The Phenomenon of «Deep Water» Influx from the Earth's Interior and its Role in the Development of the Earth

A. I. Tikhonov, I. S. Kopylov

Abstract


The phenomenon of extensive permanent influx of the «deep-water» to the hydrosphere of the Earth characterized by a high content of various chemical components, including mineral and toxic elements of deep origin is considered. Results of analysis of large amount of experimental data suggest that «deep-water» is a source of formation and permanent supplement of the ocean water with stable salinity, chemical and isotopic composition, and the formation of various mineralized water deposits. «Deep-water» can cause formation of substandard water clusters within the underground fresh water fields, affecting their ecological quality.

Keywords


hydrogeology; deep-water source; evidence of water-kind isotopes; helium; uranium; plumes; nuclear reactor

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DOI: http://dx.doi.org/10.17072/psu.geol.25.43

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