『Abstract
Fluxes of dissolved organic carbon (DOC) and nitrogen (DON) may
play an important role for losses of C and N from the soils of
forest ecosystems, especially under conditions of high precipitation.
We studied DOC and DON fluxes and concentrations in relation to
precipitation intensity in a subtropical montane Chamaecyparis
obtusa var. formosana forest in Taiwan. Our objective
was, to quantify DI\OC and DON fluxes and to understand the role
of high precipitation for DOC and DON export in this ecosystem.
From 2005 to 2008 we sampled bulk precipitation, throughfall,
forest floor percolates and seepage (60 cm) and analyzed DOC,
DON and mineral N concentrations. Average DOC fluxes in the soil
were extremely high (962 and 478 kg C ha-1 year-1
in forest floor percolates and seepage, respectively) while DON
fluxes were similar to other (sub)tropical ecosystems (16 and
8 kg N ha-1 year-1, respectively). Total
N fluxes in the soil were dominated by DON. Dissolved organic
C and N concentrations in forest floor percolates were independent
of the water flux. No dilution effect was visible. Instead, the
pool size of potentially soluble DOC and DON was variable as indicated
by different DOC and DON concentrations in forest floor percolates
at similar precipitation amounts. Therefore, we hypothesized,
that these pools are not likely to be depleted in the long term.
The relationship between water fluxes in bulk precipitation and
DOC and DON fluxes in forest floor percolates was positive (DOC
r = 0.908, DON r = 0.842, respectively, Speatman rank correlation).
We concluded, that precipitation is n important driver for DOC
and DON losses from this subtropical montane forest and that these
DOC losses play an important role in the soil C cycle of this
ecosystem. Moreover, we found that the linear relationship between
bulk precipitation and DOC and DON fluxes in forest floor percolates
of temperate ecosystems does not hold when incorporating additional
data on these fluxes from (subtropical) ecosystems.
Keywords: Dissolved organic nitrogen; Dissolved organic carbon;
Precipitation; Fluxes; Forest floor; Subtropical montane forest』
Introduction
Materials and methods
Site description
Sample collection and analysis
Calculations
Statistical analyses
Results
Discussion
Conclusions
Acknowledgements
References