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The physicochemical mechanism of the formation of planetary systems


The planets and their satellites are formed in accordance with similar mechanisms as a result of spatially periodic condensation of gaseous matter during the formation of the central body.

Using the diffusion theory one can calculate the age of the planets and explain the nature of the Titius-Bode law.

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Notes and References

  1. [1]

    Arrhenius, G. and Alfvén H.: 1976,Evolution of the Solar System, National Aeronautics and Space Administration, Washington, D. C., 1–599.

    Google Scholar 

  2. [2]

    Brandt, J. C. and Hodge, P. W.: 1967,Solar System Astrophysics, McGraw-Hill Book Company Inc., New York, 1964; Russian translation, Mir, Moscow, 1–488.

    Google Scholar 

  3. [3]

    Safronov, V. S.: 1969,Evolution of Pre-Planetary Nebula and Formation of Planets, Nauka, Moscow, 1–244.

    Google Scholar 

  4. [6]

    Nieto M. M.: 1976,The Titius-Bode Law of Planetary Distances: Its History and Theory, Pergamon Press, Oxford, 1972; Russian translation, Mir, Moscow, 1–190.

    Google Scholar 

  5. [7]

    Liesegang, R.: 1897,Z. Physik. Chem. 23, 365.

    Google Scholar 

  6. [8]

    Zeldovich, Ya. and Todes, O. M.: 1949,Zh. Fiz. Khim. 23, 180.

    Google Scholar 

  7. [9]

    Wagner, C.: 1950,J. Colloid Sci. 5, 85.

    Google Scholar 

  8. [10]

    Hirschfelder, J. O., Curtiss, C. F. and Bird, R. B.: 1961,Molecular Theory of Gases and Liquids, John Wiley and Sons, New York, 1954; Russian translation, IL, Moscow, 19–29.

    Google Scholar 

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Gladyshev, G. The physicochemical mechanism of the formation of planetary systems. The Moon and the Planets 18, 217–221 (1978).

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  • Central Body
  • Planetary System
  • Diffusion Theory
  • Physicochemical Mechanism
  • Gaseous Matter