Articles | Volume 5, issue 2
https://doi.org/10.5194/esurf-5-269-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esurf-5-269-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
17 May 2017
Research article |
| 17 May 2017
Physical theory for near-bed turbulent particle suspension capacity
Joris T. Eggenhuisen
CORRESPONDING AUTHOR
Department of Earth Sciences, Utrecht University, Heidelberglaan 2, 3584 CS Utrecht, the Netherlands
Matthieu J. B. Cartigny
Department of Geography, Durham University, South Road, Durham, DH1 3LE, UK
Jan de Leeuw
Department of Earth Sciences, Utrecht University, Heidelberglaan 2, 3584 CS Utrecht, the Netherlands
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Cited
22 citations as recorded by crossref.
- Numerical simulation of the temporal evolution of a three dimensional barchanoid dune and the corresponding sediment dynamics M. Burkow & M. Griebel 10.1016/j.compfluid.2018.02.018
- Observation of mixed grain size sediment transport rate and streamwise nearbed flow velocity in a gravel-worked bed Y. Saadi et al. 10.1051/e3sconf/202346411004
- Froude supercritical flow processes and sedimentary structures: New insights from experiments with a wide range of grain sizes K. Ono et al. 10.1111/sed.12682
- The Sediment Budget Estimator (SBE): A process model for the stochastic estimation of fluxes and budgets of sediment through submarine channel systems J. Eggenhuisen et al. 10.2110/jsr.2021.037
- Sediment Suspension by Straining‐Induced Convection at the Head of Salinity Intrusion Q. Zhang & J. Wu 10.1002/2017JC013192
- The stratigraphic evolution of a submarine channel: linking seafloor dynamics to depositional products S. Hubbard et al. 10.2110/jsr.2020.36
- Linking submarine channel–levee facies and architecture to flow structure of turbidity currents: insights from flume tank experiments J. de Leeuw et al. 10.1111/sed.12411
- Deep‐water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway S. Grundvåg et al. 10.1111/sed.13105
- The stratigraphic evolution of onlap in siliciclastic deep-water systems: Autogenic modulation of allogenic signals E. Soutter et al. 10.2110/jsr.2019.49
- Muddy sand and sandy mud on the distal Mississippi fan: Implications for lobe depositional processes A. Fildani et al. 10.1130/GES01580.1
- Which Triggers Produce the Most Erosive, Frequent, and Longest Runout Turbidity Currents on Deltas? J. Hizzett et al. 10.1002/2017GL075751
- How distinctive are flood-triggered turbidity currents? C. Heerema et al. 10.2110/jsr.2020.168
- Flow‐process controls on grain type distribution in an experimental turbidity current deposit: Implications for detrital signal preservation and microplastic distribution in submarine fans D. Bell et al. 10.1002/dep2.153
- Sedimentological regimes for turbidity currents: Depth‐averaged theory T. Halsey et al. 10.1002/2016JC012635
- The influence of a slope break on turbidite deposits: An experimental investigation F. Pohl et al. 10.1016/j.margeo.2020.106160
- Particle-scale analysis on dynamic response of turbidity currents to sediment concentration and bedforms Y. Lu et al. 10.1063/5.0191219
- Transport and Burial of Microplastics in Deep-Marine Sediments by Turbidity Currents F. Pohl et al. 10.1021/acs.est.9b07527
- Particle Size Distribution Controls the Threshold Between Net Sediment Erosion and Deposition in Suspended Load Dominated Flows R. Dorrell et al. 10.1002/2017GL076489
- The influence of basin setting and turbidity current properties on the dimensions of submarine lobe elements Y. Spychala et al. 10.1111/sed.12751
- Powerful turbidity currents driven by dense basal layers C. Paull et al. 10.1038/s41467-018-06254-6
- Stratigraphic change in flow transformation processes recorded in early post‐rift deep‐marine intraslope lobe complexes A. Martinez‐Doñate et al. 10.1111/sed.13086
- The stratigraphic record and processes of turbidity current transformation across deep‐marine lobes I. Kane et al. 10.1111/sed.12346
21 citations as recorded by crossref.
