1. Taking a picture of the Earth’s Interior with Geoneutrinos Honolulu, HI 12/15/2005 Kathrin A. Hochmuth MPI für Physik München

2. Outline: The earth` s interior Theoretical angular distribution of geoneutrinos Measuring geoneutrinos with large volume liquid scintillation detectors (LENA detector)

3. The Earth’s Interior Elementmean life (Gyr) # of neutrinos Isotopic abundance Energy released 40 K1.8410.0117%~1.4 MeV 238 U6.45699.2745%51.7 MeV 232 Th20.34100%42.5 MeV

4. What do we know about Earth’s Interior? Density obtained by monitoring seismic activities Bulk Silicate Earth Model for Crust- Mantle based e.g. on planetary and meteoritic probes Earth’s Interior still a mystery But: deepest drill-holes ~ 10km Deepest mantle material (volcanoes) ~ 100km No detailed information about the core! Only 50% of terrestrial heat flow explained!

5. What to use … Bulk Silicate Earth Model Preliminary Reference Earth Model Laboratory Experiments suggesting potassium- iron alloys in the core http://www.edu.pe.ca/southernkings/compositionch.htm

6. First steps to get a neutrino picture of the earth Using the density profile given in the Preliminary Reference Earth Model to Divide Earth into shells of constant density with Work w/ B.D. Fields

7. Simple Illustrations

8. Towards a real model Bulk Silicate Earth Model Preliminary reference earth model Neutrino Oscillations: L V ~10km vs. L M ~1000km Neglect matter effects

10. With Core……

12. Sun vs. Earth http://elvis.phys.lsu.edu/svoboda/superk.html

13. Measurable Spectra U/Th ratio measurable Conclusions for K abundance possible Note: Only 13% of uranium neutrinos and 9% of thorium above 1.8 MeV

14. Future Measurements Main backgound 13 C( ,n) 16 O reduced Large distance to nuclear power plants Increased detector volume (here 50 kton) Lena

15. Event Rates in 50 kton Continental Crust 4130 Oceanic Crust 850 Continental 9TW core 4600 Oceanic 9TW core 1300 Continental 18TW core 5020 Oceanic 18TW core 1720

16. Angle dependent measurements??? Momentum conservation (proton at rest) 2 MeV  cos  3.2 MeV  cos 

17. Challenging… Dependent on: Displacement (fixed:theory~1.5cm;CHOOZ~1.9cm) Light yield (scintillator properties) Loading of scintillator (Gadolinium, Lithium; stability?) Precision of Neutron Detection (Detector Design)

18. crust Core (mantle) Radial curve for 300 pe/MeV In collaboration with L.Oberauer, F.v.Feilitzsch, W.Potzel

19. unloaded Gd loaded

20. Mantle model Light yield 300pe/MeV 3  effect: 66060 events Gd loaded 250400 events unloaded PXE

21. Summary-what can we do? Test the U/Th of Bulk Silicate Earth Test how much of the heat is primordial Get the distribution of radioactive elements throughout the earth Test if there are radioactive elements (only potassium?) in the core Possibility of Earth Tomography

22. References: Fields, Hochmuth [hep-ph/0406001] Mantovani, Carmignani, Fiorentini, Lissia [hep-ph/0309013] Rama Murthy, van Westrenen, Fei, Nature 423 (2003) Gessmann, Wood, Earth Planet Sci Lett, 200 (2002) Lee, Jeanloz, Geophys Res Lett, 30 (2003) Dziewonski, Anderson, Phys Earth Plan Int 25, 297 (1981) Table of Nuclides: http://atom.kaeri.re.kr/index.htmlhttp://atom.kaeri.re.kr/index.html Super-K: http://elvis.phys.lsu.edu/svoboda/superk.htmlhttp://elvis.phys.lsu.edu/svoboda/superk.html Vogel, Beacom: arxiv:hep-ph/9903554 Chooz:arxiv:hep-ex/9906011 http://arxiv.org/abs/hep-ph/0401221 http://kamland.lbl.gov/Pictures/ http://www.greeklandscapes.com/maps/satellite.html http://virtual.finland.fi/netcomm/news/showarticle.asp?intNWSAID=27070

23. Merry Xmas!