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Natural levee evolution in vegetated fluvial‐tidal environments

The results elucidate the mechanisms by which levee and crevasse formation, and vegetation may fill fluvio‐tidal wetlands and affect estuary evolution, and bring new insights for geological reconstructions as well as for the future management of deltas and estuaries under sea‐level rise.
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Estuarine morphodynamics and development modified by floodplain formation

Abstract. Rivers and estuaries are flanked by floodplains built by mud and vegetation. Floodplains affect channel dynamics and the overall system's pattern through apparent cohesion in the channel…
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How debris‐flow composition affects bed erosion quantity and mechanisms: An experimental assessment

Understanding erosion and entrainment of material by debris flows is essential for predicting and modelling debris‐flow volume growth and hazard potential. Recent advances in field, laboratory and…
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Reconstruction of differential formation and phasing of crevasses in the fluvial-tidal realm of the Old Rhine

Vegetation and peat accumulation steer Holocene tidal–fluvial basin filling and overbank sedimentation along the Old Rhine River, The Netherlands

In the transformation from tidal systems to freshwater coastal landscapes, plants act as eco‐engineering species that reduce hydrodynamics and trap sediment, but nature and timing of the mechanisms…
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Levee morphology and evolution in the fluvial-tidal realm

Novel Use of Japanese Beetle Pheromone and Floral Lures to Reduce Grub Populations in Turfgrass

A system in which male and female beetles are segregated in the environment reducing the probability that beetles not trapped will mate and females move to turfgrass to oviposit is created.

Biogeomorphodynamic of fluvial-tidal levees and accommodation space infilling

Densely populated low-lying areas are under pressure of relative sea level rise and human impacts. Low-lying areas like most of The Netherlands were built with fluvial-marine sediment supply…
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