NITRIFICATION AND NITROUS-OXIDE PRODUCTION POTENTIALS IN AEROBIC SOILSAMPLES FROM THE SOIL-PROFILE OF A FINNISH CONIFEROUS SITE RECEIVING HIGH AMMONIUM DEPOSITION

Citation
Pj. Martikainen et al., NITRIFICATION AND NITROUS-OXIDE PRODUCTION POTENTIALS IN AEROBIC SOILSAMPLES FROM THE SOIL-PROFILE OF A FINNISH CONIFEROUS SITE RECEIVING HIGH AMMONIUM DEPOSITION, FEMS microbiology, ecology, 13(2), 1993, pp. 113-121
Citations number
25
Categorie Soggetti
Microbiology
Journal title
ISSN journal
01686496
Volume
13
Issue
2
Year of publication
1993
Pages
113 - 121
Database
ISI
SICI code
0168-6496(1993)13:2<113:NANPPI>2.0.ZU;2-J
Abstract
Using aerobic soil slurry technique nitrification and nitrous oxide pr oduction were studied in samples from a pine site in Western Finland. The site received atmospheric ammonium deposition of 7-33 kg N ha(-1) a(-1) from a mink farm. The experiments with soil slurries showed that the nitrification potential in the litter layer was higher at pH 6 th an at pH 4. However, the nitrification potentials in the samples from the organic and mineral horizons at pH 6 and 4 were almost equal. Also N2O was produced at a higher rate at pH 6 than at pH 4 in slurries of the litter layer samples. The reverse was true for samples from the o rganic and mineral horizons. The highest N2O production and nitrificat ion rates were measured in the suspensions of litter layer samples. Ni trification activity in field-moist soil samples was lower than the ac tivity in the slurries indicating that the availability of ammonium li mited nitrification in these soils. Acetylene (2.5 kPa) retarded nitri fication activity (70-100%) and N2O production (40-90%) in soil slurri es. Acetylene inhibited the N2O production by 40-60% during the first 3 days after its addition to field-moist samples incubated in aerobic atmosphere. After 3 days the inhibition became much lower (4-5%). The results indicate that, in soil profiles of boreal coniferous forests r eceiving ammonium deposition, chemolithotrophic nitrification may have importance in the N2O production, and that changes in soil pH affect differently nitrification as well as N2O production in litter and deep er soil layers.