Zobrazeno 1 - 10
of 33
pro vyhledávání: '"M. P. Gerasimova"'
Autor:
M. P. Gerasimova
Publikováno v:
Ежегодник Япония, Vol 52, Pp 276-296 (2023)
The author aims to answer the question of what presently contributes to the preservation of the national uniqueness of the Japanese culture and why one of the characteristic features of the Japanese is their adherence to traditions, and also to point
Externí odkaz:
https://doaj.org/article/0421b70fe1344fec94034456e69f6064
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 112, Pp 73-121 (2022)
An analysis of the soil cover of Russia as presented on the soil map on a scale of 1 : 2.5 M with the use of a new substantive-genetic soil classification system has been performed at the level of soil orders. The high level of classification-based g
Externí odkaz:
https://doaj.org/article/ae9a08f752e74fa483194e412fd7e085
Autor:
T. V. Ananko, M. I. Gerasimova
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 108, Pp 31-54 (2021)
The dark-humus soil type was included in the updated legend of the Soil Map of the Russian Federation at scale 1 : 2.5 M, converted to the system of Soil Classification of Russia. The soil profile starts with the dark-humus horizon gradually merging
Externí odkaz:
https://doaj.org/article/4fcd4af0396d46b7accfd8cb35a64f3e
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 108, Pp 5-30 (2021)
The development of the digital model of the soil map of Russia derived of the map of the Soviet Russian Federation, 1988, compiled in Dokuchaev Soil Science Institute, comprises the transfer of soil names in the initial legend to those in the new cla
Externí odkaz:
https://doaj.org/article/5551ffced1134cad88a936c3c6f429d0
Autor:
M. I. Gerasimova, M. D. Bogdanova
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 107, Pp 139-179 (2021)
The overview of publications on soil cartography in “Pochvovedenie”/“Eurasian Soil Science” journal for the period 1899–2020 demonstrates a high diversity of themes and certain trends in the number and dynamics of papers. Their total number
Externí odkaz:
https://doaj.org/article/3e454fb00bd648eaa7669f2e847105d9
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 104, Pp 223-240 (2020)
A digital version of the soil map of the Russian Federation, scale 1 : 2.5 M, is being prepared based on the analysis of the attributes of polygons with peat soils in the West-Siberian taiga and sub-taiga zones. The correction was perfomed in 795 pol
Externí odkaz:
https://doaj.org/article/51b783aecf03429f916b418871fb21e3
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 102, Pp 21-48 (2020)
The Soil Map of the Russian Federation, 1 : 2.5 M scale (1988) requires updating to include soil data that have been accumulated in the past decades, reflect real changes in the soil cover, including anthropogenic transformation, and ensure precise l
Externí odkaz:
https://doaj.org/article/bce14e414f4f4979bf7222b6bd022fe2
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 102, Pp 5-20 (2020)
The basic three-component classification system of soils of the world was published by V.M. Fridland in 1982, and its profile-genetic component was taken as a basis for the classification of soils of Russia (1997– 2004–2008). Unlike the former sy
Externí odkaz:
https://doaj.org/article/9a737c4dc60b4da189dfb70798d3668b
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 101, Pp 46-75 (2020)
V.V. Dokuchaev Soil Science Institute has initiated a project on compilation of a new Digital Soil Map of Russia on the basis of the Soil Map of the Russian Federation (SMRF) 1 : 2.5 M scale (1988) revised and interpreted in ideology and nomenclature
Externí odkaz:
https://doaj.org/article/d4463d0ca2c141f8a0971c3542b8cef7
Publikováno v:
Лëд и снег, Vol 59, Iss 3, Pp 307-318 (2019)
As a result of studies of newly fallen snow in the North of the Kola Peninsula, it was found that from January to May 2018 its density amounted, on the average, to 0.160±0.006 g/cm3 (n = 82), and pH of melted snow water - 6.87±0.14 (n = 47). Neutra
Externí odkaz:
https://doaj.org/article/03de746a83424817953db83c95bc41c3