Gpj. Draaijers et al., THE APPLICATION OF THROUGHFALL MEASUREMENTS FOR ATMOSPHERIC DEPOSITION MONITORING, Atmospheric environment, 30(19), 1996, pp. 3349-3361
An overview of the technical requirements of throughfall, stemflow and
precipitation measurements used for monitoring atmospheric deposition
to Forests is presented. A mechanistic basis is presented to link thr
oughfall fluxes to atmospheric deposition. For homogeneous forest stan
ds with a closed canopy, the overall uncertainty in annual mean soil l
oads can be as low as 10-15% if state-of-the-art measurement and analy
tical techniques are used in combination with a sufficiently large num
ber of replicate samplers. The uncertainly in atmospheric deposition e
stimates, however, is estimated much larger, i.e. up to 30% for sulphu
r and 40% for nitrogen and base cations. This is mainly attributed to
(i) uncertainties associated with the estimation of canopy exchange, a
nd (ii) dry deposition to the forest floor and understorey vegetation
which is usually not addressed in throughfall studies. Additional rese
arch on canopy exchange in relation to tree species, ecological settin
g and pollution climate is recommended, pounds and base cations, and m
ay serve as a basis for improvement of current canopy budget models. C
opyright (C) 1996 Elsevier Science Ltd