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Within the process of matter circulation, soil microorganisms play a decisive role in the biological circulation of nutrition elements, i.e. plant assimilatives, through the process of organic matter (detritus) degradation via biosynthesis (humification) and mineralization (dehumification), releasing plant assimilatives and thus enabling forests to survive as natural ecosystems. Development of appropriate physiological groups of microorganisms participating in such processes and their biological activity are prerequisites of forest ecosystem stability. The results of the research in microbiological activity of the forest soil conducted in the areas within the territory of Belgrade include 19 locations of forested areas in both state and private ownership. Preliminary research suggested that the process of ammonification is by far the most significant in both synthesis and degradation of humus for plant assimilative formation (nitrogen, phosphorus, sulphur etc.); therefore the measures undertaken must be focused on ensuring normal and regular course of such processes.

Microbiological activity of the forest soil in the areas within the territory of Belgrade