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Published on: July 30, 2019
How river rocks round: resolving the shape-size paradox.
Gabor Domokos1, Douglas J Jerolmack2, Andras Á Sipos1
1Department of Mechanics, Materials and Structures, Budapest University of Technology and Economics, Budapest, Hungary.
River rocks become rounder and smaller downstream due to abrasion. This study reveals abrasion happens in two phases: rapid rounding followed by slow size reduction, solving a long-standing paradox in sediment transport.
Area of Science:
- Geology
- Sedimentology
- Fluid Dynamics
Background:
- River sediments exhibit downstream fining (decreasing particle size) and rounding (evolving shapes).
- Abrasion is accepted as the cause of rounding, but its contribution to fining is debated, creating a shape-size paradox.
Purpose of the Study:
- To quantitatively investigate pebble abrasion as a curvature-driven flow problem.
- To resolve the paradox between observed shape change and debated size change during sediment transport.
Main Methods:
- Laboratory experiments simulating pebble transport and abrasion.
- Numerical modeling to analyze pebble shape evolution and abrasion dynamics.
Main Results:
- Pebble abrasion occurs in two distinct phases: rapid edge rounding to a convex shape, followed by slow reduction in axis dimensions.
- Abrasion is confirmed as a curvature-driven process, explaining the observed shape evolution.
Conclusions:
- The two-phase abrasion model reconciles laboratory and field observations, resolving the shape-size paradox.
- Understanding pebble shape evolution enhances the interpretation of sediment transport history in river systems.
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