Although the available data on soil NO emission are increasing, only few me
asurements have been made in temperate forests. Emissions from these forest
s are generally low, but recent studies have shown that NO emission from N-
affected forests can be much higher. In this study the emission of NO from
the door of a moderately N-affected. Norway spruce forest in Denmark was me
asured using dynamic chambers during two seasons (April 1995 and September
1995). At the same time, fluxes of CO2 and NO2, soil water content inside a
nd outside the chambers, soil temperature at 10 cm depth, soil surface temp
erature and air temperature were, recorded. The emission of NO in April was
low (< 0.3 ng N m(-2) s(-1)), whereas it was significantly higher in Septe
mber (21 ng N (-2) s(-1) with a range 0-82 ng N m(-2) s(-1)). In April the
soil surface temperature was low (< 6"C) and the soil moisture was high (26
% vol/vol). In September the soil surface temperature was high (16 degrees
C) and soil moisture was significantly lower (14% vol/vol) than in April. T
here was a high correlation between CO2 emission and NO emission. The fluxe
s of NO2 were very small and not related to NO emission. Generally, the var
iation within a single plot was small, whereas the variation between plots
was large. About half of the total variation of NO emission in September co
uld be explained by a combination of soil moisture, distance to tree trunks
, and moss cover. No significant relationship could be found between NO emi
ssion and soil surface temperature or soil temperature. Other parameters su
ch as the C/N dynamics in the soil must be taken into account to provide a
better mechanistic understanding of the NO emission. An annual emission of
3.15 kg NO-N ha(-1) yr(-1) was estimated by the amount of NH4+ in throughfa
ll. Compared to most of the previous published measurements of NO emission
from temperate forest soils, the values presented here are high and of the
same magnitude as found in N-affected forests in Central Europe.