Výsledky vyhledávání - "Bolshakov, V. N."

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Geoantineutrino Spectrum, 3He/4He-ratio Distribution in the Earth's Interior and Slow Nuclear Burning on the Boundary of the Liquid and Solid Phases of the Earth's Core

Autor: Rusov, V. D., Pavlovich, V. N., Vaschenko, V. N., Tarasov, V. A., Zelentsova, T. N., Bolshakov, V. N., Litvinov, D. A., Kosenko, S. I., Byegunova, O. A.

The description problem of geoantineutrino spectrum and reactor antineutrino experimental spectrum in KamLAND, which takes place for antineutrino energy \~2.8 MeV, and also the experimental results of the interaction of uranium dioxide and carbide wi

Externí odkaz: http://arxiv.org/abs/nucl-th/0605025

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Geoantineutrino Spectrum and Slow Nuclear Burning on the Boundary of the Liquid and Solid Phases of the Earth's core

Autor: Rusov, V. D., Pavlovich, V. N., Vaschenko, V. N., Tarasov, V. A., Zelentsova, T. N., Litvinov, D. A., Kosenko, S. I., Bolshakov, V. N., Khotyaintseva, E. N.

The problem of the geoantineutrino deficit and the experimental results of the interaction of uranium dioxide and carbide with iron-nickel and silica-alumina melts at high pressure (5-10 GPa) and temperature (1600- 22000 C) have induced us to conside

Externí odkaz: http://arxiv.org/abs/hep-ph/0402039

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Antineutrino Spectrum of the Earth and the Problem of Oscillating Geoantineutrino Deficit

Autor: Rusov, V. D., Pavlovich, V. N., Vaschenko, V. N., Tarasov, V. A., Litvinov, D. A., Bolshakov, V. N., Khotyaintseva, E. N.

The estimations of integral intensity and energy spectrum of geoantineutrino on the Earth's surface (in the absence of oscillations) from different radioactive sources (U, Th and K) are obtained on the basis of temporal evolution analysis of radiogen

Externí odkaz: http://arxiv.org/abs/hep-ph/0312296

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