Basin Model of Total Dissolved Salts Transformation in Water of a Small River (the Kirgizka River, Tomsk, Russia); IOP Conference Series: Earth and Environmental Science; Vol. 43 : Problems of Geology and Subsurface Development

Chi tiết về thư mục
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 43 : Problems of Geology and Subsurface Development.— 2016.— [012028, 6 p.]
Tác giả chính: Savichev O. G. Oleg Gennadievich
Nhiều tác giả của công ty: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра экономики природных ресурсов (ЭПР), Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра иностранных языков (ИЯПР)
Tác giả khác: Matveenko I. A. Irina Alekseevna, Titov I. V.
Tóm tắt:Title screen
The basin model of total dissolved salt transformation in river water has been developed. It was tested in the Kirgizka River, the right tributary of the Tom River (Russia, Western Siberia, Tomsk). It was shown that the river system has the capacity of selfpurification and is characterized by rather stable salt composition. It is explained by the fact that the growth in dissolved salt concentration in river water is limited to some extent by, firstly, dilution of more mineralized groundwaters drained by rivers, and, secondly, relatively low solubility of some compounds.
Ngôn ngữ:Tiếng Anh
Được phát hành: 2016
Loạt:Hydrogeochemistry and Hydrogeoecology
Những chủ đề:
Truy cập trực tuyến:http://dx.doi.org/10.1088/1755-1315/43/1/012028
http://earchive.tpu.ru/handle/11683/35135
Định dạng: Điện tử Chương của sách
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650829

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