We quantify the influence of hydrologically-induced erosion on soil organic carbon redistribution at the Holcombe’s Branch. We apply tRIBS-ECO, a spatially-explicit model of SOC dynamics built within a coupled process-based hydro-geomorphic model. We focus on the rate of carbon burial in alluvial sediments during the history of agriculture and reforestation of the site.
Dialynas, Y.G., Bras, R.L., and Richter, D.deB. (2016): Influence of erosion and deposition on soil organic carbon dynamics. Calhoun CZO 2016 Summer Science Meeting.
This Paper/Book acknowledges NSF CZO grant support.