Neutrino oscillations investigation of the base-of-the-mantle structure: simulation tools and preliminary results
- 1Institut de Physique du Globe de Paris, Université Paris Cité, Paris, France
- 2Laboratoire AstroParticule et Cosmologie, Université Paris Cité, Paris, France
- 3Department of Earth and Spatial Sciences, University of Idaho, Moscow, ID, USA
- 4Laboratoire de Géologie de Lyon : Terre, Planètes, Environnement, École Normale Supérieure de Lyon, Université de Lyon, Université Claude Bernard, Lyon, France
- 5Institut Universitaire de France, Paris, France
The origin of Large Low-Velocity Provinces (LLVPs) at the base of mantle remains a mystery, but particle physics may be able to provide another piece of the puzzle. Using a phenomenon known as neutrino oscillation, atmospheric neutrino experiments are sensitive to the electron number density inside the Earth, which is complementary to the information seismology can provide. In order to reveal lateral heterogeneities in density and chemical composition such as those expected for LLSVPs across the Earth’s lower mantle, we have developed a numerical method that allows us to compute the sensitivity of neutrino oscillation data to 3D Earth structure. Based on this approach, we will present some preliminary assessment of the potential resolving power of ongoing and future neutrino experiments.
How to cite: Pestes, R., Coelho, J., Deniz Hernandez, Y., Durand, S., Fuji, N., Mittelstaedt, E., and Van Elewyck, V.: Neutrino oscillations investigation of the base-of-the-mantle structure: simulation tools and preliminary results, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-17413, https://doi.org/10.5194/egusphere-egu24-17413, 2024.