Carbon sequestration capacity in no-till soil decreases in the long-term due to saturation of fine silt plus clay-size fraction
Lucas Antônio Telles Rodrigues, Jeferson Dieckow, Sandro José Giacomini, Anaí Sangiovo Ottonelli, Geam Pedro Pesenatto Zorzo, Cimélio Bayer
Topics & Concepts
SiltTopsoilSoil waterAgronomySaturation (graph theory)Soil scienceEnvironmental scienceLoamSoil carbonSoil organic matterChemistryGeologyMathematicsBiologyPaleontologyCombinatoricsSoil Carbon and Nitrogen DynamicsClay minerals and soil interactionsSoil and Unsaturated Flow