Proceedings of the Seventh International Conference on Hydroscience and Engineering, Philadelphia, PA, September 2006. http://hdl.handle.net/1860/732The practical determination of the potential of river bank erosion requires information on the stream flow conditions, soil composition of the banks, and the erosion rate of the soils exposed to the flow. Experiments were conducted to measure directly the soil erosion rate (SER) of soil samples extracted from boreholes using an automated version of the LeFeuvre Apparatus (LeFeuvre, 1965; LeFeuvre et al., 1970). The design and operation of the apparatus for the automatic measurement of the SER of cohesive and non-cohesive soil samples is presented. Direct measurements of the wall shear stress a...
Scientists and engineers need to predict the erosion rate of cohesive soils due to fluvial and seepa...
This study presents the comparison of experimental results with assumptions used in numerical models...
A series of 2D small-scale physical experiments were performed in the Ahlborn sediment model bed tan...
The practical determination of the potential river bank erosion requires information on the stream f...
Erosion is a ubiquitous phenomenon which occurs when shear stress exceeds the forces keeping the par...
In order to accurately predict the stability of riverbanks, model input parameters must be reliable ...
Prediction of critical shear stress and determination of erosion rate due to concentrated flow plays...
Soil erosion is an international problem that if not controlled will deprive humankind of life susta...
AbstractLess attention has been given to fluvial erosion even though, in many instances, it has been...
Soil mechanical behaviour is strictly related to its natural water content, which is primarily depen...
2015PDFTech ReportFHWA-HRT-15-033ScourCohesive soilsStreambedsSlakingCohesive soilserosion testingsl...
The present study provides an experimental contribution to a better understanding of erosion mechani...
Stream bank erosion rates are commonly modeled using the excess shear stress equation εr = kd(τ-τc)a...
The Erosion Function Apparatus (EFA) test uses site-specific soil samples acquired via thin-walled t...
This study provides fundamental examination of mass fluvial erosion along a stream bank by identifyi...
Scientists and engineers need to predict the erosion rate of cohesive soils due to fluvial and seepa...
This study presents the comparison of experimental results with assumptions used in numerical models...
A series of 2D small-scale physical experiments were performed in the Ahlborn sediment model bed tan...
The practical determination of the potential river bank erosion requires information on the stream f...
Erosion is a ubiquitous phenomenon which occurs when shear stress exceeds the forces keeping the par...
In order to accurately predict the stability of riverbanks, model input parameters must be reliable ...
Prediction of critical shear stress and determination of erosion rate due to concentrated flow plays...
Soil erosion is an international problem that if not controlled will deprive humankind of life susta...
AbstractLess attention has been given to fluvial erosion even though, in many instances, it has been...
Soil mechanical behaviour is strictly related to its natural water content, which is primarily depen...
2015PDFTech ReportFHWA-HRT-15-033ScourCohesive soilsStreambedsSlakingCohesive soilserosion testingsl...
The present study provides an experimental contribution to a better understanding of erosion mechani...
Stream bank erosion rates are commonly modeled using the excess shear stress equation εr = kd(τ-τc)a...
The Erosion Function Apparatus (EFA) test uses site-specific soil samples acquired via thin-walled t...
This study provides fundamental examination of mass fluvial erosion along a stream bank by identifyi...
Scientists and engineers need to predict the erosion rate of cohesive soils due to fluvial and seepa...
This study presents the comparison of experimental results with assumptions used in numerical models...
A series of 2D small-scale physical experiments were performed in the Ahlborn sediment model bed tan...