Temperature regime of agrosoddy-podzolic soils on slopes of different steepness

Autor:	O. A. Savoskina, M. A. Mazirov, M. V. Bannikov, Evgeny Shein
Rok vydání:	2011
Předmět:	Hydrology Snow melting Soil temperature Hydraulic conductivity Soil water Soil Science Soil science Vegetation and slope stability Geology Earth-Surface Processes Degree (temperature)
Zdroj:	Eurasian Soil Science. 44:157-162
ISSN:	1556-195X 1064-2293
DOI:	10.1134/s1064229311020104
Popis:	Soil temperature regime at the depth of 20 cm may vary considerably on different parts of a given slope. This variation may be related to the position of the particular site on the slope and to the geomorphic features of the slope, including its surface inclination. The soils of the upper steep part of the slope of southern aspect are subjected to more active warming in the spring. They are characterized by higher cumulative temperatures above 10°C. The degree of this difference depends on the particular weather conditions. The differences in the soil temperature regimes may be the reason for the unequal crop yields on the different parts of the slope.
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_________::79dd23c2c8da4ef98e705c9cc72e7187 https://doi.org/10.1134/s1064229311020104 Zobrazit plný text záznamu Plný text ve formátu PDF