wAbstract
@Most previous studies investigating controls on nitrous oxide
(N2O) emissions have relied on plot-scale
experiments and focused on relative homogeneous biotic and abiotic
factors such as soil, vegetation, and moisture. We studied soil
N2O flux at 11 chamber sites along a 620
m topographic gradient in upstate New York, USA, aiming at identifying
patterns of N2O flux and correlating them
to hydrological factors and soil substrate properties along the
gradient. The topographic gradient is a complex slope with an
overall gradient of 8%, covering plant communities of pasture,
forest, alfalfa field, and riparian area from the top to the bottom.
Mean fluxes of N2O measured from late March
to May ranged from 4.45 to 343 สg N m-2 h-1,
and these fluxes were not significantly different among chamber
sites located in different communities. With the descending of
the slope, N2O fluxes increased with the
increase of soil water content, except for the riparian site.
Statistically, N2O fluxes were not strongly
correlated with soil temperature, soil bulk density, and water
filled pore space (p0.05). Instead, strong correlations (p0.05)
were found between N2O fluxes and soil C
and N content including NO3-,
NH4+, total organic carbon, and
C/N ratio. Multiple linear regression analyses including both
soil physical and substrate properties highlighted the significance
of soil NO3- content and C/N ratio
in regulating N2O fluxes along the gradient.
Keywords: Greenhouse gases; Soil carbon; Soil nitrogen; Global
climate change; Spatial variationx
1. Introduction
2. Materials and methods
@2.1. Site description
@2.2. N2O flux measurement
@2.3. Measurement of soil temperature and moisture
@2.4. Soil sampling and laboratory analysis
@2.5. Statistical analysis
3. Results
@3.1. Soil characteristics
@3.2. N2O flux
@3.3. Environmental controls and N2O flux
4. Discussion
Acknowledgements
References