Measurement of sin 2 2  13 at the Braidwood Nuclear Reactors Jonathan Link Columbia University Research Techniques Seminar April 13, 2005

νeνe νeνe νeνe νeνe νeνe νeνe Distance Probability ν e 1.0 E ν ≤ 8 MeV 1200 to 1800 meters Sin 2 2θ 13 Reactor Experiment Basics Unoscillated flux observed here Well understood, isotropic source of electron anti-neutrinos Oscillations observed as a deficit of ν e sin 2 2θ 13 Survival Probability

The reaction process is inverse β-decay Two part coincidence signal is crucial for background reduction Minimum energy for the primary event is1.022 MeV from e + e − annihilation. Positron energy spectrum implies the neutrino spectrum The scintillator is doped with gadolinium to enhance capture Capture can also occur on hydrogen (or carbon, rarely) e p→ e + n e p→ e + n n capture n capture Reactor Neutrino Event Signature n H → D  (2.2 MeV) n m Gd → m+1 Gd  ’s (8 MeV) E ν = E e MeV (prompt) (delayed)

Braidwood Nuclear Station Located about 30 miles due south of the Lab. Operated by Exelon Nuclear. 2 Reactors with 7.17 GW thermal power 2 Reactors with 7.17 GW thermal power Well understood/favorable geology Well understood/favorable geology ─ Plant construction data ─ Site investigation (completed Jan. 05) Strong support from owner Strong support from owner Ability to optimize layout Ability to optimize layout Near Detector Far Detector

Baseline Design: Detectors 2.6 m 3.5 m Two zone design Two zone design 2.6 meter target radius 2.6 meter target radius 3.5 meter total radius 3.5 meter total radius 65 ton target 65 ton target 1000 PMT’s (coverage>25%) 1000 PMT’s (coverage >25%) 0.2% Gd Loaded Scintillator 0.2% Gd Loaded Scintillator MoreMore…

Benefits of Gd Loading No Gd: 6.1 cm mean 0.2% Gd: 4.3 cm mean No Gd: 142 μs mean 0.2% Gd: 15 μs mean Gd has a huge neutron capture cross section → faster capture times and smaller spatial separation. Helps to reduce random coincidence backgrounds. 8 MeV capture energy (compared to 2.2 MeV on H) is distinct from positron energy and rare as radioactive background. MoreMore…

Baseline Design: Site Layout Near detectors at a baseline of 286 meters (~4400 int/day) Near detectors at a baseline of 286 meters (~4400 int/day) Far detectors at a baseline of 1511 meters (~160 int/day) Far detectors at a baseline of 1511 meters (~160 int/day) All detector at a depth of 183 meters (600 ft) All detector at a depth of 183 meters (600 ft) Earth shielding is flat with an average cover of 464 mwe (as measured by our borehole investigation) Earth shielding is flat with an average cover of 464 mwe (as measured by our borehole investigation) This should be compared to ~700 mwe cover under a mountain!

Sensitivity Drivers There are four main sensitivity drivers… 1. Neutrino interaction statistics 2. Near/Far detector relative normalization 3. Backgrounds 4. Detector baseline (varies with Δm 2 ) We will look at each of these in turn. The first 3 are easily translated into measurement errors…

Simple Sensitivity Model Where N is the number of observed signal events, L is the baseline and ε is the relative efficiency (≈1). Then… Where… < 1– 3σ R means an effect is observed Statistics Relative Normalization Background

Statistics Top 30 U.S. Sites by Power Performance Ways to optimize statistics… Reactor power Reactor power ─ Braidwood is third most powerful in US Detector mass Detector mass ─ 130 ton baseline design ─ Planned upgrade to 260 tons Run time Run time ─ Straight clock time (3 years initial plus 5 years upgrade) ─ Reactor uptime (>92% at Braidwood) ─ Reduced dead time Check assumptions about optimal baseline with respect to statistical error. Check assumptions about optimal baseline with respect to statistical error.

