A. Gallardo et J. Merino, SOIL-NITROGEN DYNAMICS IN RESPONSE TO CARBON INCREASE IN A MEDITERRANEAN SHRUBLAND OF SW SPAIN, Soil biology & biochemistry, 30(10-11), 1998, pp. 1349-1358
Most models predict that high atmospheric CO2 concentrations will lead
to an increase in the C-to-N ratio of litter production in terrestria
l ecosystems. The effect of an increase in the soil C-to-N ratio on th
e nitrogen dynamics in a Mediterranean shrubland was simulated by mixi
ng with the lifter layer wood shavings with a high C-to-N ratio. Sampl
es of mineral soil, taken subsequently eight times during 404 d, were
analyzed for total C, total N, total soil carbohydrates, potential net
N mineralization, potential net nitrification and microbial biomass-N
. We found significant increases in the concentration of total carbohy
drates, C-to-N ratio and microbial biomass N in amended soils during t
he experiment, while potential net N mineralization rate and net nitri
fication rate significantly decreased; amounts of available nitrogen (
NH4+-N + NO3-N) were unaffected by the amendment treatment. However, b
y the end of the experiment, no significant differences between amende
d and control soil samples were found. The total carbohydrates-to-K2SO
4-extractable total-N ratio was the best predictor of both net mineral
ization rate and microbial biomass N, showing that the available C-to-
available-N ratio is a better indicator of N dynamics than the total C
to total N ratio. Our results support the hypothesis that increasing
C availability in soils leads to a decrease in N availability for plan
ts through the immobilization of N in microbial biomass and to an incr
ease in the temporal heterogeneity of soil properties in a Mediterrane
an shrubland. (C) 1998 Elsevier Science Ltd. All rights reserved.