Evaluation of soil erosion rates in the southern half of the Russian Plain: methodology and initial results
The Russian Plain (RP) is divided into two principally different parts. The northern half of the RP is a predominantly forested area with a low proportion of arable fields. In contrast, the southern half of the RP has a very high proportion of arable land. During the last 30 years, this agricult...
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doaj-c7aeb14efd1248d78c85d5b3c249066d2020-11-24T23:02:28ZengCopernicus PublicationsProceedings of the International Association of Hydrological Sciences2199-89812199-899X2017-03-01375232710.5194/piahs-375-23-2017Evaluation of soil erosion rates in the southern half of the Russian Plain: methodology and initial resultsV. Golosov0V. Golosov1A. Gusarov2L. Litvin3O. Yermolaev4N. Chizhikova5G. Safina6Z. Kiryukhina7Kazan Federal University, Kremlyovskaya St. 18, Kazan, 420008, RussiaLomonosov Moscow State University, Leninskie Gory, 1, Moscow, 119991, RussiaKazan Federal University, Kremlyovskaya St. 18, Kazan, 420008, RussiaLomonosov Moscow State University, Leninskie Gory, 1, Moscow, 119991, RussiaKazan Federal University, Kremlyovskaya St. 18, Kazan, 420008, RussiaKazan Federal University, Kremlyovskaya St. 18, Kazan, 420008, RussiaKazan Federal University, Kremlyovskaya St. 18, Kazan, 420008, RussiaLomonosov Moscow State University, Leninskie Gory, 1, Moscow, 119991, RussiaThe Russian Plain (RP) is divided into two principally different parts. The northern half of the RP is a predominantly forested area with a low proportion of arable fields. In contrast, the southern half of the RP has a very high proportion of arable land. During the last 30 years, this agricultural region of the RP has experienced considerable land use transformation and changes in precipitation due to climate change have altered soil erosion rates. This paper describes the use of erosion model calculations and GIS spatial analytical methods for the evaluation of trends in erosion rates in the RP. Climate change (RIHMI World Data Center, 2016), land use transformation and crop rotation modification (Rosstat, 2016; R Core Team, 2016) are the main factors governing erosion rates in the region during recent decades. It was determined that mean annual erosion rates have decreased from 7.3 to 4.1 t ha<sup>−1</sup> yr<sup>−1</sup> in the forest zone mostly because of the serious reduction in the surface runoff coefficient for periods of snowmelt. At the same time, the erosion rates have increased from 3.9 to 4.6 t ha<sup>−1</sup> yr<sup>−1</sup> in the steppe zone due to the increasing frequency of heavy rain-storms.https://www.proc-iahs.net/375/23/2017/piahs-375-23-2017.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
V. Golosov V. Golosov A. Gusarov L. Litvin O. Yermolaev N. Chizhikova G. Safina Z. Kiryukhina |
spellingShingle |
V. Golosov V. Golosov A. Gusarov L. Litvin O. Yermolaev N. Chizhikova G. Safina Z. Kiryukhina Evaluation of soil erosion rates in the southern half of the Russian Plain: methodology and initial results Proceedings of the International Association of Hydrological Sciences |
author_facet |
V. Golosov V. Golosov A. Gusarov L. Litvin O. Yermolaev N. Chizhikova G. Safina Z. Kiryukhina |
author_sort |
V. Golosov |
title |
Evaluation of soil erosion rates in the southern half of the Russian Plain: methodology and initial results |
title_short |
Evaluation of soil erosion rates in the southern half of the Russian Plain: methodology and initial results |
title_full |
Evaluation of soil erosion rates in the southern half of the Russian Plain: methodology and initial results |
title_fullStr |
Evaluation of soil erosion rates in the southern half of the Russian Plain: methodology and initial results |
title_full_unstemmed |
Evaluation of soil erosion rates in the southern half of the Russian Plain: methodology and initial results |
title_sort |
evaluation of soil erosion rates in the southern half of the russian plain: methodology and initial results |
publisher |
Copernicus Publications |
series |
Proceedings of the International Association of Hydrological Sciences |
issn |
2199-8981 2199-899X |
publishDate |
2017-03-01 |
description |
The Russian Plain (RP) is divided into two principally
different parts. The northern half of the RP is a predominantly forested
area with a low proportion of arable fields. In contrast, the southern half
of the RP has a very high proportion of arable land. During the last 30 years,
this agricultural region of the RP has experienced considerable land
use transformation and changes in precipitation due to climate change have
altered soil erosion rates. This paper describes the use of erosion model
calculations and GIS spatial analytical methods for the evaluation of trends
in erosion rates in the RP. Climate change (RIHMI World Data Center, 2016), land use transformation and crop
rotation modification (Rosstat, 2016; R Core Team, 2016) are the main factors governing erosion rates in the
region during recent decades. It was determined that mean annual erosion
rates have decreased from 7.3 to 4.1 t ha<sup>−1</sup> yr<sup>−1</sup>
in the forest zone mostly because of the serious reduction in the
surface runoff coefficient for periods of snowmelt. At the same time, the
erosion rates have increased from 3.9 to 4.6 t ha<sup>−1</sup> yr<sup>−1</sup>
in the steppe zone due to the increasing frequency of
heavy rain-storms. |
url |
https://www.proc-iahs.net/375/23/2017/piahs-375-23-2017.pdf |
work_keys_str_mv |
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