Lift or impact: modelling bedrock incision coupled with sediment dynamics
Abstract
We analyze how the process of bedrock incision by the impact of sediment grains can be described and coupled with sediment dynamics. We first point out that the key parameter is a bedrock dimensionless coefficient that describes the ratio between the volumes of impacting sediments and bedrock erosion. We then write the coupled equations by introducing a partitioning coefficient between sediment and bedrock erosion. It describes the time spent undergoing one or the other erosion process -or the proportion of depositing grains that impact bedrock. In a 1D along-stream system, the resulting equations lead to a similar description of the cover effect proposed by Sklar and Dietrich (2004), giving a rationale to their expression. In a second step, we extend the concept to lateral erosion or deposition fluxes. We develop analytical solutions for a river fed by uniform lateral sediment fluxes from hillslopes and show why the sediment load can exceed the transport capacity. We then implement the equations in the numerical code River.lab/eros, where water depth and velocity, as well as erosion and deposition fluxes, are solved with the method of precipitons. As an example, we simulate the evolution of the Rheinfall at Schaffhausen, Switzerland, a prominent knickpoint along the Hochrhein. In contrast with sediment processes, where the knickpoint slope decreases by diffusion without upstream displacements, bedrock abrasion allows knickpoints to move upstream while retaining almost the same shape. This is consistent with detachment-limited behaviour as emphasized in the theoretical part of the paper. The knickpoint shape (foot elevation and height) and retreat rates are highly dependent on the sediment load in the river. Bedrock erosion first occurs in a narrow canyon that propagates upstream, and then the river widens after the knickpoint has passed by.
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BibTeX
@article{davy2026lift,
title = {{Lift or impact: modelling bedrock incision coupled with sediment dynamics}},
author = {Philippe Davy and Wolfgang Schwanghart and Jürgen Mey and Caroline Darcel and Angela Landgraf},
journal = {Earth Surface Dynamics},
year = {2026},
month = sep,
doi = {10.5194/esurf-14-635-2026},
url = {https://insu.hal.science/insu-05740376v1},
note = {CC BY 4.0},
}
RIS
TY - JOUR
TI - Lift or impact: modelling bedrock incision coupled with sediment dynamics
AU - Philippe Davy
AU - Wolfgang Schwanghart
AU - Jürgen Mey
AU - Caroline Darcel
AU - Angela Landgraf
PY - 2026
DA - 2026/09/07
JO - Earth Surface Dynamics
DO - 10.5194/esurf-14-635-2026
UR - https://insu.hal.science/insu-05740376v1
AB - We analyze how the process of bedrock incision by the impact of sediment grains can be described and coupled with sediment dynamics. We first point out that the key parameter is a bedrock dimensionless coefficient that describes the ratio between the volumes of impacting sediments and bedrock erosion. We then write the coupled equations by introducing a partitioning coefficient between sediment and bedrock erosion. It describes the time spent undergoing one or the other erosion process -or the proportion of depositing grains that impact bedrock. In a 1D along-stream system, the resulting equations lead to a similar description of the cover effect proposed by Sklar and Dietrich (2004), giving a rationale to their expression. In a second step, we extend the concept to lateral erosion or deposition fluxes. We develop analytical solutions for a river fed by uniform lateral sediment fluxes from hillslopes and show why the sediment load can exceed the transport capacity. We then implement the equations in the numerical code River.lab/eros, where water depth and velocity, as well as erosion and deposition fluxes, are solved with the method of precipitons. As an example, we simulate the evolution of the Rheinfall at Schaffhausen, Switzerland, a prominent knickpoint along the Hochrhein. In contrast with sediment processes, where the knickpoint slope decreases by diffusion without upstream displacements, bedrock abrasion allows knickpoints to move upstream while retaining almost the same shape. This is consistent with detachment-limited behaviour as emphasized in the theoretical part of the paper. The knickpoint shape (foot elevation and height) and retreat rates are highly dependent on the sediment load in the river. Bedrock erosion first occurs in a narrow canyon that propagates upstream, and then the river widens after the knickpoint has passed by.
SN - 2196-6311
SN - 2196-632X
ER -