Potassium influence on Earth's mantle convection and Borexino data
High Energy Physics - Phenomenology
2026-02-18 v1
Abstract
High flux of geoantineutrinos K and geoneutrinos K (K-geo-()) can be obtained from reanalysis of the Borexino Phase III data. Large amounts of K should produce a significant heat flow that should affect Earth's internal processes. We present the results of the modeling of mantle convection taking into account the excess heat from K.
Keywords
Cite
@article{arxiv.2602.15386,
title = {Potassium influence on Earth's mantle convection and Borexino data},
author = {Ivan Karpikov},
journal= {arXiv preprint arXiv:2602.15386},
year = {2026}
}