KFU. Card publication. Recent trend of erosion rates in the southern half of the Russian plain

KAZAN
FEDERAL UNIVERSITY

- RUS
- 中文
- ES

RECENT TREND OF EROSION RATES IN THE SOUTHERN HALF OF THE RUSSIAN PLAIN

Form of presentation

Articles in international journals and collections

Year of publication

2018

Язык

английский

Authors, employees of KFU

Golosov Valentin Nikolaevich, author

Safina Guzel Rashitovna, author

Chizhikova Nelli Aleksandrovna, author

Other authors

Kiryukhina Zoya Pavlovna, author

Litvin Leonid Fedorovich, author

Bibliographic description in the original language

Golosov, V.N., Litvin, L.F., Shizhikova, N.A., Kiryukhina, Z.P.,Safina, G.R.: Recent trend of erosion rates in the southern half of the Russian plain. In: Eds. Miodrag Zlatić; Stanimir Kostadinov, Soil and water resources protection in the changing environment, Advances in Geoecology, Volume 45, Catena Verlag, 2018, pp. 54–64

Annotation

The territory of the Russian Plain can be divided onto two parts in relation of agricultural activity. The northern half is taiga zone with extremely high proportion of forested area and very limited areas of arable fields. Southern half of the Russian Plain is located in broad-leaf forest, forest-steppe and steppe zones and it is characterized by high proportion of arable lands with period of intensive cultivation from 300-350 years in broad-leaf landscape zone up to about one century on the south-east of steppe zone. It is one of the main agricultural regions of Russia with relatively high rates of sheet, rill and gully erosion. The latest quantitative assessment of soil losses for the entire area of the Russian Plain was undertaken in the middle of 1980th, when maps of soil losses and gully density were constructed. Modified version of USLE model and State Hydrological Institute erosion model were used for evaluation of soil losses from arable lands during warm period of year and pe

Keywords

land use change, erosion rate, climate change, Russian Plain

The name of the journal

Advances in GeoEcology

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

https://repository.kpfu.ru/eng/?p_id=180889&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Golosov Valentin Nikolaevich	ru_RU
dc.contributor.author	Safina Guzel Rashitovna	ru_RU
dc.contributor.author	Chizhikova Nelli Aleksandrovna	ru_RU
dc.contributor.author	Kiryukhina Zoya Pavlovna	ru_RU
dc.contributor.author	Litvin Leonid Fedorovich	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	Golosov, V.N., Litvin, L.F., Сhizhikova, N.A., Kiryukhina, Z.P.,Safina, G.R.: Recent trend of erosion rates in the southern half of the Russian plain. In: Eds. Miodrag Zlatić; Stanimir Kostadinov, Soil and water resources protection in the changing environment, Advances in Geoecology, Volume 45, Catena Verlag, 2018, pp. 54–64	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=180889&p_lang=2	ru_RU
dc.description.abstract	Advances in GeoEcology	ru_RU
dc.description.abstract	The territory of the Russian Plain can be divided onto two parts in relation of agricultural activity. The northern half is taiga zone with extremely high proportion of forested area and very limited areas of arable fields. Southern half of the Russian Plain is located in broad-leaf forest, forest-steppe and steppe zones and it is characterized by high proportion of arable lands with period of intensive cultivation from 300-350 years in broad-leaf landscape zone up to about one century on the south-east of steppe zone. It is one of the main agricultural regions of Russia with relatively high rates of sheet, rill and gully erosion. The latest quantitative assessment of soil losses for the entire area of the Russian Plain was undertaken in the middle of 1980th, when maps of soil losses and gully density were constructed. Modified version of USLE model and State Hydrological Institute erosion model were used for evaluation of soil losses from arable lands during warm period of year and pe	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	land use change	ru_RU
dc.subject	erosion rate	ru_RU
dc.subject	climate change	ru_RU
dc.subject	Russian Plain	ru_RU
dc.title	Recent trend of erosion rates in the southern half of the Russian plain	ru_RU
dc.type	Articles in international journals and collections	ru_RU