| Results and discussion |
A strong seasonal trend of microbial nutrient dynamics was
detected. This trend was dependent on tree species as birch and spruce groups
showed different microclimate, root distribution, shading, litter quality and
transpiration rates. It turned out that the mineral soil under birch was dryer
due to enhanced transpiration. However, the humic layer under birch was more
moist and less susceptible to drying during summer. Accordingly, the microbial
biomass in birch humus showed a different seasonal dynamic compared to spruce
humus. Birch plots had a higher soil respiration and less acidic pH. In soils
under birch microbial biomass correlated with NH4+ availability (r=0.6;
p<0.05), which often exceeded spruce plots. Respiration rates were dependent
on air temperature. We conclude that 20 year old birch trees already exerted a
positive influence on microbial mineralisation processes and on soil chemistry.
In contrast microbial biomass and respiration rates in spruce plots relied on
precipitation and on soil moisture. They declined under dry periods, which
means that in this climate microbial decomposition processes and nutrient
release may be inhibited in summer under spruce. There was no significant
difference of N2O emissions between spruce and birch plots. Highest emissions
occurred during warm and rainy weather. The availability of NO3- and NH4+ did
not seem limiting for the emission of N2O as there was no correlation between
these parameters during the vegetation period. We cannot suggest preference of
either investigated tree species in terms of green-house gas mitigation. The
results of our study emphasise the possible value of birch as a pioneer tree
species. Due to the better litter quality and the stimulation of microbial
mineralisation, birch can help in the restoration of secondary coniferous
forests and in the conversion into more stable mixed deciduous forests in this
area. According to our measurements there is no danger of enhanced nitrogen
losses, such as NO3--leaching or emission of the greenhouse gas N2O.
Figure 1:
Seasonal course of soil respiration in spruce and birch
plots.
References Schinner F., Öhlinger
R., Kandeler E., Margesin R. (Eds.) Methods in Soil Biology. Springer Verlag,
Berlin Hahn M., Gartner K., Zechmeister-Boltenstern S. (2000) Greenhouse
gas emissions (N2O, CO2 and CH4) from beech forests near Vienna with different
water and nitrogen regimes. Die Bodenkultur - Austrian Journal of Agricultural
Research 51, 115-125. |