Relative Normalization The use of a near detector eliminates the normalization uncertainty due to reaction cross section reaction cross section neutrino production in the core neutrino production in the core reactor power reactor power Truly identical detectors would eliminate the remaining sources of normalization uncertainty which are detector efficiency detector efficiency gadolinium fraction (neutron detection efficiency) gadolinium fraction (neutron detection efficiency) target mass target mass target chemistry: free proton (target particle) fraction target chemistry: free proton (target particle) fraction The last three are best measured with detector cross calibration. I won’t discuss these further

Relative Normalization II Relative detector efficiency can be measured by calibrating all detectors with the same long lifetime radioactive sources. Relative detector efficiency can be measured by calibrating all detectors with the same long lifetime radioactive sources. Gd fraction can be measured by looking at Gd to H capture ratio (statistical precision to better that 0.05%). Gd fraction can be measured by looking at Gd to H capture ratio (statistical precision to better that 0.05%). Also, control chemistry during detector filling Relative free proton count (target mass and H fraction) can be controlled by measuring flow rates and equally splitting scintillator batches during detector filling. Relative free proton count (target mass and H fraction) can be controlled by measuring flow rates and equally splitting scintillator batches during detector filling. It can only be measured by detector cross calibration with neutrinos… Requiring Movable Detectors!

Movable Detectors Spending just 8% of the run on head-to-head calibration results in a free proton calibration precision of better than 0.3%. Detector calibration techniques can be verified against head-to- head neutrino relative calibration. Detectors can be built during shaft civil construction and commissioned in the near hall while the far hall is still under construction. Detectors can be filled simultaneously and in the same location from the common scintillator batches. MoreMore…

Relative Normalization: Final Word Double CHOOZ hopes to achieve 0.6% (or better) relative normalization with fixed detectors. With four detectors there are three independent relative normalizations. So even if this is the best we could do on each pair of detectors the effective relative normalization error is An effective relative normalization error of 0.2% or better is very likely.

Background There are three types of background 1.Random coincidence ─ where two unrelated events happen close together is space and time. 2.Fast neutron ─ where a fast neutron enters the detector, creates a prompt signal, thermalizes and is captured. 3.βn decays of spallation isotopes ─ isotopes such as 9 Li and 8 He with βn decay modes can be created in a spallation with μ on 12 C. The vast majority of backgrounds are directly related to cosmic rays (cosmogenic). The background rejection methods are the source of dead time in the detector.

Background Notes The Collaboration is developing comprehensive simulation tools. In the mean time background calculations are done with a combination of Hand calculations Hand calculations Numerical integration of functions (i.e. surface μ spectrum, μ attanuation in rock) Numerical integration of functions (i.e. surface μ spectrum, μ attanuation in rock) Published data tables Published data tables Simple geometries in accepted simulation tools (MARS, Fluka and Geant4) Simple geometries in accepted simulation tools (MARS, Fluka and Geant4) The Minos near hall, with similar flat overburden, may allow us to test the validity of these calculation techniques.

MuonsAverage ENeutrons 9 Li & 8 He 0.21/m 2 / s 84 GeV178/ton/day0.078/ton/day Cosmic Rays and Related Background Surface spectrum from Gaisser μ attenuation from Groom, Mokhov & Striganov Neutron production model from Wang et al. Isotope production from Hagner et al. 4.5 Hz of μ in target and 21 Hz in veto system /m 2 /s/GeV

Random Coincidence Background Assuming KamLAND concentrations of 40 K, 232 Th and 238 U and 450 mwe Plot made by Hannah Newfield-Plunkett The rate of single events is shown on the left. One can integrate this plot in the positron and neutron signal regions to get the respective random rates. 142k/det/day “positrons” 5070/det/day “neutrons” The random coincidence of these events in 100 μs window in the right order is 0.4/detector/day. There is no tag for these events → No dead time. Reverse order events give a handle on the background rate

Fast Neutron Background 1.Two neutron captures from the same cosmic ─ This should be tagged the vast majority of the time, but it sets the tag window for tagged muons at 100 μs. 2.Proton recoil off fast neutron ─ dominate effect. 3.Fast neutron excitation of 12 C ─ interesting, but not significantly different than 2. Energy spectrum peaks at particular values (like 4.4 MeV, first excited state) There are three main processes for the prompt “positron-like” events

