KFU. Card publication. 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

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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

Form of presentation

Articles in international journals and collections

Year of publication

2015

Authors, employees of KFU

Golosov Valentin Nikolaevich, author

Other authors

Zhang X., He H., Tang Q., Zhou P.

Bibliographic description in the original language

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.

Annotation

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

Keywords

land denudation; Natural factors; Anthropogenic disturbance; Suspended sediment yield; Upper Yangtze River; Volga River

The name of the journal

Journal of Mountain Science

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=99470&p_lang=2

Resource files

File name	Size (MB)	Format
jms_2015.pdf	3,73	pdf	show / download

Full metadata record

Field DC	Value	Language
dc.contributor.author	Golosov Valentin Nikolaevich	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/eng/?p_id=99470&p_lang=2	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	Articles in international journals and collections	ru_RU