https://doi.org/10.1140/epjc/s10052-025-14338-z
Regular Article - Theoretical Physics
Neutrino oscillation tomography of the Earth with the Hyper-Kamiokande detector
1
Kavli IPMU (WPI), UTIAS, The University of Tokyo, 277-8583, Kashiwa, Chiba, Japan
2
INFN/SISSA, Via Bonomea 265, 34136, Trieste, Italy
3
Institute of Nuclear Research and Nuclear Energy, Bulgarian Academy of Sciences, 1784, Sofia, Bulgaria
Received:
28
January
2025
Accepted:
21
May
2025
Published online:
26
June
2025
Using PREM as a reference model for the Earth density distribution we investigate the sensitivity of the Hyper-Kamiokande (HK) detector to deviations of the Earth (i) core average density , (ii) lower mantle average density
) and (iii) upper mantle average density
, from their respective PREM densities. The analysis is performed by studying the effects of the Earth matter on the oscillations of atmospheric
,
,
and
. We implement the constraints on the variations of
,
and
following from the precise knowledge of the Earth mass
and moment of inertia
, as well as from the requirement that the Earth be in hydrostatic equilibrium (EHE). These constraints limit in the case of the three layer Earth density structure we are considering the maximal positive deviation of
from its PREM value to
. Considering the case of normal ordering (NO) of neutrino masses, we present results which illustrate the dependence of sensitivity to the core, lower and upper mantle average densities on the energy and zenith angle resolutions and on the value of
. We show, in particular, that in the “nominal” case of neutrino energy resolution
and zenith angle resolution
and for, e.g.,
, HK can determine the average core density
at
C.L. after 6500 days of operation with an uncertainty of (
14.5%)/+39.5% ((
9.3%/+31.7%). In the ”more favorable” case of
and
, and if
, the core density would be determined at
C.L. with an uncertainty of (
8.3%)/+9.8% ((
9.2%)/+11.3%).
© The Author(s) 2025
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Funded by SCOAP3.