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
| Parent link: | IOP Conference Series: Earth and Environmental Science Vol. 43 : Problems of Geology and Subsurface Development.— 2016.— [012028, 6 p.] |
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| Autor principal: | |
| Corporate Authors: | , |
| Outros Autores: | , |
| Resumo: | 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. |
| Idioma: | inglês |
| Publicado em: |
2016
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| Colecção: | Hydrogeochemistry and Hydrogeoecology |
| Assuntos: | |
| Acesso em linha: | http://dx.doi.org/10.1088/1755-1315/43/1/012028 http://earchive.tpu.ru/handle/11683/35135 |
| Formato: | MixedMaterials Recurso Electrónico Capítulo de Livro |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650829 |
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| 200 | 1 | |a Basin Model of Total Dissolved Salts Transformation in Water of a Small River (the Kirgizka River, Tomsk, Russia) |f O. G. Savichev, I. A. Matveenko, I. V. Titov | |
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| 225 | 1 | |a Hydrogeochemistry and Hydrogeoecology | |
| 300 | |a Title screen | ||
| 320 | |a [References: 14 tit.] | ||
| 330 | |a 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. | ||
| 461 | 0 | |0 (RuTPU)RU\TPU\network\2499 |t IOP Conference Series: Earth and Environmental Science | |
| 463 | 0 | |0 (RuTPU)RU\TPU\network\16030 |t Vol. 43 : Problems of Geology and Subsurface Development |o XX International Scientific Symposium of Students, Postgraduates and Young Scientists, 4–8 April 2016, Tomsk, Russia |v [012028, 6 p.] |d 2016 | |
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| 700 | 1 | |a Savichev |b O. G. |c geologist |c Professor of Tomsk Polytechnic University, doctor of geographical sciences |f 1967- |g Oleg Gennadievich |3 (RuTPU)RU\TPU\pers\34024 |9 17591 | |
| 701 | 1 | |a Matveenko |b I. A. |c linguist |c Professor of Tomsk Polytechnic University, Doctor of Philology |f 1967- |g Irina Alekseevna |3 (RuTPU)RU\TPU\pers\30938 |9 15176 | |
| 701 | 1 | |a Titov |b I. V. | |
| 712 | 0 | 2 | |a Национальный исследовательский Томский политехнический университет (ТПУ) |b Институт природных ресурсов (ИПР) |b Кафедра экономики природных ресурсов (ЭПР) |3 (RuTPU)RU\TPU\col\18668 |
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