For the first time, the rapid multipoint method was used to characterize th
e complex of hydrolytic bacteria in hydromorphic forest soils. The soddy-gl
ey soil differs markedly from the other hydromorphic soils by maximum value
s of the number and the diversity of hydrolytic bacteria. In the peaty-podz
olic and peat soils, the only representative of bacteria capable of decompo
sing plant and microbial remnants is Bacillus, with the dominant species be
ing Bacillus circulans. Spatial (along the soil profile) and temporal (spri
ng-autumn) changes in the taxonomic structure of soil bacterial communities
are revealed.