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arXiv · 2602.15386

Potassium influence on Earth's mantle convection and Borexino data

Ivan Karpikov
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Abstract

High flux of geoantineutrinos $^{40}$K and geoneutrinos $^{40}$K ($^{40}$K-geo-($\bar{\nu} + \nu$)) can be obtained from reanalysis of the Borexino Phase III data. Large amounts of $^{40}$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 $^{40}$K.

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Ivan Karpikov. 2026-02-17. Potassium influence on Earth's mantle convection and Borexino data. https://arxiv.org/abs/2602.15386

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