1. A Field Study on the Lithological Influence on the Interaction Between Weathering and Abrasion Processes in Bedrock Rivers.
- Author
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Larimer, Jeffrey E., Yanites, Brian J., and Jung, S. J.
- Subjects
WEATHERING ,BEDROCK ,CHEMICAL weathering ,RIVER channels ,ROCK properties ,CHEMICAL processes ,RIVER sediments ,FLUVIAL geomorphology - Abstract
Lithology is an important control on the efficiency of bedrock incision and thus the pace of landscape evolution. Rock strength is commonly considered the limiting lithologic factor that resists erosion. Yet, rock strength is a dynamic property that oscillates during advection of rock to the channel surface as damaging processes weaken rock and erosion exposes fresh rock. We approach the problem by investigating damage on bedrock surfaces that vary by the frequency they are eroded in channels of different lithologies. Our data set includes measurements of channel slope and width to characterize channel morphology, and Schmidt hammer rebound, P wave velocity, slake durability, and porosity to characterize the mechanical properties of channel surfaces. The average damage accumulation rate of lithologies ranges over 41% of the mean. We find a range of damage patterns among the different lithologies. Local surface damage increases with erosion frequency in channels comprised of coarse‐grained bedrock but decreases with erosion frequency in channels comprised of fine‐grained bedrock. We interpret these patterns to develop from lithological influences on weathering, abrasion, and the threshold of damage to erosion. The cross‐channel damage patterns between channel floors and margins are well correlated with stream power demonstrating links between microstructural rock properties, reach‐scale morphology, and landscape‐scale processes. We conclude that the morphodynamics of bedrock channels are sensitive to the lithological influences on the direction and magnitude of feedback in the coevolution of bedform morphology and the mechanical properties of the surface. Plain Language Summary: Rivers shape the landscape by carving out valleys into rock. Some types of rock are harder to carve than other types of rock, but it is not clearly understood why because there are many physical and chemical weathering processes that attack rock other than the river. Using several dry river channels, we take many measurements of rock strength along the bedrock surface that forms the river channels. We take advantage of the different channel surfaces that are either shielded or exposed to the downstream flow of river sediment to get a sense of how the bedrock is damaged by sediment impacts and by weathering. We find that the size and type of minerals that make up the bedrock influence the pattern of rock damage that develops through complex feedbacks that occur as bedrock material is either weakened or eroded thereby exposing fresher material that lies underneath. These damage patterns in turn control the shape of the channel, and therefore, the erosive potential of the flowing water. Our findings demonstrate how microscale rock properties can influence the shaping of landscapes. Key Points: Erosion frequency and surface damage modulate the spatial variability in mechanical properties of bedrock channelsGrain size and mineralogy control damage by weathering and abrasion, which influence the slope, width, and roughness of bedrock channelsThe relation between rock damage and rock‐erodibility is unique for different lithologies [ABSTRACT FROM AUTHOR]
- Published
- 2022
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