmU 1.8ppm; Th 7.2ppm
Oceanic crust 6.5kmU 0.1ppm; Th 0.4 ppm
Total Heat 40TW(U+Th)Heat = 15TWNew: GeoReactor=3-10TW ?
Overall Geo Model: U,Th (Mantle) = U, Th (Crust);
HomestakeHawaii
2900 km
6400 km
South PoleGeomanda
R
CORE
MANTLEU 0.01ppmTh 0.04ppm
Total U: 8.2x1019 gTotal Th: 33x1019 g
Borexino
Eurasian Crust
American Crust Pacific Crust
Atlantic Crust Kamland
Continental crust 35kmU 1.8ppm; Th 7.2ppm
Oceanic crust 6.5kmU 0.1ppm; Th 0.4 ppm
Total Heat 40TW(U+Th)Heat = 15TWNew: GeoReactor=3-10TW ?
Overall Geo Model: U,Th (Mantle) = U, Th (Crust);
HomestakeHawaii
2900 km
6400 km
South PoleGeomanda
R
CORE
MANTLEU 0.01ppmTh 0.04ppm
Total U: 8.2x1019 gTotal Th: 33x1019 g
LENS @ Kimballton
Borexino
Eurasian Crust
American Crust Pacific Crust
Atlantic Crust Kamland
Continental crust 35kmU 1.8ppm; Th 7.2ppm
Oceanic crust 6.5kmU 0.1ppm; Th 0.4 ppm
Total Heat 40TW(U+Th)Heat = 15TWNew: GeoReactor=3-10TW ?
Overall Geo Model: U,Th (Mantle) = U, Th (Crust);
HomestakeHawaii
2900 km
6400 km
South PoleGeomanda
R
CORE
MANTLEU 0.01ppmTh 0.04ppm
Total U: 8.2x1019 gTotal Th: 33x1019 g
Borexino
Eurasian Crust
American Crust Pacific Crust
Atlantic Crust Kamland
Continental crust 35kmU 1.8ppm; Th 7.2ppm
Oceanic crust 6.5kmU 0.1ppm; Th 0.4 ppm
Total Heat 40TW(U+Th)Heat = 15TWNew: GeoReactor=3-10TW ?
Overall Geo Model: U,Th (Mantle) = U, Th (Crust);
HomestakeHawaii
2900 km
6400 km
South PoleGeomanda
R
CORE
MANTLEU 0.01ppmTh 0.04ppm
Total U: 8.2x1019 gTotal Th: 33x1019 g
Internal Energy Sources in the Ear th and their Distr ibution
Borexino
Eurasian Crust
American Crust Pacific Crust
Atlantic Crust Kamland
Continental crust 35kmU 1.8ppm; Th 7.2ppm
Oceanic crust 6.5kmU 0.1ppm; Th 0.4 ppm
Total Heat 40TW(U+Th)Heat = 15TWNew: GeoReactor=3-10TW ?
Overall Geo Model: U,Th (Mantle) = U, Th (Crust);
HomestakeHawaii
2900 km
6400 km
South PoleGeomanda
R
CORE
MANTLEU 0.01ppmTh 0.04ppm
Total U: 8.2x1019 gTotal Th: 33x1019 g
Borexino
Eurasian Crust
American Crust Pacific Crust
Atlantic Crust Kamland
Continental crust 35kmU 1.8ppm; Th 7.2ppm
Oceanic crust 6.5kmU 0.1ppm; Th 0.4 ppm
Total Heat 40TW(U+Th)Heat = 15TWNew: GeoReactor=3-10TW ?
Overall Geo Model: U,Th (Mantle) = U, Th (Crust);
HomestakeHawaii
2900 km
6400 km
South PoleGeomanda
R
CORE
MANTLEU 0.01ppmTh 0.04ppm
Total U: 8.2x1019 gTotal Th: 33x1019 g
LENS @ Kimballton
LENS-Sol (Phase I-- 20 ton In )
Supermodule
6300 InLS mod 10x10x4008% In
=20 ton In250 ton InLS
700 SuperMod
InFree LS = 60x60x500
-1440 kg LS=1000T LS
Total LS =1250 T
=
6300 3” PMT
700 20 “ PMT
Total=7000 Ch
.Double sided 3M Reflecting Foil Cage Structure
3” PMT for InLS Mod
20” PMT for In-Free LS Super Mod
10 10
60 cm
LENS-Sol (Phase I-- 20 ton In )
Supermodule
6300 InLS mod 10x10x4008% In
=20 ton In250 ton InLS
700 SuperMod
InFree LS = 60x60x500
-1440 kg LS=1000T LS
= 60x60x500-1440 kg LS=1000T LS
Total LS =1250 T
=
6300 3” PMT
700 20 “ PMT
Total=7000 Ch
6300 3” PMT
700 20 “ PMT
Total=7000 Ch
.Double sided 3M Reflecting Foil Cage Structure
3” PMT for InLS Mod
20” PMT for In-Free LS Super Mod
10 10
60 cm