Speaker
Mr.
Valery Sinev
(INR RAS)
Description
Non direct observations demonstrate that Earth heat flux could be sufficiently larger than one measured by using of the temperature gradient method. Analysis of heat transfer channels also ensures that heat flux could be higher. At the moment data on 238U and 232Th antineutrino fluxes from KamLAND and Borexino measurements do not contradict the BSE model. Accurate measurement of all geoneutrino fluxes, including 40K antineutrino one, can clarify the situation.
Primary author
Mr.
Valery Sinev
(INR RAS)
Co-authors
Dr.
Leonid Bezrukov
(INR RAS)
