Vegetation and elevation influence the timing and magnitude of soil CO2 efflux in a humid, topographically complex watershed

摘要

In topographically complex watersheds, landscape position and vegetation heterogeneity can alter the soil water regime through both lateral and vertical redistribution, respectively. These alterations of soil moisture may have significant impacts on the spatial heterogeneity of biogeochemical cycles throughout the watershed. To evaluate how landscape position and vegetation heterogeneity affect soil CO2 efflux (F-SOIL), we conducted observations across the Weimer Run watershed (373 ha), located near Davis, West Virginia, for three growing seasons with varying precipitation. An apparent soil temperature threshold of 11 degrees C for F-SOIL at 12 cm depth was observed in our data, where F-SOIL rates greatly increase in variance above this threshold. We therefore focus our analyses of F-SOIL on instances in which soil temperature values were above this threshold. Vegetation had the greatest effect on F-SOIL rates, with plots beneath shrubs at all elevations, for all years, showing the greatest mean rates of F-SOIL (6.07 mu mol CO2 m(-2) s(-1)) compared to plots beneath closed-forest canopy (4.69 mu mol CO2 m(-2) s(-1)) and plots located in open, forest gap (4.09 mu mol CO2 m(-2) s(-1)) plots. During periods of high soil moisture, we find that CO2 efflux rates are constrained, and that maximum efflux rates occur during periods of average to below-average soil water availability. While vegetation was the variable most related to F-SOIL, there is also strong interannual variability in fluxes determined by the interaction of annual precipitation and topography. These findings add to the current theoretical constructs related to the interactions of moisture and vegetation in biogeochemical cycles within topographically complex watersheds.