Physics – Geophysics
Scientific paper
2005-08-02
Earth Planet.Sci.Lett.238:235-247,2005
Physics
Geophysics
19 pages, 6 tables, 7 figures; accepted for publication in Earth and Planetary Science Letters
Scientific paper
10.1016/j.epsl.2005.06.061
In preparation to the experimental results which will be available in the future, we study geo-neutrino production for different models of mantle convection and composition. By using global mass balance for the Bulk Silicate Earth, the predicted flux contribution from distant sources in the crust and in the mantle is fixed within a total uncertainty of +-15%. We also discuss regional effects, provided by subducting slabs or plumes near the detector. In four years a five-kton detector operating at a site relatively far from nuclear power plants can achieve measurements of the geo-neutrino signal accurate to within +-5%. It will provide a crucial test of the Bulk Silicate Earth and a direct estimate of the radiogenic contribution to terrestrial heat.
Fiorentini Gianni
Lissia Marcello
Mantovani Fabio
Vannucci Riccardo
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