Mathematics – Logic
Scientific paper
Dec 2007
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007agufm.p51c0667k&link_type=abstract
American Geophysical Union, Fall Meeting 2007, abstract #P51C-0667
Mathematics
Logic
5205 Formation Of Stars And Planets, 5455 Origin And Evolution, 5749 Origin And Evolution, 6040 Origin And Evolution
Scientific paper
In framework of the dichotomous conception of the Solar system formation /(Kompanichenko, 1992, 2005/) the origin of Earth-Moon system is considered in the common row with origin of the rest planet-satellite/(s/) systems. These systems have a lot of common peculiarities that emphasizes unity of their formation. Thus, almost all satellites turn with the same side to the maternal planets. According to the dichotomous hypothesis, all satellites were ejected from the maternal superheat planets about 4.5 Gyr. At the beginning of this process young Sun ejected superheat protoplanetary mass due to extraordinary high level of inner nonequilibrium. At this early stage of a star evolution the heat expansion may much prevail over the gravitational compression because of still insufficient mass of the synthesized heavy core. Division of some very young stars into two components was corroborated by the direct observations /(Mirabel and Rodriguez, 1999/). According to the model of Solar system formation, the triple cycle of dichotomy /(division into two components/) occurred: 1st cycle - formation of inner and outer components; 2nd - appearance of two inner and two outer components; 3rd - emergence of four inner and four outer solar planets. Then some of the superheat planets ejected satellites. The ejected from Jupiter protosatellite mass divided into 4 fragments during the double cycle of dichotomy. The following double cycle of dichotomy of each fragment had led to formation of 16 Jupiter's satellites. The spontaneous process of the initial protoplanetary mass destroying was accompanied by ejection of numerous smaller clots of matter transformed later on into hard asteroids, comets and meteorites. In context of this global process, dichotomy of the superheat Earth and Moon had led to much decrease of their energetic potential and transition to quieter character of evolution. The reduced level of inner nonequilibrium didn't allow the early Earth to eject some more superheat material, but provided its global differentiation. The following continuous geological renovation of Earth proceeds on the background of its gradual cooling and interrupts from time to time by failing splashes of endogenous activity. Reference. V. Kompanichenko /(2005/) Origin of Planetary Systems Due to Dichotomous Division of the Ejected Superheat Mass. Frontier Perspectives, 14/1, 14-25.
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