Denitrification in orthic Luvisols (Praha-Ruzyne) was observed in labo
ratory soil experiments of three water saturation levels (100, 200, an
d 300% water-filled pore space - WFPS). The 10-day preincubation at 20
to 22 degrees C stabilized the soil system in N-cycle. After that KNO
3 (5 mg NO3-N in 100 g soil) and glucose (5 mg C in 100 g soil) were a
dded and the 5-day incubation prolonged the experiment. The reduction
of nitrates and the production of N2O showed the direct relationship w
ith WFPS and the content of extractable C-ox. One set of every variant
was inhibited by acetylene to depress the N2O-reductase activity. The
nitrate reduction and N2O production slowed down (18 and 5%) in the v
ariant A of 100% WFPS. The values of Eh reached 400 to 300 mV at pH 6
to 8. The amount of extractable C-ox was consumed in 80 to 90%. The re
duction of nitrates (50 to 60%) and N2O emissions (10 to 12%) increase
d with increasing WFPS (200 to 300%). The content of extractable C-ox
decreased to zero and the exogenic carbon source was necessary. The re
dox potential was 200 to 180 mV. The CO2 production was adequate. The
acetylene inhibition was convenient.