2022
DOI: 10.1002/hyp.14657
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Geomorphically mediated carbon dynamics of floodplain soils and implications for net effect of carbon erosion

Abstract: The fate of organic carbon deposited in floodplain sediments is an important control on the magnitude and direction of the carbon flux from anthropogenically accelerated erosion and channelization of the riverine network. Globally, carbon deposition rates and mean residence time (MRT) within different geomorphic settings remains poorly constrained. We sampled soil profiles to 0.8 m depth from two geomorphic zones: active channel belt (ACB) and lowland floodplain, under long-term pasture

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Cited by 2 publications
(1 citation statement)
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“…During his studies of sediment stores in river catchments, Des Walling realized that the deposition of fine sediment could have important implications for nutrients, metals and other contaminants which are primarily or significantly transported in fluvial systems in sediment‐associated forms. In this Special Issue, Quine et al (2022) address the fate of organic carbon deposited in floodplain sediments. Investigating soil profiles to 0.8 m depth from the active channel belt and lowland floodplain under long‐term pasture in the catchment of the River Culm, South‐West England, they were able to determine using a wide range of field, laboratory and modelling techniques that sedimentation and carbon accumulation rates were 5–6 times greater in the active channel belt than in the adjacent floodplain.…”
Section: Themesmentioning
confidence: 99%
“…During his studies of sediment stores in river catchments, Des Walling realized that the deposition of fine sediment could have important implications for nutrients, metals and other contaminants which are primarily or significantly transported in fluvial systems in sediment‐associated forms. In this Special Issue, Quine et al (2022) address the fate of organic carbon deposited in floodplain sediments. Investigating soil profiles to 0.8 m depth from the active channel belt and lowland floodplain under long‐term pasture in the catchment of the River Culm, South‐West England, they were able to determine using a wide range of field, laboratory and modelling techniques that sedimentation and carbon accumulation rates were 5–6 times greater in the active channel belt than in the adjacent floodplain.…”
Section: Themesmentioning
confidence: 99%