1 / 20

Potassium Geo-neutrino Detection

Potassium Geo-neutrino Detection. Mark Chen Queen’s University Neutrino Geophysics, Honolulu, Hawaii December 15, 2005. Why Potassium Geo-neutrinos?. 16% of the radiogenic heat is from 40 K (based upon models) 3 rd isotope after 238 U and 232 Th largest flux!

akiva
Download Presentation

Potassium Geo-neutrino Detection

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Potassium Geo-neutrino Detection Mark Chen Queen’s University Neutrino Geophysics, Honolulu, Hawaii December 15, 2005

  2. Why Potassium Geo-neutrinos? • 16% of the radiogenic heat is from 40K (based upon models) • 3rd isotope after 238U and 232Th • largest flux! • K may reside in the Earth’s core [V. Rama Murthy’s talk] • K/U ratio in chondrites > in the crust • where is the potassium? do we really know how much there is?

  3. 40K Decay • 89.28% Qb=1.311 MeV • 10.72% QEC=1.505 MeV • 10.67% to 1.461 MeV state (En = 44 keV) • 0.05% to g.s. (En = 1.5 MeV) 0.0117% isotopic abundance

  4. 40K Spectrum threshold for [figure from KamLAND Nature paper]

  5. Potassium Geo-neutrino Fluxes • (5-15) × 106 cm−2 s−1for the antineutrinos • (5-15) × 105 cm−2 s−1for the 44 keV ne • (2-6) × 103 cm−2 s−1for the 1.5 MeV ne • compare to 1.44 MeV pep solar neutrinos 1.42 × 108 cm−2 s−1 you can probably forget about the ne’s

  6. 40K Detection • -e scattering • not worth investigating due to solar ne (pep, CNO) • NC nuclear excitation • not distinctive from ne or g backgrounds • NC coherent neutrino-nucleus scattering [J. Collar’s talk] • again, not distinctive from solar neutrinos • CC processes to be examined…

  7. CC Reactions for Antineutrinos • inverse b-decay • inverse b-decay requires Qb + 1.022 MeV • 40K antineutrinos endpoint 1.311 MeV • need to find Qb < 0.289 MeV • resonant orbital electron capture • resonant capture only useful over a small range of energy…not for 40K

  8. Krauss, Glashow & Schramm • Nature paper (1984) proposed radiochemical detection; listed several possible antineutrino targets with product lifetime > 1 day • e.g. 3He →3H, Qb = 18.6 keV, t½ = 12.3 years • desirable to have small logft for large cross section • ~2000 atoms produced per year per kton • ~1/3 of those come from 40K • 35Cl→35S, Qb = 167 keV, t½ = 88 days • ~2 atoms produced by geo-neutrinos per year per kton

  9. CC Antineutrino Capture • e+ is produced • detection 1.022 MeV minimum visible energy • b--decay follows • long-lived: consider radiochemical (e.g. 3H, 35S) • short-lived: consider detection – disadvantage is the distribution of b- energies and low energies

  10. KGS Error • antineutrino captures on 64Zn (0+→1+ allowed transition) • 64Cu decays to 64Ni • KGS were thinking radiochemical detection of the stable 64Ni…mentioned in paper • error: sensitive to “40K, 238U, 232Th” X

  11. Low Qb Targets for 40K • 3He, 14N, 33S, 35Cl, 63Cu • potentially sensitive to 40K geo-neutrinos • allowed transitions to ground state • KGS also identified some allowed transitions to excited states for antineutrino capture • e.g. 79Br, 151Eu have low enough Q

  12. KGS Missed One! this one is sensitive to 40K geo-neutrinos!

  13. 106Cd for Potassium Geo-neutrinos • isotopic abundance 1.25% • 0+→1+ allowed transition to the 106Ag g.s. • Qb = 194 keV, detectable e+ (1.02-1.12 MeV) • followed by a t½=24 min EC decay (a big one) • can consider direct detection of reaction • could also consider radiochemical detection of Pd • it’s a positron decay also! (not a tiny branch) • “double-positron” signature potentially distinctive

  14. Direct Detection or Radiochemical? • (n,p) reactions produce background isotopes affecting a radiochemical measurement • stopped m− capture makes a background that affects only radiochemical it’s the prompt positron that rejects the above backgrounds → deep underground location certainly helps with the above • potassium geo-neutrino event rates are going to be so small you really want zero backgrounds…direct detection is better, if possible • delayed coincidence positron-positron!

  15. Cadmium Detectors • CdWO4 scintillating crystals • 106Cd enrichment possible (Kiev group has enriched 116Cd for double beta decay search)

  16. More Cadmium Detectors • CdZnTe semiconductor detectors • COBRA experiment is testing pixelated anodes for vertex reconstruction and tracking • 1 cm3 array of CdZnTe makes a good positron identifier (separately detect 511 keV g’s)? • COBRA mentions 106Cd as an interesting b+b+ candidate geo-neutrinos “catalyze” the 106Cd b+b+ decay

  17. Backgrounds from Double Beta? • actual double beta decay of 106Cd produces both positrons at once • antineutrino capture produces two positrons separated by t½=24 min • how about accidental coincidences (24 min window) • 113Cd (12.2% isotopic abundance) b decay (Q = 320 keV) • 14.2 kHz (for 1 ton of 113Cd) • 116Cd (7.5% isotopic abundance) bb decay (Q = 2.8 MeV) • 3.7 decays per second (for 1 ton of 116Cd) high isotopic purity of 106Cd is needed unless you have positron identification

  18. nucl-ex/0508016

  19. Geo-neutrino Signal Rates 106Cd • log ft = 4.7  • Qb = 194 keV  • remember Qthreshold = 1.216 MeV; 40K antineutrinos are emitted up to 1.311 MeV in the few to ~ten events per year per kiloton

  20. Summary • going beyond the Krauss, Glashow and Schramm paper…there is a new idea for 40K geo-neutrino detection using 106Cd • 106Cd could be made into scintillating crystals or semiconductor detectors • distinctive “double-positron” signature

More Related