C. Farkas et al., Studies on certain physical soil properties in long-term soil cultivation experiments on a brown forest soil in Godollo, NOVENYTERME, 48(3), 1999, pp. 323-336
Changes in soil physical properties during the 1997 vegetation period were
studied under favourable nutrient supply conditions in a long-term soil cul
tivation experiment set up in 1994. The growing site was a rust-brown fores
t soil with moderate fertility, a shallow topsoil and moderate nutrient sup
plies. The present paper evaluates the effect of five soil cultivation vari
ants on thr, total porosity, volume mass, moisture dynamics and water reten
tion curves (pF curves) of the soil.
Analysis of variance between the treatments indicated that in all the treat
ments differences due to the cultivation effect could only be observed in t
he 0-40 cm layer. The application of direct drilling and disking over a num
ber of years resulted in significantly larger Volume mass values and lower
total porosity values compared with techniques involving soil turning and l
oosening.
It was found that the direct effect of cultivation on the pF curves could o
nly be demonstrated at the beginning of the vegetation period in the low su
ction force range. By the middle of the vegetation period (June) no signifi
cant differences could be observed between the water retention values measu
red at different suction forces. The indirect effect of cultivation was obs
erved at the end of the vegetation period (August).
The integrated effect of soil cultivation on various physical soil paramete
rs was characterised using measured soil moisture dynamics. Statistically s
ignificant differences were found between the soil moisture values in the p
loughed layer. During the period examined the soil was driest after direct
drilling, which is recommended in the literature as a way of reducing moist
ure losses. The highest moisture values were recorded after ploughing combi
ned with loosening. The results prove that results obtained under different
climatic conditions on different types of soil cannot be extrapolated; whe
rever possible, measurements should be made on the actual site.