Potassium influence on Earth's mantle convection and Borexino data
Abstract
High flux of geoantineutrinos 40K and geoneutrinos 40K (40K-geo-( + )) can be obtained from reanalysis of the Borexino Phase III data. Large amounts of 40K 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 40K.
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