The daemon kernel of the sun

Abstract

The daemon-stimulated proton decay is fully capable of providing an appreciable part of the Sun luminosity as well as nonelectron flavor component in the solar neutrino flux. This follows (1) from our experiments on detection of negative daemons in Earth-crossing orbits, which give ∆τ ex ∼ 1 µs for the decay time of a daemon-containing proton (Drobyshevski et al, 2001), and (2) from an estimate of the total number of daemons which could be captured by the Sun from the Galactic disk (up to ∼2.4·10 30 ) (Drobyshevski, 1996). Because of their huge mass (∼3·10 -5 g), the captured daemons settle down to the Sun's center to form there a kernel a few cm in size. The Earth has also such a kernel (Drobyshevski, 2001(Drobyshevski, , 2002. The outside protons diffuse gradually into the kernel to decay there with a release of energy. Physically sound estimates of the parameters of an isothermal kernel can be obtained under the assumption that it consists mainly of negative daemons. Proton decay maintains a high temperature of the daemon gas (up to ∼10 11 −10 12 K), which makes it physically collisionless and prevents kernel collapse into a black hole.