Contribution of Ue3 to geo-neutrino flux
| dc.creator | Mohanty, Subhendra | |
| dc.date | 2005-02-27 | |
| dc.date.accessioned | 2026-07-07T03:54:27Z | |
| dc.date.available | 2026-07-07T03:54:27Z | |
| dc.description | We show that a non-zero Ue3 close to the CHOOZ bound ($Sin^2 2 θ_{13} \simeq 0.16$ 90% CL) can change the geo-neutrino flux by 12%. Geo-neutrino detection in Kamland with a exposure of $3 \times 10^{32} proton-years$ is sensitive to $Sin^2 2 θ_{13}$ to the level of $0.2 (1 σ)$. For the same exposure a detector close to Himalayas can probe $Sin^2 2 θ_{13}$ down to $0.15 (1 σ)$ due to higher geo-neutrino flux from the Tibetan plate. | |
| dc.description | 2 figures | |
| dc.identifier | https://arxiv.org/abs/hep-ph/0502241 | |
| dc.identifier | http://arxiv.org/abs/hep-ph/0502241 | |
| dc.identifier.uri | http://salesiana.dossiersoluciones.com/handle/123456789/44243 | |
| dc.subject | High Energy Physics - Phenomenology | |
| dc.title | Contribution of Ue3 to geo-neutrino flux | |
| dc.type | text |