Форма представления | Тезисы и материалы конференций в зарубежных журналах и сборниках |
Год публикации | 2018 |
Язык | русский |
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Куржанова Анна Алексеевна, автор
Хайруллина Динара Николаевна, автор
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Библиографическое описание на языке оригинала |
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 |
Аннотация |
IOP Conference Series: Earth and Environmental Science |
Ключевые слова |
Chloride ion, surface ion runoff, underground ion runoff, atmospheric ion runoff, geosystem |
Название журнала |
IOP Conference Series: Earth and Environmental Science
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URL |
http://iopscience.iop.org/article/10.1088/1755-1315/107/1/012012 |
Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку |
https://repository.kpfu.ru/?p_id=176316 |
Файлы ресурса | |
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Полная запись метаданных |
Поле DC |
Значение |
Язык |
dc.contributor.author |
Куржанова Анна Алексеевна |
ru_RU |
dc.contributor.author |
Хайруллина Динара Николаевна |
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/?p_id=176316 |
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 |
Тезисы и материалы конференций в зарубежных журналах и сборниках |
ru_RU |
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