Tagging Muons at Braidwood The basic idea is to tag muons that pass near the detector so that we can reject the fast neutron background. Neutrons from farther away should mostly be ranged out. The Collaboration is considering two options for veto system 1.An integrated veto shield ─ 2 meters of liquid scintillator 2.1 meter of heavy concrete with surface detectors (RPCs?) Veto Detectors p n   n 6 meters Shielding

Fast Neutron Background in Braidwood What eludes the tagging system? 1.Veto inefficiency ─ muon gets inside the veto but is not seen by either the veto or the detector. Need very efficient veto detector. You get two shoots at each muon: entering and exiting. (99% efficiency → 0.25/detector/day) 2.Fast neutron created outside the shielding ─ calculation follows…

Fast Neutron Background in Braidwood II Using the MARS simulation package I calculate that 2087 neutrons/day will exit the rock on a collision course with the detector target. Of these 0.93% survive 1 meter heavy concrete+90 cm mineral oil and 20% of those have “positron-like” prompt event in the detector. 4 background events In 88% of the original 2087 neutrons, the parent muon passed through the veto at some point. 0.5/detector/day Problematic neutrons are more likely to be vetoed because the colinearity of the parent and daughter is more likely for the fast neutrons that survive the shielding.

Fast Neutron Dead Time The cosmic ray rate in the veto (generously assuming 100 m 2 veto area) is 21 Hz and the tag window is 100 μs… 0.2% dead time

Correlated Decay of Spallation Isotopes Correlated final state: β+n+2α Used Birks’ law to quench alphas and protons with Birks constant of cm/MeV (from Borexino PLB 525, 29). Correlated final state: β+n+ 7 Li τ ½ = 178 ms 49.5% Correlated τ ½ = 119 ms 16% Correlated

Correlated Spallation Isotopes in KamLAND KamLAND tagged correlated events closely associated with cosmic muons. Their data is consistent with 9 Li being the dominate source of correlated spallation isotope. from the thesis of Kevin McKinny

E μ (GeV) KamLAND 1300 cm Braidwood 520 cm Min I (0.33) 2.5 GeV 1.0 GeV Avg Braidwood (83) 3.4 GeV 1.3 GeV Avg KamLAND (215) 3.5 GeV 1.4 GeV GeV 1.5 GeV 9 Li Events vs. Minimum Shower Energy ~46 events at threshold of 0. Kevin McKinny’s Thesis Correlated Spallation Isotopes KamLAND/Braidwood Avg KamLAND (215) 3.5 GeV 1.4 GeV Avg Braidwood (83) 3.4 GeV 1.3 GeV Min I (0.33) 2.5 GeV 1.0 GeV GeV 1.5 GeV Scaling from KamLAND, a 1.5 GeV shower tag in Braidwood would capture ~85% of all 9 Li. A 0.5 second tag window would capture >85% of the decays. So this tag would isolate ~72% of all 9 Li. μ Energy Loss Due to Ionization

Correlated Spallation Isotopes in Braidwood Expect Li/ton/day, half decay in βn modes, 72% are tagged → 0.7/detector/day. From a simulation of muon energy loss in the Braidwood detector (based on Groom, Mokhov & Striganov + ref. therein) μ energy loss in 2.6 m sphere of scintillator. Only 3% fail E cut of <1.5 GeV With 4.5 Hz of μ and 3% tagged at 0.5 seconds → ~7% dead time Can use neutron captures following cosmic as an additional tag.

Background Summary Background Rate (<) Dead Time Random0.4/detector/daynone Fast Neutron (inside) 0.3/detector/daynone Fast Neutron (outside) 0.5/detector/day0.2% 9 Li 0.7/detector/day7% Total1.9/detector/day~7% This is where we stand today with conservative assumptions. Compare to 160 signal/detector/day at the far site (S/N~85) With a 10-20% uncertainty in the BG rate, sensitivity to sin 2 2θ 13 in the simple model is 0.01 (90% CL) at Δm 2 =2.5×10 -3.

