『Abstract
Profiles of subsurface soil CO2 concentration,
soil temperature, and soil moisture, and throughfall were measured
continuously during the years 2005 and 2006 in 16 locations at
the free air CO2 enrichment facility situated
within a temperate loblolly pine (Pinus taeda L.) stand.
Sampling at these locations followed a 4 by 4 replicated experimental
design comprised of two atmospheric CO2 concentration
levels (ambient [CO2]a, ambient
+ 200 ppmv, [CO2]e) and two soil
nitrogen (N) deposition levels (ambient, ambient + fertilization
at 11.2 gN m-2 year-1).
The combination of these measurements permitted indirect estimation
of belowground CO2 production and flux profiles
in the mineral soil. Adjacent to the soil CO2
profiles, direct (chamber-based) measurements of CO2
fluxes from the soil-litter complex were simultaneously conducted
using the automated carbon efflux system. Based on the measured
soil CO2 profiles, neither [CO2]e
nor N fertilization had a statistically significant effect on
seasonal soil CO2, CO2
production, and effluxes from the mineral soil over the study
period. Soil moisture and temperature had different effects on
CO2 concentration depending on the depth.
Variations in CO2 were mostly explained by soil temperature at
deeper soil layers, while water content was an important driver
at the surface (within the first 10 cm), where CO2
pulses were induced by rainfall events. The soil effluxes were
equal to the CO2 production for most of the time, suggesting that
the site reached near steady-state conditions. The fluxes estimated
from the CO2 profiles were highly correlated
to the direct measurements when the soil was neither very dry
nor very wet. This suggests that a better parameterization of
the soil CO2 diffusivity is required for
these soil moisture extremes.
Keywords: Soil CO2 dynamics; Climate change;
Elevated atmospheric CO2; Nitrogen deposition;
Fertilization; Loblolly pine』
Introduction
Methods
Site description
Measurements
Data processing
Statistical analyses
CO2 fluxes and production
Results and discussion
Subsurface CO2 concentrations
Effects of the treatments
C dynamics at different depths and time-scales
Rainfall-induced variation in C near the soil surface
CO2 production and fluxes
Effect of the treatments
Soil CO2 storage
Vertical distribution and dynamics of CO2
fluxes and production
Limitations to comparisons between direct measurements and indirect
estimates of CO2 flux
Conclusions
Acknowledgments
References