Sedimentary rates driven by laboratory lock-exchange turbidity currents flowing over gravel and vegetated beds

Turbidity currents are key agents in sediment transport and bed reshaping, influencing geological records, organic carbon fluxes and pollutant transport. While extensively studied over smooth beds, their interaction with rough beds, such as gravel or vegetated substrates, remains poorly understood. Existing studies suggest bed roughness slows flow and alters deposition, but a comprehensive understanding of how grain-size affects current dynamics and sedimentation patterns is lacking. In this study, we addressed key knowledge gaps on the influence of bed roughness and vegetation on turbidity current dynamics and sedimentation by conducting a comprehensive series of lock-exchange flume experiments. Six bed grain-sizes, multiple flow depths, and sediment concentrations were tested and compared with previous experiments on simulated and real vegetation. Results demonstrate that increasing bed roughness significantly reduces turbidity current velocity and enhances near-source sediment deposition. Greater deposits close to the source result in more non-uniform sediment distribution, with less deposition along the gravel bed. Conversely, smooth beds facilitate longer sediment transport and more uniform deposition. Flow regimes were observed to shift from inertial to drag-dominated as a function of bed configuration, with vegetated and coarse-grained beds inducing comparable hydraulic resistance. Sediment deposition patterns were closely linked to bed roughness and influenced clogging processes via unimpeded static percolation. Overall, the findings reveal a strong feedback between substrate morphology and turbidity current behaviour, with important implications for turbidite formation, sedimentary structure development, and hyporheic exchange dynamics. • Vegetated and macrorough beds impose similar flow resistance on turbidity currents • Turbidity current velocity decreases as bed grain size increases • Deposition rates decrease as bed roughness increases.

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Publication Details

Journal
Sedimentary Geology
Published
2025-10-09
DOI
https://doi.org/10.1016/j.sedgeo.2025.106978
Primary Topic
Hydrology and Sediment Transport Processes
Type
article
Field-Weighted Citation Impact
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article

Sedimentary rates driven by laboratory lock-exchange turbidity currents flowing over gravel and vegetated beds

Jordi Colomer, Marianna Soler, Luca Solari, Teresa Serra et al.
Sedimentary Geology
Hydrology and Sediment Transport Processes
article

Sedimentary rates driven by laboratory lock-exchange turbidity currents flowing over gravel and vegetated beds

Jordi Colomer, Marianna Soler, Luca Solari, Teresa Serra, Marco Mancini
article en

Abstract

Turbidity currents are key agents in sediment transport and bed reshaping, influencing geological records, organic carbon fluxes and pollutant transport. While extensively studied over smooth beds, their interaction with rough beds, such as gravel or vegetated substrates, remains poorly understood. Existing studies suggest bed roughness slows flow and alters deposition, but a comprehensive understanding of how grain-size affects current dynamics and sedimentation patterns is lacking. In this study, we addressed key knowledge gaps on the influence of bed roughness and vegetation on turbidity current dynamics and sedimentation by conducting a comprehensive series of lock-exchange flume experiments. Six bed grain-sizes, multiple flow depths, and sediment concentrations were tested and compared with previous experiments on simulated and real vegetation. Results demonstrate that increasing bed roughness significantly reduces turbidity current velocity and enhances near-source sediment deposition. Greater deposits close to the source result in more non-uniform sediment distribution, with less deposition along the gravel bed. Conversely, smooth beds facilitate longer sediment transport and more uniform deposition. Flow regimes were observed to shift from inertial to drag-dominated as a function of bed configuration, with vegetated and coarse-grained beds inducing comparable hydraulic resistance. Sediment deposition patterns were closely linked to bed roughness and influenced clogging processes via unimpeded static percolation. Overall, the findings reveal a strong feedback between substrate morphology and turbidity current behaviour, with important implications for turbidite formation, sedimentary structure development, and hyporheic exchange dynamics. • Vegetated and macrorough beds impose similar flow resistance on turbidity currents • Turbidity current velocity decreases as bed grain size increases • Deposition rates decrease as bed roughness increases.

Sedimentary GeologyVol. 489
Universitat de Girona (ES), University of Florence (IT)
Openalex Percentile: Top 73%
Hydrology and Sediment Transport Processes
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