Results of long-term studies of gas formation in silts of fish hatcher
y ponds under different operating conditions are presented. Methane co
nstituted up to half of the total volume of bottom gas. Methanogenesis
proceeded most actively in July and August (up to 8 mg C/liter/day).
Methanogenesis from acetate was slightly dominant, conceivably due to
a high rate of acetogenesis (5 mg C/liter/day). Methanogenesis contrib
uted about 20% to the total anaerobic process of organic matter destru
ction in silt. Bottom gas content depended on the intensities of fish
feeding and water exchange. Up to 25% of generated methane was oxidize
d in upper silt layers and near-bottom water, which affected the oxyge
n regime of fish hatchery ponds and the condition of fish brood.