On Geoneutrinos

Bezrukov, L.; Kurlovich, A. S.; Лубсандоржиев, Б.; Sinev, V. V.; Zavarzina, V. P.; Morgalyuk, V. P.

doi:10.1051/epjconf/201612502004

Cited by 4 publications

(1 citation statement)

References 12 publications

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“…In the previous 19th International Seminar on High Energy Physics, Quarks-2016, we discussed the problem of geo-neutrino [3]. In this work we demonstrated that the experimental data on geo-neutrinos allow to admit that masses of U, Th and K in the Earth can be up to m U = 1.7 • 10 17 kg, m T h = 6.7 • 10 17 kgandm K /m Earth ∼ 2%.…”

Section: Introductionmentioning

confidence: 80%

Geo-neutrino, Earth heat flux, Earth electricity

et al. 2018

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We discussed the idea of big value of potassium abundance in the Earth. We showed that Borexino single event spectrum permit the potassium abundance up to 2% instead of the CNO neutrino flux contribution. Works [5], [6] introduce the idea that fast α particles are appeared in nuclear processes in solar core plasma. The reactions of these α particles with CNO nuclei can suppress the CNO neutrino flux. We demonstrated the connection between the existence of Earth’s electric field and the big value of 40K geo-neutrino flux because the both phenomena are the sequences from Hydride Earth model.

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Section: Introductionmentioning

confidence: 80%

Geo-neutrino, Earth heat flux, Earth electricity

et al. 2018

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How Geoneutrinos can help in understanding of the Earth heat flux

Bezrukov

Kurlovich

Лубсандоржиев

et al. 2017

J. Phys.: Conf. Ser.

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Abstract. The Hydride Earth model predictions of geoneutrino flux and intrinsic Earth heat flux are discussed. The geoneutrino flux predicted by the model can be adjusted to the experimental one. The predicted intrinsic Earth heat flux is significantly larger than model dependent experimental value obtained under assumption that the main heat transfer mechanism is a thermal conductivity. We introduce an additional mechanism of heat transfer in the Earth's crust, namely the energy transfer by hot gases produced in the Earth crust at great depths. The experimental data supporting this idea, in particular the temperature profiles measured in the Kola super deep borehole, are discussed.

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