Zobrazeno 1 - 6
of 6
pro vyhledávání: '"S. A. Avetyan"'
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 114, Pp 29-65 (2023)
At the end of the 20th century, a geoinformation database on soil degradation in Russia, relied on the soil map of Russia at a scale of 1 : 5 million, was developed under the leadership of V.S. Stolbovoy. As part of the development of this problem an
Externí odkaz:
https://doaj.org/article/4a814978b3884d9b8f4869e10ba86db3
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 94, Pp 38-56 (2018)
The paper presents the results of the of the country's plowed area assessment on the basis of the Unified State Register of Soil Resources of Russia, a digital land cover map created on the basis of MODIS satellite data, and study of plowed land area
Externí odkaz:
https://doaj.org/article/e2e8da692da9437dba18659a7f1ff376
Autor:
Vladimir Stolbovoy, S. A. Avetyan, A. L. Ivanov, E. A. Shishkonakova, A. N. Kashtanov, I. Yu. Savin
Publikováno v:
Doklady Earth Sciences. 493:654-657
The last map of anthropogenic soil erosion in Russia was compiled more than 20 years ago on a scale of 1 : 5 000 000. In recent years, additional data on soil erosion have been accumulated. New mapping approaches have appeared that enable us to prese
Publikováno v:
Moscow University Soil Science Bulletin. 73:95-99
Agriculture in the northern Meshchera lowlands is experiencing considerable difficulties due to both natural causes and the socioeconomic situation in Vladimir oblast. Some properties of reclaimed (drained) sod-podzolic soils remain sufficiently stab
Publikováno v:
Moscow University Soil Science Bulletin. 72:1-6
Specific features of the structure and composition of the soil cover in the Salym-Irtysh interfluve, Western Siberian Lowland, are studied with consideration of the capabilities of digital mapping. The properties of predominating and accompanying soi
Publikováno v:
Eurasian Soil Science. 45:651-656
The morphology of the profile, some chemical properties, and particle-size distribution of the automorphic soils developed from lacustrine-alluvial loamy-clayey deposits in the Sredneobskaya Lowland are considered. The soils of the West Siberian midd