Zobrazeno 1 - 9
of 9
pro vyhledávání: '"E. Yu. Sukhacheva"'
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 116, Pp 26-42 (2023)
Today the rate of anthropogenic transformations of the soil cover significantly exceeds the rate of its natural restoration. According to a modern digital soil map at a scale of 1 : 200,000 in the Leningrad Region anthropogenically modified subtypes
Externí odkaz:
https://doaj.org/article/d31da0f452164bd1a19209446525c8a6
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 83, Pp 140-158 (2016)
Forestry of Lisino is the perspective area for the organization and conduction of soil and ecologic monitoring. It is characterized by ecosystems, typical for the North-West, which are least altered by anthropogenic impact. Also it is characterized b
Externí odkaz:
https://doaj.org/article/fc24f2378e0847c2aaf46eed98d964e8
Publikováno v:
Biology Bulletin. 49:2397-2409
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1cf9fad73aa36841a51dbb36fe64c8c9
https://doi.org/10.1134/s1062359022120147
https://doi.org/10.1134/s1062359022120147
Publikováno v:
Eurasian Soil Science. 51:1008-1020
The origin, structure, composition, and properties of soil humus horizons in functional zones of St. Petersburg have been studied. The radiocarbon age of organic matter in the humus horizons varies from 500 to 2700 years, which attests to the natural
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a10af4ece4bbd8e9a5a66f190ef89f2
https://doi.org/10.1134/s1064229318090016
https://doi.org/10.1134/s1064229318090016
Publikováno v:
Eurasian Soil Science. 50:1395-1405
Data on the concentrations of natural (226Ra, 232Th and 40K) and artificial (137Cs) radionuclides and on the physicochemical properties of chernozems sampled in different years are presented. In 1952, upon the creation of the Penza-Kamensk state shel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d8b7ba55c5a1fd1bc326dcc4c0573991
https://doi.org/10.1134/s106422931712002x
https://doi.org/10.1134/s106422931712002x
Publikováno v:
Eurasian Soil Science. 49:1-7
A new notion—an acidic trace of pedogenesis in the field of soil acidity—is suggested. This notion implies a three-dimensional representation of the distribution of soil acidity in the soil profile and can be graphically shown in three two-dimens
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c198027f32628406f4885dc504f547e5
https://doi.org/10.1134/s1064229316010087
https://doi.org/10.1134/s1064229316010087
Publikováno v:
Eurasian Soil Science. 47:1227-1237
For the comprehensive description of the acidity of a two-phase ion-exchange system, we should analyze two curves of the ionite titration by a strong base in water and salt solutions and find the quantitative relationships between the corresponding p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bd7201efe852b47bce685696c7ea2d13
https://doi.org/10.1134/s1064229314120072
https://doi.org/10.1134/s1064229314120072
Publikováno v:
Moscow University Soil Science Bulletin. 69:147-155
Two profiles of weakly podzolised, well drained soils of abraded moraine plains in northwestern Russia are studied. The profiles are located at the edges and on the upper parts of slopes. They are developed upon two-layered rocks: stony sand-sandy lo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d901866f803a3399be38f46d58d3ce94
https://doi.org/10.3103/s0147687414040048
https://doi.org/10.3103/s0147687414040048
Autor:
Boris Aparin, E. Yu. Sukhacheva
Publikováno v:
Eurasian Soil Science. 47:650-661
For the first time, a soil map of St. Petersburg has been developed on a scale of 1 : 50000 using MicroStation V8i software. The legend to this map contains more than 60 mapping units. The classification of urban soils and information on the soil cov
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef1551ae357721a1390257d835e0267c
https://doi.org/10.1134/s1064229314070035
https://doi.org/10.1134/s1064229314070035