Sustained effects of atmospheric [CO2] and nitrogen availability on forest soil CO2 efflux |
| |
Authors: | A. Christopher Oishi Sari Palmroth Kurt H. Johnsen Heather R. McCarthy Ram Oren |
| |
Affiliation: | 1. Division of Environmental Science & Policy, Nicholas School of the Environment, Duke University, , Durham, 27708‐0328 NC, USA;2. Coweeta Hyrdologic Laboratory, Southern Research Station, USDA Forest Service, , Otto, 28763 NC, USA;3. Department of Forest Ecology & Management, Swedish University of Agricultural Sciences (SLU), , Ume?, SE‐901 83 Sweden;4. Southern Research Station, USDA Forest Service, , Research Triangle Park, 27709 NC, USA;5. Department of Microbiology and Plant Biology, University of Oklahoma, , Norman, 73019 OK, USA;6. Department of Civil & Environmental Engineering, Pratt School of Engineering, Duke University, , Durham, 27708‐0271 NC, USA |
| |
Abstract: | Soil CO2 efflux (Fsoil) is the largest source of carbon from forests and reflects primary productivity as well as how carbon is allocated within forest ecosystems. Through early stages of stand development, both elevated [CO2] and availability of soil nitrogen (N; sum of mineralization, deposition, and fixation) have been shown to increase gross primary productivity, but the long‐term effects of these factors on Fsoil are less clear. Expanding on previous studies at the Duke Free‐Air CO2 Enrichment (FACE) site, we quantified the effects of elevated [CO2] and N fertilization on Fsoil using daily measurements from automated chambers over 10 years. Consistent with previous results, compared to ambient unfertilized plots, annual Fsoil increased under elevated [CO2] (ca. 17%) and decreased with N (ca. 21%). N fertilization under elevated [CO2] reduced Fsoil to values similar to untreated plots. Over the study period, base respiration rates increased with leaf productivity, but declined after productivity saturated. Despite treatment‐induced differences in aboveground biomass, soil temperature and water content were similar among treatments. Interannually, low soil water content decreased annual Fsoil from potential values – estimated based on temperature alone assuming nonlimiting soil water content – by ca. 0.7% per 1.0% reduction in relative extractable water. This effect was only slightly ameliorated by elevated [CO2]. Variability in soil N availability among plots accounted for the spatial variability in Fsoil, showing a decrease of ca. 114 g C m?2 yr?1 per 1 g m?2 increase in soil N availability, with consistently higher Fsoil in elevated [CO2] plots ca. 127 g C per 100 ppm [CO2] over the +200 ppm enrichment. Altogether, reflecting increased belowground carbon partitioning in response to greater plant nutritional needs, the effects of elevated [CO2] and N fertilization on Fsoil in this stand are sustained beyond the early stages of stand development and through stabilization of annual foliage production. |
| |
Keywords: | automated soil respiration measurements
FACE
nitrogen fertilization
Pinus taeda
primary productivity soil water content |
|
|