Observation of Geo-Neutrinos

TL;DR

This paper reports the first detection of geo-neutrinos using the Borexino detector, providing insights into Earth's interior and ruling out a high-power geo-reactor hypothesis with high statistical significance.

Contribution

It presents the first observation of geo-neutrinos at over 3σ significance, demonstrating the detector's capability to probe Earth's radioactive processes.

Findings

Detected 9.9 geo-neutrino events with high confidence

Rejected the hypothesis of a geo-reactor above 3 TW in Earth's core

Measured reactor anti-neutrinos consistent with oscillation models

Abstract

Geo-neutrinos, electron anti-neutrinos produced in beta decays of naturally occurring radioactive isotopes in the Earth, are a unique direct probe of our planet's interior. We report the first observation at more than 3$\sigma$ C.L. of geo-neutrinos, performed with the Borexino detector at Laboratori Nazionali del Gran Sasso. Anti-neutrinos are detected through the neutron inverse beta decay reaction. With a 252.6 ton-yr fiducial exposure after all selection cuts, we detected 9.9^{+4.1}_{-3.4}(^{+14.6}_{-8.2}) geo-neutrino events, with errors corresponding to a 68.3%(99.73%) C.L. From the $\ln{\cal{L}}$ profile, the statistical significance of the Borexino geo-neutrino observation corresponds to a 99.997% C.L. Our measurement of the geo-neutrinos rate is 3.9^{+1.6}_{-1.3}(^{+5.8}_{-3.2}) events/(100ton-yr). This measurement rejects the hypothesis of an active geo-reactor in the Earth's core with a power above 3 TW at 95% C.L. The observed prompt positron spectrum above 2.6 MeV is compatible with that expected from european nuclear reactors (mean base line of approximately 1000 km). Our measurement of reactor anti-neutrinos excludes the non-oscillation hypothesis at 99.60% C.L.