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| Format: | Preprint |
| Published: |
2026
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| Subjects: | |
| Online Access: | https://arxiv.org/abs/2602.15386 |
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| _version_ | 1866911451906572288 |
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| author | Karpikov, Ivan |
| author_facet | Karpikov, Ivan |
| contents | High flux of geoantineutrinos $^{40}$K and geoneutrinos $^{40}$K ($^{40}$K-geo-($\barν + ν$)) 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. |
| format | Preprint |
| id |
arxiv_https___arxiv_org_abs_2602_15386 |
| institution | arXiv |
| publishDate | 2026 |
| record_format | arxiv |
| spellingShingle | Potassium influence on Earth's mantle convection and Borexino data Karpikov, Ivan High Energy Physics - Phenomenology High flux of geoantineutrinos $^{40}$K and geoneutrinos $^{40}$K ($^{40}$K-geo-($\barν + ν$)) 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. |
| title | Potassium influence on Earth's mantle convection and Borexino data |
| topic | High Energy Physics - Phenomenology |
| url | https://arxiv.org/abs/2602.15386 |