dm ice
play

DM-Ice Reina Maruyama University of Wisconsin - Madison SNOWMASS - PowerPoint PPT Presentation

DM-Ice Reina Maruyama University of Wisconsin - Madison SNOWMASS 2013: Cosmic Frontier Workshop March 6 - 8, 2013 http://www.physics.wisc.edu/~maruyama/ Wednesday, March 6, 13 1. Experiment Status and Target Mass Currently in Operation:


  1. DM-Ice Reina Maruyama University of Wisconsin - Madison SNOWMASS 2013: Cosmic Frontier Workshop March 6 - 8, 2013 http://www.physics.wisc.edu/~maruyama/ Wednesday, March 6, 13

  2. 1. Experiment Status and Target Mass Currently in Operation: DM-Ice17 Proposed Full-Scale: DM-Ice 17 kg of NaI(Tl), operation since 2011 250 kg of ultra-pure NaI(Tl) Funding: NSF-Polar Programs & Proposed deployment: Dec. 2015 NSF-CAREER for R&D First results expected in Spring DM-Ice Snowmass - March 2013 2 Wednesday, March 6, 13

  3. 2. Fiducial Target Mass DM-Ice diameter is limited to ~65 cm by the ice drill. DM-Ice17: 2 modules (pressure vessels) 5” dia x 5” long, 1 crystal / module total mass: 17 kg of NaI(Tl) DM-Ice: 2 modules 5” dia x 15” long, 7 crystals/module total mass: 250 kg of NaI(Tl) Multi-crystal events veto. DM-Ice Snowmass - March 2013 3 Wednesday, March 6, 13

  4. 3. Backgrounds Going from DM-Ice17 to DM-Ice • Background goal: < 1 cpd/keV ee /kg in 2 - 10 keV ee (factor of 10 reduction) • Contamination levels in DM-Ice17 estimated from in-ice data and radio- assay, verified by simulation • Dominant background in DM-Ice17: 40 K & 210 Pb in the crystals • Surrounding ice is extremely clean, drill ice is clean enough • Ultra-clean crystals are under development (see F . Calaprice’s talk) • Cleaner PMT, Pressure Vessel, & Quartz are available • Direct muon interaction contribute O(10 -5 ) below other backgrounds • Muon monitor & tag with IceCube Alpha region in DM-Ice17 vs. Simulation Crystal contamination in DM-Ice17 & DAMA preliminary DM-Ice17 DAMA nat K 500 ppb < 20 ppb 232 Th 50 ppt 0.5 - 7.5 ppt 238 U (upper part of 7.5 ppt 0.7 - 10 ppt chain) 238 U (below Pb-210) 2 mBq/kg 5 - 30 μ Bq/kg DM-Ice Snowmass - March 2013 4 Wednesday, March 6, 13

  5. Backgrounds and Calibration: DM-Ice17 In-ice data, DM-Ice17, Crystal-1 [Counts/keV/7.5 kg/718 hrs] 239 keV ( 212 Pb from 232 Th) • Energy = integral(waveform) 352 keV ( 214 Pb from 238 U) 583 keV ( 208 Tl from 232 Th) • Detectors calibrated using internal 609 keV 214 Bi from 238 U) lines 1173 & 1333 keV ( 60 Co) • Spectra compared & verified with 1460 keV ( 40 K) source calibration at Madison and Boulby ‣ 207 Bi (569.7 & 1063.66 keV) Energy [keV] ‣ 60 Co (122.06 & 136.5 keV), ‣ 57 Co (1173.34 & 1332.50 keV) • Calibration stable over >18 months Boulby Madison DM-Ice Snowmass - March 2013 5 Wednesday, March 6, 13

  6. Low Energy Spectrum Energy Spectrum < 150 keV ––– July 2011 125 I (67.3 keV) Peak counts v. time cpd/keV/kg ––– April 2012 125 I&X6rays 125 I&(67.3&keV) 210 Pb&(46.5&keV)&+& 129 I&(40&keV) 210 Pb&on&surface?&(12&keV) keV • 7 - 10 cpd/keV ee /kg between 8 - 30 keV ee . • Low energy region calibrated with internal lines from Pb-210, I-125, & I-129 • Cosmogenic activation of 125 I observed with T 1/2 = 59.4 days • K-40 line at 3.2 keV also visible. DM-Ice Snowmass - March 2013 6 Wednesday, March 6, 13

  7. 4. Detector Discrimination • We currently use PSD to eliminate instrumental effects, e.g. “thin-pulses” that seem to originate in the PMTs in the ROI, but not used in physics events. • At higher energies, it is possible to use PSD discriminate between gammas, alphas, and nuclear recoil. In the energy region of interest, PSD is not effective and will not be used. Physics Events Instrumental Events >100 keV “Thin Pulses” ATWD ch0 center xtal, pmt-0 center xtal, pmt-1 ADC Time (ADC units, 600 ns window) EM Interference <100 keV DM-Ice Snowmass - March 2013 7 Wednesday, March 6, 13

  8. 5. Energy Threshold single&photo6electron&spectrum DM-Ice Goal: • < 2 keV ee threshold pedestal 1pe DM-Ice17: • Analysis threshold: 8 keV ee is robust, analysis in progress down to ~ 2 keV ee ––– July 2011 cpd/keV/kg with single crystals ––– April 2012 • Light collection: 5 - 6 pe/keV • Each PMT triggered at fraction of pe Energy Spectrum < 150 keV DM-Ice Snowmass - March 2013 8 keV Wednesday, March 6, 13

