Early Spring Surface Runoff from Grassland and Arable Land

Surface runoff is regarded as an undesirable phenomenon because it deprives plants and soil of precipitation water and reduces its penetration underground. It is also the cause erosion and flooding. The occurrence and depth of a frozen soil layer is the main factor which determines the amount of surface runoff in winter. A well-developed surface and/or sub-surface layer of frozen soil is practically impenetrable for water. This layer results from ice-forming processes, which are influenced by snow melting due to diurnal fluctuations in temperature in early spring, partial thaws, winter rainfalls, and thermocapillary processes taking place in frozen soil

CHANGES OF SOIL AGRICHEMICAL CHARACTERISTICS IN PASTURES INFLUENCED BY MINERAL FERTILIZING

Abstract HEJDUK,

CA Event Actionability

No abstract availabl

AUTUMN TERMS OF SOWING OF TURF GRASSES AND LEGUMES AND THEIR INITIAL DEVELOPMENT

Abstract AMBRUZ, J., HEJDUK, S.: Autumn terms of sowing of turf grasses and legumes and their initial development. Acta univ. agric. et silvic. Mendel. Brun., 2011, LIX, No. 6, pp. 9-1

Data from: Establishment of a hemiparasite Rhinanthus alectorolophus and its density-dependent suppressing effect on a grass: A case study from golf roughs

Data from: Establishment of a hemiparasite Rhinanthus alectorolophus and its density-dependent suppressing effect on a grass: A case study from golf roughs. Agronomy Journal. DOI: 10.1002/agj2.20300 All relevant data supporting the results of our study. 1. the file host_data.txt includes the data from our host suitability experiment (Rhinanthus biomass in response to 12 hosts) 2. the file fertilization_data.txt includes the data from our fertilization trials (fescues biomass and height in response to Rhinanthus and its density