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Jeroen Nachtergaele

Researcher at Katholieke Universiteit Leuven

Publications -  42
Citations -  4634

Jeroen Nachtergaele is an academic researcher from Katholieke Universiteit Leuven. The author has contributed to research in topics: Erosion & Surface runoff. The author has an hindex of 28, co-authored 42 publications receiving 4168 citations. Previous affiliations of Jeroen Nachtergaele include National Fund for Scientific Research & Université catholique de Louvain.

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Gully erosion and environmental change: importance and research needs

TL;DR: In this article, the authors highlight the need for monitoring, experimental and modelling studies of gully erosion as a basis for predicting the effects of environmental change (climatic and land use changes) on gully degradation rates.
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Resistance of soils to concentrated flow erosion: A review

TL;DR: In this paper, all available data on the resistance of topsoils to concentrated flow erosion in terms of channel erodibility (Kc) and critical shear stress (τcr) has been collected together with all soil and environmental properties reported in literature to affect the soil erosion resistance.
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Spatial evaluation of a physically-based distributed erosion model (LISEM)

TL;DR: In this paper, the authors used LISEM to simulate an extreme erosion event in a small agricultural catchment in the Belgium loam belt, and measured rill and gully volumes and the thickness of sediment deposits.
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Thresholds for gully initiation and sedimentation in Mediterranean Europe

TL;DR: In this paper, a negative power relationship of the form S = aAb was fitted through all datasets, and defined as the mean topographical threshold for gullying in the respective area, suggesting a dominance of overland flow and an influence of subsurfaceflow.
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Sediment export by water from an agricultural catchment in the Loam Belt of central Belgium

TL;DR: In this article, an agricultural drainage basin of 250 ha was selected in the Belgian Loam Belt to evaluate sediment export by water and water discharge was continuously measured at the outlet of the catchment and suspended sediment samples were taken proportional with discharge during rainfall events.