Zobrazeno 1 - 7
of 7
pro vyhledávání: '"K. B. Anisimov"'
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 87, Pp 114-127 (2017)
The dynamics of the soil water potential and soil temperature at different depths during the year was studied. As the object of the investigation we took soddy-podzolic clay loamy weakly gleyed soils of Zelenogradskiy base of Soil Science Institute.
Externí odkaz:
https://doaj.org/article/c53fe8e4c05643e584c027a1be37e17c
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 82, Pp 71-87 (2016)
Every ecological group of plants including hygrophytes, mesophytes and xerophytes is characterized by a definite narrow interval of the soil water potential, in which the values of relative transpiration cannot be lower than the optimal level (1.0-0.
Externí odkaz:
https://doaj.org/article/ab0e118ad8bf498a9eb8e5cdbc9b84c5
Autor:
N. A. Muromtsev, K. B. Anisimov
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 77, Pp 78-93 (2015)
Under consideration is the dynamics of moisture reserves and soil water potential in different parts of the catena represented by soddy-podzolic slightly gleyed soil. Peculiar features in the development of moisture reserves have been identified in d
Externí odkaz:
https://doaj.org/article/9fb5e99a79df4d84b91115588f8cbe8f
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 76, Pp 111-125 (2014)
The experimental studies permitted to determine the ratio between infiltration and transpiration of the ground water in a soddy podzolic soil, that accounts for 0.3-0.6 under dried conditions of atmospheric moistening, 2.6-2.9 as an average value for
Externí odkaz:
https://doaj.org/article/e5d1259bb0864643ad65d237a832503e
Publikováno v:
Бюллетень Почвенного института им. В.В. Докучаева, Vol 0, Iss 73, Pp 121-149 (2014)
The paper is devoted to the analysis and evaluation of peculiar features of the water regime in loam-sandy soils of Oman. The total water volume taken up by potatoes has been determined in different modes of pre-irrigation soil moisture (70, 80% of M
Externí odkaz:
https://doaj.org/article/c53ddfa229f24db3b4f2b5d827df8fd6
Publikováno v:
Dokuchaev Soil Bulletin. 82:71-87
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3889812284fe3502a7a6fa232f97df13
https://doi.org/10.19047/0136-1694-2016-82-71-87
https://doi.org/10.19047/0136-1694-2016-82-71-87
Publikováno v:
Eurasian Soil Science. 48:742-747
The regularities of water infiltration and evaporation of groundwater at different depths of the groundwater table were established for soddy-podzolic and dark gray forest soils. The recharge of the soils with moisture from the groundwater decreased
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::74342bf6cab1909914d66d631ef90c4b
https://doi.org/10.1134/s106422931507008x
https://doi.org/10.1134/s106422931507008x