4.. De r p h 0 Its V. F. - The pr~ncipal planetary source of natural waters. Intern. Geol. Review, Washington 1962, v. 6, nr 8.
5. Do r ph 0 lz W. F. - Gidrosfera i chlor. LitoL polezn. iskop., 1963, nr 1.
6. D {) r p h 0 I z W. F. - Opyt koliczestwiennoj charakteristiki ziemnoj gidrosfery i chlora. Dokl. AN SSSR, 1963, t. 150, nr 3.
7. D {) r u h 0
1
z W. F. - 0 glubinnoj gidrosfere. Sborn. ProbL proischozdienija niefti. GIN ANUkr. SSR, 1966.
SUMMARY
New" quantitative character of the Earth's hydro-spheres is given, one of these hydrospheres, i.e. the underground hydrosphere, being subdivided into:
1-the upper hydrosphere, free and physical-chemically bounded, and 2 - the lower hydrosphere, free ooly
in the supercritical fluidal state. Down to a depth of about 5 km, the free ground waters of the hyperge-nesis zone' distinguish themselves by a circular dy-namics, below - down to the Mohorovil!il: surface -by. a radial. dynamics upwards. The last phenomenon depends upon the potential difference between the upper aJIld ' lower parts of the llthosphere for all
kinds' of mechanical, thermal, chemical, electro-magnetic energy, a.o. This leads, by filtration and diffusion processes, to the transportation of fluid' upwards. The filtration of liquids is due
to
the difierence in mobility of constituents. The fluids move in the lower part of the lithosphere, too, pro-bably· also in the upper part of the Earth's mantle.The most part of the free lIlatural water, not only of the surface but also of the upper part of the hydrosphere, belongs to chloride mineralized and
brine-like solutions that make the hydrochlorozone of the Earth. These chloride waters from the upper parts of the hydrochlorozones no doubt belong to calcium and magnesium. ones; in the upper parts they change into
a
natrium. type here.The above planetary geochemical stratification may be explained by the mobility of bivalent calCium and magnesium ions, in comparison with the mono-valent natrium ions, under changing thermodynamical conditions in the lithosphere upwards.
8. Fir s 0 f f V. A. - The Earth's twin. Science News, v. 52, Penguin Books, Hormonds-Worth .. 1959.
9. Katterfeld G. N. - Lik Ziemli i je;lo proi-schozdienije, Moskwa, 1962.
10. Rub e y W. W. - Geologic history of sea water. Bull. Geo!. Soc. Am. 1951, v. 62.
11. W i ern ads k i j W. I. - Istorija prirodnych wad. Gos, chim. izd. Leningrad, 1933--36.
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