Energy Spectrum Fit Neutrino Energy Fitting the energy spectrum takes advantage of the significant differences between the signal and backgrounds. With the Phase II upgrade the experiment is sensitive to the shape deformation due to oscillations. May extend sensitivity to > 3M events/near det ~3M events/det~12K events/det Tagged 1800 events/det Tagged

Baseline Optimization The baseline optimization is sensitive to three effects: 1. Oscillation wavelength ( 1/Δm 2 ) 2. Event statistics which fall off like 1/L 2 3. To the level of systematic error (S/N is a function of L which also varies as 1/L 2 ) Kinematic Phase = 1.27Δm 2 L/E Optimize in terms of the invariant, kinematic phase, and the percent of systematic error in terms of statistical error. With Δm 2 =2.5×10 -3 and 150% systematic error… L≈1500 meters

Braidwood Status Completed preliminary MOU with Exelon in September 04 Completed preliminary MOU with Exelon in September 04 Submitted R&D proposal to NSF and DOE in September 04 Submitted R&D proposal to NSF and DOE in September 04 Completed geological site investigation in January 05 which included Completed geological site investigation in January 05 which included ─ 600+ foot bore holes at both the near and far site. ─ Geophysics tests included: audio-televiewer, passive gamma, resistance probe, calipers and water pressure tests.

GZA GeoEnvironmental, Inc. Recent Geological Site Investogation Sand and clay ……………….. 37' Carbondale Shale & Sandstone Maquoketa Shale ………………… 140' Maquoketa Limestone ………………… 207' Maquoketa Shale ………………… 271" Galena Limestone & Dolomitic Limestone ………………… 467" Platteville Limestone & Dolomitic Limestone NO TAKE Zones Depth 410 to 450 Depth 450 to 490 Depth 490 to 530 Depth 530 to 570 Depth 570 to 610 Depth 590 to 630 Water Pressure Testing Audio Televiewer and Geophysics Suite

GZA GeoEnvironmental, Inc. Background Radiation at Depth One of the standard geophysics probes measures the natural gamma radiation. Measures rock porosity For us it confirms that the background radiation in dolomitic limestone is low. Near Shaft Far Shaft

Braidwood Status Completed preliminary MOU with Exelon in September 04 Completed preliminary MOU with Exelon in September 04 Submitted R&D proposal to NSF and DOE in September 05 Submitted R&D proposal to NSF and DOE in September 05 Completed geological site investigation in January 05 which included Completed geological site investigation in January 05 which included ─ 600+ foot bore holes at both the near and far site. ─ Geophysics tests include: audio-televiewer, passive gamma, resistance probe, calipers and water pressure tests. ─ Demonstrated a constructive working relationship with Exelon and the Braidwood staff. We await the guidance of NuSAG. We await the guidance of NuSAG.

Conclusions The measurement rests on our ability to understand the near/far relative normalization and to reduce and understand backgrounds. Each piece of the relative normalization can be measured and verified by at least two independent methods. This redundancy is critical to ensure that the high precision goals of the experiment will be meet. Initial, conservative studies indicate that a background of 1 to 2 events/detector/day is achievable. Significant improvement is likely.

Conclusions Sensitivity studies indicate that the Δm 2 region preferred by Super-K (1.5×10 -3 < Δm 2 < 3.0×10 -3 ) will be covered down to 0.01 (90% CL) in sin 2 2θ 13. Phase II, where two detectors are added at the far site for an additional 5 years of running, can extend the reach to or better. Phase II could confirm a rate deficit in the baseline experiment with an observation of the shape deformation. Braidwood is an excellent site to make this important measurement!

Question Slides

CHOOZ and Palo Verde Results sin 2 2  13 < 0.18 at 90% CL (at  m 2 =2.0×10 -3 ) Future experiments should try to improve on these limits by at least an order of magnitude. Down to sin 2 2  In other words, a 1% measurement is needed! < ~ Neither experiments found evidence for e oscillation. This null result eliminated  → e as the primary mechanism for the Super-K atmospheric deficit.

Two Zones Design With just two zones some of the Gd capture energy can escape the scintillator undetected. This may result in relative norm. bias. Calibrating detectors to the capture peak virtually eliminates this potential bias. Back…

Detector Use a rail system for easy transport. The detector needs to carry its electronics and front-end DAQ as these components also play a role in detector efficiency. Multiple far detectors may be used to maintain portability while increasing total volume. Detectors need to fit in the shaft (Diameter ≤7 meters) Detectors Designed to Move 8 meters 9 meters Back…

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