Size fractionation of trace elements in the surface water and groundwater of the Ganjiang River and Xiushui River basins, China / E. A. Soldatova [et al.]

Уровень набора: (RuTPU)RU\TPU\network\2499, IOP Conference Series: Earth and Environmental ScienceАльтернативный автор-лицо: Soldatova, E. A., hydrogeologist, engineer-researcher of Tomsk Polytechnic University, 1989-, Evgeniya Aleksandrovna;Guseva, N. V., hydrogeologist, Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences, 1984-, Natalia Vladimirovna;Sun, Z.;Mazurova, I. S., hydrogeologist, engineer of Tomsk Polytechnic University, 1991-, Irina SergeevnaКоллективный автор (вторичный): Национальный исследовательский Томский политехнический университет (ТПУ), Институт природных ресурсов (ИПР), Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ);Национальный исследовательский Томский политехнический университет (ТПУ), Институт природных ресурсов (ИПР), Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ), Научно-образовательный центр "Вода" (НОЦ "ВОДА"), Проблемная научно-исследовательская лаборатория гидрогеохимии (ПНИЛ ГГХ)Язык: английский.Серия: Hydrogeochemistry and Hydrogeoecology. Geionformation Systems in Hydrogeochemictry and HydrogeoecologyРезюме или реферат: The research of trace element behaviour and size fractionation is significant to understand the processes in the water-rock system. Moreover, the aqueous speciation of trace elements is strongly related to their distribution and toxicity. In this research, trace elements behaviour and their size fractionation are investigated in the natural water (the surface water and shallow groundwater) of the Ganjiang River and Xiushui River basins. Trace element concentrations were measured by ICP-MS. The authors estimated the size fractionation of the trace elements between suspended forms (>0.45 [mu]m) and dissolved fractions, which included truly dissolved (1 kDa) and colloidal particles (0.45 [mu]m-1 kDa)), after filtration through a 0.45 [mu]m acetate cellulose membrane filter. The distinct features of the trace element size fractionation were identified. The size fractionation of the trace elements under different conditions (in the surface water and shallow groundwater) was studied..Примечания о наличии в документе библиографии/указателя: [References: 15 tit.].Аудитория: .Тематика: электронный ресурс | труды учёных ТПУ | фракционирование | микроэлементы | поверхностные воды | подземные воды | реки | Китай Ресурсы он-лайн:Щелкните здесь для доступа в онлайн | Щелкните здесь для доступа в онлайн
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[References: 15 tit.]

The research of trace element behaviour and size fractionation is significant to understand the processes in the water-rock system. Moreover, the aqueous speciation of trace elements is strongly related to their distribution and toxicity. In this research, trace elements behaviour and their size fractionation are investigated in the natural water (the surface water and shallow groundwater) of the Ganjiang River and Xiushui River basins. Trace element concentrations were measured by ICP-MS. The authors estimated the size fractionation of the trace elements between suspended forms (>0.45 [mu]m) and dissolved fractions, which included truly dissolved (1 kDa) and colloidal particles (0.45 [mu]m-1 kDa)), after filtration through a 0.45 [mu]m acetate cellulose membrane filter. The distinct features of the trace element size fractionation were identified. The size fractionation of the trace elements under different conditions (in the surface water and shallow groundwater) was studied.

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