Preprints
https://doi.org/10.5194/egusphere-2025-1541
https://doi.org/10.5194/egusphere-2025-1541
24 Apr 2025
 | 24 Apr 2025
Status: this preprint is open for discussion and under review for Earth Surface Dynamics (ESurf).

New experiments to probe the role of fractures in bedrock on river erosion rate and processes

Marion Fournereau, Laure Guerit, Philippe Steer, Jean-Jacques Kermarrec, Paul Leroy, Christophe Lanos, Hélène Hivert, Claire Astrié, and Dimitri Lague

Abstract. River erosion via abrasion and plucking is a fundamental process that impacts, among others, landscape evolution, sediment transport, and hillslope dynamics. It results from complex interactions between climate, tectonics, topography and the erodibility of bedrock. Despite its significant role, bedrock erodibility remains poorly understood as it is thought to aggregate several parameters. Among these, fractures in bedrock are assumed to exert a strong control over erosion and thus, on landscape evolution. However, there is no systematic study of the impact of fracture geometry and density on bedrock river erosion.

Due to the complex interactions at play, we investigate this question via an experimental approach. We develop an erosion mill apparatus designed to erode a fractured concrete disk with a diameter of 17 cm. We simulate fractures by embedding a 3D-printed plastic mesh in the concrete, using BVOH—a plastic that softens in cold water—creating mechanical heterogeneities with a controlled pattern. We explore 10 different geometries and run 4 additional experiments without fractures for control. We record the topographic evolution every 2 minutes by photogrammetry and derive erosion maps by measuring elevation changes between successive scans. To our knowledge, this is the first study of its kind. Our results show that while fractures influence the relative contributions of abrasion and plucking, no clear relationship emerges between average erosion rates and fracture density or dip angle. However, we observe that the occurrence of plucking is related to the density and the dip angles of fractures, and is favoured by intermediate density that scales with the size of the impactors, and intermediate dip angle that ease the removal of blocks. We suggest that the main impact of plucking is to change the location of erosion, increasing the eroded surface area rather than accelerating overall erosion rates. However, but as plucking accounts for at most one-third of the total erosion, its occurrence does not significantly affect average erosion rates. These findings emphasize the role of fractures on erosion mode and location rather than erosion rates, and highlight the need to further explore the impact of fractures on riverbed erosion.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
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Marion Fournereau, Laure Guerit, Philippe Steer, Jean-Jacques Kermarrec, Paul Leroy, Christophe Lanos, Hélène Hivert, Claire Astrié, and Dimitri Lague

Status: open (until 10 Jun 2025)

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  • RC1: 'Comment on egusphere-2025-1541', Alexander Neely, 01 May 2025 reply
Marion Fournereau, Laure Guerit, Philippe Steer, Jean-Jacques Kermarrec, Paul Leroy, Christophe Lanos, Hélène Hivert, Claire Astrié, and Dimitri Lague
Marion Fournereau, Laure Guerit, Philippe Steer, Jean-Jacques Kermarrec, Paul Leroy, Christophe Lanos, Hélène Hivert, Claire Astrié, and Dimitri Lague

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Short summary
River bedrock erosion can occur by polishing and by the removal of entire blocks. We observe that when there is no to little fractures most erosion occurs by polishing whereas with more fractures, blocks can be removed at once leading to different patterns of erosion and riverbed morphology. Fractures affect barely mean erosion rate but change the location and occurrence of block removal. Our results highlight how river bedrock properties influence erosion processes and thus landscape evolution.
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