Claim · model-written summary
As grass stands grow older, soil density increases as it reaches equilibrium values.
Verbatim
e3“As grass stands grow older, soil density increases as it reaches equilibrium values, their moisture increases as a result of a decrease in evaporative intensity, and the porosity and porosity of aeration decrease, but the effect of grasses on the physical properties of the soil increases”
Title
HYDROPHYSICAL SOIL FEATURES UNDER MIXED AGE PLANT FORMATION IN RECLAIMED AGROLANDSCAPE
D. А. Ivanov; М. V. Rublyuk Vestnik of the Russian agricultural science 1970. doi:10.30850/vrsn/2019/3/26-29
Other claims from this paper (11)
- Intervention effect Grass sowing is an effective method of regulating the water-air properties of soils in the agrolandscape.
- Association About 43% of the spatial variability of water-physical soil indicators on the moraine hill agroland is due to grass stands.
- Association As grass stands grow older, soil moisture increases as a result of a decrease in evaporative intensity.
- Association As grass stands grow older, the porosity and aeration porosity of soils decrease.
- Association As grass stands grow older, the effect of grasses on the physical properties of the soil increases.
- Association Young grass stands (1 and 2 years of life) determine one-third of the spatial variability of water-physical indicators of landfill sites.
- Association Older grass stands determine half of the spatial variability of water-physical indicators of landfill sites.
- Association The plant component of the agrolandscape has the maximum effect on the spatial variability of soil density (62.3%).
- Association The plant component of the agrolandscape has the maximum effect on the spatial variability of soil porosity (51.5%).
- Association Vegetation determines 36% of the variability of soil moisture in the agrolandscape.
- Association Vegetation determines 22% of the variability of soil aeration porosity in the agrolandscape.