COS 38-7 - Changes in soil respiration along a nitrogen availability gradient in high-elevation red spruce forests

Tuesday, August 9, 2011: 3:40 PM
6A, Austin Convention Center
Kenneth R. Smith1, Benjamin Hedin2, Bradley P. Breslow3, Brenden E. McNeil4, William T. Peterjohn1 and Richard B. Thomas5, (1)Biology, West Virginia University, Morgantown, WV, (2)Allegheny College, Meadville,, PA, (3)Plant Biology, North Carolina State University, Raleigh, NC, (4)Department of Geology and Geography, West Virginia University, Morgantown, WV, (5)Department of Biology, West Virginia University, Morgantown, WV
Background/Question/Methods

Nitrogen deposition can strongly influence carbon and nitrogen cycling in forest ecosystems. Studies using N additions have shown that carbon sequestration in soil organic matter can increase due to lower soil respiration. We tested this hypothesis along an existing N availability gradient in the southern Appalachian Mountains. Four 200-m plots were established in red spruce (Picea rubens) communities along a modeled gradient of N deposition representing low (3.83 kg ha-1 yr-1) to high (9.72 kg ha-1 yr-1) wet deposition inputs. From June to November 2010, soil respiration was measured weekly using a LI-8100 soil CO2 flux system along with simultaneous measurements of soil temperature and moisture. At each site, soil samples were collected for C and N analyses. Red spruce leaf samples were also collected during July 2010 for foliar C, N, and d15N analyses.

Results/Conclusions

Soil respiration was significantly related to both soil temperature (R2 = 0.37) and soil moisture (R2 = 0.04) across all red spruce stands. Stronger relationships were observed relating soil respiration to soil C:N and foliar characteristics of spruce stands suggesting that increased N availability was associated with increased soil respiration. Mean soil respiration increased as soil C:N declined to low values typically associated with high rates of net nitrification (R2 = 0.70 and 0.75 for organic soil and mineral soil, respectively). Mean soil respiration also increased as both foliar d15N increased (an integrated index of greater N availability; R2 = 0.90) and foliar N increased (R2 = 0.93). Collectively, these results are in contrast to those of several previous studies and suggest that the net effect of N on the components of soil respiration (microbial & fine root respiration) results in an overall stimulation of carbon losses to the atmosphere. We hypothesize that although higher N availability might decrease the decay of high-lignin litter that is often found in coniferous forests, a greater N concentration in fine roots will stimulate autotrophic respiration to a much greater extent.

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