Jw. Nijburg et Hj. Laanbroek, THE FATE OF N-15-NITRATE IN HEALTHY AND DECLINING PHRAGMITES-AUSTRALIS STANDS, Microbial ecology, 34(3), 1997, pp. 254-262
The dissimilatory nitrate-reducing processes, denitrification, and dis
similatory nitrate-reduction to ammonium were studied in freshwater la
ke sediments within healthy and degrading Phragmites australis (reed)
stands. The samples from the healthy vegetation site contained roots a
nd rhizomes. Cores were supplied with 1.9-5.2 mu g N-15-NO3- g(-1) dry
sediment in the laboratory and subsequently incubated for 8 h at 20 d
egrees C, in the dark. The N-15 compounds were determined before (natu
ral percentage of N-15) and after 1 and 8 h of incubation. The uptake
of N-15 by the roots and rhizomes in the healthy vegetation was 61%. N
itrogen losses, interpreted as denitrification, accounted for 25 and 8
4% of the added N-15-NO3- in sediment from the healthy and degrading v
egetation sites, respectively. The percentages of nitrate reduced to a
mmonium were 4 and 9% in sediment from the healthy vegetation and degr
ading vegetation sites, respectively. The percentage of N-15-total N i
n the sediment of the healthy vegetation site was 10%, whereas for the
degrading vegetation site this percentage was 7%. The percentage of n
itrate reduced to ammonium could be potentially underestimated by the
percentage of N-15 measured in the sediment. In this case, in healthy
and degenerating P. australis stands, the percentage of produced ammon
ium accounted for 14-16%. The nitrate reduction rates were calculated
based on an incubation period of one hour. The denitrification rate in
sediment from the degrading vegetation site was higher than from the
healthy vegetation site. The rate of dissimilatory nitrate reduction t
o ammonium was almost tenfold higher in sediment from the degrading ve
getation site compared to sediment from the healthy vegetation site. T
he significantly lower percentages of dissimilatory nitrate reduction
to ammonium and denitrification in the healthy stand compared to the d
egrading stand was probably due to the presence of roots and rhizomes.
In the sediments of healthy and degrading P. australis stands, denitr
ification was the main nitrate-reducing process.