Formation of the Solar System: A New Theory of the Creation by V.I. Ferronsky, S.V. Ferronsky

By V.I. Ferronsky, S.V. Ferronsky

Analysis of the orbital movement of the Earth, the Moon and different planets and their satellites resulted in the invention that each one our bodies within the sunlight approach are relocating with the 1st cosmic pace in their proto mom and dad. The suggest orbital pace of every planet is the same as the 1st cosmic speed of the Protosun, the radius of that's equivalent to the semi-major axis of the planet’s orbit. an analogous applies for the planets’ satellites. all of the small planets, comets, different our bodies and the solar itself persist with this legislation, a discovering that has additionally been confirmed through astronomical observations. The theoretical strategies in line with the Jacobi dynamics clarify the method of the process construction and rot, in addition to the character of Kepler’s laws.

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McGraw Hill, New York, pp 357–424 Newton I (1934) Mathematical principles of natural philosophy and his system of the world (Trans. from Latin by Andrew Mott, 1729). Cambridge University Press, Cambridge Schmidt OY (1957) Four lectures on origin of the earth. Academy of Sciences of USSR Publishing House, Moscow Spenser JH (1956) The origin of the solar system. In: Physics and chemistry of the earth, vol 1. Pergamon, London, pp 1–16 Chapter 2 Physical Meaning of Hydrostatic Equilibrium of Celestial Bodies Abstract It was shown earlier that the fundamentals of classical dynamics, based on hydrostatics, do not satisfy the solution of dynamical problems of celestial bodies (Ferronsky and Ferronsky 2010; Ferronsky et al.

V. ” At that time, the thoughts of scientists were engaged with how to solve the principle problem of a body’s orbital motion. Now, we search its correct solution. Recall briefly the conditions of a body in hydrostatic equilibrium. By definition, hydrostatics is a branch of hydromechanics which studies the equilibrium of a liquid and gas and the effects of a stationary liquid on immersed bodies relative to the chosen reference system. 1) where is the pressure, is the density, and F is the mass force.

36) where u, v, and ! are the components of the velocity of liquid particles; p is the liquid pressure; is the density; and X, Y, and Z are the components of the volumetric forces. , the pressure and the density as a function of the coordinates with known values of X, Y, Z, and the given boundary conditions. For that purpose, in addition to Eq. 36), the equation of continuity is written in the form @ @ . u/ @ . v/ @ . 37) If the density of liquid depends only on pressure, then the extra equation of state will be presented by the relation D f (p), and for the incompressible liquid, it is D const.

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