The KamLAND and Borexino experiments have observed, each at ~4σ level, signals of electron antineutrinos produced in the decay chains of thorium and uranium in the Earth's crust and mantle (Th and U geoneutrinos). Various pieces of geochemical and geophysical information allow an estimation of the crustal geoneutrino flux components with relatively small uncertainties. The mantle component may then be inferred by subtracting the estimated crustal flux from the measured total flux. We find that crust-subtracted signals show hints of a residual mantle component, emerging at ~2.4σ level by combining the KamLAND and Borexino data. The inferred mantle flux, slightly favoring scenarios with relatively high Th and U abundances, within ~1σ uncertainties is comparable to the predictions from recent mantle models.

The Earthʼs mantle and geoneutrinos.

FIORENTINI, Giovanni;MANTOVANI, Fabio;XHIXHA, Gerti
2013

Abstract

The KamLAND and Borexino experiments have observed, each at ~4σ level, signals of electron antineutrinos produced in the decay chains of thorium and uranium in the Earth's crust and mantle (Th and U geoneutrinos). Various pieces of geochemical and geophysical information allow an estimation of the crustal geoneutrino flux components with relatively small uncertainties. The mantle component may then be inferred by subtracting the estimated crustal flux from the measured total flux. We find that crust-subtracted signals show hints of a residual mantle component, emerging at ~2.4σ level by combining the KamLAND and Borexino data. The inferred mantle flux, slightly favoring scenarios with relatively high Th and U abundances, within ~1σ uncertainties is comparable to the predictions from recent mantle models.
2013
Geoneutrino, Earth's mantle, KamLAND, Borexino, Terrestrial radiogenic heat power
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11392/1823708
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