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- W154938510 abstract "The geochemical mobility of uranium in the normal conditions of pH, oxidation-reduction, salimity and uranium content of vadose waters is of the same order as the calcium and sodium mobility. A strongly anomalous uranium content is geochemically stable. Therefore, the hydrography is the fundamental factor determining the shape of the halos of hydrogeochemical surface dispersion of uranium. The processes of mutual dilution and mixing of surface waters depend on hydrography. The known phenomena, that can lessen the mobility of uranium, are realized in the ground water environment, and the border of surface oxidizing environment. The phenomena do not affect the operational criteria of the strategic hydrogeochemical prospecting in surface waters, but they are important in determining the underground regions escaping hydrogeochemical strategic exploration. The writers describe the employed apparatus and methods of uranium determination by fluorimetric methods. (auth)" @default.
- W154938510 created "2016-06-24" @default.
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- W154938510 date "1960-01-01" @default.
- W154938510 modified "2023-09-27" @default.
- W154938510 title "THE HYDROGEOCHEMICAL PROSPECTION OF URANIUM" @default.
- W154938510 hasPublicationYear "1960" @default.
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