309-4 Modeling Actual and Attainable Soil and Terrestrial Carbon.

Poster Number 927

See more from this Division: SSSA Division: Pedology
See more from this Session: Pedology: I (includes student competition)
Tuesday, November 4, 2014
Long Beach Convention Center, Exhibit Hall ABC
Share |

Sabine Grunwald, Soil and Water Science Department, University of Florida, Gainesville, FL, Pasicha Chaikaew, University of Florida, Gainesville, FL and Xiong Xiong, University of Florida, Saint Paul, MN
Given the complexity and heterogeneity of soil-landscapes, research gaps still exists to quantify soil and terrestrial carbon and identify suitable adaptation and management options to optimize natural carbon capital in context of imposed changes, such as land use and global climate change. Our objectives were to: i) assess the spatially-explicit relationships between soil organic carbon (SOC) and environmental factors, and ii) assess actual (TerrCactual) and attainable (TerrCattain) terrestrial carbon consisting of below-ground (soil) and above-ground (biomass) carbon. A total of 234 soil samples in the topsoil (0-20 cm) were collected between 2008 and 2009 across the Suwannee River Basin in Florida, U.S. Biomass data was retrieved from the National Biomass Carbon Data. A comprehensive set of 172 environmental and human covariates was compiled from multiple data sources to predict and validate SOC stocks and TerrCactual using Random Forest (RF) The STEP-AWBH conceptual model (with S: Soil, T: Topography, E: Ecology, P: Parent material, A: Atmosphere, W: Water, B: Biota, and H: Human factors), RF, and simulated annealing were used in conjunction to model TerrCattain. In the simulation model, the STEP factors were kept constant, whereas the AWBH factors were varied by 10, 20, and 30 percent to assess TerrCattain. Results suggest that biotic, soil, parent material, topographic, and water-related factors play crucial roles in determining SOC storage, while human factors fade from being strong predictors. Even though climatic factors were minor predictors, mean annual precipitation and monthly mean temperature in summer months were significant to explain SOC and terrestrial stocks. The TerrCattain stocks derived by the model presented slightly larger amounts than the TerrCactual stocks within the whole basin. The basin-wide TerrCactual was 179.4 Tg C and the TerrCattain was 183.7 Tg C.
See more from this Division: SSSA Division: Pedology
See more from this Session: Pedology: I (includes student competition)