SEDIMENT PRODUCTION AND TRANSPORT ON HILLY LANDSCAPES
Soil production rates are quantified using the in situ produced cosmogenic radionuclides, 10Be and 26Al, extracted from bedrock beneath the soil mantle. Nuclide concentrations are used to infer both local and catchment-averaged (when measured from stream sediments) erosion rates as extensive studies have demonstrated elsewhere. Hillslope sediment transport processes have been quantified by other studies using segmented rods, short-lived isotopes (under very constrained conditions), and fallout 10Be. I show how both short-lived isotopes and a new method of using optically stimulated luminescence can be used where soil production or erosion rates are known to determine the dominant transport mechanisms. Specific examples from southeastern Australia (using OSL) and the Hubbard Brook experimental watershed in New Hampshire (using the short-lived isotopes 210Pb, 7Be, and 137Cs) show how thoroughly the soil profiles are bioturbated and emphasize the role of overland flow in shaping the landscape.
A Monte Carlo model helps connect the nuclide results with the transport results to suggest that grain movements are independent and random. The model also suggests that 20 % of the transported soil was removed by overland flow over roughly the last 10 ka. This helps explain the divergence of field observations from a prediction of slope morphology and soil depth based on a simple diffusion model. These field results further support a new transport model that combined expressions for simple creep, depth-dependent creep and overland flow to predict soil thickness and suggest how a landscape evolves in response to climatic and tectonic forces.