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作 者:Olga GASKOVA Vitaly ISUPOV Alexander VLADIMIROV Stepan SHVARTSEV
机构地区:[1]Sobolev Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences [2]Novosibirsk State University [3]Institute of Solid State Chemistry and Mechanochemistry, Siberian Branch of Russian Academy of Sciences [4]Tomsk State University [5]Tomsk Branch of the Trofimuk Institute of Oil and Gas Geology and Geophysics, Siberian Branch of Russian Academy of Sciences
出 处:《Acta Geologica Sinica(English Edition)》2014年第S1期135-136,共2页地质学报(英文版)
基 金:supported by the SB RAS Interdisciplinary Integration project 110;by the RFBR grant 13-0500032;by program to improve the competitiveness of Tomsk State University
摘 要:1 Introduction The attractiveness of Shaazgai-Nuur Soda Lake(pH9.2-9.4)as an alternative metal source is explained by the high concentration of dissolved uranium(~1 mg/l)due to the location of water drainage territory within the Tsagan-1 Introduction The attractiveness of Shaazgai-Nuur Soda Lake(pH9.2-9.4)as an alternative metal source is explained by the high concentration of dissolved uranium(~1 mg/l)due to the location of water drainage territory within the Tsagan-
关 键 词:saline lakes URANIUM ARSENIC SORPTION thermodynamic model CALCITE goethite.
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