2008 Joint Annual Meeting (5-9 Oct. 2008): Contributions of Subsurface Horizons and Coarse Fragments to Carbon and Nutrient Pools in Forest Soils of the Southern Appalachians.

762-1 Contributions of Subsurface Horizons and Coarse Fragments to Carbon and Nutrient Pools in Forest Soils of the Southern Appalachians.



Wednesday, 8 October 2008: 8:05 AM
George R. Brown Convention Center, 362C
T.R. Fox, Department of Forestry, Virginia Polytechnic Institute and State Univ, 228 Cheatham Hall, Blacksburg, VA 24061, Eric Sucre, Forestry, Virginia Tech Department of Forestry, 228 Cheatham Hall, Blacksburg, VA 24061, M. Paige Parrish, Department of Forestry, Virginia Polytechnic Institute and State University, 228 Cheatham Hall, Blacksburg, VA 24061 and John Tuttle, USDA-NRCS, 1670 Skyland Drive, Wilkesboro, NC 28697
Forest soils in the southern Appalachians very greatly in soil depth and coarse fragment content. The impact of subsurface horizons and coarse fragments throughout the profile must be determined to accurately estimate soil carbon and nutrient pools. We determined total soil carbon and nutrient pools at seven sites in the southern Appalachians of Virginia and West Virginia. Quantitative soil pits were excavated to a minimum depth of 1 meter to determine surface and subsurface horizon fine fraction carbon and nutrient concentrations. Coarse fragments were also determined in each horizon. Carbon and nutrient content of the fine fraction and coarse fragments were determined. Significant concentrations of carbon and nutrients were found in these coarse fragments derived from shale and sandstone.   Estimates of ecosystem carbon and nutrient pools are significantly underestimated based on concentrations in the fine fraction of the surface mineral soil. In particular, significant quantities of base cations, such as Mg2+ and Ca2+, are present in coarse fragments in these soils. Spatial variability in soil depth at several of these sites was evaluated using ground penetration radar. Average depth to bedrock and coarse fragment content were estimated from the GPR data collected by developing a method for analyzing the volume occupied by coarse fragments. These data revealed that depth to bedrock varied dramatically over relatively short distances.  To accurately estimate landscape level carbon and nutrient pools in the Appalachians, the contributions subsurface horizons, coarse fragments and spatial variability in these soil properties must be included.