Passive flux samplers were used to determine the ammonia exchange on a
n inland heath in Denmark over the last 2 years. The samplers measured
the horizontal ammonia flux directly. Data were sampled continuously
for periods of 1-4 weeks. The micro-meteorological gradient method was
used with passive flux samplers and cup anemometers at different heig
hts above the vegetation in order to calculate the vertical fluxes of
ammonia. First a fixed sampler system was used with tubes mounted in f
our orthogonal horizontal directions. This system has been successfull
y applied to measure the emission from fertilized crops. Adapting this
type of sampler to measure the deposition to heathlands did not prove
to be straightforward. The precision of the calculated ammonia concen
trations vias too poor to give an acceptable accuracy for the concentr
ation gradient. The problems were (a) driving rain which entered the t
ubes, (b) too few measuring points in each concentration profile, and
(c) too long sampling periods to allow for the low-concentration level
s above the heath arsa and the detection limits. Therefore, a passive
flux sampler mounted on a wind vane and fitted with a rain shelter was
developed. Results from the first 5 weekly periods are very promising
, yielding accurate concentration gradients. The advantages of the pas
sive flux samplers on the wind vane are (a) the minimum measuring peri
od can be approximately halved compared to the fixed samplers,(b) some
of the directional correction terms used with the fixed passive flux
samplers are dispensed with, and (c) the field and laboratory work is
minimized. (C) 1998 Elsevier Science Ltd. All rights reserved.