  9. 6. Sensitivity versus WIMP mass • DM-Ice goal: test DAMA’s claim for detection of DM annual modulation • Use the same target mass: NaI(Tl) • 500 kg-yr with (2-DAMA years) • < 5 cpd/keV/kg (DAMA: ~1 cpd/keV/kg) • Decouple possible seasonal effects from dark matter modulation arXiv:1106.1156 500 kg•year NaI detector sensitivity (2 - 4 keV) with 1, 2, and 5 dru background DM-Ice Snowmass - March 2013 9 Wednesday, March 6, 13

  10. 7. Experimental Challenges • Development of Ultra-pure NaI powder and crystals by ANAIS, Princeton, KIMS, DM-Ice... (see also F . Calaprice’s talk) • ultra-pure developed • crystals grown w/ ~40 ppb potassium • currently tracking down 210 Pb R&D Crystals ANAIS Collaboration, Dec. 2012 • Maintaining the capability to drill 70cm dia. 2500 m deep holes at the South Pole • 86 holes, up to 20 holes, in one season demonstrated by IceCube • Most of the equipment still at S. Pole but slowly being reassigned • Key personnel still available Drill & Deployment Towers IceCube Drill - 3/4/2013 Blaise Kuo Tiong DM-Ice Snowmass - March 2013 10 Wednesday, March 6, 13

  11. 8. Annual Modulation Detector Uptime: DM-Ice17 • Commissioning and optimization from Feb - June 2011 • Data run since June 2011 • 99.8% uptime for most weeks with well defined down time for occasional power cycling + pedestal and dark noise runs 7 days/point DM-Ice Snowmass - March 2013 11 Wednesday, March 6, 13

  12. Detector Monitoring: DM-Ice17 • Monitored quantities: • Temperature of the boards • ~10°C above surrounding ice • Fast (2-3 weeks) decrease during freeze-in • slower decrease over a few data run months after freeze-in • Pressure follows similar trend as temperature (ADC resolution limited) • Values recorded every 2 sec. before April 2012. Every 60 sec. since April 2012. data run DM-Ice Snowmass - March 2013 Wednesday, March 6, 13

  13. Detector Monitoring: DM-Ice17 • High voltage of each PMT • commissioning run until day 167 data run • Single PMT total trigger rate • General decay over time Trigger rate (individual PMT) • single trigger rate variation seems data run mostly in the noise change monitoring frequency • coincidence trigger rate at low energy under study DM-Ice Snowmass - March 2013 Wednesday, March 6, 13

  14. 9. Unique Capabilities Gran Sasso Canfranc PICO-LON Gran Sasso Northern DAMA/Libra ANAIS KIMS Princeton-NaI 250kg 250 kg Hemisphere etc... R&D running starting in 2014? South Pole ANDES Lab Southern DM-Ice (proposed) ice rock Hemisphere 17 kg running expected start R&D for 250 kg 2018 2017 under development Several Groups conducting ultra-pure crystal with several vendors to go to the full scale DM-Ice: • NaI dark matter search in an entirely different environment • South Pole offers: • Ultra-clean and ultra-stable environment • Seasonal variation unambiguously different from dark matter modulation • IceCube offers muon monitoring and veto as well as experience • NSF-run South Pole Station for logistical support DM-Ice Snowmass - March 2013 14 Wednesday, March 6, 13

  15. 10. Determining WIMP properties and astrophysical parameters • DAMA sees annual modulation at 9 σ ✴ ... but is it dark matter? • 15 years since first claim of observation of modulation • alternate hypotheses (backgrounds) raised but no definitive answers • NaI in northern hemisphere will test background hypotheses • Southern hemisphere experiment test background AND dark matter hypotheses • As DM experiments grow bigger, there will be many unexplained near-threshold events. J. Hall, Aspen 2012 Time to figure out what’s going on in DAMA. DM-Ice Snowmass - March 2013 15 Wednesday, March 6, 13

  16. Imagine...& a&world&where&we&know&the&origin&of&DAMA’s&signal. Wednesday, March 6, 13

  17. DM-Ice Collaboration Shanghai Jiao Tang University Xiangdong Ji, Changbo Fu University of Wisconsin – Madison Penn State Reina Maruyama , Francis Halzen, Karsten Doug Cowen, Ken Clark Heeger, Albrecht Karle, Matthew Kauer, Carlos Pobes, Walter Pettus, Zachary NIST-Gaithersburg Pierpoint, Antonia Hubbard, Bethany Reilly Pieter Mumm University of Sheffield University of Stockholm Neil Spooner, Vitaly Kudryavtsev, Dan Walker, Chad Finley, Per Olof Hulth, Klas Hultqvist, Christian Walach Matt Robinson, L. Thompson, Sam Telfer, Calum McDonald DigiPen Charles Duba, Eric Mohrmann University of Alberta Darren Grant Boulby Underground Science Facility Sean Paling University of Illinois at Urbana-Champaign SNOLAB Liang Yang Bruce Cleveland Fermilab Lauren Hsu *Special Thanks to the IceCube Collaboration* DM-Ice Snowmass - March 2013 17 Wednesday, March 6, 13

Download Presentation
Download Policy: The content available on the website is offered to you 'AS IS' for your personal information and use only. It cannot be commercialized, licensed, or distributed on other websites without prior consent from the author. To download a presentation, simply click this link. If you encounter any difficulties during the download process, it's possible that the publisher has removed the file from their server.

Recommend


More recommend