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Results from various studies published during the last decades suggest that soil erosion could be playing an important role in the global carbon (C) cycle. One of the major uncertainties is related to the effect that lateral fluxes of sediment and C may have on soil C dynamics and on its distribution within the

Calibración y aplicación de un modelo de erosión y dinámica del carbono (SPEROS-C) a doce pequeñas cuencas del sureste español