This experiment was performed under laboratory conditions in three replicat
ions. Three types of horticultural soil were put in plastic pots using 200
dm(3) per pot. Prior to filling the pots, the soils were carefully mixed wi
th dusty elementary sulfur at 0.0, 1.0, 2.0, 3.0, 4.0 and 5.0 g.dM(-3) and
incubated for three months at 18-20 degreesC, maintaining moisture at 60% o
f capillary water holding capacity. After 90 days the samples were taken fo
r the determination of active acidity in H2O, hydrolytic acidity (H) and to
tal of bases (S). Based on the results of the assay, the total exchange cap
acity (T) and degree of base saturation (V) were computed from the formulas
: T = S + H and V = S.T-1.100. In addition, the activity of dehydrogenases,
urease and acid and alkaline phosphatase was determined.
Elementary sulfur was found to have an effect on physicochemical and bioche
mical properties of horticultural soil. The highest rate of sulfur reduced
pH (in H2O) from 6.7 to 3.9, the total of exchange bases by 3-fold, the tot
al exchange capacity by 1.2-fold and the degree of base saturation by 2.4-f
old. It also depressed the activity of dehydrogenases by 12.6-fold, urease
by 74.1-fold, acid phosphatase by 1.8-fold and alkaline phosphatase by 4.1-
fold. Sulfur applied at 5 g.dm(-3) increased hydrolytic acidity by 9-fold.