- Numerical simulation of the temporal evolution of a three dimensional barchanoid dune and the corresponding sediment dynamics M. Burkow & M. Griebel 10.1016/j.compfluid.2018.02.018
- Observation of mixed grain size sediment transport rate and streamwise nearbed flow velocity in a gravel-worked bed Y. Saadi et al. 10.1051/e3sconf/202346411004
- Froude supercritical flow processes and sedimentary structures: New insights from experiments with a wide range of grain sizes K. Ono et al. 10.1111/sed.12682
- The Sediment Budget Estimator (SBE): A process model for the stochastic estimation of fluxes and budgets of sediment through submarine channel systems J. Eggenhuisen et al. 10.2110/jsr.2021.037
- Sediment Suspension by Straining‐Induced Convection at the Head of Salinity Intrusion Q. Zhang & J. Wu 10.1002/2017JC013192
- The stratigraphic evolution of a submarine channel: linking seafloor dynamics to depositional products S. Hubbard et al. 10.2110/jsr.2020.36
- Linking submarine channel–levee facies and architecture to flow structure of turbidity currents: insights from flume tank experiments J. de Leeuw et al. 10.1111/sed.12411
- Deep‐water sand transfer by hyperpycnal flows, the Eocene of Spitsbergen, Arctic Norway S. Grundvåg et al. 10.1111/sed.13105
- The stratigraphic evolution of onlap in siliciclastic deep-water systems: Autogenic modulation of allogenic signals E. Soutter et al. 10.2110/jsr.2019.49
- Muddy sand and sandy mud on the distal Mississippi fan: Implications for lobe depositional processes A. Fildani et al. 10.1130/GES01580.1
- Which Triggers Produce the Most Erosive, Frequent, and Longest Runout Turbidity Currents on Deltas? J. Hizzett et al. 10.1002/2017GL075751
- How distinctive are flood-triggered turbidity currents? C. Heerema et al. 10.2110/jsr.2020.168
- Flow‐process controls on grain type distribution in an experimental turbidity current deposit: Implications for detrital signal preservation and microplastic distribution in submarine fans D. Bell et al. 10.1002/dep2.153
- Sedimentological regimes for turbidity currents: Depth‐averaged theory T. Halsey et al. 10.1002/2016JC012635
- The influence of a slope break on turbidite deposits: An experimental investigation F. Pohl et al. 10.1016/j.margeo.2020.106160
- Particle-scale analysis on dynamic response of turbidity currents to sediment concentration and bedforms Y. Lu et al. 10.1063/5.0191219
- Transport and Burial of Microplastics in Deep-Marine Sediments by Turbidity Currents F. Pohl et al. 10.1021/acs.est.9b07527
- Particle Size Distribution Controls the Threshold Between Net Sediment Erosion and Deposition in Suspended Load Dominated Flows R. Dorrell et al. 10.1002/2017GL076489
- The influence of basin setting and turbidity current properties on the dimensions of submarine lobe elements Y. Spychala et al. 10.1111/sed.12751
- Powerful turbidity currents driven by dense basal layers C. Paull et al. 10.1038/s41467-018-06254-6
- Stratigraphic change in flow transformation processes recorded in early post‐rift deep‐marine intraslope lobe complexes A. Martinez‐Doñate et al. 10.1111/sed.13086
1 citations as recorded by crossref.
Latest update: 23 Nov 2024
Short summary
Suspension of particles in turbulent flows is one of the most widely occurring physical phenomena in nature, yet no theory predicts the sediment transport capacity of the wind, avalanches, pyroclastic flows, rivers, and estuarine or marine currents. We derive such a theory from universal turbulence characteristics and fluid and particle properties alone. It compares favourably with measurements and previous empiric formulations, making it the first process-based theory for particle suspension.
Suspension of particles in turbulent flows is one of the most widely occurring physical...
