Abstract:
The general regularities of the redistribution of secondary element compositions in the biosphere between the solid and liquid phases (lithosphere, hydrosphere) were established. This process is most active in biogeochemical barriers, as a result of this process is the overall relative increasing in the solid phase a concentration of chemical elements by decreasing their prevalence in the environment. A quantitative evaluation of the universal constants of the nonlinearity of the evolution of the elemental composition of the biosphere was carried out.
Key words:nonlinearity, general laws, methodology, biosphere, elemental composition, living matter, lithosphere, hydrosphere.
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