Weathering-mediated bedrock erosion

Summary: Tools for modeling the weathering-mediated erosion of bedrock. The focus is on environments with no soil or talus accumulation: for example, on steep bedrock channel walls.

Graph of erosion rate vs weathering number

Abstract

Weathering in bedrock river channels is important, just as on rockslopes and soil-mantled hillslopes, but relatively little studied. Sub-aerial weathering in particular weakens rock exposed during stage variation and makes it more susceptible to mechanical erosion. Such erosion modifies the depth-profile of rock weathering, which in turn modifies the process of weakening. Here we study how these interactions lead to a steady-state erosion rate.

We define rock weakness to be its propensity to erosion by flow-driven particle-impact wear. Experiments indicate such weakness is inversely proportional to tensile strength squared, and that weakening takes place through wetting/drying, freeze/thaw and thermal cycling at rates that diminish in a roughly exponential fashion with depth. Therefore here we equate weakening explicitly with weathering.

Two speeds control the erosion rate: (i) the speed ${\lambda} {\eta_0}$ that weathering-driven weakening propagates into the rock, where ${\eta_0}$ is the weathering rate of fresh rock and ${\lambda}$ is the e-folding depth; (ii) the raw speed of erosion of fresh rock ${u}_0$. Model behavior is parameterized by a dimensionless number equal to the ratio of these two speeds, which we call the weathering number ${\mathcal{W}}$.

For small ${\mathcal{W}}<0.25$ and slow weathering relative to erosion, the two speeds simply add and the erosion rate is approximately ${\lambda}{\eta_0} + {u_0}$. However, for ${\mathcal{W}} \gg 2.5$ and relatively fast weathering, the predicted behavior is counter-intuitive: the erosion rate is asymptotically the geometric mean of the two speeds $\sqrt{ {\lambda} {\eta_0} {u_0} }$.

The rate of weathering alone never limits the rate of erosion, and so the concept of weathering limitation does not apply in the traditional sense.

Code

The code is provided as a Python package and Jupyter notebooks.

References

  1. Inoue, T., Yamaguchi, S., and Nelson, J. M., 2017.. "The effect of wet-dry weathering on the rate of bedrock river channel erosion by saltating gravel", Geomorphology, 285, 152–161.

  2. Li, K., Ma, L., Li, X., and Peng, S., 2016. "Effect of drying-wetting cycles on triaxial compression mechanical properties of sandstone", Journal of Engineering Science and Technology Review, 9, 66–73.

  3. Stark, C.P., and Stark, G.J., 2022. "The direction of landscape erosion", Earth Surface Dynamics, 10: 383-419.

Project links

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Newer release available (0.1.34)

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Credits

Author: Colin P. Stark

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Data verified by PyPI on Jun 18, 2026
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License

GNU General Public License v3 (GPLv3)

Requires

Python >=3.14

Tags

geomorphology erosion bedrock weathering

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