Form of presentation | Conference proceedings in international journals and collections |
Year of publication | 2018 |
Язык | русский |
|
Kurzhanova Anna Alekseevna, author
Khayrullina Dinara Nikolaevna, author
|
Bibliographic description in the original language |
Khayrullina D.N., Kurzhanova A.A. The genetic structure of the chloride ion runoff on the example of karst and non-karst geosystems of Archangelsk oblast / D.N. Khayrullina, A.A. Kurzhanova // IOP Conference Series: Earth and Environmental Science. – 2018. – Vol. 107, Is. 1. – Art. № 012012 |
Annotation |
IOP Conference Series: Earth and Environmental Science |
Keywords |
Chloride ion, surface ion runoff, underground ion runoff, atmospheric ion runoff, geosystem |
The name of the journal |
IOP Conference Series: Earth and Environmental Science
|
URL |
http://iopscience.iop.org/article/10.1088/1755-1315/107/1/012012 |
Please use this ID to quote from or refer to the card |
https://repository.kpfu.ru/eng/?p_id=176316&p_lang=2 |
Resource files | |
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Full metadata record |
Field DC |
Value |
Language |
dc.contributor.author |
Kurzhanova Anna Alekseevna |
ru_RU |
dc.contributor.author |
Khayrullina Dinara Nikolaevna |
ru_RU |
dc.date.accessioned |
2018-01-01T00:00:00Z |
ru_RU |
dc.date.available |
2018-01-01T00:00:00Z |
ru_RU |
dc.date.issued |
2018 |
ru_RU |
dc.identifier.citation |
Khayrullina D.N., Kurzhanova A.A. The genetic structure of the chloride ion runoff on the example of karst and non-karst geosystems of Archangelsk oblast / D.N. Khayrullina, A.A. Kurzhanova // IOP Conference Series: Earth and Environmental Science. – 2018. – Vol. 107, Is. 1. – Art. № 012012 |
ru_RU |
dc.identifier.uri |
https://repository.kpfu.ru/eng/?p_id=176316&p_lang=2 |
ru_RU |
dc.description.abstract |
IOP Conference Series: Earth and Environmental Science |
ru_RU |
dc.description.abstract |
This paper deals with the estimate the structure of the chloride ion runoff from the karst (on the example of the Sula river basin) and non-karst (on the example of the Vaga river basin) geosystems of Arkhangelsk oblast. The contribution of the surface component predominates in the structure of the chloride ion runoff.For example, the input of surface ion runoff is 49% (for the Sula river basin), 55% (for the Vaga river basin). In time aspect the highest values of variability of the components of the chloride ion runoff are noted for karst geosystems and vary from 38.5% to 55.4% and from 24.7% to 42.9% ? for non-karst geosystems.Finally, there is prevalence of the local factors influence because the atmospheric component decreases while ion runoff increases. |
ru_RU |
dc.language.iso |
ru |
ru_RU |
dc.subject |
Chloride ion |
ru_RU |
dc.subject |
surface ion runoff |
ru_RU |
dc.subject |
underground ion runoff |
ru_RU |
dc.subject |
atmospheric ion runoff |
ru_RU |
dc.subject |
geosystem |
ru_RU |
dc.title |
The genetic structure of the chloride ion runoff on the example of karst and non-karst geosystems of Archangelsk oblast |
ru_RU |
dc.type |
Conference proceedings in international journals and collections |
ru_RU |
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