『Abstract
Information about the impact of nitrogen (N) deposition on the
fate of deposited N in peatland ecosystems is lacking. Thus we
investigated the fate of experimentally added 15N in
long-term N-fertilized treatments in a Sphagnum-dominated
ombrotrophic bog. Fertilization significantly stimulated vascular
plant and suppressed Sphagnum and Polytrichum moss
growth. N content in peat, mosses, and vascular plants was raised
by the fertilizer addition and reached a maximum at 3.2 g m-2
N input level with phosphorus (P) and potassium (K) addition.
Most of N was retained in the vegetation and upper 10 cm of the
peat. When N deposition equalled 1.6 g m-2 and less,
or 3.2 g m-2 N with P and K addition, no inorganic
N leaching was observed on the plots. This result indicates that
co-fertilization with P and K raised the N retention capacity
and that critical N loads with respect to N saturation depend
on P and K availability. Most of the deposited 15N
was recovered in the bulk peat, which may be related to a rapid
immobilization of inorganic N by microorganisms and mycorrhizal
assimilation. Increase of N, P, and K fertilization increased
the contribution of vascular plants to N retention significantly
and reduced those of mosses. The increase was mainly related to
enhanced productivity, vascular biomass and N content in tissues;
the reduced retention by mosses resulted from both reduced moss
biomass and assimilation. The study shows that the N filter function
of ombrotrophic bogs will be influenced by interactions with other
nutrients and shifts in plant community structure.
Keywords: Peatland; Bog; Nitrogen deposition; Nitrogen saturation;
Nitrogen retention』
Introduction
Materials and methods
Study sites
Experimental design and field sampling
Chemical analyses
Calculations and statistics
Results
Effects of fertilization on ecosystem structure and biomass
Nitrogen contents and concentrations
Retention of 15N
15N balance and 15N retention efficiency
Discussion
N retention by mosses
N retention in peat
N retention in vascular plants
N saturation and importance of P and K
Conclusions
Acknowledgements
References