Summary A loam from the Frilsham and one from the Wickham Series were incubated at 50 and 90 per cent of their water contents at saturation with 100 μg NH 4 NO 3 ‐N g −1 soil in the presence and absence of C 2 H 2 (0.5 per cent, v/v). Acetylene inhibited nitrification in both soils, but had no effect on mineralization of N. No denitrification (measured as the production of N 2 O in the presence of C 2 H 2 ) occurred during incubation at 50 per cent saturation. At 90 per cent saturation, denitrification resulted in a loss of 28.4 and 36.7 μg N g −1 after 48 h from the Frilsham and Wickham soils, respectively. The concurrent inhibition of nitrification had no effect on the extent of denitrification at this time. In the Wickham soil, NO 3 − was exhausted after 168 h incubation in the presence of C 2 H 2 and denitrification was underestimated by 13 μg N g − . The data suggested that concurrent inhibition of nitrification during measurement of denitrification using the C 2 H 2 inhibition technique is most likely to affect the estimate of denitrification loss when NO 3 − supply is limited by the inhibition of nitrification.
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J. C. Ryden (1982) studied this question.
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