Facebook Instagram Twitter RSS Feed PodBean Back to top on side

Specific features of water infiltration into soil with different management in winter and early spring period

In: Journal of Hydrology and Hydromechanics, vol. 58, no. 3
Stanislav Hejduk - Klaudius Kasprzak
Detaily:
Rok, strany: 2010, 175 - 180
Kľúčové slová:
Infiltration, Cryopedosphere, Surface Runoff, Thawing and Freezing, Soil Tillage, Grassland.
URL originálneho zdroja: http://www.ih.savba.sk/jhh
O článku:
The paper deals with the effects of agricultural soils management on surface runoff in winter and early spring period. Cryogenic processes that take place in soils can cause temporary reduction of infiltration capacity of soil. In the periods of snow-thawing and rain these phenomena induce conditions promoting the occurrence of surface runoff and floods. Effects of agricultural soils management on surface runoffs were studied at the research station in Brno-Kníničky, Czech Republic, from 1965 to 2002. The aim of this research was to find out the differences between the winter surface runoff from experimental plots under winter wheat crop sown after plowing and under perennial forage crops without tillage. On soils without plowing, the decrease of soil infiltration rate occurred faster and was more intensive than on loose soils. During ten winter periods the average surface runoff from perennial forages was significantly higher (2.05 times) than from wheat crop (runoff coefficients 0.239 vs. 0.489).
Ako citovať:
ISO 690:
Hejduk, S., Kasprzak, K. 2010. Specific features of water infiltration into soil with different management in winter and early spring period. In Journal of Hydrology and Hydromechanics, vol. 58, no.3, pp. 175-180. 0042-790X (until 2019) .

APA:
Hejduk, S., Kasprzak, K. (2010). Specific features of water infiltration into soil with different management in winter and early spring period. Journal of Hydrology and Hydromechanics, 58(3), 175-180. 0042-790X (until 2019) .