2007
DOI: 10.1029/2005jb004212
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Geoantineutrino spectrum and slow nuclear burning on the boundary of the liquid and solid phases of the Earth's core

Abstract: [1] We give an alternative description of the data produced in the KamLAND experiment. Assuming the existence of a natural nuclear reactor on the boundary of the liquid and solid phases of the Earth's core, a geoantineutrino spectrum is obtained. This assumption is based on the experimental results of V. Anisichkin and his collaborators on the interaction of uranium dioxide and uranium carbide with iron-nickel and silica-alumina melts at high pressure (5-10 GPa) and temperature (1600-2200°C), which led to the … Show more

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Cited by 37 publications
(96 citation statements)
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“…With that end in view we have compared the Gaussian ensemble statistics (41) with well-known computational experimental data [8,[23][24][25][26][27] and have obtained a good accordance of calculation data with the theoretical dependence, which is described by the Gaussian symplectic ensemble statistics (see Table 1 and Figure 4). Thus, we can conclude that the wave velocity u (see Equation (34)) is predetermined by the following approximate equality…”
Section: The Wigner Quantum Statistics and Generalized Condition For mentioning
confidence: 99%
See 1 more Smart Citation
“…With that end in view we have compared the Gaussian ensemble statistics (41) with well-known computational experimental data [8,[23][24][25][26][27] and have obtained a good accordance of calculation data with the theoretical dependence, which is described by the Gaussian symplectic ensemble statistics (see Table 1 and Figure 4). Thus, we can conclude that the wave velocity u (see Equation (34)) is predetermined by the following approximate equality…”
Section: The Wigner Quantum Statistics and Generalized Condition For mentioning
confidence: 99%
“…The corresponding system of differential equations, which describes the kinetics of Feoktistovs U-Pu fuel cycle with consideration of delayed neutrons, i.e., the kinetics of initiation and propagation of neutron-fission wave n(x, t), is as follows [23] ∂n(x, t) ∂t…”
Section: Computation 3d-experiments and Verification Of The Wigner Quamentioning
confidence: 99%
“…KamLAND data restrict the power of an Earth-centered georeactor to be less than 20% of the terrestrial heat flow [Abe et al, 2008]. This eliminates some georeactor models [Rusov et al, 2007] yet allows others, including one recently highlighted model that suggests a georeactor at the core-mantle boundary [Ball, 2008]. An antineutrino detector operating at a location where the flux from human-made reactors is minimal, such as at Hanohano in the mid-Pacific, would be sensitive to georeactors with power as low as a few percent of the terrestrial heat flow.…”
Section: Investigating the Deep Earthmentioning
confidence: 99%
“…Now let us consider geophysical consequences induced by the significant increase of the Earth liquid core temperature. It is known that the induced fission cross-section of 238 U, which is the natural fuel for the georeactor (Rusov et al, 2007), strongly depends on the ambient temperature Т (σ f ~T 4 ) in the resonance region. It means that the nuclear burning rate on the boundary of the liquid and solid phases of the Earth core increases with ambient temperature growth.…”
Section: Computational Experimentsmentioning
confidence: 99%
“…Moreover, this low interaction between solar wind and the Earth magnetosphere is veiled by the intrinsic variations of the Earth's magnetic field due to the specificities of the Earth liquid core kinetics and the stochastic properties of magnetic field energy source, i.e. slow nuclear burning on the boundary of liquid and solid phases of the Earths core (the georeactor of 30 TW) (Rusov et al, 2007).…”
Section: Computational Experimentsmentioning
confidence: 99%