| Форма представления | Статьи в зарубежных журналах и сборниках |
| Год публикации | 2015 |
|
Голосов Валентин Николаевич, автор
|
| Другие авторы |
Zhang X., He H., Tang Q., Zhou P. |
| Библиографическое описание на языке оригинала |
1. Golosov V., Zhang X., He H., Tang Q., Zhou P. Principal denudation processes and their contribution to the fluvial suspended sediment yields in the Upper Yangtze Basin and Volga River basin. Journal of Mountain Science vol.12, no.1, 2015, p. 101-122. doi 10.1007/s11629-014-2975-7. |
| Аннотация |
This paper synthesized the principal land denudation processes and their role in determining riverine suspended sediment yields (SSY) in two typical geographical environments of the Upper Yangtze River Basin and the Volga River Basin. In the Upper Yangtze River Basin, natural factors including topography, climate, lithology and tectonic activity are responsible for the spatial variation in the magnitude of denudation rates. Human disturbances have contributed to the temporal changes of soil erosion and fluvial SSY during the past decades. On one hand, land use change caused by deforestation and land reclamation has played an important role in the acceleration of sediment production from the central hilly area and lower Jinsha catchment; On the other hand, diverse soil conservation practices (e.g., reforestation, terracing) have contributed to a reduction of soil erosion and sediment production since late 1980s.It was difficult to explicitly decoupling the effect of mitigation measures |
| Ключевые слова |
land denudation; Natural factors; Anthropogenic disturbance; Suspended sediment yield; Upper Yangtze River; Volga River |
| Название журнала |
Journal of Mountain Science
|
| Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку |
https://repository.kpfu.ru/?p_id=99470 |
| Файлы ресурса | |
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Полная запись метаданных  |
| Поле DC |
Значение |
Язык |
| dc.contributor.author |
Голосов Валентин Николаевич |
ru_RU |
| dc.date.accessioned |
2015-01-01T00:00:00Z |
ru_RU |
| dc.date.available |
2015-01-01T00:00:00Z |
ru_RU |
| dc.date.issued |
2015 |
ru_RU |
| dc.identifier.citation |
1. Golosov V., Zhang X., He H., Tang Q., Zhou P. Principal denudation processes and their contribution to the fluvial suspended sediment yields in the Upper Yangtze Basin and Volga River basin. Journal of Mountain Science vol.12, no.1, 2015, p. 101-122. doi 10.1007/s11629-014-2975-7. |
ru_RU |
| dc.identifier.uri |
https://repository.kpfu.ru/?p_id=99470 |
ru_RU |
| dc.description.abstract |
Journal of Mountain Science |
ru_RU |
| dc.description.abstract |
This paper synthesized the principal land denudation processes and their role in determining riverine suspended sediment yields (SSY) in two typical geographical environments of the Upper Yangtze River Basin and the Volga River Basin. In the Upper Yangtze River Basin, natural factors including topography, climate, lithology and tectonic activity are responsible for the spatial variation in the magnitude of denudation rates. Human disturbances have contributed to the temporal changes of soil erosion and fluvial SSY during the past decades. On one hand, land use change caused by deforestation and land reclamation has played an important role in the acceleration of sediment production from the central hilly area and lower Jinsha catchment; On the other hand, diverse soil conservation practices (e.g., reforestation, terracing) have contributed to a reduction of soil erosion and sediment production since late 1980s.It was difficult to explicitly decoupling the effect of mitigation measures |
ru_RU |
| dc.language.iso |
ru |
ru_RU |
| dc.subject |
|
ru_RU |
| dc.title |
Principal denudation processes and their contribution to the fluvial suspended sediment yields in the Upper Yangtze Basin and Volga River basin. Journal of Mountain Science |
ru_RU |
| dc.type |
Статьи в зарубежных журналах и сборниках |
ru_RU |
|
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