Effects of Atmospheric CO 2 Enrichment on Soil CO 2 Efflux in a Young Longleaf Pine System

Abstract

The southeastern landscape is composed of agricultural and forest systems that can store carbon (C) in standing biomass and soil. Research is needed to quantify the effects of elevated atmospheric carbon dioxide (CO 2 ) on terrestrial C dynamics including CO 2 release back to the atmosphere and soil sequestration. Longleaf pine savannahs are an ecologically and economically important, yet understudied, component of the southeastern landscape. We investigated the effects of ambient and elevated CO 2 on soil CO 2 efflux in a young longleaf pine system using a continuous monitoring system. A significant increase (26.5%) in soil CO 2 efflux across 90 days was observed under elevated CO 2 ; this occurred for all weekly and daily averages except for two days when soil temperature was the lowest. Soil CO 2 efflux was positively correlated with soil temperature with a trend towards increased efflux response to temperature under elevated CO 2 . Efflux was negatively correlated with soil moisture and was best represented using a quadratic relationship. Soil CO 2 efflux was not correlated with root biomass. Our data indicate that, while elevated CO 2 will increase feedback of CO 2 to the atmosphere via soil efflux, terrestrial ecosystems will remain potential sinks for atmospheric CO 2 due to greater biomass production and increased soil C sequestration.