The dynamics of cellulase activity (CA) was followed during incubation
of ombrotrophic peat at different moisture levels. The highest CA was
observed at the lowest tested humidity of peat (40 to 60%). During th
e course of incubation, CA gradually increased over two weeks, reachin
g the maximum value of 0.4 mg reducing sugars (RS)/(h dm(3)) on the ni
nth day. Feat with a high moisture content (92 - 93%) preserved low CA
[0.05 mg RS/(h dm(3))], characteristic for the native peat. On the ba
sis of the dynamic data, it was concluded that the rise of CA in dried
peat was due to the activation of microorganisms, including hydrolyti
c ones, by the stress of drying and rewetting rather than to optimizat
ion of the peat water regime per se. This conclusion was confirmed in
special experiments with peat samples subjected to drying-rewetting cy
cles. The highest CA was always observed immediately after rewetting d
ried peat. During subsequent incubation under high moisture content (9
2 - 93%), CA remained high, oscillating within the range from 0.4 to 1
.0 mg RS/(h dm(3)).