P. Gundersen, EFFECTS OF ENHANCED NITROGEN DEPOSITION IN A SPRUCE FOREST AT KLOSTERHEDE, DENMARK, EXAMINED BY MODERATE NH4NO3 ADDITION, Forest ecology and management, 101(1-3), 1998, pp. 251-268
The fate and effects of increased N deposition were investigated by ex
perimental manipulation in a mature Norway spruce plantation at Kloste
rhede, western Denmark. The ambient N deposition was 15-20 kg Nha(-1)y
r(-1). Addition of 35 kg Nha(-1)yr(-1) as ammonium nitrate to a 500-m(
2) plot was carried out by handspraying monthly for 4 years. During th
e first year the spray was labeled with N-15. Tree growth was depresse
d by 4 successive spring or summer droughts throughout the treatment y
ears. The nitrogen concentration in needles increased in the third yea
r of treatment and critical low P concentrations (0.6-1 mg Pg(-1)) dev
eloped possibly as a combined effect of drought and N stress on roots
and mycorrhizae. Reduced retranslocation of N was indicated by increas
ed concentration and flux of N in needle litterfall. Increased uptake
of N was observed in all parts of the trees and the fraction of the in
put N taken up was increased from 32 to 43%, whereas the fraction immo
bilized in the soil was decreased from 40 to 33% of the input N. The d
ecomposition remained unchanged, whereas the net N mineralization was
increased 85% over the control. The effect on net mineralization may h
ave resulted from saturation of the immobilization process rather than
from an increase in gross mineralization. Soil respiration was not af
fected, indicating that microbial activity did not respond. Nitrificat
ion and denitrification were not important in either control or treate
d soils. Soil solution chemistry responded promptly to nitrogen applic
ations. Nitrate concentrations increased at all depths, and nitrate le
aching increased from < 0.3 to 4.2 kg Nha(-1)yr(-1) by the third year.
Reduced biological control on nitrate leaching was indicated by incre
ased nitrate concentration in soil water at the end of the growing sea
son. Ammonium concentrations increased down to 15 cm depth, but all am
monium was retained in the system. Despite the increased nitrate leach
ing, 92% of the total inputs were retained. No changes in concentratio
ns of other major ions due to the N additions were detectable. The eff
ects of the successive droughts on growth and nutrient cycling caused
significant interaction on the response to N addition. Continuation of
the N addition treatment will be necessary to observe the full respon
se of the simulated deposition increase in this forest. (C) 1998 Elsev
ier Science B.V.