Zobrazeno 1 - 6
of 6
pro vyhledávání: '"A V Dembovetskiy"'
Autor:
E. V. Shein, A. G. Bolotov, A. V. Dembovetskiy, D. Yu. Usenko, N. A. Kharkhardinov, Yu. I. Vernyuk
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 117, Pp 5-22 (2023)
The classification of soils water regimes a basic scientific basis in the form of an interdependent relationship between the movement of water and the formation of a soil profile, i. e. it is soil-genetic classification. This kind of classification p
Externí odkaz:
https://doaj.org/article/d8218d3a563044e5af651e53de4f7851
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 110, Pp 5-21 (2022)
At the experimental field of VNIIMZ (Tver region, village Emmauss) laid a series of 8 soil sections. The first three sections of the southern slope are confined to the transit-accumulative, transit and eluvial-transit microlandscape with a complex of
Externí odkaz:
https://doaj.org/article/e936f1cca1c848caa2b9fecca177de45
Autor:
A A Kokoreva, A V Dembovetskiy, Z S Ezhelev, A G Bolotov, V M Stepanenko, K V Shishkin, I A Abramyan
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 862:012042
Autor:
F. D. Mikayilov, G. V. Kharitonova, Evgeny Shein, N. S. Konovalova, S. A. Erol, A. V. Dembovetskiy
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 547:012010
An unexpectedly high infiltration capacity was determined for heavy-textured, clayey alluvial calcareous soils (Calcic Haploxerepts) in central Anatolia, Turkey, presumably due to the specific mineralogical contents. In order to unravel the phenomeno
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 368:012045
The main indicators characterizing the surface properties of soils formed on the eluvium of Triassic clays of the Kostroma region have been studied. The categories of specific surface area and the degree of soil hydrophilicity have been calculated. L
Publikováno v:
Procedia Environmental Sciences. 19:558-563
Technogenic soil (technozem) was created on the surface of the former sludge pond of the iron-ore quarry in the course of land rehabilitation. The upper chernozemic layer in the technozem was underlain by sandy or loamy layers. The soil land reclamat