Uranium in the mineralized lakes of Altai Krai / V. P. Isupov [et al.]

Уровень набора: Doklady Earth Sciences = 1933-Альтернативный автор-лицо: Isupov, V. P., Vitaly;Kolpakova, M. N., hydrogeologist, assistant Professor of Tomsk Polytechnic University, candidate of geological and mineralogical Sciences, 1987-, Marina Nikolaevna;Borzenko, S. V.;Shatskaja, S. S.;Shvartsev, S. L., Russian hydrogeologist, Doctor of Geological and Mineralogical sciences, Professor of the TPU, Member of the Academy of Natural sciences, 1936-, Stepan Lvovich;Dolgushin, A. P.;Arzamasova, G. M.Коллективный автор (вторичный): Национальный исследовательский Томский политехнический университет (ТПУ), Институт природных ресурсов (ИПР), Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)Язык: английский.Страна: .Резюме или реферат: Data on the physicochemical properties (pH, Eh, salinity) and content of U and other trace elements (As, Li, B, Br, I, Sr) are provided for the mineralized lakes of the Kulundinskaya steppe of Altai Krai. The sodic lakes of the region are characterized by higher U238 contents (up to 4 mg/l). The U contents in the lake waters are positively correlated with the sum of carbonate and hydrocarbonate ions and the pH of waters and are negatively correlated with salinity. These data confirm the presence of an economic U-bearing zone of the ground reservoir oxidation located along the eastern slope of the Platovskoe uplift in the northwestern direction along the boundary with Kazakhstan..Примечания о наличии в документе библиографии/указателя: [References: p. 1070 (8 tit.)].Аудитория: .Тематика: электронный ресурс | труды учёных ТПУ Ресурсы он-лайн:Щелкните здесь для доступа в онлайн
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[References: p. 1070 (8 tit.)]

Data on the physicochemical properties (pH, Eh, salinity) and content of U and other trace elements (As, Li, B, Br, I, Sr) are provided for the mineralized lakes of the Kulundinskaya steppe of Altai Krai. The sodic lakes of the region are characterized by higher U238 contents (up to 4 mg/l). The U contents in the lake waters are positively correlated with the sum of carbonate and hydrocarbonate ions and the pH of waters and are negatively correlated with salinity. These data confirm the presence of an economic U-bearing zone of the ground reservoir oxidation located along the eastern slope of the Platovskoe uplift in the northwestern direction along the boundary with Kazakhstan.

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